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Tytuł:
Filtration of mixtures forming compressible sediments
Filtracja mieszanin tworzących osady ściśliwe
Autorzy:
Piecuch, T.
Piekarski, J.
Malatyńska, G.
Powiązania:
https://bibliotekanauki.pl/articles/1818925.pdf
Data publikacji:
2013
Wydawca:
Politechnika Koszalińska. Wydawnictwo Uczelniane
Tematy:
compressible sediments
filtration
Opis:
W niniejszej publikacji, rozpatrzono od strony teoretycznej proces filtracji mieszaniny cieczy i ciała stałego napływającej na siatkę filtracyjną. Ten rodzaj procesu filtracji jest charakterystyczny dla urządzeń filtracyjnych takich jak: filtry próżniowe, prasy filtracyjne oraz filtry ciśnieniowe w mniejszym stopniu wirówki filtracyjne [10, 17–22, 25–27].Bazą rozważań jest więc ogólny zapis według równania (10) przedstawiony dla procesu filtracji z tworzeniem osadu ściśliwego na siatce filtracyjnej przy uproszczonym założeniu, że cała objętość zawiesiny (VN) nadana do procesu filtracji, przykładowo próżniowej lub ciśnieniowej [1–3, 23, 24, 33–39] zostanie zatrzymana na siatce filtracyjnej (VNβN), a więc zagęszczenie filtratu będzie równe zero. Zatem równanie (10) przyjmie postać (11). W równaniu tym, jak wyżej, przyjmijmy dla uproszczenia wywodu matematycznego pewne nowe stałe, a mianowicie, zapiszmy stałą A w postaci (12). Następnie stałą B określmy według zapisu (13) (13), oraz stałą C ujmijmy według zapisu (14). Biorąc pod uwagę powyższe uproszczenia można przedstawić rozwiązanie ogólne równania różniczkowego(11) procesu filtracji ze zmiennym ciśnieniem w postaci całki (15). Rozpatrzmy poszczególne przypadki rozwiązania całki zapisanej równaniem (15). Dla B=1 całka przyjmie postać (16). Dla B=0,5; xB=x0,5= , całka (15) ma postać (17) Podstawiając =t, mamy x=t2, a stąd dx=2tdt, i tym sposobem całkę (17) z funkcji niewymiernej sprowadzamy do całki z funkcji wymiernej j (18) Funkcję podcałkową f(t), która jest funkcją wymierną niewłaściwą przedstawiamy w postaci (19) i całkując obustronnie otrzymujemy (20). Ostatecznie uwzględniając wynik (20) w całce (18) i wracając do wyjściowej zmiennej x otrzymamy, że całka wyraża się wzorem (21).W szczególności, jeśli dolna granica całkowania jest ustalona i wynosi a=0, natomiast górna granica całkowania jest zmienna, to otrzymamy rozwiązanie równania filtracji w postaci (22). Dla B=2/3; xB=x2/3= całka (15) ma postać (23). Poprzez podstawienie =t, mamy x=t3, dx=3t2dt, i całkę z funkcji niewymiernej (23) sprowadzamy do całki z funkcji wymiernej (24). Całkę tego typu oblicza się przedstawiając funkcję podcałkową f(t), która jest funkcją wymierną niewłaściwą, w postaci (25). Uwzględniając rozkład (25) w całce (24) i korzystając ze wzoru (26), otrzymamy (27). Uwzględniając ten wynik we wzorze (24) oraz wracając do podstawienia t= otrzymamy ostatecznie, że całka (23) wyraża się wzorem (28). W szczególności, jeżeli dolna granica całkowania jest ustalona i wynosi a=0, natomiast górna granica całkowania jest zmienna, to otrzymamy ogólne rozwiązanie równania filtracji wg zapisu (29). Dla B=1/3; xB=x1/3= całka (15) ma postać (30). Poprzez podstawienie =t, mamy x=t3, oraz dx=3t2dt i całkę (30) sprowadzamy do całki funkcji wymiernej postaci (31). Funkcja podcałkowa f(t) jest funkcją wymierną niewłaściwą, a więc dzieląc licznik przez mianownik przedstawiamy ją w postaci (32). Uwzględniając rozkład (32) w całce (31) i całkując obustronnie otrzymamy, że całka stojąca po prawej stronie ma postać (33). Następnie wracając do wyjściowej zmiennej tj. do podstawienia t= otrzymamy, całkę ogólną postaci (34). W szczególności, jeżeli dolna granica całkowania jest ustalona i wynosi a=0, natomiast górna granica całkowania jest zmienna, to dla B=2/3 całkę (30), wyrażamy za pomocą funkcji (35). Z przeprowadzonej analizy teoretycznej wynikają pewne ogólne wnioski dla badaczy procesu filtracji – w tym przypadku procesu filtracji przez siatkę filtracyjną z tworzeniem osadu ściśliwego w trakcie trwania procesu na tej siatce. Otóż: nie można ustalić jednakowej formuły ogólnego równania filtracji takiego, w którym wystąpi parametr ściśliwości osadu w ogólnym zapisie fizykalnym (tutaj B=sO), do którego to równania będzie można podstawiać wprost dowolne wartości współczynnika ściśliwości sO, w granicach pomiędzy wartością zero oraz jeden i określać przepływ medium przez taką przegrodę porowatą – tu siatkę filtracyjną, w przypadku procesu filtracji z tworzeniem osadów ściśliwych na siatce filtracyjnej – chcąc korzystać z ogólnego zapisu równania różniczkowego filtracji, należy je każdorazowo najpierw rozwiązać poprzez całkowanie podstawiając najpierw do tego równania, konkretną wartość współczynnika ściśliwości (sO=B). Końcowe fizykalne zapisy tych rozwiązań, dla wybranych współczynników ściśliwości sO przedstawiono w tablicy 1, przed ewentualnym wykorzystaniem ogólnego równania różniczkowego filtracji, jako równania wyjściowego, na podstawie którego chcemy wyliczyć przepływ (wydatek objętościowy) należy najpierw ustalić wartość stałej b0 z zapisu empirycznego (5) dla określenia wartości parametru przepuszczalności K; a więc parametru przepuszczalności, który musi być znany, wyznaczenie wartości współczynników stałych, które występują w zapisie ogólnego równania filtracji (11) (a więc t’, b0) będzie przedmiotem badań Autorów publikacji dla konkretnych, typowych mieszanin, które można spotkać w bieżącej praktyce inżynierskiej i będzie przedmiotem kolejnych publikacji Autorów jako dalszy ciąg badań podstawowych nad procesem filtracji, przeprowadzona powyżej analiza teoretyczna procesu filtracji osadów ściśliwych wskazuje jednoznacznie, że wykorzystywanie w praktyce ogólnego równania różniczkowego procesu filtracji poprzez jego rozwiązanie, tj. całkowanie, przy założonej (a więc w praktyce znanej wartości współczynnika ściśliwości sO=B) jest jednak bardzo trudne i skomplikowane, a tym samym nie rokuje pozytywnych perspektyw bieżącego wykorzystywania przez projektantów tego równania.
Źródło:
Rocznik Ochrona Środowiska; 2013, Tom 15, cz. 1; 39-58
1506-218X
Pojawia się w:
Rocznik Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Radionuclide activities in sediments on the northern coast of Spitsbergen
Autorzy:
Wojtasik, Barbara
Świrydowicz, Sławomir
Burska, Dorota
Nowiński, Kamil
Powiązania:
https://bibliotekanauki.pl/articles/2042160.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
137Cs
Arctic
fjords
freshwater sediments
marine sediments
natural radionuclides
Svalbard
Źródło:
Polish Polar Research; 2017, 38, 3; 291-312
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość skaleni w utworach neoplejstoceńskich okolic Częstochowy
Content of feldspars in the Neopleistocene sediments in the vicinity of Częstochowa
Autorzy:
Kobojek, Sławomir
Powiązania:
https://bibliotekanauki.pl/articles/945142.pdf
Data publikacji:
1997
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
feldspars
Częstochowa
Neopleistocene sediments
Źródło:
Acta Universitatis Lodziensis. Folia Geographica Physica; 1997, 1
1427-9711
2353-6063
Pojawia się w:
Acta Universitatis Lodziensis. Folia Geographica Physica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Microplastics in coastal sediments of Ełckie Lake (Poland)
Autorzy:
Rogowska, Weronika
Skorbiłowicz, Elżbieta
Skorbiłowicz, Mirosław
Trybułowski, Łukasz
Powiązania:
https://bibliotekanauki.pl/articles/2025997.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
microplastics
lake
coastal sediments
Opis:
Plastics are materials with many properties that make them extremely popular in everyday life and various industries. Studies show that plastic debris is global pollution and widespread in virtually all ecosystems. This study aimed to assess the coastal sediments of Ełckie Lake in terms of the presence of microplastics. Samples of sediments (n = 37) from the coastal zone of Ełckie Lake were drawn from different areas, including urban, rural, and tourist locations, and beaches. After the coastal sediment samples taking, they were subjected to density separation, filtration, and visual evaluation using the Olympus BX63 fluorescent microscope. Particles were classified according to the category of visible characteristics of microplastics including size, shape and colour. The results of the study showed the presence of microplastics in 84% of the examined coastal sediment samples of Ełckie Lake. Fibres, flakes, granules, and foils (films) had found in 58%, 45%, 32%, and 13% of the samples that contained microplastic, respectively. The majority of the detected microplastic was 0.5–1 mm in size and black was the dominant colour. Spatial variability was perceived in microplastic concentrations, giving premises to the assumption of dependence between local human activity and the content of particles.
Źródło:
Studia Quaternaria; 2021, 38, 2; 109-116
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Epizody kaolinitowe w profilu Brody--Lubienia - zapis efektu cieplarnianego (?) we wczesnym toarku
Autorzy:
Brański, P.
Powiązania:
https://bibliotekanauki.pl/articles/183387.pdf
Data publikacji:
2008
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
epizody kaolinitowe
kaolin sediments
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 165-166
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
DDT i jego metabolity w powierzchniowych osadach jezior i rzek Polski
DDT and its metabolites in surface sediments of lakes and rivers of Poland
Autorzy:
Bojakowska, I.
Stasiuk, M.
Gąsior, J.
Powiązania:
https://bibliotekanauki.pl/articles/2062812.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
pestycydy chloroorganiczne
osady rzeczne
osady jeziorne
chlorinated pesticides
river sediments
lake sediments
Opis:
W 300 próbkach osadów rzecznych i 150 próbkach osadów jeziornych pobranych z obszaru Polski oznaczono zawartość p,p’-DDT, p,p’-DDE, p,p’-DDD metodą chromatografii gazowej z detekcją wychwytu elektronów (GC-ECD). W osadach rzecznych maksymalna zawartość p,p’-DDT wynosiła 2780 μg/kg, p,p’-DDD – 913 μg/kg, a p,p’-DDE – 298 μg/kg. Obecność p,p’-DDT stwierdzono w 38,9%, p,p’-DDE – 90,0%, a p,p’-DDD – 78,4% próbek. Stosunek p,p’-DDD/p,p’-DDT w osadach rzecznych wahał się od 0,08 do 46,3, a stosunek p,p’-DDE/p,p’-DDT mieścił się w zakresie 0,04–24,7. W osadach jeziornych zawartość p,p’-DDT odnotowano do 4,7 μg/kg, p,p’-DDE – 63,5 μg/kg, a p,p’-DDD – 70,1 μg/kg. Obecność p,p’-DDT stwierdzono w 36% próbek, p,p’-DDD w 96,67%, a metabolit p,p’-DDE we wszystkich próbkach. Stosunek p,p’-DDD/p,p’-DDT w osadach jeziornych wahał się od 0,4 do 112,2, a stosunek p,p’-DDE/p,p’-DDT – od 0,2 do 163,8. W osadach jeziornych stwierdzono wysoką korelację zawartości związków z grupy DDT z zawartością Cd, Hg, Zn i Pb oraz znaczącą korelację z zawartością fosforu i siarki, podczas gdy w osadach rzecznych stwierdzono tylko bardzo słabą korelację z TOC.
The contents of p,p’-DDT, p,p’-DDE, p,p’-DDD were determined in 300 samples of river sediments and 150 samples of lake sediments, collected from the whole area of Poland, by using the GC-ECD method. In river sediments the maximum contents were as follows: p,p’-DDT – 2780 μg/kg, p,p’-DDD – 913 μg/kg, and p,p’-DDE – 298 μg/kg. The presence of p,p’-DDT was detected in 38.9% of the samples, p,p’-DDE – in 90.0%, and p,p’-DDD – in 78.4%. The ratio of p,p’-DDD/p, p’-DDT in river sediments ranged from 0.08 to 46.3, and the ratio of p,p’-DDE/p,p’-DDT was in the range of 0.04–24.7. In the lake sediments the contents of p,p’-DDT ranged up to 4.7 μg/kg, p,p’-DDE – up to 63.5 μg/kg, and p,p’-DDD – up to 70.1 μg/kg. The presence of p,p’-DDT was detected in 36% of the samples, p,p’-DDD – in 96.67%, and the metabolite p,p’-DDE – in all samples. The ratio of p,p’-DDD/p,p’-DDT in lake sediments ranged from 0.4 to 112.2, and the ratio of p,p’-DDE/p,p’-DDT was in the range of 0.2–163.8. In the lake sediments, a high correlation of the contents of DDTs with the concentrations of Cd, Hg, Pb and Zn, and a significant correlation with the phosphorus and sulphur content were found. In the river sediments, a weak correlation with the TOC content is the only one noticed.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2012, 450; 9--16
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowe możliwości rewitalizacji małych zbiorników wodnych
New opportunities for the revitalization of small bodies of water
Autorzy:
Eymontt, Andrzej
Wierzbicki, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/460789.pdf
Data publikacji:
2017-06
Wydawca:
Mazowieckie Biuro Planowania Regionalnego w Warszawie
Tematy:
osady denne
odmulanie
nawozy organiczne
bottom sediments
extraction of sediments
organic fertilizers
Opis:
Znaczny postęp technologii wydobywania osadów z dna zbiorników wodnych i przetwarzania ich na wysoko wartościowe nawozy organiczne stworzył nowe możliwości ich rekultywacji. Te nowe możliwości mogą być dobrze wykorzystane przy aktualizacji Planu Zagospodarowania Przestrzennego Województwa Mazowieckiego, a także przy realizacji zobowiązań Polski wobec Unii Europejskiej w zakresie Ramowej Dyrektywy Wodnej oraz planów odnowy dróg wodnych w Polsce. Wspomniany postęp manifestuje się możliwością wydobywania osadów dennych o dużej koncentracji składnika stałego (ok. 30%) pochodzenia organicznego i mineralnego, a więc o małej zawartości wody, która jest następnie sorbowana przez zmikronizowaną biomasę (np. słomę) lub skałę (np. opokę) o właściwościach bakteriobójczych. Dzięki opracowanej kompleksowej technologii wydobywania, a następnie przetwarzania ww. osadów na kalibrowany nawóz organiczny, stworzone są nowe możliwości podniesienia urodzajności gleb lekkich (ok. 60% w Polsce), a także zmniejszenia kosztów rewitalizacji małych zbiorników wodnych. Technologia wydobywania osadów została opracowana i wdrożona w Instytucie Technologiczno-Przyrodniczym z siedzibą w Falentach wspólnie z firmą Łukomet, dzięki współfinansowaniu z Europejskiego Funduszu Rozwoju Regionalnego nadzorowanemu przez Mazowiecką Jednostkę Wdrażania Projektów Unijnych.
Significant advances in technology of extracting sediments from the bottom of water bodies and processing them into high-value organic fertilizers has created new opportunities for their reclamation. These new opportunities can be used advantageously when the Spatial Development Plan of Mazovia is updated, as well as in the implementation of Poland's commitments towards the European Union in the framework of the Water Framework Directive and the plans for waterway rehabilitation in Poland. This progress is manifested by the possibility of extracting bottom sediments with high concentrations of solid (about 30%) of organic and mineral origin and having a low water content which is then sorbed by micronized biomass (e.g. straw) or rock (e.g. opoka) with bactericidal properties. Thanks to the developed comprehensive mining technology and subsequent processing of the aforementioned sediments for calibrated organic fertilizer, new possibilities for increasing the yield from light soils (about 60% in Poland), as well as reducing the cost of revitalization of small water reservoirs. Sediment extraction technology was developed and implemented at the Institute of Technology and Natural Sciences, based in Falenty together with firm Łukomet, thanks to co-financing from the European Regional Development Fund supervised by the Mazovian Unit for the Implementation of EU Projects.
Źródło:
MAZOWSZE Studia Regionalne; 2017, 21; 61-75
1689-4774
Pojawia się w:
MAZOWSZE Studia Regionalne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pleistocene deposits in the Southern Egyptian Sahara: lithostratigraphic relationships of sedimentsand landscape dynamics at Bir Tarfawi
Autorzy:
Hill, Christopher L.
Schild, Romuald
Powiązania:
https://bibliotekanauki.pl/articles/2026009.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
sediments
lithofacies
stratigraphy
groundwater
Pleistocene
Opis:
The sedimentological and lithostratigraphic record from north-central Bir Tarfawi documents the presence of Pleistocene basin-fill deposits. Three topographic basins were created as a result of deflation during climate episodes associated with lowering of the local groundwater table. In each case, the three deflational basins or topographic depressions were subsequently filled with sediments; these basin aggradations coincided with changes from arid climate conditions to wetter conditions and a rise in the groundwater table. The oldest and highest sedimentary remnant is associated with Acheulian artifacts and may reflect spring-fed pond and marsh conditions during a Middle Pleistocene wet climate episode. Lithofacies for a lower stratigraphic sequence (the “White Lake”) documents deposition in a perennial lake that varied in extent and depth and is associated with Middle Paleolithic artifacts. A third episode of deflation created a topographic low that has been filled with Late Pleistocene sediments that are associated with Middle Paleolithic artifacts and fossil remains. Lateral and vertical variations in the lithofacies of this basin-fill sequence and the sediments of the “grey-green” lake phases provide a record of changing hydrologic conditions. These hydrologic conditions appear to reflect variations in water-table levels related to groundwater recharge and, at times, local rains.
Źródło:
Studia Quaternaria; 2017, 34; 23-38
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Algal pigments in Hornsund (Svalbard) sediments as biomarkers of Arctic productivity and environmental conditions
Autorzy:
Krajewska, Magdalena
Szymczak-Żyła, Małgorzata
Kowalewska, Grażyna
Powiązania:
https://bibliotekanauki.pl/articles/2042142.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
HPLC
Pigments
sediments
Spitsbergen
Źródło:
Polish Polar Research; 2017, 38, 4; 423-443
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Scale of pollutions with heavy metals in water and sediment of River Ibër from landfill in Kelmend, Kosovo
Autorzy:
Kadriu, Sadija
Sadiku, Milaim
Kelmendi, Mensur
Mulliqi, Ismet
Aliu, Mehush
Hyseni, Arbër
Powiązania:
https://bibliotekanauki.pl/articles/89156.pdf
Data publikacji:
2019
Wydawca:
Politechnika Wrocławska. Wydział Geoinżynierii, Górnictwa i Geologii. Instytut Górnictwa
Tematy:
river
waters
sediments
heavy metals
Opis:
Pollution with heavy metals and waters in Mitrovica with surroundings, both in the past and in present days, is a preoccupation for the citizens of Mirtovica, as well as for the other inhabitants living around it. Such a problem has been a concern which still continues for a number of researchers who have been dealing with this issue, and who still continue to be preoccupied with the issue of heavy metal (habitat) pollution in this part of Kosovo. Heavy metal's contamination of the environment's main components, dates back to the 1970s/90s to this date. This pollution, especially of the rivers, is due to the industrial activity taking place in the Trepça Combine and the presence of industrial landfill sites of this Combine near the flow of two main rivers: the Sitnica and Ibër River waters, in the city of Mitrovica. The focus of our study, this time consists solely in the research and illumination of pollution with these heavy metals and waterworks of the Ibër River, as a result of the pollution caused by the industrial waste landfill located in Kelmend village. In the paper, we have attempted to show the concentration of heavy metals in sediment and water, by pointing at four sample sites of the Ibër river: in the Bosniak U1 neighborhood, then in the flow in front the U2 landfill, discharge flows from landfill U3 and a certain distance from the U4 landfill.
