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Tytuł:
Water management problems at the Bukówka drinking water reservoir’s cross-border basin area in terms of its established functions
Autorzy:
Wiatkowski, M.
Rosik-Dulewska, C.
Powiązania:
https://bibliotekanauki.pl/articles/124624.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
drinking water reservoir
water management
cross-border basin area
water quality
Opis:
The paper covers the analysis of water management problems in the cross-border reservoir basin of Bukówka, located at the Bóbr river, at 271+540 km of its course, below the Czech-Polish border, in Dolnośląskie Voivodeship. The problems of water management in the context of the reservoir’s functions have been analyzed; these are: flood control, the provision of water during low water level periods for the Water Treatment Plant in Marciszów, the provision of drinking water for the city of Wałbrzych as well as the provision of proper flow in the Bóbr river bed downstream from the reservoir. Due to its localization right below the border with the Czech Republic, the reservoir is exposed to a number of problems. The study has found that the main problems of water management in the basin area included unsatisfactory state of water and wastewater management in the basin, unsatisfactory state of the surface water quality in the basin area of the reservoir, poor condition of streams and drainage ditches, improper arrangement of arable lands and large downslopes and a lack of monitoring stations on tributaries of the reservoir. It has been found that the hydrochemical conditions in the Bukówka reservoir’s section are unfavorable for it. From the eutrophication point of view, the water flowing into the tank is characterized by a large content of nutrients, especially nitrates, phosphates and BOD5. In order to counteract eutrophication it is necessary to lower the concentration of nutrients in the water flowing into the tank. One of the basic ways to do so is to restore the water and wastewater management in the reservoir’s basin. Studies in the Bukówka reservoir provide important information concerning the state of the purity of the water supplying the reservoir. In order to obtain accurate information on the state of purity, a monitoring of hydrological and water quality should be continued. The studies are a part of the strategy of protection of the quality of transboundary waters, proposed in the Convention on the Protection and Use of Transboundary Watercourses and International Lakes of 1992.
Źródło:
Journal of Ecological Engineering; 2015, 16, 2; 52-60
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Statistical Analysis of Parameters of Selected Worldwide Yacht Ports and Marinas in Terms of Design Guidelines
Autorzy:
Gucma, L.
Drwięga, K.
Butrymowicz, R.
Powiązania:
https://bibliotekanauki.pl/articles/320548.pdf
Data publikacji:
2018
Wydawca:
Polskie Forum Nawigacyjne
Tematy:
statistical analysis
design guidelines
port parameters
yacht port
marina
turning basin area
Opis:
In relation to the current development of the sailing, modernization and development of yacht ports and marinas are necessary. The preparations process, stages of the design, analyses and finally construction of yacht ports is time-consuming and laborious. In the article a statistical analysis of selected design parameters was described. In order to carry out the analysis a database was created based on 210 ports from different regions of the world such as: Europe, North America, Australia and South Asia. Google Earth was used to obtain the actual values of the analyzed parameters. Most of achieved results was described in the form of tables or graphs.
W związku z bieżącym rozwojem żeglarstwa, konieczna jest modernizacja oraz rozwój portów jachtowych i marin jachtowych. Proces przygotowania, etapy projektowania, analizy i wreszcie budowa portów jachtowych jest czasochłonna oraz pracochłonna. W artykule opisano statystyczną analizę wybranych parametrów projektowych. W celu przeprowadzenia analizy stworzono bazę danych opartą na 210 portach z różnych regionów świata, np: Europa, Ameryka Północna, Australia i Azja Południowa. Do uzyskania rzeczywistych wartości analizowanych parametrów wykorzystano Google Earth. Większość uzyskanych wyników została opisana w formie tabel lub wykresów.