Źródło:
Mining Science; 2019, 26; 147-155
2300-9586
2353-5423
Pojawia się w:
Mining Science
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Micromorphology of cryoconite on Garabashi and Skhelda glaciers and soils of Baksan Gorge, Mt. Elbrus, Central Caucasus
Autorzy:
Abakumov, Evgeny
Tembotov, Rustam
Kushnov, Ivan
Polyakov, Vyacheslav
Powiązania:
https://bibliotekanauki.pl/articles/16538453.pdf
Data publikacji:
2022
Wydawca:
Polska Akademia Nauk. Czasopisma i Monografie PAN
Tematy:
Russia
Caucasus
sediments
weathering
deglaciation
Opis:
In the Central Caucasus region, the intense process of deglaciation is identified as caused by cryoconite formation and accumulation. The fine earth materials were collected on the surfaces of Skhelda and Garabashi glaciers as well as from zonal soils of Baksan Gorge and were studied in terms of chemical, particle-size, and micromorpholo-gical features. Supraglacial sediments are located at the glacial drift area of material and, thus, due to transfer of these sediments to the foothill area, their fine earth material can affect micromorphological and chemical characteristics of adjacent zonal soils. Thin sections of mineral and organo-mineral micromonoliths were analyzed by classic micromorphological methods. Data obtained showed that the weathering rates of cryoconite and soil minerals are different. The cryoconite material on the debris-covered Skhelda Glacier originated from local massive crystalline rocks and moraines, while for Garabashi Glacier the volcanic origin of cryoconite is more typical. Soils of Baksan Gorge are characterized by more developed microfabric and porous media, but their mineralogical composition is essentially inherited from sediments of glacial and periglacial soils. These new data could be useful for understanding the process of evolution of the mineral matrix of cryoconite to the soil matrix formed at the foot of the mountain.
Źródło:
Polish Polar Research; 2022, 43, 1; 1-20
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palaeoecology of the Holsteinian lake in vicinity of Wilczyn (eastern Poland) based on molluscan studies
Autorzy:
Szymanek, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060329.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
palaeoecology
molluscs
Holsteinian
lacustrine sediments
Opis:
Malacological studies of two profiles of the Holsteinian (Mazovian) Interglacial from eastern Poland – Roskosz and Wilczyn 1/12 – are presented. They are connected with the northern part of the Wilczyn palaeolake and seems to document palaeoecological changes in the part of the climatic optimum and the post-optimal period. Mollusc communities are typical of lake environs. The latter is supported by biometry of Pisidium moitessierianum. Higher energy conditions are evidenced by rheophile species P. henslowanum and P. nitidum in the lowermost part of the Roskosz section. Mollusc assemblages with Lithoglyphus jahni, with Valvata piscinalis and Bithynia tentaculata as well as with Valvata piscinalis are distinguished at Roskosz. They record changes in aquatic vegetation and depth conditions. Malacofauna from Wilczyn 1/12 is dominated by V. piscinalis, V. piscinalis f. antiqua and B. tentaculata. Limited contribution of temperate gastropods Viviparus diluvianus and L. jahni as well as the occurrence of some cold-loving forms indicate a deterioration of thermal conditions. Shallow-water habitats and expansion of reed zones are inferred from proportions of Bithynia shells and opercula.
Źródło:
Geological Quarterly; 2013, 57, 4; 637--648
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Technical note: Stability of a levee made of bottom sediments from a dam reservoir
Autorzy:
Koś, K.
Zawisza, E.
Powiązania:
https://bibliotekanauki.pl/articles/178768.pdf
Data publikacji:
2014
Wydawca:
Politechnika Wrocławska. Oficyna Wydawnicza Politechniki Wrocławskiej
Tematy:
bottom sediments
hydraulic embankments
stability
Opis:
Stability analysis of a levee made of the bottom sediments from Czorsztyn-Niedzica Reservoir is presented in the paper. These sediments were classified as silty sands and, based on the authors’ own research, their geotechnical parameters were beneficial, so the possibility of using this material for the hydraulic embankments was considered. Stability and filtration calculations were carried out for a levee that had the same top width – 3 m, slope inclinations 1:2 and different heights: 4, 6 and 8 m. Two methods were used: analytical and numerical. Calculations were carried out without and with a steady and unsteady seepage filtration. Based on the analysis carried out it was stated that the levee made of the bottom sediments is stable even at the height of 8.0 m, although because of the seepage on the downstream side it is recommended to use a drainage at the toe of the slope.
Źródło:
Studia Geotechnica et Mechanica; 2014, 36, 4; 65-70
0137-6365
2083-831X
Pojawia się w:
Studia Geotechnica et Mechanica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Polychaetes of Antarctic sublittoral in the proglacial zone (King George Island , South Shetland Islands)
Autorzy:
Siciński, Jacek
Powiązania:
https://bibliotekanauki.pl/articles/2052063.pdf
Data publikacji:
2004
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
Polychaeta
sublittoral
bottom sediments
Źródło:
Polish Polar Research; 2004, 25, 1; 67-96
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Seismoacoustic studies within Wijdefjorden, Spitsbergen
Autorzy:
Kowalewski, Włodzimierz
Rudowski, Stanisław
Zalewski, S. Maciej
Powiązania:
https://bibliotekanauki.pl/articles/2052887.pdf
Data publikacji:
1990
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
bottom sediments
geophysics
Źródło:
Polish Polar Research; 1990, 11, 3-4; 287-300
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Application of the USBR equation for surveying balance of sediment yield in Dez River branches in Iran
Autorzy:
Fuladipanah, M.
Makvandi, A.
Powiązania:
https://bibliotekanauki.pl/articles/208109.pdf
Data publikacji:
2013
Wydawca:
Politechnika Wrocławska. Oficyna Wydawnicza Politechniki Wrocławskiej
Tematy:
sediments
rivers
osady rzeczne
rzeki
Opis:
Accurate determination of mean annual sediment load (MASL) of natural rivers will affect administrative aspects of water planning in dams. The MASL in Dez River in the southwest Iran has been considered. Sezar and Bakhtiari are its two branches. The amount of MASL was predicted by the USBR equation with three scenarios: using mean value of sediment discharge, using probabilistic classification of river flow data and using separation of wet and dry months. The results show that the USBR equation can be used to evaluate MASL in the Dez basin.
Źródło:
Environment Protection Engineering; 2013, 39, 3; 185-195
0324-8828
Pojawia się w:
Environment Protection Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Investigation of the pulse reflected from bottom sediments
Autorzy:
Nowak, Ł.
Szymczak, W.
Powiązania:
https://bibliotekanauki.pl/articles/332780.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Akustyczne
Tematy:
bottom sediments
pulse reflected
hydroacoustics
Opis:
The paper describes method of determining time proceeding of the echo pulse arising as an effect of reflection of sampling pulse given with the known form from layered sea bottom. The main goal of presented model is to afford theoretical data that could be used as a point of reference for the experimental data obtained with SES 2000 Standard parametric echosounder. Basic formulas, computation algorithm with its implementation in Matlab language and examples of obtained results are described. Numerical simulations results are compared with experimental data. The laboratory station enabling computing acoustic impedance of sediments and parameters of sampling and echo pulse in different distances from antenna is presented.
Źródło:
Hydroacoustics; 2009, 12; 159-166
1642-1817
Pojawia się w:
Hydroacoustics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Accumulation of 137Cs in bottom sediments of the Curonian Lagoon
Autorzy:
Lujaniene, G.
Vilimaite. -Šilobritiene, B.
Jokšas, K.
Powiązania:
https://bibliotekanauki.pl/articles/148785.pdf
Data publikacji:
2005
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
caesium
sorption
desorption
bottom sediments
Opis:
Measurements of activity concentrations and speciation of 137Cs in bottom sediments of the Curonian Lagoon were carried out in samples collected in 1999-2003. In addition, the sorption-desorption processes of caesium in disturbed bottom sediments of fresh and sea water systems were investigated in long-term experiments (up to 375 days) in order to better understand the caesium behaviour during the Baltic Sea water flooding events to the Curonian Lagoon. The modified Tessier method was used to study caesium associations with geochemical phases of bottom sediments. The effect of carbonate coatings of bottom sediments on the Cs sorption-desorption process was observed. The comparative analyses of 137Cs solid phase speciation in bottom sediments after 241 and 375 days of the sorption experiment with that of the 137Cs speciation, determined in the same sediment sample before the sorption experiment, indicated that after 375 days of sorption the equilibrium was not reached, however, the Cs distribution in geochemical phases was found to be close to equilibrium. The desorption experiments evidenced the release of caesium into solution from regular exchange complex and transfer from other phases to the frayed edge sites on the layered clay minerals with its further fixation in the crystal lattice. The remobilization of "fixed" caesium was not observed, on the contrary, the redistribution of caesium with its subsequent fixation in clay minerals was observed, and on a time scale its fixation kinetics was comparable with the sorption experiment. This study showed that flooding events of sea water contaminated with caesium can cause a significant accumulation of caesium in the bottom sediments of the Curonian Lagoon and result in the redistribution of 137Cs activity concentration in the bottom sediments from one area to another.
Źródło:
Nukleonika; 2005, 50, 1; 23-29
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Characteristics of Spatial Distribution of Phosphorus and Nitrogen in the Bottom Sediments of the Water Reservoir Poraj
Autorzy:
Rozpondek, K.
Rozpondek, R.
Pachura, P.
Powiązania:
https://bibliotekanauki.pl/articles/123884.pdf
Data publikacji:
2017
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
bottom sediments
spatial distribution
eutrophication
Opis:
The aim of this study was to determine the content of phosphorus and nitrogen in the bottom sediments of the Poraj Reservoir located on the Warta River, along with defining their spatial distribution and the relationship between these elements and organic matter, aluminum and iron. Samples of bottom sediments were collected on the basis of regular measurement grid of 46 points located in the area of the water reservoir Poraj. The collected samples were analyzed in terms of content of following elements, which values are in range: total phosphorus (TP) 0.06 – 5.06 g/kg, total nitrogen (TN) 0.17 – 9.66 g/kg, organic matter (OM) 0.49 – 28.41% of solid content, aluminum (Al) 2.44 – 145.15 g/kg and iron (Fe) 0.28 – 16.50 g/kg. By using of GIS system, spatial distribution of obtained results of laboratory analyzes were interpolated (Inverse Distance Weighted method was used). On basis of spatial distribution it was noted that in northern part of water reservoir bottom sediments have greater values of TP, TN and OM than in southern part. The study also included calculation of correlation between: OM and TN (n=46, R2 = 0.9335), TN and Fe (n=46, R2 = 0.8782), TN and Al (n=46, R2 = 0.8629), OM and Fe (n=46, R2 = 0.8243), OM and Al (n=46, R2 = 0.7981), TP and Fe (n=46, R2 = 0.7456), TP and Al (n=46, R2 = 0.6209). The presented pilot studies show that the potential content of phosphorus, nitrogen and organic matter in the sediments of the water reservoir Poraj can reach a significant level. The need to plan and carry out further research allowing the evaluation of the properties of the analyzed elements and examining their potential impact on water quality in the tested water reservoir was stated.
Źródło:
Journal of Ecological Engineering; 2017, 18, 4; 178-184
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Content of Heavy Metals in Bottom Sediments of Selected City Rivers of the Podlasie Province
Autorzy:
Skorbiłowicz, M.
Skorbiłowicz, E.
Górska, M.
Powiązania:
https://bibliotekanauki.pl/articles/124842.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
heavy metals
river
bottom sediments
Opis:
The purpose of the work was to determine the relationship between the state of the water environment quality of selected rivers (Zn, Cr, Pb, Cd and Cu tests in bottom sediments), and the sources of pollution resulting from the close proximity to the cities, through which they flow. The following rivers were selected for the study: the Biała river flowing through the city of Białystok, the Narew river flowing through the city of Tykocin and the village of Złotoria, the Supraśl river flowing through the village of Michałowo and Gródek as well as the Biała river flowing through the city of Bielsk Podlaski. The sediments were collected four times from the same points in 2016 in the period from July to October. The sediment samples were collected from the points located on rivers before and beyond towns and villages. The contents of the following metals were tested in the bottom sediment samples: Zn, Cr, Pb, Cd and Cu. The analyses were carried out applying the flame absorption spectrometry method. The statistical multivariate CA and FA analyzes were used. The highest contents of Zn, Pb and Cr were recorded in the bottom sediments from the following rivers: Biała (Białystok) and Biała inflow of Orlanka (Bielsk Podlaski), which resulted from the anthropogenic activity. The research also showed the impact of the agricultural activity due to the slightly elevated Cd level.
Źródło:
Journal of Ecological Engineering; 2018, 19, 4; 197-206
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mercury contamination of bottom sediments in water reservoirs of southern Poland
Autorzy:
Koniarz, T.
Tarnawski, M.
Baran, A.
Florencka, N.
Powiązania:
https://bibliotekanauki.pl/articles/184703.pdf
Data publikacji:
2015
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
mercury
bottom sediments
reservoirs
geoaccumulation parameters
Opis:
The aim of this study was to assess the mercury concentration in bottom sediments, collected from eight reservoirs located in south-eastern Poland. A DMA-80 Mercury Analyser was used for the analysis of the concentration of mercury in bottom sediments. Concentration of mercury in sediments was between 0.01–0.18 mg∙kg−1. The research results show that 13 samples are above the Polish Hg background level. Only 9 samples are below the background level. Generally, the sediments belonged to class I and II (unpolluted and moderately polluted sediments). The concentration of mercury in bottom sediments follows the order: Rybnik (highest) > Bagna Rzeszowskie > Rzeszów > Ożanna > Brzóza Stadnicka > Brzóza Królewska > Głuchów > Narożniki (lowest). The low mercury content in sediments is related to absent or limited anthropogenic sources of this metal. Elevated concentrations of Hg in bottom sediments of the reservoirs in Rybnik and Bagna Rzeszowskie are related to their proximity to large agglomerations and industrial plants. Organic matter was likely to be the most important factors controlling the concentration and distribution of mercury in the studied sediments.
Źródło:
Geology, Geophysics and Environment; 2015, 41, 2; 169-175
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The problem of the identification of relict rock glaciers on sedimentological evidence
Autorzy:
Żurawek, R.
Powiązania:
https://bibliotekanauki.pl/articles/294394.pdf
Data publikacji:
2003
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
sediments
ground ice
relict rock glaciers
Opis:
In order to establish sedimentological criteria for the identification of relict rock glaciers, a study of published information about the internal structure of both active and relict rock glaciers has been carried out. The literature survey revealed that there is no single lithological feature which could independently serve as a proof of the decisive role of ground ice for the transport of rock debris. However, a sequence of a bouldery mantle and a core composed of diamict, together with a layering which dips steeply up-slope are the strongest premises for the elimination of any process other than that associated with a cold environment. Certainly, in attempting to distinguish between a moraine and relict rock glacier, the geo-morphological setting must be taken into account and, notwithstanding this, an effective differentiation is often virtually impossible. Sedimentological parameters such as grain size distribution, sorting and grain morphology are largely controlled by the properties of the source rock and, as such, they are of no value in attempts to identify relict rock glaciers.
Źródło:
Landform Analysis; 2003, 4; 7-15
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Plutonium and americium in sediments of Lithuanian lakes
Autorzy:
Remeikis, V.
Gvozdaite, R.
Druteikiene, R.
Plukis, A.
Tarasiuk, N.
Špirkauskaite, N.
Powiązania:
https://bibliotekanauki.pl/articles/148886.pdf
Data publikacji:
2005
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
plutonium isotopes
americium
sediments
isotopic composition
Opis:
The assessment of contribution of the global and the Chernobyl NPP (Nuclear Power Plant) accident plutonium and americium to plutonium pollution in sediments of Lithuanian lakes is presented. Theoretical evaluation of activity ratios of 238Pu/239+240Pu and 241Pu/239+240Pu in the reactor of unit 4 of the Chernobyl NPP before the accident was performed by means of the ORIGEN-ARP code from the SCALE 4.4A program package. Non-uniform distribution of radionuclides in depositions on the Lithuanian territory after nuclear weapon tests and the Chernobyl NPP accident is experimentally observed by measuring the lake sediment pollution with actinides. The activity concentration of sediments polluted with plutonium ranges from 2.0 š 0.5 Bq/kg d.w. (dry weight) in Lake Asave . lis to 14 š 2 Bq/kg d.w. in Lake Juodis. The ratio of activity concentrations of plutonium isotopes 238Pu/239+240Pu measured by á-spectrometry in the 10-cm-thick upper layer of bottom sediment varies from 0.03 in Lake Juodis to 0.3 in Lake Žuvintas. The analysis of the ratio values shows that the deposition of the Chernobyl origin plutonium is prevailing in southern and south-western regions of Lithuania. Plutonium of nuclear weapon tests origin in sediments of lakes is observed on the whole territory of Lithuania, and it is especially distinct in central Lithuania. The americium activity due to 241Pu decay after the Chernobyl NPP accident and global depositions in bottom sediments of Lithuanian lakes has been evaluated to be from 0.9 to 5.7 Bq/kg.
Źródło:
Nukleonika; 2005, 50, 2; 61-66
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Persistent Organic Pollutants (POPs) and Polycyclic Aromatic Hydrocarbons (PAHs) in surface sediments from selected fjords, tidal plains and lakes of the North Spitsbergen
Autorzy:
Sapota, Grażyna
Wojtasik, Barbara
Burska, Dorota
Nowiński, Kamil
Powiązania:
https://bibliotekanauki.pl/articles/2051704.pdf
Data publikacji:
2009
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
sediments
PAHs
PCBs
OCPs
Źródło:
Polish Polar Research; 2009, 30, 1; 59-76
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Late Pleistocene and Holocene relief remodelling in the Ebbadalen-Nordenskiöldbreen region in Olav V Land, central Spitsbergen
Autorzy:
Kłysz, Piotr
Lindner, Leszek
Marks, Leszek
Wysokiński, Lech
Powiązania:
https://bibliotekanauki.pl/articles/2053119.pdf
Data publikacji:
1989
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
Quaternary
landforms and sediments
Źródło:
Polish Polar Research; 1989, 10, 3; 277-301
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The influence of litho- and pedogenic processes on Luvisols formation of selected area of Vistula Glaciation
Autorzy:
Jaworska, H.
Dąbkowska-Naskręt, H.
Kobierski, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060473.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
luvisols
lithological discontinuity
lessivage
glacial sediments
Opis:
The objective of the study was to determine the effect of litho- and pedogenic processes on soils of the selected area of Vistula Glaciation, based on profile distribution of unweathered components such as titanium, zirconium and silica in relation to their morphology, mineralogy, micromorphology and physicochemical properties. The predominant type of soilin the study area are Luvisols. Analysis of texture allowed to classify the investigated soils to sandy silts with loamy material as their subsoil. In the bulk soil silica dominates and its content was in the range 71.4 to 88.6%. The content of TiO2 within the profiles is fairy similar, without clear patterns in the profile distribution. The total content of zirconium in the samples was in range of 95.13 to 212.15 mg x kg-1. In the profile distribution of zirconium higher content of Zr was observed in the upper horizons compared to the top layerin all of theanalysed profiles, indicating different origin of soil material. Statistical analysis showed positive correla- tion between the total content of zirconium and the content of fraction 0 0.05-0.002 mm (correlation coefficient value: 0.692384; significance level - p < 0.05) and negative correlation between zirconium and clay content (correlation coefficient: -0.668157; p < 0.05). The lithologic discontinu i ty within profiles of the investigated soils has been additionally has proved by X-ray analysis of the clay fraction. The micromorphological analysis confirmed the complex genesis of the studied soils. The results of the study clearly showed an overall inhomogeneity and stratification of the soils. Studied Luvisols did not form as weath- ering product of homogeneous bedrock. Changes in granulometric and chemlcal composition within soil profiles are the consequence of translocation of clay fraction during lessivage as well as lithologic discontinul ty of the solum.
Źródło:
Geological Quarterly; 2014, 58, 4; 685--694
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution and sources of n-alkanes in surface sediments of Taihu Lake, China
Autorzy:
Yu, Y.
Li, Y.
Guo, Z.
Zou, H.
Powiązania:
https://bibliotekanauki.pl/articles/205298.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
n-alkanes
surface sediments
Taihu Lake
Opis:
The last study on n-alkanes in surface sediments of Taihu Lake was in 2000, only 13 surface sediment samples were analysed, in order to have a comprehensive and up-to-date understanding of n-alkanes in the surface sediments of Taihu Lake, 41 surface sediment samples were analyzed by GC-MS. C10 to C37 were detected, the total concentrations of n-alkanes ranged from 2109 ng g−1 to 9096 ng gg−1 (dry weight). There was strong odd carbon predominance in long chain n-alkanes and even carbon predominance in short chain n-alkanes. When this finding was combined with the analysis results of wax n-alkanes (WaxCn), carbon preference index (CPI), unresolved complex mixture (UCM), hopanes and steranes, it was considered that the long chain n-alkanes were mainly from terrigenous higher plants, and that the short chain n-alkanes mainly originated from bacteria and algae in the lake, compared with previous studies, there were no obvious anthropogenic petrogenic inputs. Terrestrial and aquatic hydrocarbons ratio (TAR) and C21−/C25+ indicated that terrigenous input was higher than aquatic sources and the nearshore n-alkanes were mainly from land-derived sources. Moreover, the distribution of short chain n-alkanes presented a relatively uniform pattern, while the long chain n-alkanes presented a trend that concentrations dropped from nearshore places to the middle of lake.
Źródło:
Archives of Environmental Protection; 2016, 42, 1; 49-55
2083-4772
2083-4810
Pojawia się w:
Archives of Environmental Protection
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Preliminary assessment of agriculture influence on heavy metal content in bottom sediments of small water reservoirs and in rushes
Autorzy:
Szydłowski, K.
Podlasińska, J.
Powiązania:
https://bibliotekanauki.pl/articles/100909.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
Tematy:
agriculture
ecology
heavy metals
sediments
ponds
Opis:
The main purpose of the paper was to determine the influence of catchment management on the bottom sediments quality of small water reservoirs as well as to determine toxic metal content in rushes. Samples of bottom sediments were collected in winter 2013 year, form 4 sediment layers (0-5, 5-10, 10-20 and 20-30 cm) at three points along the body of water. The 48 samples were collected. Soil material was prepared according to the procedures used in soil science, the analysis was performed for the fraction with a particle diameter of less than 1 mm. Plant samples from single species aggregations were randomly cut from 5 to 10 locations of 20-50 m2 area. From these samples the average composite sample was prepared. The total content of such elements as Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, Zn was determined by atomic absorption spectrometry (using the Thermo Scientific iCE 3000 series spectrometer) after prior digestion in the mixture (5:1) of concentrated acids HNO3 (65%) and HClO4 (60%). Total Hg content was determined by the AMA 254 analyzer. Between the small water reservoirs adjacent to the areas where organic farming is used, and the reservoirs adjacent to the areas with mineral fertilization there are statistically significant differences in the concentrations of such metals as nickel (layers: 0-5, 5-10, 10-20 and 0-30 cm), as well as cobalt, chromium and iron (in a layer 5-10 cm). It has been found that some plants accumulate higher amounts of heavy metals (average values). Based on obtained results it can be stated that rushes actively captures large amounts of elements reaching studied objects and thereby protect the surface water of the reservoirs from contamination.
Źródło:
Infrastruktura i Ekologia Terenów Wiejskich; 2017, III/1; 949-962
1732-5587
Pojawia się w:
Infrastruktura i Ekologia Terenów Wiejskich
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dynamics of Changes in Microbiological Composition of Stored Sediments
Autorzy:
Sałata, A.
Stoińska, R.
Dąbek, L.
Powiązania:
https://bibliotekanauki.pl/articles/125293.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
sediments
stormwater treatment plant
microbiological analysis
Opis:
The composition of the sediments formed in the process of stormwater pretreatment is diversified and depends on many parameters, mainly on the quality of stormwater and the land use of the catchment. The stormwater sediments are characterized by heterogeneous chemical and microbiological composition. The aim of this paper was the microbiological evaluation of the sediments from four stormwater catchments in terms of hazard to humans and the environment. The pH, and the content of organic and mineral matter were determined for the examined sediments. The microbiological analysis included the determination of the total number of psychrophilic, mesophilic, and coliform bacteria, including E. coli, and also the number of faecal Enterococci, Salmonella and Shigella. The study was conducted for fresh deposits and those stored for one year in order to determine the dynamics of changes in their biological activity.
Źródło:
Journal of Ecological Engineering; 2018, 19, 6; 241-246
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spatial Diversity Characterising Certain Chemical Substances in Sediments of Besko Reservoir
Autorzy:
Piwińska, D.
Gruca-Rokosz, R.
Bartoszek, L.
Czarnota, J.
Powiązania:
https://bibliotekanauki.pl/articles/125420.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
sediments
organic matter
phosphorus
heavy metals
Opis:
The article reports the conducted analyses of certain chemical parameters characterising the sediments of Poland’s Besko Reservoir. Specifically, determinations concerned the pH value, percentage organic matter (OM), total organic carbon (TOC), total nitrogen (TN), carbonates (CO32-), total phosphorus (TP) and its fractions, as well as heavy metals (Fe, Al, Cr, Cu, Ni, Cd, Zn, Mn). The sediments have a slight alkaline reaction, with pH values correlating positively with the high content of carbonates. The sediments have low organic matter content, while organic carbon accounts for about 30% of OM. The values for the C:N ratio point to an allochthonous origin for organic matter. The analysis of phosphorus fractionation showed that inorganic phosphorus (IP) is predominant at every research station. The lowest percentage for a fraction was in turn obtained for NAIP. This testifies to a slight anthropogenic impact of the catchment area. The sediments can be classified as of the 2nd purity class (according to PIG), due to their highest concentration of chromium. According to Müller’s classification, the sediments can be classified as purity class 3 (i.e. with moderate contamination). The values noted for the EF coefficient confirm a very strong enrichment by chromium ions. In addition, chromium, copper, nickel and cadmium have a negative effect on aquatic organisms. The results show that the sediments can be used for example in building and maintaining hydraulic structures.
Źródło:
Journal of Ecological Engineering; 2018, 19, 1; 104-112
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Seasonal variation in heavy metal distribution in the sediments of selected dams in Nasarawa State, Nigeria
Autorzy:
Gav, B. L.
Aremu, M. O.
Etonihu, A. C.
Powiązania:
https://bibliotekanauki.pl/articles/1109614.pdf
Data publikacji:
2018
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Dams
Heavy metal
Seasonal variations
sediments
Opis:
The study was carried out to ascertain seasonal variation in heavy metal distribution in sediments from Dams located in Nasarawa State, Nigeria. Sediment samples were collected twice each at two different seasons for two years from May to September, 2014 and November-December, 2014 to March, 2015 for wet and dry seasons, respectively. Similarly, sediment samples were collected from May to September, 2015 and November-December, 2015 to March, 2016 for wet and dry seasons, respectively. The samples were then assessed for heavy metal properties, using atomic absorption spectrophotography (AAS). Analysis of variance (ANOVA) was then applied. The mean results of the heavy metal levels showed high values in dry seasons and low values in wet seasons in the two years of the study. Herein, the results of ANOVA revealed significant difference in the heavy metal concentrations between the seasons, dams and years. Our study also indicated that for heavy metals, the levels determined in sediments were within the WHO acceptable standards, except for Pb and Mn. These exceeded the WHO acceptable standards for drinking water. Based on these results, the dam waters are, therefore, polluted and unsuitable for human consumption, except after treatment.
Źródło:
World News of Natural Sciences; 2018, 20; 148-159
2543-5426
Pojawia się w:
World News of Natural Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Seismostratigraphy of bottom sea sediments in some areas of the Spitsbergen Archipelago
Autorzy:
Kowalewski, Włodzimierz
Rudowski, Stanisław
Zalewski, S. Maciej
Żakowicz, Krystyna
Powiązania:
https://bibliotekanauki.pl/articles/2053281.pdf
Data publikacji:
1987
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
geophysics
seismoacoustic
bottom sediments
Źródło:
Polish Polar Research; 1987, 8, 1; 3-23
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrochemiczne konsekwencje zasilania zbiorników przepływowych wodami zanieczyszczonymi
Hydrochemical consequences of feeding flow-through reservoirs with contaminated water
Autorzy:
Jaguś, A.
Rzętała, M.
Powiązania:
https://bibliotekanauki.pl/articles/1819396.pdf
Data publikacji:
2012
Wydawca:
Politechnika Koszalińska. Wydawnictwo Uczelniane
Tematy:
surface sediments
quality
lake
heavy metals
Opis:
The research concerned flow-through reservoirs fed with contaminated river water. The aim of the research was to recognize the impact of reservoirs on fluvial transportation of contaminants. Three reservoirs, situated in the Upper-Silesian region (southern Poland) and operating in different environmental conditions, were selected for the research: Pogoria I reservoir - operating in the quasi-natural direct catchment (with fluvial load of industrial-municipal wastewater), Przeczyce reservoir - under agricultural anthropopressure, and Dzierzno Due reservoir - under urban-industrial anthropopressure. The research included analyses of the quality of river water flowing into and leaving the reservoirs and calculation of contaminant loads at the inflows and outflows. The research showed that Pogoria I reservoir neutralised inflowing contaminants, thus purifying the river water. Nitrogen and phosphorus compounds were particularly efficiently retained. Electrolytic conductance of water in Pogoria was reduced by up to 50%. Przeczyce reservoir was alimented with eutrophic water (especially rich in biogenic elements) from agricultural land. The reservoir accumulated contaminants at the initial stage of the research. After several years, however, it started releasing some of the accumulated substances, causing an increase in contamination of river water with e.g. organic substances. The data concerning Przeczyce reservoir revealed that reservoirs can purify water from some substances and simultaneously cause an increase in contamination with other substances. Selectivity of hydrochemical impact of reservoirs was particularly visible in case of Dzierzno Due reservoir, which received wastewater from the urban-industrial catchment. It largely reduced the loads of suspended matter, phosphates or zinc, among other substances, at the same time causing secondary contamination with substances like ammonia, lead or cadmium. The results of the research show individuality of reservoirs in terms of their impact on fluvial transportation of substances. It might be believed, however, that each reservoir which is fed with contaminated water will have at least partly (selectively) contaminating impact in the course of time. That should be related to increasing eutrophication in conditions of limited capacity of accumulation of contaminants in the limnic environment. Detailed assessment of transfer of substances by a particular reservoir would require individual research for that reservoir.
Źródło:
Rocznik Ochrona Środowiska; 2012, Tom 14; 632-649
1506-218X
Pojawia się w:
Rocznik Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The facies and biota of the oldest exposed strata of the Eocene La Meseta Formation (Seymour Island, Antarctica)
Autorzy:
Tatur, A. E.
Krajewski, K. P.
lvalle de, R. A.
Powiązania:
https://bibliotekanauki.pl/articles/2058745.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Antarctica
Seymour
Eocene
sediments
goethite
thanatocoenosis
Opis:
La Meseta Formation is made up of estuarine and shallow marine, fossiliferous clastic deposits 720 m thick that provides a unique record of marine and terrestrial biota of Antarctic ecosystems preceding continental glaciation in the Oligocene. The lower limit of this formation has been poorly known, and therefore it has been carefully investigated. The lowest part of the La Meseta Formation, at the southern bank of a palaeodelta, is represented by relics of a prograding sequence of sediments deposited in the wave-dominated part of a deltaic system in the offshore and lower and upper shoreface environments. The sequence is completed landwards by younger tidal plain sediments deposited at 40 m lower altitude in a relatively protected, central estuarine basin, which was dominated by tidal activity and influenced by periodic fluvial inflow. These strata were deposited during a late Paleocene or Ypresian/Lutetian lowstand of sea level, which might reflect a glaciation event or glacioisostatic rebound of land following deglaciation of hypothetic Antarctic inland glaciers. Forced regression of sea level and seaward expansion of a deltaic freshwater environment, led to local extinction of a unique assemblage of marine echinoderms, bryozoans, corals and brachiopods. These marine fossils, representing a thanatocoenosis, are perfectly preserved due to syngenetic goethite permineralisation. This process owed its origin to excess reactive iron coming from sulphide-rich bedrock through weathering processes and acid sulphate drainage of the neighbouring land area.
Źródło:
Geological Quarterly; 2011, 55, 4; 345-360
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Differences in shell size of the bivalve Varicorbula between marginal parts of the Vienna and Danube basins
Autorzy:
Fuksi, T.
Powiązania:
https://bibliotekanauki.pl/articles/184316.pdf
Data publikacji:
2016
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Middle Miocene
marine sediments
molluscan community
Opis:
Middle Miocene marine sediments in the Vienna and Danube Basins provide opportunities for analysis of spatial and temporal variations in the composition of molluscan communities and variations in species abundance and size. Varicorbula gibba (Olivi 1792) is an opportunistic bivalve with high tolerance to hypoxic conditions and variations in salinity (Holmes & Miller 2006) that appears in the Oligocene and persists to present, occurring in the tropical and northern temperate Eastern Atlantic and in the Mediterranean. Varicorbula belongs to one of the most frequent species in the benthic communities in the Paratethys during the Middle Miocene. However, spatial and temporal variations in taphonomic preservation and in abundance, size, and shape of this genus is poorly known – insights into such variations would improve paleoenvironmental interpretations. Molluscan assemblages with Varicorbula gibba (Olivi 1792) were collected from boreholes located in the western (Vienna basin) and eastern (Danube basin) margins of the Malé Karpaty Mountains (Slovakia). Boreholes intersect sediments of the Studienka Formation (Vienna Basin) respective Madunice Formation (Danube Basin) that belong mainly to the Upper Badenian stage (Janočko et al. 2003, Kováč et al. 2004). We have selected assemblages with more than 20 Varicorbula specimens from sediment samples sieved with 1 mm mesh size. A well preserved shelly material contains presently more than 130 specimens of Varicorbula , with ongoing screening of additional samples. We measured dimensions of four morphological variables (in mm). Shell length, shell height, posterior shell length and upper shell height were measured on all specimens. The valves were photographed and the dimensions were measured using ImageJ image analysis software. We used principal component analysis (PCA) and bivariate and multivariate allometric analyses to investigate ontogenetic and spatial variations in size and shape. We find that this taxon shows significant regional-scale differences in size distribution between the coeval Upper Badenian sediments in the Vienna and Danube basins, with significantly smaller size in the Danube Basin. In subtidal muds in the northern parts of the Vienna Basin, Varicorbula gibba achieves very high proportional community-level abundance and its median shell width ranges between 6–10 mm. Specimens from low-energy muddy sediments of the Vienna basin show low levels of taphonomic damage but are frequently bored by naticids snails that produce the trace fossil Oichnus paraboloides (Bromley 1981, Pek et al. 1997). In contrast, muddy sands from the northeastern margin of the Danube Basin; community composition is more even and median width ranges just between 3–4 mm. The higher sandy content and lower sedimentation rates (as evidenced by higher taphonomic damage, with higher proportion of bored specimens (by muricid snails – Oichnus simplex, in the Danube Basin; Bromley 1981) imply that the regional size differences can partly positively correlate with nutrient supply. Morphometric analyses indicate that height and width of individuals of this taxon undergo significant ontogenetic allometry and that smaller-sized individuals in the Danube Basin have a smaller width/ height ratio. Therefore, some shape differences in the height-width ratio between the two basins are unrelated to ontogenetic allometric effects (because height-width ratio changes even during the ontogeny).
Źródło:
Geology, Geophysics and Environment; 2016, 42, 1; 71-72
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Metals in organs of bottom sediments and aquatic plants of the Ełk River and its tributaries
Autorzy:
Skorbiłowicz, E.
Skorbiłowicz, M.
Zamojska, E.
Wójtowicz, P.
Powiązania:
https://bibliotekanauki.pl/articles/184486.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
river
metals
bottom sediments
aquatic plants
Opis:
The aim of the work was to analyze the content of Ni, Pb and Cd in organs (root, stem, leaf) Typha latifolia L. and Nuphar lutea as well as bottom sediments of the Ełk River and selected tributaries. An attempt was also made to indicate the factors and processes governing the behavior of the investigated metals in the water environment of the examined rivers. The research object was the Ełk River with its three tributaries - the Gawlik River, the Binduga River and the Kuwasy Canal. Samples of bottom sediments, leaves, stems and roots of Typha latifolia L. and Nuphar lutea were collected in August of 2015. The content of metals was determined by flame atomic absorption spectrometry (F-AAS). The results of analyses of sediments and plant material indicate a lack of environmental pollution by nickel (2.58-8.50 mg-kg-1) and lead (3.82-15.99 mg-kg-1) of the Ełk River and its tributaries whereas the cadmium content ranged from 0.16-0.76 mg-kg-1. Nuphar lutea and Typha latifolia L. showed a varied capacity to accumulate nickel (1.20-10.51 mg-kg-1) and lead (0.04-14.16 mg-kg-1), occurring primarily in the roots. The smallest concentration of nickel and lead was recorded in the stems. The highest concentration of cadmium (2.56 mg-kg-1) was noted in the roots and the lowest (0.01 mg-kg) in the leaves. Factor analysis pointed to the processes of mobilizing elements from bottom sediments as a result of pH drop and their uptake by macrophyte roots and sorption processes of metal ions by macrophytes from river waters and their intensive accumulation in bottom sediments.
Źródło:
Geology, Geophysics and Environment; 2018, 44, 3; 281-293
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Relationships between the properties of bottom surf ace sediments and the condition of phyto- and zoobenthos of the Puck Bay (1987-1999)
Autorzy:
Dubrawski, R.
Kruk-Dowgiałło, L.
Powiązania:
https://bibliotekanauki.pl/articles/1920565.pdf
Data publikacji:
2000
Wydawca:
Instytut Morski w Gdańsku
Tematy:
Puck Bay
bottom suiface sediments
zoobenthos
Opis:
Basing on investigations of bottom suiface sediments of the outer Puck Bay (1995, 1999) and the inner Puck Bay (1987, 199 I, 1996), their condition and the absolute quality was determined in accordance with the adopted classification { 3]. Carried out at the same time investigations of the condition and composition of phyto- and zoobenclws allowed determining the relationships between the biotic and abiotic components of the Puck Bay bottom. In the paper, results of correlation analysis are presented. They indicate strong relationships between selected systems of components. These results show also that loading of the sediments with organic matter has a significant influence on the properties of the environment and on the biocenoses of the investigated water area.
Źródło:
Biuletyn Instytutu Morskiego w Gdańsku; 2000, 27, 1; 45-57
1230-7424
2450-5536
Pojawia się w:
Biuletyn Instytutu Morskiego w Gdańsku
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Monitoring the Evolution of Redox Changes in Sediments made Possible by Electrochemical Multilayer Probes
Autorzy:
Popa, Radu
Moga, Ioana Corina
Nealson, Kenneth H.
Cimpoiasu, V.M.
Powiązania:
https://bibliotekanauki.pl/articles/2134093.pdf
Data publikacji:
2022
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
sensor
sediments
SPEAR
multielectrode
redox interface
Opis:
Marine sediments with rapid oxic/anoxic transitions are difficult to monitor in real time. Organic overload that may lead to anoxia and buildup of hydrogen sulfide can be caused by a variety of factors such as sewage spills, harbor water stagnation, algal blooms and the vicinity of aquaculture operations. We have tested a novel multiprobe technology (named SPEAR) on marine sediments to evaluate its performance in monitoring sediments and overlaying water. Our results show the ability of the SPEAR probes to distinguish electrochemical changes at 2-3 mm scale and at hourly cycles. SPEAR probes have the ability to identify redox interfaces and redox transition zones in sediments, but do not use micromanipulators (which are cumbersome in field and underwater applications). We propose that the best target habitats for SPEAR-type monitoring are rapidly evolving muddy deposits and sediments near aquaculture operations where pollution with organics stresses the ecosystem.
Źródło:
Archives of Metallurgy and Materials; 2022, 67, 3; 1037--1041
1733-3490
Pojawia się w:
Archives of Metallurgy and Materials
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrography, hydrochemistry and composition of sapropel of Shatsk Lakes
Autorzy:
Khilchevskyi, Valentyn
Ilyin, Leonid
Pasichnyk, Mykhailo
Zabokrytska, Myroslava
Ilyina, Olga
Powiązania:
https://bibliotekanauki.pl/articles/2174355.pdf
Data publikacji:
2022
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
bottom sediments
lake
sapropel
Shatsk Lakes
Opis:
The purpose of the study presented in the article is to implement modern hydrographic characteristics of freshwater of the Shatsk Lakes (28 lakes in Volyn Polissya, Ukraine) by typing water bodies according to the requirements of the EU Water Framework Directive, assessment of the chemical composition of lake water and bottom sediments (sapropel), determination of the opportunity for their recreational use in the special status of the district as a national park. Despite the presence of the two large lakes (Svityaz - 26.2 km2 and Pulemetske - 15.5 km2), very small lakes with a water surface area of less than 0.5 km2 (64%) are dominating in the Shatsk group. Mineralisation of calcium-hydrocarbonate lake waters is 115-303 mg∙dm-3 and calcium-sulphate aqueous extract of sapropel is - 318-1451 mg∙dm-3. Using a Piper diagram, it was found that there is genetic homogeneity between surface and groundwater, indicating a significant share of groundwater in the water supply of lakes. There are eight species of sapropel deposits in 19 lakes of the district. A wide range of chemical composition and physical and mechanical properties of sapropel deposits of the Shatsk Lakes allow us to consider them as an important resource for agriculture and industry. We found that sapropel from Shatsk Lakes meets the requirements for therapeutic mud and can be used for therapeutic and health purposes.
Źródło:
Journal of Water and Land Development; 2022, 54; 184--193
1429-7426
2083-4535
Pojawia się w:
Journal of Water and Land Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wykorzystanie metali ciężkich w określaniu wieku osadów
The use of heavy metals in estimation of the age of deposits
Autorzy:
Ciszewski, D.
Powiązania:
https://bibliotekanauki.pl/articles/295082.pdf
Data publikacji:
2010
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
osady rzeczne
procesy fluwialne
metale ciężkie
wiek osadów
river sediments
fluvial processes
heavy metals
age of sediments
Opis:
Od początku lat 80. XX w. zróżnicowanie koncentracji metali ciężkich zaczęto wykorzystywać do oceny wieku głównie osadów fluwialnych. Charakterystyczne piki, spadki lub wzrosty tych koncentracji na wykresach porównuje się z archiwalnymi danymi o charakterystycznych zmianach produkcji lub emisji metali na obszarze zlewni. Metoda daje najdokładniejsze wyniki przy istnieniu 1-2 dużych źródeł ścieków na obszarze zlewni i wyraźnych zmianach wielkości ich zrzutów. Zazwyczaj wykonuje się kilka profili w osadach pozakorytowych, analizując zawartość metali we frakcji drobnoziarnistej. Ograniczenia w jej stosowaniu wynikają z dokładności istniejących zapisów historii gospodarczej zlewni oraz postdepozycyjnej migracji metali istotnej szczególnie w poziomach położonych poniżej zwierciadła wody.