Źródło:
Annual of Navigation; 2018, 25; 205-217
1640-8632
Pojawia się w:
Annual of Navigation
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Narzędzia planistyczne w gospodarowaniu wodami służące osiąganiu dobrego stanu wód w regionie wodnym Warty
Llanning tools in water management useful in achieving a good status of water system in the area of the Warta river
Autorzy:
Misiewicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/407522.pdf
Data publikacji:
2014
Wydawca:
Instytut Badawczo-Rozwojowy Inżynierii Lądowej i Wodnej Euroexbud
Tematy:
gospodarka wodna
jednolite części wód powierzchniowych
korzystanie z wód
obszar dorzecza
obszary chronione
region wodny
water management
unitary elements of surface waters
using waters
basin area
protected areas
water area
Opis:
Artykuł ma na celu przybliżenie relacji oraz zakresu rzeczowego podstawowych dokumentów planistycznych w gospodarowaniu wodami, których wdrażanie służy osiągnięciu lub wspomaga osiągnięcie dobrego stanu/potencjału jednolitych części wód – podstawowych jednostek hydrograficznych wskazanych w Ramowej Dyrektywie Wodnej w oparciu, o które realizowane są poszczególne elementy procesu planowania tj. ocena stanu wód, wskazanie celów środowiskowych, wskazanie działań niezbędnych do osiągniecia tych celów, czy też ocena ryzyka nieosiągnięcia celów. Przedstawienie zakresu, hierarchii oraz relacji pomiędzy dokumentami planistycznymi tj. plan gospodarowania wodami na obszarze dorzecza, warunki korzystania z wód regionu wodnego oraz zlewni ułatwi zrozumienie złożoności procesu planowania w gospodarowaniu wodami oraz zwróci uwagę na konieczność uwzględniania zapisów ww. dokumentów w ramach procedur prowadzonych m.in. w celu wydania pozwoleń wodnoprawnych.
The article aims at presenting the relations and the subject area range of basic planning documents in water management, the implementation of which helps to achieve or supports the achievement of a good status/potential of unitary elements of water system – basic hydrographic units identified in Water Framework Directive. They serve as the basis for implementing particular elements of the planning process, i.e. assessing the water status, identifying the environmental aims, identifying the actions necessary to achieve these aims, or evaluating the risk of not achieving the aims. The presentation of the range, hierarchy and the relations between the planning documents, that is the water management plan in the river basin and the conditions of water use in the water area and the basin, will make it easier to understand the complexity of the planning process in reference to water management. It will also draw attention to the necessity of taking into consideration the above-mentioned docu-ments in the procedures carried out (inter alia) to issue legal permissions regarding waters.
Źródło:
Zeszyty Naukowe. Inżynieria Lądowa i Wodna w Kształtowaniu Środowiska; 2014, 11; 7-17
2082-6702
Pojawia się w:
Zeszyty Naukowe. Inżynieria Lądowa i Wodna w Kształtowaniu Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wykorzystanie doświadczeń międzynarodowych dla potrzeb rekultywacji i zagospodarowania zwałowisk odpadów pogórniczych
Use of International Experiences or the Needs of Reclamation and Management of Post Mining Waste Dumps
Autorzy:
Gawor, Łukasz
Warcholik, Witold
Dolnicki, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/439319.pdf
Data publikacji:
2016
Wydawca:
Uniwersytet Pedagogiczny im. Komisji Edukacji Narodowej w Krakowie
Tematy:
Górnośląskie Zagłębie Węglowe (GZW)
odpady pogórnicze
procesy rekultywacyjne
zwałowiska po górnictwie węglowym
dumping grounds after coal mining
mining wastes
reclamation processes
Upper Silesian Coal
Basin area (USCB)
Opis:
Odpady pogórnicze, składowane na zwałowiskach (hałdach) są elementem krajobrazu każdegozagłębia górniczego. Zwałowiska pogórnicze, zarówno podpoziomowe, jak i nadpoziomowe, wymagająefektywnej rekultywacji technicznej i biologicznej oraz racjonalnego zagospodarowania, m.in. w kierunkuparkowo-rekreacyjnym, dydaktycznym i sportowym. Efektywność rekultywacji omawianych obiektów ściślewiąże się z ich negatywnym oddziaływaniem na środowisko, a w szczególności z zagrożeniami samozapłonemi pożarami. Te zagadnienia łączą się również z odzyskiem surowców z odpadów i dotyczą głównie materiiwęglowej. Opisywane obiekty stanowią bowiem bardzo często perspektywiczne antropogeniczne złożawtórne. Procesy odzysku są uzasadnione ekonomicznie, a ich przebieg regulują odpowiednie akty prawne.W artykule przedstawiono doświadczenia z wybranych europejskich zagłębi górniczych (Wielka Brytania– rejon Cardiff, Belgia, Niemcy – Zagłębie Ruhry, Czechy) w zakresie rekultywacji i zagospodarowania zwałowiskpogórniczych. Zaprezentowano kierunki zagospodarowania, możliwe do wykorzystania na zwałowiskachzlokalizowanych na terenie Polski, na przykładzie obszaru Górnośląskiego Zagłębia Węglowego (GZW).