The changes in heavy metal concentrations are used for estimation of the age of fluvial sediments since the recent decades of 20th century. Characteristic peaks, sudden drops or increases of metal concentrations in vertical profiles of overbank sediments are usually compared with archival data of metal production or emission in the drainage basin. Method gives the best results with 1-2 large pollution sources in a drainage basin with marked changes in quality and quantity of discharged effluents. Usually several or more profiles are performed and metal content is analyzed in fine sediment fraction. The method is usually limited by accuracy and availability of archival data from industrial history of a drainage basin and by postdepositional mobilization of heavy metals which could be significant below average groundwater level.
Źródło:
Landform Analysis; 2010, 12; 31-34
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The development of unconsolidated sedimentary coastal cliffs (Pobrzeże Kaszubskie, Northern Poland)
Autorzy:
Uścinowicz, G.
Jurys, L.
Szarafin, T.
Powiązania:
https://bibliotekanauki.pl/articles/2060378.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
cliff coast
landslides
soft sediments
Southern Baltic
Opis:
In the course of fieldwork based on geological and landslide mapping and spatial analyses of map information at least 2 types of landslides were identified. Type I: simple landslides developed in homogeneous and undisturbed rocks, for instance – loams, clays and sands. This type of landslide includes many examples developed mainly on the stretch (segment of the studied area) approximately between 132.25 and 133.50 km and 128.50 and 129.50 km of the Polish coastline. Type II: complex landslides in which the movement and displacement of rock masses occurs under complex geological and hydrogeological conditions. The complex factors are determined by phenomena such as glaciotectonics, discontinuities of rock layers and thrust zones; the slip surface occurs at considerable depths, and sometimes several slip surfaces can be distinguished. These landslide types are located in the vicinity of Jastrzębia Góra and Rozewie, near km 134 and 131.5. Prediction of the formation of this landslide types is difficult. Even if long-term observations are available, the mass movement, variable over time, is difficult to interpret. It is clear that the changes are continuous, but occur with varying intensity. Proper recognition of the types of mass movement is crucial to establishing the appropriate methods to prevent their development.
Źródło:
Geological Quarterly; 2017, 61, 2; 491--501
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chemical composition of soil and lake sediments - an indicator of geological processes in Lithuania
Autorzy:
Gregorauskiene, V.
Kadunas, V.
Powiązania:
https://bibliotekanauki.pl/articles/2059444.pdf
Data publikacji:
2000
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Lithuania
trace elements
soil
lake sediments
geoindicators
Opis:
Long-term multipurpose geochemical studies in Lithuania show that the chemical composition of surface sediment can be used as an indicator of geological process: duration of weathering, soil formation and thickness of sediment. The chemical composition of upper and lower soil layers and of lake sediments gives information on past sedimentation: the type and age of Quaternary deposits and the location and depth of Pleistocene glaciolacustrine basins. We therefore have a baseline to predict changes in surface chemistry provoked by current anthropogenic pressures.
Źródło:
Geological Quarterly; 2000, 44, 4; 347-354
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Lithological features of Vistula River channel deposits in the light of micromorphological analysis
Autorzy:
Bielawska, M.
Powiązania:
https://bibliotekanauki.pl/articles/294771.pdf
Data publikacji:
2015
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
micromorphology
alluvial sediments
Vistula river
Central Poland
Opis:
The aim of the study was to identify and assess the lithological features typical for alluvial sediments of Vistula River from the natural part of its course on 603 km of the river course. For this purpose, the micromorphological analysis was carried out for a sample taken from the surface of a tree covered island. The analysis is laborious, but its great advantage is that it allows to determine the detailed characteristics of undisturbed sediments, supplying other lithological studies. Examined thin section showed fractionation lamination within medium and fine sands, interbedded with coarser grains with some organic admixtures. Detailed analysis allows to detect gradual and sudden changes of discharge energy.
Źródło:
Landform Analysis; 2015, 29; 3-8
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assessing Spatial Distributions of Total Trace Elements Content in Bottom Sediments of Dzierżno Duże Water Reservoir – Geostatistics-Based Studies
Autorzy:
Rozpondek, R.
Rozpondek, K.
Powiązania:
https://bibliotekanauki.pl/articles/123432.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
bottom sediments
spatial distribution
trace elements
geostatistics
Opis:
The aim of this study was to assess the spatial distributions of total trace elements content in the bottom sediments of Dzierżno Duże water reservoir, along with the comparison of the accuracy and characteristics of Kriging and IDW interpolations. On the basis of regular measurement grid consisting of 53 points, bottom sediments samples were collected. Mean values of total trace elements content in bottom sediments of Dzierżno Duże were as follows: Zn – 410 mg/kg, Pb – 57 mg/kg, Cr – 36 mg/kg, Cu – 40 mg/kg, Cd – 5 mg/kg, Ni – 16 mg/kg and Ba – 267 mg/kg. According to the geochemical quality classification, the concentrations of Cd in 32% of samples were assigned to class IV (heavily contaminated), 45% to class III (contaminated), Zn in 42% samples to class III with 1 sample in class IV and 26% to class II (slightly contaminated), Pb in 9% to class III and 58% to class II, Cu in 4% to class III and 68% to class II, Cr in 17% to class II, Ni in 55% to class II, Ba in 8% to class III and 61% in class II. Coefficient of determination was determined between each case of trace elements content. The highest correlation (R2 in range from 0.81 to 0.96) was observed between Zn and Pb, Zn and Cu, Zn and Cr, Zn and Ni, Pb and Cu, Pb and Cr, Cu and Cr, Cr and Ni. Significant correlation (R2 in range from 0.70 to 0.80) occurred between: Zn and Cd, Pb and Ni, Cu and Ni, Cd and Ni. The lowest correlations (R2 in range from 0.25 to 0.70) were observed between concentration of Ba and the rest of trace elements. Two different interpolation methods were chosen for the purpose of generating spatial distributions – Inverse Distance Weighted and Ordinary Kriging. These methods were chosen for purpose of obtaining optimal accuracy result of spatial distributions. The distributions of trace elements content were classified by means of geochemical criteria. In the case of accuracy comparison between IDW and Ordinary Kriging, the former had slightly better results in terms of mean value and root mean square. The generated spatial distributions allowed to determine the most contaminated areas, which were mainly northern-central and southern-central parts of water Dzierżno Duże reservoir.
Źródło:
Journal of Ecological Engineering; 2018, 19, 3; 52-60
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Accumulation of Heavy Metals in Organs of Aqueous Plants and its Association With Bottom Sediments in Bug River (Poland)
Autorzy:
Skorbiłowicz, E.
Skorbiłowicz, M.
Malinowska, D.
Powiązania:
https://bibliotekanauki.pl/articles/124487.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
heavy metal
bottom sediments
aquatic plant
river
Opis:
The article presents the results of studies upon metals (Pb, Zn, Cr, Ni, Cu, Co) in bottom sediments and in various parts of the aquatic plants taken from the Bug river (Poland). The metal contents in the examined environmental elements were determined by AAS technique. The aim of this study was to evaluate the content of metals in bottom sediments and macrophytes (root, stem, leaf) occurring in the Bug river. It was hypothesized that the heavy metal content in plant tissues reflects the amount of metals in sediments. It has been shown that the average metal distribution in the examined plants present in the Bug river and bottom sediments was as follows: Pb, Zn, Co, and Cu sediments>root>leaf>stem, while in the case of Ni and Cr, the contents were greater in roots than in sediment (root>sediment>leaf>stem), although the differences in contents were not large. The study showed that most metals are present in roots and only a small part of them is transported to the stem and leaves. The size of the metal movement within plants may depend on their contents. It was found that for Ni, Cr and Cu in 2014, the bioaccumulation factor was above one, which confirms the high efficiency of metals uptake from the environment as evidenced by statistical analysis. Bioaccumulation factor (BF) was smaller than one for Pb, Co and Zn, confirming the high ability to retain metals in the root. Aquatic plants are an effective barrier for the surface water by accumulating heavy metals in their biomass. Macrophytes are proposed to monitor the river pollution.
Źródło:
Journal of Ecological Engineering; 2016, 17, 4; 295-303
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assessment of heavy metal pollution in bottom sediments of small water reservoirs with different catchement management
Autorzy:
Podlasińska, J.
Szydłowski, K.
Powiązania:
https://bibliotekanauki.pl/articles/101221.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
Tematy:
agriculture
ecology
heavy metals
sediments
ponds
classification
Opis:
The main purpose of this work was to determine the degree of negative impact of heavy metals accumulated in the water sediments to aquatic organisms. Samples of sediments were collected in winter 2013, from 4 layers of sediment (0-5, 5-10, 10-20 and 20-30 cm) at three points along the water reservoir. Sediments were prepared for analysis in accordance with the procedures applied in soil science. The analysis was carried out for the fraction with a particle diameter less than 1 mm. The total content of such elements as Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb and Zn, was determined by atomic absorption spectrometry (using the Thermo Scientific iCE 3000 series spectrometer) after digestion in a mixture (5:1) of concentrated acid HNO3 (65 %) and HClO4 (60%). The total Hg content was obtained by using the AMA 254 analyzer. Only the lead content in the analyzed samples of bottom sediments exceeded the contamination value given by polish law (the Regulation of the Minister of Environment). According to the classification of PGI samples of sediments are classified mainly as medium polluted sediments (Class II), with the exception of zinc and lead concentrations (Class III). Due to the value of the indicator of sediments ecological risk (Er) for cadmium, the examined sediments from small water reservoirs no. 1 and 2 should be classified as deposits with a higher rate of environmental contamination risk. The sediments from small water reservoirs no. 3 and 4 belong to the class of a much higher index of contamination risk. On the basis of the PER indicator (a degree of potential envi ronmental risk) the sediments from small water reservoirs located within the area of organic farming can be classified as contaminated by heavy metals to a moderate degree. On the other hand, the analyzed sediments of small water reservoirs no. 3 and 4 were classified as deposits with a severe degree of heavy metal contamination. On the basis of the LAW classification one can say that the bottom sediments of examined ponds were classified into different classes depending on the analyzed chemical element.
Źródło:
Infrastruktura i Ekologia Terenów Wiejskich; 2017, III/1; 987-997
1732-5587
Pojawia się w:
Infrastruktura i Ekologia Terenów Wiejskich
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Quaternary evolution of a Carpathian Foothills area: An example from the East Carpathians of Poland
Autorzy:
Zuchiewicz, W.
Zasadni, J.
Powiązania:
https://bibliotekanauki.pl/articles/191928.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Quaternary sediments
tectonic geomorphology
neotectonic evolution
Polska
Opis:
The East Carpathian Foothills of Poland witnessed two episodes of relief planation in the Pliocene, followed by formation of Early Pleistocene strath terraces preserved on flat-topped meander spurs in the San River valley at altitudes of 100-120 m above recent floodplains. In the following stages, intense erosion produced of a flight of strath terraces that are provisionally dated to the Narevian or Sanian-1 (Menapian or Elsterian-1; 75-80 m), Sanian-2 (Elsterian-2; 40-60 m), Odranian and Wartanian (Drenthe, Warthe; 20-30 m), and Vistulian (Weichse- lian; 8-16 m) times. During glacial stages, solifluction deposits mantled the feet of gentle slopes being coeval with fluvial deposition and accumulation of loesses and loess-like sediments on either side of the San River valley, particularly intense in the Weichselian. Interglacial warmings fostered downcutting of the pre-existing fluvial sediments as well as formation of fossil soils within loess sequences and deposition of peat in abandoned channels. In the Late Pleistocene and at the beginning of the Holocene, diversified tectonic movements took place leading to displacement of Weichselian and Holocene straths. During the Holocene, in turn, cut-and-fill terrace steps were shaped, organogenic sediments filled abandoned channels and oxbow lakes, and slopes became re-modelled by landslides and slopewash. The pattern of different types of relief, together with spatial distribution of topolineaments and some photolineaments in the eastern portion of the Polish Outer Carpathians, has been shaped due to mutual interactions between climatic, lithologic and tectonic factors. Well-pronounced topolineaments either follow fault-related zones of weakness, are associated with dense network of extensional cross-fold joints, or indicate recent reactiva-tion of some faults and/or joint sets.
Źródło:
Annales Societatis Geologorum Poloniae; 2010, 80, No 3; 327-345
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The content and composition of organic matter in bottom sediments of the Rybnik reservoir - preliminary studies
Autorzy:
Baran, A.
Mierzwa-Hersztek, M.
Gondek, K.
Szara, M.
Tarnawski, M.
Powiązania:
https://bibliotekanauki.pl/articles/184606.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
bottom sediments
organic matter
buffer capacity
pollutions
Opis:
Organic matter has important influences on the fate of environmental pollution in water dam reservoirs. The aim of the studies was to assess content of organic matter fractions in Rybnik reservoir bottom sediments, and to determine their influence on the content of heavy metals and PAHs. In three sediment samples, the content of C organic (Corg), C extracted (Cex), C humic acid (Cha), C fulvic acid (Cfa) and C non-hydrolyzed (Cnh), buffer capacity, and content of heavy metals and PAHs was analyzed. We found the highest content of Corg, Cex, Cha, Cfa and Cnh in sample 3 (the outlet, near the dam), while the lowest content was found in sample 2 (middle). The fraction of Cnh was dominant in sediment sample 3 (outlet, near dam) and 1 (inlet), whereas the fraction of Cha dominated in sample 2 (middle). Rybnik bottom sediments are characterized by their high buffer capacities (samples 3, 1) shaped among others by the high content of organic matter. The high organic matter content in samples 3 (outlet) and 1 (inlet) and also high total contents of heavy metals and PAHS in these sediments demonstrate that these pollutants have a strong affinity for organic matter in the sediments. Moreover, the highest mobility of metals, from sample 2 (middle), is connected with the low content of organic matter substances and the low buffer capacities of sediments.
Źródło:
Geology, Geophysics and Environment; 2018, 44, 3; 309-317
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Eulalia picta Kinberg, 1866 – tube builder or specialized predator?
Autorzy:
Pabis, Krzysztof
Sobczyk, Robert
Powiązania:
https://bibliotekanauki.pl/articles/2042149.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Admiralty Bay
Antarctic
Eteoninae
Phyllodocidae
sediments
Tubes
Źródło:
Polish Polar Research; 2017, 38, 4; 485-491
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Diffusive Fluxes of CH4 and CO2 at the Sediment-Overlying Water Interface in Reservoir Ecosystems
Autorzy:
Gruca-Rokosz, R.
Powiązania:
https://bibliotekanauki.pl/articles/123672.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
methane
carbon dioxide
greenhouse gasses
reservoir
sediments
Opis:
The work detailed here concerned the CH4 and CO2 fluxes at the sediment-overlying water interface in Maziarnia and Nielisz Reservoirs, SE Poland. The research in question was conducted in the period of 2009-2011, the samples of sediment and overlying water were collected at two stations located in the upper and lower parts of each reservoir. The concentrations of CO2 and CH4 in pore water and overlying water were measured with the headspace method, using a Pye Unicam gas chromatograph (PU-4410/19) equipped with a methane analyzer allowing low CO2 concentrations to be detected. Diffusive fluxes of the analyzed gases at the sediment-overlying water interface were calculated on the basis of Fick’s first law, and were found to range from -0.01 to 3.48 mmol×m-2×d-1 for CH4 and from -1.27 to 47.02 mmol×m-2×d-1 for CO2. Comparable fluxes elsewhere typify the reservoirs experiencing far-reaching eutrophication. No dependent relationships were found between the values calculated for fluxes and either season of the year or sediment characteristics.
Źródło:
Journal of Ecological Engineering; 2018, 19, 5; 158-164
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Features of Heavy Metals Accumulation in Bottom Sediments of the Southern Bug Hydroecosystem
Autorzy:
Mitryasova, Olena
Koszelnik, Piotr
Gruca-Rokosz, Renata
Smirnov, Victor
Smirnova, Svitlana
Bezsonov, Yevgen
Zdeb, Monika
Ziembowicz, Sabina
Powiązania:
https://bibliotekanauki.pl/articles/124229.pdf
Data publikacji:
2020
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
heavy metals
hydroecosystem
bottom sediments
concentration ratio
Opis:
The performed studies allowed determining the peculiarities of heavy metals accumulation in the sediments, as well as the nature of their distribution in the hydroecosystem Southern Bug (Ukraine). Geochemical anomalies are formed in the zones of influence of industrial and urban agglomerations. Technogenic pollutions of bottom sediments with heavy metals affects the qualitative state of the water environment and can cause cumulative toxicosis on the hydrobiont population in the zones of geochemical anomalies formation, namely in the area of influence of the Nova Odessa and Mykolaiv cities. The mechanism of the cumulative toxicosis emergence is accompanied by chronic effects of low concentrations on hydrobionts with an excess of permissible fluctuations on a regional background, which ultimately contributes to the development of intoxication.
Źródło:
Journal of Ecological Engineering; 2020, 21, 3; 51-60
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Quality of Bottom Sediments of Midfield Ponds and Their Evaluation for the Potential Threat of the Aquatic Environment
Autorzy:
Szydłowski, K.
Brysiewicz, A.
Wesołowski, P.
Podlasińska, J.
Powiązania:
https://bibliotekanauki.pl/articles/125468.pdf
Data publikacji:
2017
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
midfield ponds
sediments
surface water
heavy metals
Opis:
The study aimed at the evaluation of the quality of bottom sediments and evaluation of potential threat to the aquatic environment. Cadmium, cobalt, chromium, copper, nickel, lead, zinc and mercury concentration in the separate layers of the sediments in the pond at Żelisławiec decreased with the depth of bottom sediments. On the other hand, the highest concentrations of the studied elements occurred in the deepest layer of sediments in the pond at Stare Czarnowo. The level of the potential ecological risk (PER) for the sediments of the Żelisławiec pond classifies them as sediments with low quality of the potential ecological risk, whereas the sediments from the pond at Stare Czarnowo are classified as moderate level of the potential ecological risk. In both ponds, the highest Igeo values were reported for zinc and lead.
Źródło:
Journal of Ecological Engineering; 2017, 18, 1; 65-71
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Możliwości wykorzystania osadów dennych pochodzących z rzeki San
Possibility of use of bottom sediments derived from the San River
Autorzy:
Maj, K.
Koszelnik, P.
Powiązania:
https://bibliotekanauki.pl/articles/401405.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
osady denne
jakość osadów
metale ciężkie
PCB
WWA
bottom sediments
quality of bottom sediments
heavy metals
PCB-s
Opis:
Osady denne są wydobywane z dna rzek, jezior, kanałów, zbiorników retencyjnych oraz stawów w celu zwiększenia ich pojemności retencyjnej oraz poprawy walorów użytkowych. Wydobyty urobek, który nie zawiera substancji szkodliwych może być odpowiednio wykorzystany. Kierunek zagospodarowania osadów dennych jest uzależniony od ich właściwości chemicznych i fizycznych. W pracy przedstawiono możliwości wykorzystania osadów dennych w rolnictwie, leśnictwie i budownictwie. Omówiono kryteria decydujące o technologii zagospodarowania osadów dennych. Ponadto zaproponowano własny schemat postępowania z wybagrowanymi osadami dennymi oparty na polskim prawodawstwie. Opierając się na wyżej wymienionym schemacie zaprezentowano potencjalne sposoby wykorzystania osadów dennych pochodzących z rzeki San. Charakterystyka chemiczna tych osadów wskazuje na ich umiarkowane zanieczyszczenie substancjami organicznymi i metalami ciężkimi, dlatego też mogą być zastosowane do użyźniania gruntów ujętych w Rozporządzenie Ministra Środowiska z dnia 9 września 2002 r. w sprawie standardów jakości gleby oraz standardów jakości ziemi (Dz.U. 2002 Nr 165 poz. 1359).
Bottom sediments are extracted from the bottom of river, lakes, canals, reservoirs, and ponds in order the enhance their capacity and to improve the retention values. Excavated spoils, that does not contain harmful substances may be used. The direction of the management of bottom sediments depends on their chemical and physical properties. At work are examples of the use of bottom sediments in agriculture, forestry and construction. Discusses the criteria for sediment management technology. Proposed their own scheme to use dredging sediments in compliance with the Polish legislation. Based on the above diagram shows the potential ways to use bottom sediment from river San. Physico-chemical characteristics of the sediments indicates on their moderate pollution of organic substances and heavy metals, be used to fertilize the land included in the Regulation of Minister of the Environment of 9 September 2002 on the quality of soil and earth quality standards (2002 No 165 pos. 1359).
Źródło:
Inżynieria Ekologiczna; 2016, 48; 147-152
2081-139X
2392-0629
Pojawia się w:
Inżynieria Ekologiczna
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Variability of textural characteristics of sandur deposits of Flaajókull and Falljókull (SE Iceland)
Autorzy:
Angiel, Piotr
Mikulska, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/2032503.pdf
Data publikacji:
2006-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
sandur
coarse clastic sediments
grain size parameters
Iceland
Opis:
Studies conducted on the sandurs of Flaajókull and Falljókull aimed at the reconstruction of the dynamics of braided rivers based on the grain size parameters of deposits. The goal of the project was to estimate the degree of deposit transformation and of changes of grain size characteristics as related to the length of transport in contemporary sandur rivers.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2006, 12; 111-117
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Preliminary suggestions on the Pleistocene palaeovegetation around the Biśnik Cave (Częstochowa Upland, Poland) based on studies of molecular fossils from cave sediments
Autorzy:
Krajcarz, Maciej T.
Gola, Marek R.
Cyrek, Krzysztof J.
Powiązania:
https://bibliotekanauki.pl/articles/2026713.pdf
Data publikacji:
2010
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
cave sediments
biomarkers
n-alkanes
gas chromatography
palaeoenvironment
Opis:
Bioenik Cave is an im por tant site of Mid dle Palaeo lithic, with the lon gest se quence of Neanderthal set tle ment phases in Cen tral Eu rope. In the pre vi ous stud ies of the Bioenik sed i ments, dif fer ent el e ments of palaeoenvironment in the pe ri - ods of Neanderthal oc cu pa tion have been re cog nised, ex cept of palaeovegetation, which could not be de rived be cause of lack of pre served plant mi cro- or macrofossils. The cur rent work is an at tempt to re con struct palaeovegetation in vi - cin ity of the Bioenik Cave, us ing anal y sis of com po si tion of plant-de rived n-al kanes, pre served in sed i ments. In our study, we an a lyzed one sam ple from each of the sed i ment’s lay ers 11 – 19c (early Late Pleis to cene and late Mid dle Pleis to cene). Abun dant n-al kanes (mostly n-C27, n-C29 and n-C31) were found in all the sam pled lay ers ex cept for the lay ers 12, 16 and 19d, show ing no al kanes at all. There is clear di ver si fi ca tion of n-al kanes com po si tion and CPI (car bon pref er ence in dex) val ues be tween lay ers. Anal y sis of this com po si tion, al lows us to claim that the lay ers 11 and 14 were ac cu mu lated when the cave’s vi cin ity was cov ered by dense co nif er ous for ests, hence upon warm cli mate. The lay ers 19, 19a lower, 19b and 19c, pre sumably orig i nated dur ing cold pe ri ods when open wood lands or grass lands dom i nated. The other an a lyzed lay ers could be con nected with in ter me di ate veg e ta tion in form of open wood land. How ever, not all of the achieved re sults stay in com pli ance with the ac tual stra tig ra phy, es tab lished bas ing on lithological data and palaeo ec ol ogy of fos sil fauna, and we hope that ex pla na tion of this dis crep ancy would be pos si ble af ter more ex ten sive stud ies of mo lec u lar fos sils are done.
Źródło:
Studia Quaternaria; 2010, 27; 55-61
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Preliminary report on unique laminated holocene sediments from the Garun Lake in Egypt
Autorzy:
Marks, Leszek
Salem, Alaa
Welc, Fabian
Nitychoruk, Jerzy
Chen, Zhongyuan
Zalat, Abdelfattah
Majecka, Aleksandra
Chodyka, Marta
Szymanek, Marcin
Tołoczko-Pasek, Anna
Powiązania:
https://bibliotekanauki.pl/articles/2027070.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Holocene
laminated sediments
Qarun Lake
Faiyum Oasis
Egypt
Opis:
The Lake Qarun (Faiyum Oasis, northern Egypt) is a relic of the much larger Holocene lake. Past lake levels and extensions were reconstructed, based on setting of archaeological sites scattered along northern paleoshores of the ancient lake. However, geoarcheological works did not yield enough data to establish continuous environmental history of the lake. A deep drilling FA-1 on the southeastern shore of the lake, performed in 2014, supplied with a core, 26 m long that is the one of the longest lake sediment cores in northeastern Africa. The basal section of the core consisted of thin-laminated diatom marly deposits, underlain at the Late Pleistocene/Holocene boundary by coarse-grained sands. The sediment lamine were quite well developed, especially in the lower part of the core. Preliminary results indicated annually deposited sediment sequence with seasonality signals provided by microlamine of diatoms, calcite, organic matter and clastic material. Early Holocene varved sediments from the Faiyum Oasis supplied with exceptional paleoenvironmental data for northeastern Africa, which enriched a record from previous logs drilled at the southwestern margin of the Qarun Lake.
Źródło:
Studia Quaternaria; 2016, 33; 35-46
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dumpstones as records of overturning ice rafts in a Weichselian proglacial lake (Rügen Island, NE Germany)
Autorzy:
Pisarska-Jamroży, M.
Van-Loon, A. J. T.
Bronikowska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060089.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dumpstones
dropstones
ice-rafted debris
Weichselian
glaciolacustrine sediments
Opis:
Dumpstones and dropstones up to 0.8 m in size occur in a silty/sandy Weichselian glaciolacustrine succession near Dwasieden on Rügen Island in the SW Baltic Sea (NE Germany). The deposits are exceptional because two levels of dumpstones and dropstones are present, suggesting two dumping phases interrupting characteristic fine-grained glaciolacustrine sedimentation. Plastic downwarping of sediments below the dumpstones and dropstones result in soft-sediment deformation structures. The distribution and orientation of the long axes of the clasts are useful tools for the reconstruction of the state of the lake bottom, as well as for the water depth. The horizontal position of the gravels and boulders (parallel to the bedding) suggests deposition in relatively shallow-water. The dumping events are linked to iceberg rafting in a glacial lake during the Weichselian Glaciation (MIS 2).
Źródło:
Geological Quarterly; 2018, 62, 4; 917-924
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Próba zastosowania zestalonych osadów ściekowych do budowy ekranów akustycznych
Application of solidified sewage sediments in construction of acoustic screens
Autorzy:
Sadowska, J.
Powiązania:
https://bibliotekanauki.pl/articles/2071269.pdf
Data publikacji:
2010
Wydawca:
Stowarzyszenie Inżynierów i Techników Mechaników Polskich
Tematy:
osady ściekowe
ekrany akustyczne
sewage sediments
acoustic screens
Opis:
Osady ściekowe jako odpady produkcyjne każdej oczyszczalni ścieków, w zasadzie podlegająutylizacji, która najczęściej polega na ich składowaniu na wydzielonych składowiskach. Zgodnie z obowiązującą ustawą o odpadach, nakazuje ona pracodawcy, aby każdy odpad podlegał gospodarczemu wykorzystaniu. Dalsze przetwarzanie osadów ściekowych do konkretnego ich zastosowania jest już procesem recyklingu. W artykule przedstawiono próbę zastosowania zestalonych (spiekanych) osadów ściekowych, jakie powstają na oczyszczalni ścieków w Nowem n/Wisłą, do budowy ekranów akustycznych, prezentując wyniki badań tego problemu.
Sewage sediments as waste produced in a wastewater treatment plant are usually utilized in separated storage fields. According to the Waste Management Act employers are obliged to utilise economically waste material.; Further processing of sewage sediments for their specific usage is treated as recycling. The paper presents an attempt to apply solidified (sintered) sewage deposits produced in the wastewater treatment plant in Nowe n/Wisłą, in construction of acoustic screens.
Źródło:
Inżynieria i Aparatura Chemiczna; 2010, 5; 103-104
0368-0827
Pojawia się w:
Inżynieria i Aparatura Chemiczna
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chemiczne frakcjonowanie cynku w osadach rzecznych dorzecza południowej i środkowej Wisły
Chemical fractionation of zinc in bottom sediments of the southern and middle Vistula River drainage basin
Autorzy:
Świetlik, R.
Rabajczyk, A.
Trojanowska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074652.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
cynk
frakcjonowanie
osaday rzeczne
zinc
fractionation
river sediments
Opis:
In Poland, the average Zn contents in river sediments keep up the level 100 mg/kg. The largest accumulations of zinc (up to 10 000 mg/kg), found in river sediments in the Upper and Lower Silesia area, are the result of mining and industrial activity in these regions. In the remaining parts of the country the contents are clearly smaller, except for the conurbation areas (Lis & Pasieczna, 1995). At present, forecasts of behavior of me- tals present in solid environmental samples are usually based on results of chemical fractionation. In this approach, metals are extracted by treating samples with solutions of increasing solubilization potential and simulating extgraction of metals under natural and anthropogenically modified environmental conditions (Rauret, 1998). The studies covered speciation of zinc in river sediments of the Nida and Radomka drainage basins. The chemical fractionation of zinc was conducted in accordance with three-stage procedure of sequential extraction BCR (at present, Standard Measurement and Testing Program), worked out by Ure et al. (1993). The aim of investigations was to compare forms of occurrence of zinc in sediments of rivers flowing through areas differing in geochemical background and characterized by differences in content of anthropogenic zinc. The speciation of zinc in sediment samples from the Radomka drainage basin gave results clearly different from those for sediments from the Nida drainage basin, which may reflect differences in land use. The content of zinc in the studied samples was found to change for 8 mg/kg in bottom deposits of Radomka River at Domaniów to 267 mg/kg in those of Mleczna River at Firlej in the Radomka drainage basin and from 88 mg/kg in sediments of Maskalis River at Brzezie to 101 mg/kg in those of the Brzeźnica River at Raków in the Nida drainage basin.
Źródło:
Przegląd Geologiczny; 2009, 57, 12; 1101-1105
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Detection of near-surface geological heterogeneity at Starunia palaeontological site and vicinity (Carpathian region, Ukraine) based on microgravity survey
Autorzy:
Porzucek, S.
Madej, J.
Powiązania:
https://bibliotekanauki.pl/articles/191491.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
geophysics
microgravity
Quaternary sediments
Starunia
Carpathian region
Ukraine
Opis:
Results of a microgravity survey performed in the abandoned Starunia ozokerite mine (Carpathian region, Ukraine), where in the early 20th century well preserved remains of large, extinct mammals were found, are discussed in the paper. A number of gravity anomalies indicating the geological heterogeneity at the sub-Quaternary strata have been observed. The assumed measurement observations also enabled the authors to interpret the results in view of density changes in the Quaternary strata. Most of the registered microanomalies coincide with the high-halite and ozokeritic Miocene salt-bearing Vorotyshcha beds. The distribution of the microanomalies reveals neither their correlation with the thickness of overburdens, nor any gravity impact of numerous abandoned wells. Gravity anomalies were mostly connected with the lithology of sediments and rocks obtained from geological boreholes drilled in the years 2007 and 2008, on the basis of which the anomalies' origin could be determined. A concentric, relatively negative gravity microanomaly of ca. 25 m in diameter was registered in the place, where very well preserved relics of the woolly rhinoceros had been found. They may be indicative of the existence of Pleistocene lakes (and/or palaeoswamps), into which the woolly rhinoceroses had sunk. Hence, an assumption can be made that the further search for successive zoological relics can be made in areas with similar anomalies under the low-density sub-Quaternary subcrop.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 3; 365-374
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Potential effect of pH on the leaching of heavy metals from sediments of the Carpathian dam reservoirs
Autorzy:
Szarek-Gwiazda, E.
Powiązania:
https://bibliotekanauki.pl/articles/184689.pdf
Data publikacji:
2014
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Carpathian reservoir
sediments
heavy metals
buffer capacity
pH
Opis:
Eutrophication processes occurring in the Carpathian dam reservoirs (southern Poland) have resulted in a drastic increase of incidences of decrease of pH and oxygen content in near-bottom water, which may affect metal remobilization from the sediment. The study is aimed to determine the buffer capacity and effects of decreasing pH on the remobilization of heavy metals (Cd, Pb, Cu, Zn, Mn and Fe) from sediments of the Dobczycki Reservoir (DR), the Czorsztyński Reservoir (CR), and the Rożnowski Reservoir (RR), the right side tributary of the Vistula River. Buffering capacity and the leaching of heavy metals from sediments accompanied with an increase in acidity were analyzed in 0.00-0.24 M HNO3 solutions. Studied sediments had a high buffer capacity. Buffer capacity of sediments at studied sites of the DR and CR was different due to differences in the composition of sediments. The reservoir sediments had a variable ability to release heavy metals with increasing acidity. At pH ~5 and pH ~3, a considerable leaching of Mn (up to 60% and 85% of the total amount, respectively), Cd (up to 35% and 56% respectively), Pb (up to 25% and 39%), the lower leaching of Cu (up to 18% and 30%) and Zn (up to 14% and 20%), and the lowest leaching of Fe (below 5%) were found. The decrease of pH of the water-sediment system caused by eutrophication processes may affect the mobilization of certain heavy metals (mainly Mn, Cd and Pb) from sediment into the water column of the studied Carpathian reservoirs.
Źródło:
Geology, Geophysics and Environment; 2014, 40, 4; 349-358
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wielkopolska epoka lodowa : osady i formy glacjalne w wybranych stanowiskach Wielkopolski
Autorzy:
Kasprzak, L.
Ewertowski, M.
Szuman, I.
Powiązania:
https://bibliotekanauki.pl/articles/294982.pdf
Data publikacji:
2011
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
Weichselian ice sheet
glacial sediments and landforms
Polska
Opis:
Glacial environment is characterised by a very wide variety of sediments. In contrast to other sedimentary environments it is difficult to determine the leading unit. Therefore, more often the complexes of sediments and forms are examined, rather than individual facies indicator. The aim of this paper is to present a diversity of forms and sediments in Wielkopolska (in selected study area, which will be presented during the excursion) with an attempt to interpret their sedimentary environment. The authors do not concentrate on discussion about the importance of frontal or areal deglaciation in the formation and differentiation of forms and sediments. They emphasise the importance of depositional effectiveness.
Źródło:
Landform Analysis; 2011, 16; 155-186
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wybrane właściwości chemiczne osadów dennych wód otwartych w zlewni Raszynki
Selected chemical characteristics of the bottom sediments in the Raszynka River catchment
Autorzy:
Dąbkowski, S. L.
Pawłat-Zawrzykraj, A.
Powiązania:
https://bibliotekanauki.pl/articles/338662.pdf
Data publikacji:
2003
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
osady denne
wody powierzchniowe
bottom sediments
surface water
Opis:
Artykuł przedstawia wyniki analiz wybranych wskaźników chemicznych osadów dennych wód Raszynki, jej dopływów oraz Stawów Raszyńskich. Odczyn osadów w większości przypadków jest obojętny lub lekko kwaśny, optymalny dla rozwoju fauny i flory środowiska wodnego. Przeważają osady mineralne lub z domieszką substancji organicznej. Zawartość azotu ogólnego i pojemność sorpcyjna zależą od pojemności substancji organicznej w osadach. Osady nie są skażone chemicznie.
The article presents results of analyses of selected chemical indicators of the bottom depo sit taken from the Raszynka River, its tributaries and several ponds located in the catchment. Reaction (pH) of the sediments was mostly neutral or slightly acidic – optimum for the growth of aquatic flora and fauna. Mineral sediments with small admixtures of organic matter prevailed. Concentration of total nitrogen and sorption capacity depended on the content of organic matter in the sediments. The analysis indicate that contamination of the bottom sediments does not exceed standards.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2003, T. 3, z. spec. (6); 141-148
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Fluwialna geneza ogniwa wielkopolskiego na podstawie danych z obszaru środkowej Polski
Fluvial origin the Wielkopolska member based on data from the central Poland
Autorzy:
Widera, M.
Powiązania:
https://bibliotekanauki.pl/articles/170153.pdf
Data publikacji:
2012
Wydawca:
Poltegor-Instytut Instytut Górnictwa Odkrywkowego
Tematy:
neogen
osady fluwialne
geneza
Neogene
fluvial sediments
origin
Opis:
Osady drobnoklastyczne zalegające w stropie neogenu na Niżu Polskim nie mają wyjaśnionej genezy. Osady te są bardzo ważną kopaliną, często towarzyszącą wydobyciu węgla brunatnego. Wśród badaczy istnieją różne hipotezy na temat ich powstania, często wzajemnie wykluczające się, tj. jeziorna, morska i rzeczna, albo ich kombinacje. Na podstawie danych otworowych z okolic Poznania oraz obserwacji ścian odkrywek w KWB Konin dostarczono dowodów potwierdzających rzeczne pochodzenie osadów ogniwa wielkopolskiego. Ponadto wskazano na anastomozujący typ rzek, które doprowadziły do powstania izolowanych litosomów piaszczystych w otoczeniu osadów iłowo-mułowych.
Fine-grained sediments rested at the top of Neogene in the Polish Lowlands until now have not explained the origin. Be-cause they are very important minerals, often accompanied by lignite mining, certainly require further research. Among resear-chers, there are various hypotheses about their origin, often mutually exclusive, i.e. a lake, sea and evidence of the fluvial origin of the Wielkopolska. Member has been provided. Additionally, it has been indicated the anastomosing type of rivers that led to the of solated sandy bodies, which are surrounded by clayey-silty sediments.
Źródło:
Górnictwo Odkrywkowe; 2012, 53, 1-2; 109-118
0043-2075
Pojawia się w:
Górnictwo Odkrywkowe
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Biodegradation of bottom sediments of Turawa Lake
Autorzy:
Latała, A.
Wierzba, S.
Powiązania:
https://bibliotekanauki.pl/articles/779843.pdf
Data publikacji:
2007
Wydawca:
Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
Tematy:
osad denny
biopreparat
biodegradacja
bottom sediments
biopreparation
biodegradation
Opis:
In this work we tested biopreparations developed in our laboratory for their ability to degrade the organic matter of the bottom sediments of Turawa Lake. The biodegradation was conducted under laboratory conditions for 6 weeks. For the testing purposes, there were three variants of biopreparations that contained autochthonous strains originating from our own collection and their mixture. The testing showed that the introduction of the biopreparations to the bottom sediment resulted in a significant increase of the number of bacteria, which consequently brought about the reduction of organic compounds in the sediment. In the case of all the variants, the number of bacteria increased by order of 10^2 - 10^4 CFU/g after 42 days of biodegradation. Among the tested biopreparations, the most effective one was the mixture of the autochthonous strains and those originating from the collection. After biopreparation was applied, a drop of content of carbohydrates by 66.94%, fatty matter by 83.33% and proteins by 74.42% was noted.
Źródło:
Polish Journal of Chemical Technology; 2007, 9, 2; 73-77
1509-8117
1899-4741
Pojawia się w:
Polish Journal of Chemical Technology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution of Nickel, Copper and Cobalt in the Grain Fractions of Bottom Sediments of the Sokołda River and its Tributaries (Poland)
Autorzy:
Skorbiłowicz, Elżbieta
Skorbiłowicz, Mirosław
Misztal, Wojciech
Powiązania:
https://bibliotekanauki.pl/articles/123363.pdf
Data publikacji:
2020
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
metals
heavy metals
bottom sediments
grain fraction
rivers
Opis:
In recent years, the interest in the occurrence of heavy metals in the natural environment has been observed. The heavy metal contamination can lead to serious environmental problems. The aim of the study was to estimate the total content of heavy metals: Ni, Cu and Co, in the surface layer of the bottom sediments of the Sokołda river and its tributaries, and to determine the relationship between the grain size and scope of their metal content. Determination of metals in the bottom sediment samples was performed by means of atomic absorption spectrometry (ASA). The research on the Sokołda river and its tributaries showed low levels of Ni, Cu and Co. It was proven that the majority of studied metals were contained in the smallest clay fraction <0.02 mm. On the other hand, the least studied metals were accumulated in 1.0–0.2 mm and 0.2–0.1 mm fractions. The 1.0–0.2 mm and 0.2–0.1 mm fractions contain around 80% of the tested metal forms, while the 0.02–0.063 mm and <0.02 mm fractions – only a few percent. This speaks for the determination of metals in the 1.0–0.1 mm fraction, that contains both coarser and clay fractions, and thus most reliably reflects the actual load of pollutants carried by the sediment. Studies have shown that the main sources of pollution in the Sokołda river catchment are primarily surface runoff, and to a lesser extent, wastewater (municipal and industrial).
Źródło:
Journal of Ecological Engineering; 2020, 21, 1; 89-97
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Osady okruchowe strefy płytkowodnej oraz plażowej wybranych regionów Indonezji
Detrital sediments of shallow marine and beach zone in selected regions of Indonesia
Autorzy:
Szamałek, K.
Zglinicki, K.
Marciniak-Maliszewska, B.
Konopka, G.
Powiązania:
https://bibliotekanauki.pl/articles/169883.pdf
Data publikacji:
2015
Wydawca:
Poltegor-Instytut Instytut Górnictwa Odkrywkowego
Tematy:
osady okruchowe
prace geologiczne
detrital sediments
geological exploration
Opis:
W ramach prospekcyjnych prac geologicznych na obszarze wschodniej Indonezji dokonano wstępnego rozpoznania plażowych oraz morskich osadów okruchowych. Przedmiotem badań były również odpady powydobywcze (tailing) powstałe w wyniku przerobu piasków kasyterytonośnych pozyskiwanych wzdłuż wybrzeży wyspy Bangka (Indonezja Zachodnia). Celem badań było określenie potencjału złożowego wybranych regionów Indonezji. Przeprowadzone wstępne badania wykazały, że najbardziej perspektywicznym regionem występowania pierwiastków krytycznych jest rejon Indonezji Zachodniej, gdzie w obszarze alimentacji występują głównie skały magmowe kwaśne. W osadach antropogenicznych stwierdzono obecność minerałów – nośników lekkich (monacyt) oraz ciężkich pierwiastków ziem rzadkich (ksenotym), które mogą stanowić sumarycznie nawet do 39% masy próbek. Dodatkowo z osadów można odzyskać cyrkon oraz minerały żelaza i tytanu. Odmienny charakter mają utwory badane na obszarze Indonezji Wschodniej (Halmahera, Nowa Gwinea). We frakcji ciężkiej stwierdzono obecność minerałów o znaczeniu złożowym głównie magnetytu, spinelu chromowego, hematytu, rutylu oraz ilmenitu, co jest typowe dla osadów występujących w pozycji geotektonicznej łuków wysp i basenów marginalnych.