Mining wastes disposed on dumping grounds (tips) are parts of the landscape of every mining basin. Post mining waste dumps require efficient technical and biological reclamation and rational management. Efficiency of reclamation of examined objects is inseparable connected with their negative environmental impacts, particularly self-ignition and fire hazards. These problems are also connected with recovery of secondary resources, mainly coal particles. Described objects belong though to the perspective anthropogenic secondary deposits. Processes of recovery are economically justified and their course is controlled by legal regulations. In the paper there are presented experiences from chosen European mining basins (UK, Belgium, Germany, Czech Republic) in range of reclamation and management of post mining dumping grounds, There are proposed direction of management, which could be used on coal mining waste dumps in Poland, exemplified on the Upper Silesian Coal Basin area (USCB).
Źródło:
Prace Komisji Geografii Przemysłu Polskiego Towarzystwa Geograficznego; 2016, 30, 3; 228-238
2080-1653
Pojawia się w:
Prace Komisji Geografii Przemysłu Polskiego Towarzystwa Geograficznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Water balances in the smaller drainage areas of the Tywa River basin (1961-1990)
Bilanse wodne zlewni cząstkowych dorzecza rzeki Tywa (1961-1990)
Autorzy:
Jezierski, G.
Zygas, M.
Zajner, Z.
Zych, N.
Powiązania:
https://bibliotekanauki.pl/articles/84817.pdf
Data publikacji:
1999
Wydawca:
Akademia Pomorska w Słupsku
Tematy:
water balance
smaller drainage area
Tywa River
river basin
drainage
hydrology
Źródło:
Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 1999, 03
1643-0115
Pojawia się w:
Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assessment of Application Conditions of Infiltration Basins for Regulation of Urban Rainwater Drainage
Autorzy:
Tkachuk, Olexander
Yaruta, Yana
Shevchuk, Olha
Powiązania:
https://bibliotekanauki.pl/articles/2027819.pdf
Data publikacji:
2022
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
water drainage
infiltration basin
surface drainage
urban area
surface runoff quality
Opis:
Regulation of surface runoff in urban areas with temporary delay by infiltration basins of rainwater in the places of their precipitation and with gradual drainage through the existing reservoirs of small diameters is the most appropriate under the conditions of intensive building development, wear and imperfection of surface drainage systems, especially combined sewerage. Evaluation of application conditions and basic parameters of infiltration basins in surface drainage regulation was carried out on the basis of own experimental studies of infiltration basin fragment with upper typical vegetation layer, numerical computer modeling of surface runoff formation in urban areas, its regulation using infiltration basins and analysis of previous studies. Its water absorption, filtration and clearing indicators were defined on the basis of experimental studies. The self-regenerative restoring function of a vegetative layer, working conditions under the flooded and not flooded conditions were established and defined. According to the amount of suspended solids, BOD, oxidation, pH and dissolved oxygen, the quality of rain runoff when filtering water through the upper vegetation layers of infiltration basins decreases to the normative values.
Źródło:
Journal of Ecological Engineering; 2022, 23, 2; 191-195
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Elsterian ice sheet dynamics in a topographically varied area (southern part of the Racibórz–Oświęcim Basin and its vicinity, southern Poland)
Autorzy:
Salamon, T.