Within the framework of geological exploration in the Eastern Indonesia, preliminary examination of beach and shallow marine sediments, have been conducted. The subject of this study were also tailings formed during processing of cassiterite bearing sand, mined alongside the shores of Bangka (Western Indonesia). Aim of this study was to assess the potential of occurrence of mineral deposits in the selected perspective areas. Initial laboratory results show that the most promising region, in terms of occurrence of critical elements is Western Indonesia (Bangka – Belitung province), where felsic magmatic rocks occur. Monazite and xenotime were detected here in abundance (up to 39%w) in anthropogenic deposits. What is more these deposits are the potential source of zircon and various Fe and Ti minerals. Different mineralogical and geochemical character of sampled eastern Indonesian deposits (Halmahera, New Guinea) is the result of distinct geotectonic position of sediment sources – intraoceanic magmatic arcs and marginal basins. Here, identified minerals of economic importance are: magnetite, hematite, ilmenite and chromium spinels.
Źródło:
Górnictwo Odkrywkowe; 2015, 56, 5; 14-20
0043-2075
Pojawia się w:
Górnictwo Odkrywkowe
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pressuremeter test in glaciated valley sediments (Andorra, Southern Pyrenees). Part 1, An improved approach to their geomechanical behaviour
Autorzy:
Turu, V.
Powiązania:
https://bibliotekanauki.pl/articles/295218.pdf
Data publikacji:
2007
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
glaciated valley sediments
Andorra
Southern Pyrenees
geomechanical behaviour
Źródło:
Landform Analysis; 2007, 5; 89-94
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Seasonal Changes of Phosphorus Release from the Bottom Sediments of Rusalka Lake During the Restoration Process
Sezonowe zmiany uwalniania fosforu z osadów dennych w jeziorze Rusałka w trakcie zabiegów rekultywacyjnych
Autorzy:
Kowalczewska-Madura, K.
Dondajewska, R.
Gołdyn, R.
Powiązania:
https://bibliotekanauki.pl/articles/388232.pdf
Data publikacji:
2011
Wydawca:
Towarzystwo Chemii i Inżynierii Ekologicznej
Tematy:
osady denne
fosfor
rekultywacja
bottom sediments
phosphorus
restoration
Opis:
Paper presents a comparative study of phosphorus (P) internal loading from bottom sediments in Rusalka Lake in years 2006 and 2007, when restoration measures were conducted and in 2005, a year before restoration. Internal loading of P decreased as an effect of applied treatment. The mean loading in 2005 was 9.07 mg P m–2 d–1, whilst in next two years it was 4.36 mg P m–2 d–1 and 2.28 mg P m–2 d–1, respectively. The reduction reached 51 % in 2006 and 75 % in 2007. A domination of P release was noted in 2005 and 2006, amounting in summer to 38.1 mg P m–2 d–1 in the deepest place of the lake and 15.6 mg P m–2 d–1 in the littoral zone. A period of accumulation supremacy was observed in spring 2007, reaching 4.9 mg P m–2 d–1 in the littoral and 2.8 mg P m–2 d–1 in the profundal.
Praca prezentuje zmiany uwalniania fosforu z osadów dennych w jeziorze Rusałka w latach 2006–2007, kiedy prowadzono rekultywację zbiornika z użyciem siarczanu(VI) żelaza(III). W wyniku przeprowadzonych zabiegów rekultywacyjnych zasilanie wewnętrzne w fosfor z osadów dennych wyraźnie zmniejszyło się. Średnie zasilanie wewnętrzne przed wykonaniem zabiegów rekultywacyjnych wynosiło 9,07 mg P m–2 d–1, w kolejnym zmniejszyło się do 4,36 mg P m–2 d–1 (redukcja o 51 %), a w ostatnim roku do 2,28 mg P m–2 d–1 (redukcja o 75 %). W latach 2005 i 2006 stwierdzano wydzielanie fosforu z osadów dennych, dochodzące w okresie letnim do 38,1 mg P m–2 d–1 w obrębie głęboczka i do 15,6 mg P m–2 d–1 w litoralu. W ostatnim roku badań wiosną, nie następowało wydzielanie P z osadów, a kumulacja P osiągnęła 4,9 mg P m–2 d–1 w litoralu i 2,8 mg P m–2 d–1 na głęboczku.
Źródło:
Ecological Chemistry and Engineering. A; 2011, 18, 2; 219-224
1898-6188
2084-4530
Pojawia się w:
Ecological Chemistry and Engineering. A
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Lagoon sediments in the central part of the Vistula spit: geochronology, sedimentary environment and peculiarities of geological settings
Autorzy:
Bitinas, A.
Boldyrev, V.
Damušyte, A.
Grigiene, A.
Vaikutiene, A.
Žaromskis, R.
Powiązania:
https://bibliotekanauki.pl/articles/1205004.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
gyttja
lagoon sediments
neotectonics
Vistula Spit
Baltic Sea
Opis:
Lagoon gyttja layers occurring in anomalously high position (up to 2.5 m above the present-day sea level) are known from the central part of the Vistula Spit (Kaliningrad region of the Russian Federation). Complex investigations of lagoon sediments (gyttja, sand), including radiocarbon (14C) dating as well as mollusc, pollen and diatom analyses, have been carried out in 2004–2005. The results of these investigations indicate that the lagoon sediments were deposited in the Late Subboreal–Early Subatlantic period in a shallow freshwater, overgrown basin periodically influenced by brackish water. The anomalously high level of the lagoon gyttja is determined by neotectonic activity of Earth’s crust blocks.
Źródło:
Polish Geological Institute Special Papers; 2008, 23; 9-20
1507-9791
Pojawia się w:
Polish Geological Institute Special Papers
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Constraints of the MAX4781 CMOS Solution for Electrode Switching in Multilayer Electrochemical Probes
Autorzy:
Cimpoiasu, V.M.
Radulescu, F.
Nealson, K.H.
Moga, Ioana Corina
Popa, R.
Powiązania:
https://bibliotekanauki.pl/articles/2106598.pdf
Data publikacji:
2022
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
sensor
SPEAR
multielectrode
redox interface
sediments
electrochemical gradients
Opis:
The most common means to analyze redox gradients in sediments is by push/pulling electrochemical probes through sediment’ strata while repeating measurements. Yet, as electrodes move up and down they disrupt the texture of the sediment layers thus biasing subsequent measurements. This makes it difficult to obtain reproducible measurements or to study the evolution of electrochemical gradients. One solution for solving this problem is to eliminate actuators and electrode movements altogether, while instead deploying probes with numerous electrodes positioned at various depths in the sediment. This mode of operation requires electrode switching. We discuss an electrode-switching solution for multi-electrode probes, based on Complementary Metal-Oxide-Semiconductor (CMOS) multiplexors. In this solution, electrodes can be individually activated in any order, sequence or time frame through digital software commands. We discuss constraints of CMOS-based multilayer electrochemical probes during cyclic voltammetry.
Źródło:
Archives of Metallurgy and Materials; 2022, 67, 2; 691--694
1733-3490
Pojawia się w:
Archives of Metallurgy and Materials
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Distribution of Metals in Sediments of the Likova, Kumanova and Pçinja Rivers: Spring Season
Autorzy:
Ejupi, N.
Korça, B.
Durmishi, B. H.
Durmishi, A.
Ejupi, E.
Ismaili, M.
Jashari, A.
Shabani, A.
Powiązania:
https://bibliotekanauki.pl/articles/123812.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
metals
pollution
physical-chemical parameters
sediments
river water
Opis:
The pollution of rivers is an important issue because the utilization of polluted water has a direct effect on the health of people and other living beings, economy, etc. Sediments represent a very suitable indicator for monitoring and detecting pollution sources of river waters. The aim of this study is to analyze the contents of selected metals in the sediments of the rivers Likova, Kumanova and Pçinja rivers. The water samples were taken in June 2014 from six sampling stations. Several physicochemical parameters of rivers were determined and the contents of twenty-two metals was indicated in the sediment samples taken from these rivers. The obtained physico-chemical quality of the water from these rivers resulted in classification to the first/second category. The sediments were mostly polluted by Al, Ca, Na and Mg. The metals that exceeded the Dutch standard were: Ba, Ni, Zn, Cr and Cu. The order of metals in sediments was as follows: Fe > Al > Ca > Na > Mg > K > Mn > Ba > Sr > Cr > Zn > V > Ni > Cu > Pb > Li. The study results reveal a mild pollution in rivers caused by urban, agricultural and industrial activities.
Źródło:
Journal of Ecological Engineering; 2018, 19, 3; 80-92
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ashes from Sewage Sludge and Bottom Sediments as a Source of Bioavailable Phosphorus
Autorzy:
Ciesielczuk, T.
Rosik-Dulewska, C.
Poluszyńska, J.
Ślęzak, E.
Łuczak, K.
Powiązania:
https://bibliotekanauki.pl/articles/125013.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
phosphorus
bioavailability
ash
sewage sludge
bottom sediments
extraction
Opis:
Phosphorus is an element necessary for the growth of plants. As phosphate rock gets depleted, it becomes an increasingly scarce resource. Therefore, it seems necessary to implement simple methods of cheap and effective phosphorus recovery from waste. The ashes of municipal sewage sludge and bottom sediments constitute particularly valuable sources of phosphorus. However, these materials usually carry significant amounts of pollutants, including heavy metals. Optimization of ash phosphorus sequential extraction methods from a thermal conversion of sewage sludge and bottom sediments allows to select an effective and simple technology of phosphorus recovery, while maintaining low heavy metal pollution, which is one of the main restrictions in use of ashes. Determination of an amount of bioavailable phosphorus is therefore a basis for estimation of the possibility of using it from waste. Extraction using the Golterman method or shaking out with calcium lactate or Trougs reagent indicates that the ashes from sewage sludge and bottom sediments are rich sources of bioavailable phosphorus, which could find use under field conditions as a viable alternative to fertilizers containing fossil phosphorus.
Źródło:
Journal of Ecological Engineering; 2018, 19, 4; 88-94
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochemistry of waters and bottom sediments in landslide lakes in Babiogórski National Park
Autorzy:
Sala, Dariusz
Rzepa, Grzegorz
Powiązania:
https://bibliotekanauki.pl/articles/2086487.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
bottom sediments
water
trace elements
Babiogórski National Park
Opis:
The aim of this work was to assess the contamination of the landslide lakes located within Babiogórski National Park. For this purpose, samples of water and bottom sediment from 12 lakes were collected. Chemical analyses of the waters (including main cation and anion concentrations, trace-metal levels and selected physicochemical parameters) and of the sediments (including heavy metals) were performed. The waters are acidic to neutral and are characterized by low mineralization. Concentrations of trace elements are commonly low. Elevated levels of Fe, Mn and Al are probably related to natural geochemical processes. The sediments are strongly contaminated by Cd, whereas other trace metals levels are at their hydrogeochemical background. The high level of Cd contamination is most probably related to long-range industrial emissions.
Źródło:
Mineralogia; 2011, 42, 1; 63--72
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochemistry of waters and bottom sediments in landslide lakes in Babiogórski National Park
Autorzy:
Sala, D.
Rzepa, G.
Powiązania:
https://bibliotekanauki.pl/articles/2086539.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
bottom sediments
water
trace elements
Babiogórski National Park
Opis:
The aim of this work was to assess the contamination of the landslide lakes located within Babiogórski National Park. For this purpose, samples of water and bottom sediment from 12 lakes were collected. Chemical analyses of the waters (including main cation and anion concentrations, trace-metal levels and selected physicochemical parameters) and of the sediments (including heavy metals) were performed. The waters are acidic to neutral and are characterized by low mineralization. Concentrations of trace elements are commonly low. Elevated levels of Fe, Mn and Al are probably related to natural geochemical processes. The sediments are strongly contaminated by Cd, whereas other trace metals levels are at their hydrogeochemical background. The high level of Cd contamination is most probably related to long-range industrial emissions.
Źródło:
Mineralogia; 2011, 42, 1; 63--72
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka osadów dennych zbiornika zaporowego młyny oraz możliwość rolniczego ich wykorzystania
Characteristics of bottom sediments of retention reservoir młyny and a possibility of their agricultural use
Autorzy:
Gałka, B.
Wiatkowski, M.
Powiązania:
https://bibliotekanauki.pl/articles/338890.pdf
Data publikacji:
2010
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
osady denne
zbiornik wodny
metale ciężkie
makroelementy
wykorzystanie rolnicze osadów
bottom sediments
reservoir
heavy metals
macroelements
agricultural use of sediments
Opis:
W pracy przestawiono charakterystykę właściwości fizykochemicznych osadów dennych zbiornika Młyny na rzece Julianpolka oraz ocenę możliwości ich rolniczego wykorzystania na podstawie koncentracji pierwiastków śladowych (Ni, Zn, Pb, Cu). Badania wykazały następujące zawartości metali (w mg·kg-¹): Pb - 3-109, Zn - 25-302, Cu - 39-79 oraz Ni - 10-69. Zgodnie z klasyfikacją osadów wodnych PIG, osady denne z niektórych części zbiornika Młyny należy zaliczyć do zanieczyszczonych. Wartości indeksów geoakumulacyjnych Igeo kwalifikują osady do klasy 1., to jest osadów nieobciążonych lub umiarkowanie obciążonych. Według wytycznych PIOŚ i IUNG, jakość osadów odpowiada glebom o II stopniu zanieczyszczenia, które stwarzają ograniczenia dotyczące uprawy niektórych roślin konsumpcyjnych. Jednak zgodnie z rozporządzeniami Ministra Środowiska (w sprawie rodzaju oraz stężeń substancji, które powodują, że urobek jest zanieczyszczony, oraz w sprawie standardów jakości gleby i ziemi) badane osady nie są zanieczyszczone, co oznacza, że mogą być stosowane do rekultywacji lub ulepszania gruntów o przeznaczeniu rolniczym lub leśnym, z wyjątkiem osadów położonych w najbliższym sąsiedztwie zapory.
The paper presents a characteristic of physical and chemical properties of bottom sediments from retention reservoir Młyny located on the Julianpolka River and an assessment of their usefulness for agricultural application, based on the concentration of trace elements (Ni, Zn, Pb, Cu). Heavy metal concentrations (in mg·kg-¹) were: Pb 3-109, Zn 25-302, Cu 39-79, and Ni 10-69. According to classification of bottom sediments quality used by Polish Geological Institute, the sediments under study were contaminated in some parts of reservoir. The values of geo-accumulation index Igeo qualify sediments to the class 1, which involves not polluted or moderately polluted sediments. According to the standards of the State Inspectorate for Environmental Protection and the Institute of Soil Science and Plant Cultivation, sediment quality was comparable with that of soils of the 2nd level of heavy metal contamination. According to these standards, production of vegetables is not allowed in soils or sediments of such quality. However, two regulations of the Ministry of Environment (a) on the kind and concentration of substances that pollute bottom sediments, and (b) on soil and earth quality standards, classify the sediments under study as uncontaminated, with the exception of sediments located in the close proximity of the dam. Bottom sediments of the reservoir Młyny are suitable for reclamation and improvement of soils in agriculture and forestry.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2010, 10, 4; 53-63
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena zanieczyszczenia osadów w zbiornikach wodnych w aspekcie użytkowania gruntów
Assessment of sediment contamination in water reservoirs in the aspect of land use
Autorzy:
Jaguś, A.
Rzętała, M. A.
Rzętała, M.
Powiązania:
https://bibliotekanauki.pl/articles/126386.pdf
Data publikacji:
2013
Wydawca:
Towarzystwo Chemii i Inżynierii Ekologicznej
Tematy:
region górnośląski
zbiornik wodny
osady deltowe
osady denne
zanieczyszczenie gruntów
Upper Silesian region
water reservoir
delta sediments
bottom sediments
land contamination
Opis:
Powstawanie osadów w misach zbiorników wodnych jest niepożądane, gdyż wiąże się z ich zamulaniem oraz wzrostem żyzności wód. Osady mogą być również środowiskiem akumulacji mikrozanieczyszczeń. Podjęte badania dotyczyły oceny możliwości wykorzystania osadów do prac ziemnych, warunkowanego stopniem ich zanieczyszczenia. Badano osady deltowe i denne w wybranych zbiornikach wodnych regionu górnośląskiego. Określano stężenia metali śladowych (As, Ba, Cd, Co, Cr, Cu, Ni, Pb, Zn) zgodnie z przepisami prawnymi, dotyczącymi warunków dopuszczenia wykorzystania osadów. Badania wykazały znaczny stopień zanieczyszczenia osadów, zwłaszcza barem, kadmem, ołowiem i cynkiem. Stężenia tych metali często dopuszczały możliwość wykorzystania osadów tylko na terenach przemysłowych, a w niektórych przypadkach wykorzystanie nawet tam byłoby niedopuszczalne. Pod względem zawartości kobaltu i niklu (stężenia stosunkowo niskie) część badanych osadów mogłaby być wykorzystana na wszelkich terenach, nawet objętych ochroną prawną. Zanieczyszczenie chromem i miedzią na ogół dyskwalifikowało wykorzystanie osadów na terenach chronionych, jednak byłoby ono możliwe na obszarach rolniczych i leśnych. Stopień zanieczyszczenia osadów odzwierciedlał wpływy antropogenne na dany zbiornik, na ogół znaczące w obszarze badań. Możliwości wykorzystania osadów ze zbiorników regionu górnośląskiego na potrzeby prac ziemnych są zatem bardzo ograniczone.
Formation of sediments in basins of water reservoirs is an unfavourable aspect, because it is related to siltation and increased fertility of water. Sediments may also be the environment for accumulation of microcontaminants. The aim of the research was to determine the possibility to use the sediments in earthworks, depending on the degree of their contamination. The research included studies of delta and bottom sediments in selected reservoirs of the Upper Silesian region. Concentrations of trace metals (As, Ba, Cd, Co, Cr, Cu, Ni, Pb, Zn) were determined, according to legal regulations regarding the conditions for permitted use of sediments. The research showed a large degree of contamination of sediments, particularly with barium, cadmium, lead and zinc. Concentrations of these metals often allowed for the use of sediments only in industrial areas, and in some cases even industrial use would be forbidden. Considering the contents of cobalt and nickel (relatively low concentrations), some of the analysed sediments could be used in all kinds of land, including legally protected areas. Contamination with chromium and copper generally disqualified the sediments from use in protected areas, but it would be possible to use them in agricultural and forested land. The degree of sediment contamination reflected anthropogenic impact on a given reservoir, which generally was significant in the research area. Therefore, the potential use of sediments from water reservoirs in the Upper Silesian region is largely limited.
Źródło:
Proceedings of ECOpole; 2013, 7, 1; 349-355
1898-617X
2084-4557
Pojawia się w:
Proceedings of ECOpole
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochemiczna zmienność pierwiastków ziem rzadkich i metali ciężkich w osadach profundalu i litoralu wybranych jezior Polski
Geochemical variability of rare earth elements and heavy metals in profundal and littoral sediments from selected lakes of Poland
Autorzy:
Małecka, K.
Powiązania:
https://bibliotekanauki.pl/articles/2062779.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
osady jeziorne
REE
metale ciężkie
lake sediments
heavy metals
Opis:
Z 30 jezior położonych na pojezierzach Pomorskim, Wielkopolsko-Kujawskim i Warmińsko-Mazurskim pobrano po 2 próbki osadów (ze strefy litoralnej i profundalnej). Do badań wytypowano jeziora położone na podłożu o jednorodnej budowie geologicznej. Połowa z nich leży na podłożu o małej przepuszczalności (gliny, iły) i połowa na obszarach o dużej przepuszczalności (piaski, żwiry). Po roztworzeniu w wodzie królewskiej w próbkach osadów jeziornych oznaczono zawartość REE (La, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu) metodą ICP-MS oraz As, Cd, Co, Cu, Hg, Mo, Ni, Pb, Sn, V, W, Zn metodą ICP-OES. Osady jezior położonych na glinach i iłach charakteryzowały się większą zawartością pierwiastków REE, metali ciężkich i arsenu w stosunku do osadów jezior położonych na piaskach i żwirach. Większe zawartości REE występują w strefie litoralnej w porównaniu ze strefą profundalną, co wskazuje, że na ich zawartość wpływa głównie skład chemiczny podłoża zlewni, czynnik antropogeniczny odgrywa mniejszą rolę. Dystrybucja metali ciężkich i arsenu zależy od rodzaju podłoża, na którym powstała misa jeziorna i głębokości sedymentacji – gromadzą się one głównie w strefie profundalnej.
Sixty sediment samples were collected from 30 glacial lakes of Pomerania, Wielkopolska-Kujawy and Warmia-Masuria Lakelands. The influence of the lake basin lithology and sedimentation zone on the contents of the elements in sediment was investigated. The samples were digested in Aqua Regia and analysed by ICP-MS methods and ICP-OES techniques for REE contents (La, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu). As, Cd, Co, Cu, Hg, Mo, Ni, Pb, Sn, V, W, Zn contents were determined by ICP-OES method. The sediments show higher contents of REE in the littoral zone than in the profundal zone. The sediments from the lakes located on low-permeable glacial sediments are more abundant in heavy metals and REE in relation to the sediments from the lakes located on highly permeable glacial sediments. Distribution of the trace elements in lake sediments is strongly dependent on the type of geological formations on which the lake is developed and on the sedimentation zone of the lake. REE are preferentially accumulated in the littoral zone contrary to the heavy metals that are accumulated in the deepest zone of the lake. Factor analysis proves that the presence of REE and heavy metals in the lake sediment is associated with the type of geological formation.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2012, 450; 63--74
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The significance of subfossil Cladocera in stratigraphy of Late Glacial and Holocene
Autorzy:
Szeroczyńska, Krystyna
Powiązania:
https://bibliotekanauki.pl/articles/2027068.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
stratigraphy
“ecostratigraphy” – biostratigraphy
climate
lakes
lacustrine sediments
subfossil Cladocera
Opis:
This pa per pres ents dis cus sion on the re sults of sub fos sil Cla do cera analy ses from five lakes in Po land (Przedni Staw Lake, Per es pilno Lake, Gooeci¹¿ Lake, Imio³ki- fossil lake and Os trow ite Lake). The Cla do cera are rep re sented in sediments by re mains of plank tonic (Bos mini dae, Daph ni dae) and lit to ral (Chy do ri dae) forms. Cla do ceran as sem blage phases (“ecos tra tigra phy”) were de ter mined on the ba sis of changes in domi nance of in di ca tor spe cies and past ecologi cal con di tions were re con structed. The re sults are be ing dis cussed from the view point of cli mate change and anthro po genic ac tiv ity and their role in the lake evo lu tion. Moreo ver, an at tempt to use the cla do ceran phases for stra tigraphic di vi sion of the Late Gla cial and Holo cene was made. Dur ing the Bøl ling/Al lerød in ter sta dial, dis tin guished on the ba sis of pol len analy sis, Cla do cera in di cated short phase of bad con di tion (dry or cold?), proba bly as the Old Dryas cli mate re sults. The be gin ning of Holo cene is char ac ter ized, in moun tain and low land lakes, by high in -crease in the number of spe cies and speci mens of Cla do cera. This de scribed clear warm ing and marked the bound ary Late Gla cial/Holo cene. It was in di cated that the “ecos tra tigra phy” based on Cla do cera can be use ful for cli ma to stratigra phy, if cli mate was the ma jor fac tor con trol ling the de vel op ment of fresh wa ter lakes.
Źródło:
Studia Quaternaria; 2006, 23; 37-45
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evolution of the Late Neogene and Eopleistocene fluvial system in the foreland of the Sudetes Mountains, SW Poland
Autorzy:
Badura, J.
Przybylski, B.
Powiązania:
https://bibliotekanauki.pl/articles/973652.pdf
Data publikacji:
2004
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
fluvial sediments
Neogene
Eopleistocene
Lower Silesia
SW Poland
palaeogeography
Opis:
The oldest Cainozoic fluvial deposits in Lower Silesia date from the Oligocene. During the Middle and Late Miocene times, the fluvial system of this region was only slightly modified, especially in the foreland of the West and Middle Sudetes Mts. River lengths changed, following the migration of the North Sea shorelines. A rapid rebuilding of the fluvial system took place in the foreland of the East Sudetes Mts. either in the Late or Middle Miocene. Till that time, the main river valley of this region - the Nysa Kłodzka River, related to the Paczków and Kędzierzyn Grabens - used to flow towards the East, to a bay of the Paratethys sea. The new main river, pre-Odra, started to flow towards the North not before the Grodków Graben cut meridionally the Meta-Carpathian Swell. We are of the opinion that deposits of the Poznań Formation originated in an fluvial environment because no marine and/or limnic deposits have hitherto been discovered in the area of Lower Silesia above the uppermost of the Middle-Polish lignite seams (Henryk). The pre-Odra River drained the eastern part of Lower Silesia, and flowed towards the North, at least to the Poznań region. This main river captured such smaller rivers, as: the pre-Vistula, pre-Olza, pre-Ostravica, pre-Opava, pre-Nysa Kłodzka, and pre-Bystrzyca. Rivers draining the West Sudetes Mts. flowed first towards the North, to the region of the present-day Middle Odra River, and there turned to the West. It is conceivable that these rivers curved westwards just along the line of the present-day Wrocław - Magdeburg marginal stream valley ("Pradolina"). Since the Pliocene, the Sudetic rivers have started to transport coarser, sandy, and even gravelly material to a more distant foreland. Alluvial deposits of this phase occur exclusively on uplands. Coarse-grained sediments recognized in the bottom of deep erosional incisions were redeposited under subglacial conditions during the Mesopleistocene glaciations. The presented new interpretation of origin of the Poznań Formation basin and detailed recognition of Pliocene and Eopleistocene river system should initiate a new line of research into the Late Neogene and Eopleistocene sediments.
Źródło:
Annales Societatis Geologorum Poloniae; 2004, 74, No 1; 43-61
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Origin of fine-grained clastic sediments in caves of the Hoher Göll massif (the Northern Calcareous Alps, Austria)
Autorzy:
Kicińska, Ditta
Powiązania:
https://bibliotekanauki.pl/articles/2055866.pdf
Data publikacji:
2021
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
cave sediments
heavy minerals
Augenstein Formation
Northern Calcareous Alps
Opis:
The Hoher Göll Massif is situated 20 km south of Salzburg and belongs to the Northern Calcareous Alps (Austria). It is a ridge ca. 11 km long and 3 km wide with the highest summit Hoher Göll (2522 m a.s.l.), encircled by deeply incised valleys with bottoms ca. 2,000 m below it. Cave clastic deposits were studied in the Hochschartehöhlensystem, Dämchenhöhle and Hintere caves. The caves belong to the Giant Cave Level, with the exception of part of the Hochschartehöhlensystem, that is Der Sprechender Steine Cave, the highest parts of which belong to the Ruin Cave Level. The sources of the cave sediments have been identified from the composition of the heavy fractions. Preliminary studies of the Hoher Göll caves reveal that the cave fills were derived from the Oligocene to earliest Miocene Augenstein Formation, the deposits of the Palaeo-Inn River and the siliciclastic basal strata of the Northern Calcareous Alps. The clastic material deposited as the Augenstein Formation was transported from southern parts of the Eastern Alps and by the Palaeo-Inn river from their western part. According to heavy minerals, the sources of the clastic material were on the Palaeozoic terrains, the post-Palaeozoic sequence, and the Middle Austroalpine Unit. Later, during or after the mountain uplift, weathered materials from the Augenstein and Palaeo-Inn deposits were eroded and transported from the surface into caves by allogenic streams. Some of the sediments were likely to have been transported later to the Giant Cave Level from the southern part of the Northern Calcareous Alps.
Źródło:
Annales Societatis Geologorum Poloniae; 2021, 91, 4; 363--373
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena stanu osadów dennych wybranych jezior powiatu poznańskiego
Assessment of Bottom Sediments from Selected Lakes of Poznań Region
Autorzy:
Karwacka, A.
Niedzielski, P.
Staniszewski, R.
Powiązania:
https://bibliotekanauki.pl/articles/1818634.pdf
Data publikacji:
2015
Wydawca:
Politechnika Koszalińska. Wydawnictwo Uczelniane
Tematy:
jeziora
osady denne
biogeny
metale
lakes
sediments
biogenes
metals
Opis:
Lakes, which led to environmental receiver plants, are under ever-increasing pressure from human and are the best object of study to assess the impact of anthropogenic activities on the state of eutrophication. In this assessment beyond the biological and physico-chemical conditions of the lake ecosystem, an important role is played by the impact of bottom sediments in these waters, which only allow to fully determine the level of anthropogenic pressure on the body of water. It is in the bottom sediments are accumulated pollution of the lake. Under favorable conditions in sediments accumulated dirt can again be released into the depths, acting potential source of danger for the whole ecosystem. Therefore, the aim of the study was to determine the susceptibility of selected lakes Powiat Poznański degradation and to assess the quality of these reservoirs bottom sediments.
Źródło:
Rocznik Ochrona Środowiska; 2015, Tom 17, cz. 2; 1684-1698
1506-218X
Pojawia się w:
Rocznik Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Przyrodnicze wykorzystanie osadów dennych w świetle obowiązujących przepisów
Natural usage of bottom sediments on the base of existing law rules
Autorzy:
Ciesielczuk, T.
Kusza, G.
Karwaczyńska, U.
Powiązania:
https://bibliotekanauki.pl/articles/1819531.pdf
Data publikacji:
2011
Wydawca:
Politechnika Koszalińska. Wydawnictwo Uczelniane
Tematy:
osady denne
przepisy prawne
nawożenie
bottom sediments
legislation
fertilization
Opis:
Wyniki przeprowadzonych badań metali ciężkich pozwalają zakwalifikować trzy spośród pięciu badanych osadów dennych jako możliwe do przyrodniczego wykorzystania na glebach użytkowanych rolniczo lub glebach terenów przemysłowych. Osady z Kanału Wińskiego (OS I) oraz ze zbiornika śródpolnego (OS II) mogą być z powodzeniem stosowane do nawożenia organicznego gleb. Jednak dwa kolejne badane osady zawierają ponadnormatywne ilości metali (cynku, kadmu i ołowiu) co eliminuje je z zastosowania nawozowego. Jednak zawartość pestycydów eliminuje wszystkie badane osady (za wyjątkiem prób OS 0) z użycia do zabiegów nawożenia gleb uprawnych z uwagi na znaczne przekroczenia dopuszczalnych stężeń DDT i jego metabolitów oraz g-HCH, aldryny i endryny. Natomiast osady OS I i OS II mogą być stosowane na glebach terenów uprzemysłowionych. W związku z tym każda partia osadu dennego, nawet ze zbiorników narażonych na antropopresję w niewielkim stopniu, powinna być szczegółowo zbadana przed zastosowaniem nawozowym. Działanie takie umożliwia szczegółowe wskazanie terenu, na którym mogą być stosowane lub podjęcie decyzji o zaniechaniu wykorzystania takiego materiału. Podobnie postępuje się z pozostałością po fermentacji metanowej, która ma być wykorzystana jako nawóz. Aby poszerzyć możliwości wykorzystania osadów dennych do celów nawozowych konieczna byłaby zmiana przepisów poprzez włączenie osadów do grupy nawozów naturalnych, oraz opracowanie dopuszczalnych stężeń zanieczyszczeń organicznych oraz nieorganicznych.
This paper attempts to assess the quality of sediments derived from surface water, in order to assess their suitability for use as fertilizers or as material for ground reclamation procedures. Bottom sediments contain high amounts of organic matter and this base could be a potential source of easily accessible nutrients and organic matter, which could increase the water capacity of soil and moreover contribute to the stabilization of soil pH. The studied sediments came mostly from small water reservoirs (small lakes and canals) supplied by rainwater. Sample OS 0 (shown as "reference sample") was taken from small reservoir with small forest catchment area. Samples OS I - OS IV were exposed to the impact of: agriculture, rainwater coming from industrial areas, non-ferrous met-al smelter and rainwater from city recreational areas. All samples were taken by Eckman-Birge sediment sampler. In the studied samples basic parameters for general characterization (pH, organic matter content, hydration) were defined. The main investigated parameters include heavy metals and organochlorine pesticides content, both of which are required for the analysis according to the polish law, enactment 2002 No. 165 pos.1359. The studied bottom sediments, although originated from different reservoirs, were organic and all belong to gytia sediment type. High amounts of organic matter in all examined samples allowed the comparison of recorded concentrations of heavy metals and pesticides. One of the tested samples was different - sediment OS III. This sample was contaminated with petroleum compounds originating from the maneuver yard from industry plant. Obtained results indicates the high contents of heavy metal in samples exposed to industrial effluents and metal smelter. In this case, such deposits cannot be applied as fertilizers on agricultural soils. The content of pesticides in the studied sediments was high and all tested samples (except "reference? sample OS 0), showed supranormal quantities. On this basis, the test samples OS I - IV OS are not suitable for the use on natural soils used for agriculture, but the first two investigated sediments (OS I OS II) can be used on soils of industrialized areas. In the group of chlorinated pesticides, in tested samples high concentrations of DDT and g-HCH compounds were recorded. The use of sediments as fertilizers, materials for improving soil parameters, or for ground reclamation is increasing, due to decreasing amounts of good quality organic fertilizers (e.g. manure) and difficulty in saving utilization sediments from dredging water reservoirs. The reported results indicate the real possibility of using bottom sediments as organic fertilizers, especially when they came from small reservoirs or lakes with uncontaminated catchment areas.
Źródło:
Rocznik Ochrona Środowiska; 2011, Tom 13; 1327-1337
1506-218X
Pojawia się w:
Rocznik Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New evidences of Holocene tectonic and volcanic activity of the western part of Lake Sevan (Armenia)
Autorzy:
Avagyan, Ara
Sahakyan, Lilit
Meliksetian, Khachatur
Karakhanyan, Arkadi
Lavrushin, Vasily
Atalyan, Tatul
Hovakimyan, Hayk
Avagyan, Seda
Tozalakyan, Petros
Shalaeva, Evgenia
Chatainger, Christine
Sokolov, Sergey
Sahakov, Arkadi
Alaverdyan, Gagik
Powiązania:
https://bibliotekanauki.pl/articles/2059674.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
active fault
gas emission
lake sediments
palaeomagnetism
lake tsunami
Opis:
The purpose of this paper is to present new data on active geological processes in the Lake Sevan Basin and to show its multidisciplinary aspects. The investigations of its structures, recent lake sediments, and lake floor gas emission allow a better understanding of the history of geological development and the recent tectonic and volcanic activity of the basin. This paper summarizes underwater investigations of active geological features of Lake Sevan, undertaken for the first time in Armenia. More than 30 aligned underwater-source related gas emission points were discovered. The gas contains carbon dioxide of volcanic or volcanogenic-metamorphogenic origin and can be related to unloading of deep fluid systems. This allows defining the Noratus-Kanagegh Fault segment trace below the recent Lake Sevan floor sediments. The discovery of the subaqueous segment of active fault shows the presence of another natural hazard of lake tsunami related to possible future co-seismic rupture. The recent sediments of the northwestern Lake Sevan coastline are sandwiched between two blocky lava flows. The radiocarbon dating of bones of bovine mammals (with entire skull), found ~15 cm from the cover of the lake sediments, suggests that the upper blocky basaltic-andesite layer can be a result of eruption younger than ~3400 years BP. About 80 m of the Noratus sequence sediments have been sampled for palaeomagnetic study and the age of 3.1-2.3 Ma for the lower part (42 m) is obtained. The upper and post-Gelasian activity of the Noratus-Kanagegh Fault is proven by a cross-cutscoria layer of 2.30 ±0.15 Ma K/Ar age.
Źródło:
Geological Quarterly; 2020, 64, 2; 288--303
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A new Eemian Interglacial to Early Vistulian site at Łanięta, central Poland
Autorzy:
Balwierz, Z.
Roman, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059929.pdf
Data publikacji:
2002
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Central Poland
Eemian Interglacial
Early Vistulian
lake sediments
palynostratigraphy
Opis:
The Łanięta site with fossil lake deposits is situated just in front of the maximum extent of Vistulian Glaciation ice. Palynological analysis shows that lake accumulation lasted through the Eemian Interglacial and almost the whole Early Vistulian, the longest record of this time interval in this part of Poland. Two warm interstadial-rank oscillations (Brörup and Odderade) and two stadials have been distinguished during the Early Vistulian. The older of these is correlated with the Herning Stadial while younger one equates with the Rederstal Stadial of the German succession.
Źródło:
Geological Quarterly; 2002, 46, 2; 207-218
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Organic geochemical study of the Lower Miocene Kremna Basin, Serbia
Autorzy:
Perunović, T.
Stojanović, K.
Simić, V.
Kašanin-Grubin, M.
Šajnović, A.
Erić, V.
Schwarzbauer, J.
Vasić, N.
Jovančićević, B.
Brčeski, I.
Powiązania:
https://bibliotekanauki.pl/articles/191854.pdf
Data publikacji:
2014
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Kremna Basin
lacustrine sediments
organic matter
mineralogy
biomarkers
pyrolysis
Opis:
The Kremna Basin is located in southwest Serbia, in the Zlatibor area, which is part of the Internal Dinarides. This basin is noteworthy because of the type of bedrock drainage, which it represents. It was formed on ultrabasic rocks and volcanic materials that influenced the occurrence of organic matter (OM) in the basin fill. The objective of the study was to determine the organic geochemical characteristics of sediments from the central part of the Kremna Basin. The sediments studied belong to an intrabasinal facies, in which two sequences were distinguished. The lower sequence occurs at depths of 216–343 m, while the upper sequence is found from 13.5–216 m. At the start of basin development (265–343 m) sedimentation took place in shallow alkaline water, rich in Mg ions. Through time, a slight deepening of the basin occurred. This was followed by chemical deposition of carbonates (216–265 m). The most important change in the sedimentary environment occurred with the formation of sediments marking the transition between the sequences (at about 200 m). Sediments from the lower sequence are characterized by the dominance of dolomite and magnesite. There are indications of volcanic activity, i.e. tuff layers and the presence of searlesite. The upper sequence is characterized by the prevalence of calcite and dolomite. The amounts of MgO, Na2O and B are higher in the lower sequence, whereas the CaO content is higher in the upper sequence. The sediments contain different amounts of immature OM (late diagenesis). Biomarker analysis shows diverse precursors of the sedimentary OM: methanogenic archaea, photosynthetic green sulfur bacteria (Chlorobiaceae), bacterivorous ciliates, various bacteria, both photosynthetic and non-photosynthetic, the green unicellular microalga, Botryococcus braunii race A (exclusively in the upper sequence) and terrestrial plants. The lower sequence contains lower amount OM, composed primarily of kerogen II/III and III types, indicating a higher contribution of the allochtonous biomass of land plants from the lake catchment, particularly in the lower part. The sediments of the upper sequence are enriched in autochthonous aquatic OM, which comprises mostly kerogen I, I/II and II types. The transition from the lower sequence to the upper one is associated with a decrease in pristane to phytane ratio, gammacerane index and content of C28 steroids, absence or significantly lower amount of squalane, absence of C24 and C25 regular isoprenoids, 8-methyl-2-methyl-2-(4,8,12-trimethyltridecyl) chroman and C30 hop-17(21)-ene. Pyrolytic experiments showed that the sediments of the upper sequence, rich in aquatic OM, at a catagenetic stage could be a source of liquid hydrocarbons. The values of hopane, sterane and phenanthrene maturation parameters indicate that through pyrolysis at 400°C the samples investigated reached a value of vitrinite reflectance equivalent of approximately 0.70%. It was estimated that the sediments should be found at depths of 2300–2900 m in order to become active source rocks. The calculated minimum temperature, necessary for catagenetic hydrocarbon generation, is between 103 and 107°C.
Źródło:
Annales Societatis Geologorum Poloniae; 2014, 84, 3; 185-212
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structural and textural response to dynamics of fluvioglacial processes of the Rzymsko esker sediments, Central Poland
Autorzy:
Frydrych, M.
Powiązania:
https://bibliotekanauki.pl/articles/184781.pdf
Data publikacji:
2016
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
glacifluvial sediments
clast shape
esker
Central Poland
Warta Glaciation
Opis:
The study was conducted in the Rzymsko esker, in the Eastern part of the Turek Upland Plain, within the range of the Warta Glaciation (Saalian II). The form was accumulated in a tunnel valley, which was partially filled with esker sediments. Lithofacies analysis, extended by a detailed analysis of clasts, made it possible to identify a considerable variability of sedimentation conditions. At the initial stage, transport and accumulation of sediments took place in the conditions of high energy hydraulic flows or hyperconcentrated flows. The flow energy rose cyclically, which was recorded as sediments coarsening. Deposits of boulders as well as massive and cross-bedded gravels were identified, a record of catastrophic glacial floods. During the later stage of esker formation, sandy and gravelly sediments were accumulated in an open crevasse. The strong erosional force of subglacial water is confirmed by an extremely high content of local rocks in the gravelly fraction (30–87%) and its very good roundness. Zingg shape analysis (1935) revealed a clear predominance of oblate forms among local clasts and equant fennoscandian erratics. A dependency was also found between the processing method and petrographic characteristics.
Źródło:
Geology, Geophysics and Environment; 2016, 42, 4; 411-428
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Management of liquid wastes on floating docks in the aspect of its impact on the environment
Autorzy:
Marcinowski, P.