Powiązania:
https://bibliotekanauki.pl/articles/2060370.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ice sheet dynamic
fore-mountain area
subglacial till
Elsterian Glaciation
Ostrava Basin
Opis:
During the Elsterian Glaciation, the Scandinavian Ice Sheet, before reaching its maximum extent, advanced over the mountainous foreland of Southern Poland, which was characterized by a substrate of increasingly varied relief. One such area was the hilly Rybnik Plateau of the southern part of the Racibórz–Oświęcim Basin, located directly north of the Ostrava Basin and Moravian Gate, where the ice sheet advanced far south and formed a large lobe. In this study, till from the Łaziska site, located in southern part of the Rybnik Plateau, was analysed and interpreted. The till was deposited at the top of an W–E oriented ridge composed of Neogene clays. The study indicates that a high basal water pressure occurred at the base of the ice sheet, favouring a basal mechanism of ice sheet movement. Till fabric and kinematic structures indicate that ice flowed easily from the west over the ridge, parallel to its axis. Reconstructed patterns of ice flow direction reflect an ice sheet that was characterized by a strong spatially varied dynamics. The Odra Valley was the main corridor of fast flowing ice to the Ostrava Basin, from where ice was distributed radially in different directions. The second corridor of actively flowing ice was probably located in the Ruda palaeovalley to the north of the Rybnik Plateau. In the central part of the Rybnik Plateau, ice flow was restricted. This less dynamic ice sheet behaviour resulted mostly from the much higher location of the area. This study indicates that the large morphological and lithological variations of the ice sheet substrate induced varied frictional resistance, producing a spatially varied stress field within the ice sheet. This generated active zones of streaming ice adjacent to more passive zones. Potential switching between neighbouring active zones transporting ice towards the ice sheet margin is postulated.
Źródło:
Geological Quarterly; 2017, 61, 2; 465--479
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The thermal waters of Podhale, southern Poland: history of research, genesis and utility
Autorzy:
Małecka, D.
Powiązania:
https://bibliotekanauki.pl/articles/2059181.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
thermal waters
artesian basin
recharge area
age of water
geothermal energy
Tatra Mts.
Opis:
This paper outlines hypotheses relating the dip of Tatra strata beneath the Podhale Flysch to deep groundwater flow through the systems of fissures and karst caverns. Attempts by J. Gołąb and S. Sokołowski to constrain hypotheses through a series of exploratory-exploitational drillings led to the discovery in 1963 of thermal artesian waters in the Tatra foreland. These are of meteoric origin with total dissolved solids from 0.2 g/dm3 in the Tatra area to 3.0 g/dm3 in the central and near-Pieniny parts of the basin. Palaeogene strata are important in controlling the hydrogeology of the Podhale artesian basin. The Tatra Mountains are a recharge area for the Podhale basin whereas the Pieniny Klippen Belt seems to be an impermeable shield preventing further groundwater flow to the north. Within the southern flank of the basin the groundwaters are used as a local source of drinking water as well as to supply thermal baths in Zakopane. Furthermore, the geothermal energy from the Podhale basin provides a supply of clean, environment-friendly domestic heating.
Źródło:
Geological Quarterly; 2003, 47, 2; 195-210
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Human impact on the plant cover of four villages in SE Poland
Autorzy:
Kotanska, M.
Buziak-Chmielowiec, E.
Dabrowska, A.
Gladysz, M.
Jakielaszek, A.
Wojcik, T.
Powiązania:
https://bibliotekanauki.pl/articles/790607.pdf
Data publikacji:
2015
Wydawca:
Uniwersytet Przyrodniczy w Poznaniu
Tematy:
human impact
plant cover
village
rural area
Sandomierz Basin
anthropopressure
anthropogenic factor
Polska
Opis:
The observation of the rapid rate of plant cover transformation caused by urbanization and agricultural technology was the inspiration for undertaking the study in rural areas. The study was carried out in the Sandomierz Basin in four typical villages with varying degrees of the anthropogenic impact. The changes observed included: Koszyce Małe – evident transformation of fields and meadows into building land; Kolbuszowa Dolna – intensive changes in land use, abandonment of fields and meadows, and river regulation; Roźwienica – emergence of new habitats for plant colonization after reclamation of land previously occupied by a brick factory and a landfill; Krzeczowice – intensive crop cultivation and unchanged land use. In 2009–2010, floristic investigations with the patrol method were carried out in these areas. The historical-geographical classification and indices of the anthropogenic changes of the flora were employed in the analysis. Substantially, domination of synanthropic species over non-synanthropic spontaneophytes was noted in the analysed floras. In the synanthropic species group, the proportion of apophytes was 3-fold higher than that of anthropophytes. Archaeophytes were more abundant than kenophytes. The flora of Krzeczowice, an area affected by long-term anthropopressure, was by approx. 30% less abundant than that in the other villages; it was also characterised by the highest synanthropization index, apophytization index, and index of apophytism of spontaneophytes. In turn, the flora found in Kolbuszowa Dolna was rich due to the presence of a wide variety of habitats; it was characterised by the lowest apophytization index accompanied by the highest anthropophization index.