Biernacka, J.
Olesiejuk-Kowalska, M.
Powiązania:
https://bibliotekanauki.pl/articles/260382.pdf
Data publikacji:
2005
Wydawca:
Politechnika Gdańska. Wydział Inżynierii Mechanicznej i Okrętownictwa
Tematy:
dock
liquid wastes
bed sediments
environment investigations
GC-MS
Opis:
State of environment pollution in the area of operation of a floating dock was investigated. In the taken samples of liquid wastes, outboard water and bed sediments were determined values of their basic physical and chemical parameters as well as concentration of poly-cyclic aromatic hydrocarbons, butyl tin compounds ((Bt)3 SnCl, (Bt)2 SnCl2 , BtSnCl3 , (Bt)4 Sn), polychlorinated biphenyls (PCB 28, PCB 52, PCB 101, PCB 138, PCB 153, PCB 180) as well as heavy metals (Zn, Cd, Pb, Cu, Ni, Cr, Co, Fe, Mn, As, Hg).
Źródło:
Polish Maritime Research; 2005, S 1; 15-19
1233-2585
Pojawia się w:
Polish Maritime Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Uranium isotopes in waters and bottom sediments of rivers and lakes in Poland
Autorzy:
Pietrzak-Flis, Z.
Kamińska, I.
Chrzanowski, E.
Powiązania:
https://bibliotekanauki.pl/articles/147251.pdf
Data publikacji:
2004
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
activity concentrations
238U
234U
water
bottom sediments
Opis:
Activity concentrations of 238U, 234U and 235U were determined in waters and bottom sediments in two main rivers in Poland (the Vistula and Odra rivers) with their tributaries, in four coastal rivers and in six lakes. Concentrations of 238U and 234U were compared with the concentrations of 226Ra determined in another study. As compared with concentrations in coastal rivers and in lakes, enhanced concentrations of the radionuclides were observed in water and bottom sediments in the upper and middle courses of the Vistula river, whereas in the Odra river the enhanced concentrations were present only in the bottom sediments. The enhanced concentrations in the Vistula river result from the discharge of coal mine waters from the Upper Silesian Coal Basin, and they indicate that the discharge was continued. The enhanced concentrations in the Odra river observed only in bottom sediments indicate that the discharge occurred in the past. The 234U/238U ratio for the bottom sediments was close to unity, indicating that these isotopes were close to equilibrium, whereas for water the average ratio was from 1.2 for lakes to 1.5 for the Vistula river, demonstrating the lack of equilibrium.
Źródło:
Nukleonika; 2004, 49, 2; 69-76
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Plant macrofossils from the Czyżów Complex deposits of the Szczerców outcrop, central Poland
Autorzy:
Myśkow, E.
Krzyszkowski, D.
Wachecka-Kotkowska, L.
Wieczorek, D.
Powiązania:
https://bibliotekanauki.pl/articles/184237.pdf
Data publikacji:
2016
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
fluvial sediments
plant macrofossils
Holsteinian
Czyżów Complex
Central Poland
Opis:
The paper presents the results of research into the plant macrofossils found in the tectonic Kleszczów Graben, within Mesopleistocene sandy sediments. A number of samples were collected at eight locations from river sediments containing variously sized fragments of plants, mostly from greenish sands overlying Neogene sediments. The structural characteristics of the sediments show a cyclic record of the formation of point bars, their washing out at supercritical conditions, and their aggradation by fine-grained material during flow waning. Based on lithological and structural studies, it has been demonstrated that the sands accumulated in an environment of a meandering river, whose valley bottom was covered with fairly dense vegetation, inhibiting the influx of mineral material to the floodplain from the surroundings – the valley or glacial plateau slopes. The aim of further analysis was to identify the plant genera of the individual macrofossils (about 40 specimens). The most numerous macrofossils were observed in the middle layers of the profile, within sandy megaripple structures, where mostly fragments of Fraxinus and Acer wood were present. In other layers, several fragments of Pinus and three pieces of Populus wood were identified. Additionally, young stems of dicotyledonous plants and fragments of rhytidome (the outer bark of a tree) were found. The results are discussed in combination with considerations on the deposition of the Czyżów Complex in the Bełchatów outcrop, and on the occurrence of local flora.
Źródło:
Geology, Geophysics and Environment; 2016, 42, 3; 325-336
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość metali ciężkich w osadach dennych cieku o zlewni rolniczej na przykładzie rzeki Gowienica
The content of heavy metals in bottom sediments of the watercourse in agricultural catchment on the example of the river Gowienica
Autorzy:
Szydłowski, K.
Rawicki, K.
Burczyk, P.
Powiązania:
https://bibliotekanauki.pl/articles/401120.pdf
Data publikacji:
2017
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
osady denne
metale ciężkie
Gowienica
bottom sediments
heavy metals
Opis:
Analizie chemicznej poddano próbki osadów dennych pochodzących z rzeki Gowienica. Próbki pobierano w latach 2014 i 2015 w wybranych punktach badawczych, które wyznaczono w zależności od sposobu zagospodarowania i użytkowania terenów przyległych. W pozyskanym materiale oznaczono zawartość całkowitą metali ciężkich tj.: Cd, Co, Cr, Ni, Pb oraz Hg. Na podstawie uzyskanych wyników analiz chemicznych wykazano podwyższone stężenia ołowiu, niklu, chromu oraz rtęci, które przekraczały wartości progowe, powyżej których obserwuje się szkodliwe oddziaływanie zanieczyszczeń (TEL). Nie stwierdzono natomiast ponadnormatywnych stężeń tych zanieczyszczeń dla wyznaczonej wartości granicznej (PEL) powyżej której obserwuje się szkodliwe oddziaływanie zanieczyszczeń na organizmy. Przeprowadzone analizy chemiczne wykazały jednak przekroczenia wartości naturalnej kobaltu (tło geochemiczne 2,0 mg⋅kg-1) dla osadów wodnych Polski w poszczególnych punktach badawczych. Przyczyną tych przekroczeń w pobranych osadach dennych były najprawdopodobniej spływy powierzchniowe z pól i łąk w formie nawozów i środków ochrony roślin oraz dopływ ścieków bytowych.
The samples of bottom sediments for chemical analysis were collected from Gowienica river and its tributaries. The samples were collected in 2014 and 2015 from the established sampling points on differently managed and utilized adjacent areas. Total content of heavy metals, i.e.: Cd, Co, Cr, Ni, Pb and Hg were measured in the collected material. The results indicate that the concentrations of lead, nickel, chromium and mercury exceeded the level indicating the harmful impact of pollution (TEL) , but none of the analyzed heavy metals exceeded the limit (PEL) above which harmful effects of pollution on organisms can be observed. However, according to another classification (LAW), the analyzed sediments were between two classes (unpolluted deposits – Class I), and unpolluted / moderately polluted deposits (class I-II). Nevertheless, a chemical analysis showed that the natural cobalt concentration (geochemical background; 2.0 mg⋅kg-1) for aquatic sediments in Poland was exceeded. The reasonfor the exceed cobalt concentration in natural sediments was, most probably, the surface runoffs from fields and meadows in the form of fertilizers, plant protection products and the domestic waste water.
Źródło:
Inżynieria Ekologiczna; 2017, 18, 4; 218-224
2081-139X
2392-0629
Pojawia się w:
Inżynieria Ekologiczna
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena toksyczności osadów w Zbiorniku Włocławskim
Assessment of sediment toxicity from the Włocławski Reservoir
Autorzy:
Trojanowska-Olichwer, A.
Powiązania:
https://bibliotekanauki.pl/articles/271448.pdf
Data publikacji:
2013
Wydawca:
Górnośląska Wyższa Szkoła Pedagogiczna im. Kardynała Augusta Hlonda
Tematy:
toksyczność
Phytotoxkit
osady
zbiornik zaporowy
toxicity
sediments
dammed reservoir
Opis:
Celem pracy była ocena ekotoksyczności osadów ze Zbiornika Włocławskiego, drugiego pod względem wielkości polskiego zbiornika zaporowego. Badania przeprowadzono przy użyciu mikrobiotestów Phytotoxkit, w których analizuje się hamowanie kiełkowania nasion i hamowanie wzrostu korzeni trzech gatunków roślin (duliściennych Lepidium sativum, Sinapis alba, monoliściennych: Sorgum saccharatum). Wrażliwość badanych roślin obniżała się zgodnie z następującym schematem: L. sativum < S. alba, < S. saccharatum. Uzyskane wyniki wykazały silne zróżnicowanie przestrzenne fitotoksyczności wzdłuż zbiornika (r=0,71, p<0,05), przy czym najwyższe wartości obserwowano tuż poniżej miasta Płocka (hamowanie kiełkowania nasion = -47% oraz hamowanie wzrostu korzeni = 79%); wartości te stopniowo obniżały się w kierunku tamy (hamowanie kiełkowania nasion = -81% oraz hamowanie wzrostu korzeni = 22%). Wpływ metali na toksyczność osadów nie był jednoznaczny. W pracy podjęto dyskusję na temat innych możliwych przyczyn toksyczności osadów w rejonie miasta Płocka.
The aim of this study was to estimate the ecotoxicity of sediments from the Włocławski Resevoir, Poland's second largest dammed reservoir. Research was carried out using Phytotoxkit microbiotests, which measured the inhibition of seed germination and root growth retardation of three plant species (dicotyl Lepidium sativum, Sinapis alba, monocotyl Sorgum saccharatum). The sensitivity of the plants tested decreased according to the following gradient: L. sativum < S. alba, < S. saccharatum. The results obtained showed strong spatial diversification of phytotoxicity along the reservoir ((r=071, p<005)), with the highest values just below the city of Płock (inhibition of seed germination = -47%, and inhibition of root growth = 79%), and gradual decreasing diversification towards the dam (inhibition of seed germination = -81% and inhibition of root growth = 22%). The effect of the metals on sediment toxicity was not clear. Other possible causes of sediment toxicity in the region of Płock are discussed.
Źródło:
Journal of Ecology and Health; 2013, R. 17, nr 3, 3; 103-109
2082-2634
Pojawia się w:
Journal of Ecology and Health
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Quantification of Heavy Metals in the Sediment ecosystem of Ulhas River flowing along Dombivli City of Mumbai
Autorzy:
Jadhav, Amol M.
Singare, Pravin U.
Powiązania:
https://bibliotekanauki.pl/articles/1194028.pdf
Data publikacji:
2015
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Dombivli
Mumbai
Ulhas River
heavy metals
industrial pollution
sediments
Opis:
The Dombivli city near Mumbai has rapid industrialized. However the improper environmental planning has resulted in discharge of industrial waste effluents from the industrial belt into the Ulhas River. These wastes from these industries include various toxic heavy metals which subsequently accumulate in the sediments of Ulhas River. This day by day increasing tremendous pollution load has provoked us to carry the systematic and detailed study of heavy metal content in the sediment samples collected along the Ulhas River along the Dombivli City, near Mumbai. The study was conducted in year 2012 and 2013. The study was carried out in along the banks of Ulhas River near the discharge of effluents from Dombivli Industrial belt Phase I and Phase II. Accordingly the sampling points were identified. The analysis for the majority of the toxic heavy metals like Cadmium (Cd), Copper (Cu), Nickel (Ni), Chromium (Cr), Cobalt (Co), Iron (Fe), Lead (Pb), Mercury (Hg), Arsenic (As) and Zinc (Zn), in sediment samples was done. From the results of our study, it can be concluded that there is a need of systematic and regular monitoring of pollution level along the Ulhas River so as to generate the data on accumulation of heavy metals in the river sediments which will further help in improving the industrial waste treatment technology adopted along the Dombivali industrial belt. It is expected that such scientific studies will help to gauge the extent of pollution in order to avoid long term irreparable damage to the ecosystem.
Źródło:
World Scientific News; 2015, 10; 1-16
2392-2192
Pojawia się w:
World Scientific News
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Quaternary valley levels and river terraces in the western part of the Holy Cross Mountains
Autorzy:
Dzierżek, Jan
Lindner, Leszek
Cabalski, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/2025214.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Holy Cross Mountains
Quaternary
palaeogeography
valley sediments
fluvial forms
Opis:
According to the current state of research five sand-gravel accumulation levels of Quaternary age are visible in the morphology of the western part of the Holy Cross Mountains, within the Wierna Rzeka, Hutka and Bobrza river valley systems and the lower stretches of the Biała Nida and Czarna Nida river valleys. Two upper levels (V and IV) correspond to valleys formed during the Odranian Glaciation-Saalian, MIS6 and its reccesional phases under the influence of proglacial and extraglacial waters beyond the extent (to the east) of the maximal ice-sheet limit of this glaciation, reaching to the present-day Leśnica-Gnieździska-Łopuszno line. Two lower levels (III and II) are terraces that were typically formed during the climatic conditions thatprevailed during Vistulian stadials. Sands and gravels of the three upper levels (V−III) contain numerous debris flow deposits and cryoturbation structures documenting periglacial conditions during their accumulation. The lowermost level (I) is a typical Holocene floodplain.
Źródło:
Studia Quaternaria; 2019, 36; 109-118
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Marine Environment Around Iceland: Hydrography, Sediments and First Predictive Models of Icelandic Deep-sea Sediment Characteristics
Autorzy:
Ostmann, Alexandra
Schnurr, Sarah
Arbizu, Pedro Martínez
Powiązania:
https://bibliotekanauki.pl/articles/2051158.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Icelandic waters
MARS and randomForest models
sediments
IceAGE project
Źródło:
Polish Polar Research; 2014, 2; 151-176
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ageing of organic matter in incubated freshwater sediments; in fer ences from C and H isotope ratios of methane
Autorzy:
Szynkiewicz, A.
Modelska, A.
Jedrysek, M-O.
Kurasiewicz, M.
Mastalerz, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059090.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
methanogenic pathways
carbon and hydrogen isotopes
incubation
freshwater sediments
Opis:
The freshwater sediments were incubated under anaerobic conditions for 570 and 879 days to in vestigate the potential variations in methanogenic pathways due to increasing sediment age and recalcitrance of organic matter. The methanogenic pathways did not shift from acetate fermentation toward CO2 reduction, as indicated by the observed variations of the isotopic composition of methane in natural conditions. It appeared, however, that the observed decrease of methane concentration (from 86 to 39%) and continuous in crease in d13C(CH4) (from –69.7 to –59.0‰) and dD(CH4) values (from –381 to –320‰) resulted mainly from exhaustion of at least one methanogenic substratein the incubated sediments. To better understand processes controlling the variations of delta exp.13C(CH4) and deltaD(CH4) values relative to ageing of organic matter, the method of principal component analysis (PCA) was used. This method offers good comparison of the relation ships between variables when a larger number of parameters control a given process in the same time period. In this study, the PCA indicated three distinctive factors that controlled decomposition of organic matter during the incubation. Factor 1 explained 33% of observed variations among the variables and had positive (0.93–0.92) loadings for electric conductivity and DIC concentration and negative loading for delta exp.13C(CH4) val ues (–0.72). Factor 2 accounted for 28% and had high posi ive loading for deltaD(CH4) value (0.86) and high negative loading for methane concentration (–0.81). Factor 3 accounted for 19% and exhibited high positive loadings for temperature (0.90) and delta exp.13C(DIC) value (0.69). Factors 1 and 2 were directly linked to the methanogenesis and indicated that bigger accumulation of bio-products in sediments is likely important for variations of delta exp.3C and deltaD of methane. This study shows that method of principal component analysis might be a useful tool while studying biogeochemical carboncy cleduring early digenesis of freshwater sediments.
Źródło:
Geological Quarterly; 2008, 52, 4; 383-383
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New approach to garnet redistribution during aeolian transport
Autorzy:
Lisá, L.
Buriánek, D.
Uher, P.
Powiązania:
https://bibliotekanauki.pl/articles/2059212.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Weichselian
Pleistocene
Czech Republic
aeolian sediments
garnet composition
provenance
Opis:
Garnet composition within Late Pleistocene (Weichselian) loess and loess-like deposits was studied in 13 samples of sediment heavy mineral fractions from Moravia and Silesia (Czech Republic). Four areas differing in garnet chemistry were identified, and some regional trends in garnet composition changes were documented. The data obtained support the generally accepted conclu ion of prevailing westerly winds during Weichselian loess deposition. Metamorphic rocks of the Bohemian Massif together with contributions fromig neous (mainly granitic) and sedimentary rocks were indicated as a source for the Weichselian loess and loess-like deposits studied. Local differences in garnet composition depend on the basement source rocks, on prevailing wind direction, on regional geomorphology and on transport distance.
Źródło:
Geological Quarterly; 2009, 53, 3; 333-340
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Dobrotiv Formation (Miocene) in the Boryslav-Pokuttya and Sambir nappes of the Ukrainian Carpathians : a record of sedimentary environmental change in the development of the Carpathian Foredeep Basin
Autorzy:
Oszczypko, N.
Uchman, A.
Bubniak, I.
Powiązania:
https://bibliotekanauki.pl/articles/2060063.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
non-marine
deltaic sediments
molasse
mammal and bird footprints
Opis:
The late Early Miocene Dobrotiv Formation, a 700–800-m-thick unit, was deposited in a subsiding platform margin, which become involved in the marginal part of the Outer Eastern Carpathian accretionary wedge. The sedimentary succession from the Sloboda Conglomerate up to the Dobrotiv Formation records a transition from alluvial fan through fan-delta to deltaic deposits, followed by the fluvial plain-channel facies of the Stebnyk Formation. The deltaic deposits are mud-dominated, with poorly developed thickening-up packets of beds. Efficient sediment accumulation was balanced by subsidence caused by subsurface loading. Emerged parts of the deltaic sedimentary system include tetrapod footprints and raindrop imprints. The general absence of mudcracks in the Dobrotiv Formation suggests a humid climate. Deposits of the Sloboda, Dobrotiv and Stebnyk formations form fining- and thinning-upwards clastic wedge successions along the Ukrainian Carpathians.
Źródło:
Geological Quarterly; 2014, 58, 3; 393--408
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Characteristics of the macro - and microelements in benthic sediments of selected mid-field ponds
Autorzy:
Brysiewicz, A.
Ligocka, K.
Powiązania:
https://bibliotekanauki.pl/articles/101069.pdf
Data publikacji:
2018
Wydawca:
Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
Tematy:
benthic sediments
mid-field ponds
macroelements
microelements
chemical composition
Opis:
The agricultural landscape of Western Pomerania is characterised by frequent occurrence of small, post-glacial water ponds commonly called mid-field ponds. They serve numerous important functions, both with regard to agriculture and ecology. Due to their specific location in the agricultural landscape, they are exposed to permanent and strong anthropic pressure, which often translates into pollution of surface water and benthic sediments with macro-and microelements. This study attempts to assess and determine the level of macro – and microelements in benthic sediments, depending on the type of agricultural production, on the example of selected mid-field ponds. The assessed benthic sediments of both ponds were characterised by varied macro - and microelement levels, depending on the collection site and the depth of their deposition. Based on the performed chemical analyses it was found that both observation points in the pond Żelisławiec were characterised by the highest concentrations occurring in the top layer (0-5 cm), which is related to the fact that there are areas of agriculture in the pond basin with the use of mineral and organic fertilisation and occurrence of higher water erosion. And the other assessed mid-field pond (Stare Czarnowo) showed the highest concentration of microelements in the middle layer, 5-15 cm. Statistical analyses revealed that statistically significant differences were observed only for potassium levels, depending on the type of agricultural production in the basin of both assessed ponds. This may result from various types of agricultural crops (Brassica napus L. var. napus and ×Triticosecale Wittm. ex A.Camus) and intense fertilization of arable land in Stare Czarnowo. Statistically significant differences in particular layers of sediment confirm that depending on the type of agricultural activity, mid-field ponds are supplied with various mineral matter at different times, resulting in its accumulation in benthic sediments.
Źródło:
Infrastruktura i Ekologia Terenów Wiejskich; 2018, IV/1; 939-950
1732-5587
Pojawia się w:
Infrastruktura i Ekologia Terenów Wiejskich
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Bottom Sediments as an Element of the Krąpiel River Ecosystem
Autorzy:
Raczyńska, M.
Machula, S.
Łukaszewicz, P.
Raczyński, M.
Powiązania:
https://bibliotekanauki.pl/articles/125464.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
bottom sediments
Krapiel river
breeding of salmonids
bottom fauna
Opis:
Research on the structure of sediments was carried out in 2015 in the river Krąpiel and its tributaries. The main objectives of this study were to classify the types of sediments with grain size analyzing according three different criteria, as well as influence of the substrate on the abundance and diversity of macrobenthic organisms, and to determine the quality of the ground for natural breeding of salmonids. It was found that according to Polish standards, bottom sediments of the Krąpiel river and its tributaries belong to the coarse – gravel type or sandy – gravel type, whereas according to the method used in Anglo-Saxon countries – these are sandy sediments. It was also shown that the grain size of bottom sediments of the Krąpiel river and its tributaries determine friendly living environment for macroinvertebrates and for breeding salmonids.
Źródło:
Journal of Ecological Engineering; 2016, 17, 2; 121-127
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł

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