Źródło:
Steciana; 2015, 19, 2
1689-653X
Pojawia się w:
Steciana
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Application of ITS-2 Model for Flood Hydrograph Simulation in Large-Size Rainforest Watershed, Indonesia
Autorzy:
Tunas, I. Gede
Powiązania:
https://bibliotekanauki.pl/articles/124788.pdf
Data publikacji:
2019
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
flood management
hydrology model
river basin
peak flow
tropical area
Institut Teknologi Sepuluh Nopember
Opis:
Nowadays, the increasing intensity of extreme rainfall and changes in land use have triggered massive floods in various regions of Indonesia. The changes in the characteristics of these two parameters cause an increase in the peak and duration of the flood over time. Peak and duration of flood estimation might be very useful for the national and local government because it is closely related to the effectiveness of prevention and mitigation plan in the future. A hydrograph-based model constitutes one approach to estimating them simultaneously. The objective of this research is to examine the application of ITS-2 – a synthetic unit hydrograph (SUH) model which was developed at Sepuluh Nopember Institute of Technology (ITS) in 2017 – for estimating the peak flood discharge as a basis for planning disaster mitigation programs. This study was carried out by testing the reliability of the ITS-2 Model using the Nash-Sutcliffe Efficiency (NSE) indicator by comparing the measured unit hydrograph and synthetic unit hydrograph derived using the model, optimizing the parameters of the model, and then analyzing the transformation of rainfall-flood discharge in the Gumbasa Watershed, one of the major watersheds in Central Sulawesi Province, Indonesia. This catchment is part of the Palu watershed, which is largely a tropical rainforest conservation area known as the Lore Lindu National Park. The input model is based on the design rainfall with a certain return period using the frequency analysis where the data was obtained from the rainfall stations in the study area. The results of the research showed that the performance of the ITS-2 model was still very good with the NSE above 80%. The difference in the peak discharge of these two unit hydrographs is relatively low, with a deviation below 10%. The optimal values of the ITS-2 Model parameter coefficients consisting of C1, C2, and C3 were achieved at 1.29, 0.33 and 1.88, respectively. The results of the hydrograph analysis based on a 1-year to 100-year return period indicate that peak flood discharge ranges from 100 m3/sec to 550 m3/sec. From a series of analyses and tests that have been conducted in the previous and current research, it can be concluded that the ITS-2 Model can be applied to various watershed sizes, especially in Indonesia.
Źródło:
Journal of Ecological Engineering; 2019, 20, 7; 112-125
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The earliest ostracods from the Ordovician of the Prague Basin, Czech Republic
Autorzy:
Lajblová, K.
Kraft, P.
Powiązania:
https://bibliotekanauki.pl/articles/138871.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Ostracoda
Middle Ordovician
Barrandian area
Prague Basin
taxonomy
palaeobiogeography
ordowik
Barrandian
dorzecze
Praga
systematyka
paleobiogeografia
Opis:
The earliest ostracods from the Bohemian Massif (Central European Variscides) have been recorded from the Middle Ordovician of the Prague Basin (Barrandian area), in the upper Klabava Formation, and became an abundant component of fossil assemblages in the overlying Šárka Formation. Both early ostracod associations consist of eight species in total, representing mainly eridostracans, palaeocopids, and binodicopids. The revision, description, or redescription of all species and their distribution in the basin is provided. Their diversification patterns and palaeogeographical relationships to ostracod assemblages from other regions are discussed.
Źródło:
Acta Geologica Polonica; 2014, 64, 4; 367-392
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Groundwater vulnerability to pollution in degraded coal mining areas: modifying the DRASTIC method using the factor of exploitation impact on land surface
Autorzy:
Krogulec, Ewa
Bukowski, Przemysław
Niedbalska, Katarzyna
Trzeciak, Joanna
Zabłocki, Sebastian
Powiązania:
https://bibliotekanauki.pl/articles/27310140.pdf
Data publikacji:
2023
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
groundwater vulnerability to pollution
mining area
coal activities
mining exploitation phases
Upper Silesia Coal Basin
Polska
Opis:
Mining activities such as underground exploitation of hard coal deposits and open cast mining are strong factors on groundwater depending on mine life cycle phases. The impact of coal mining activities on groundwater have been reported from many countries. In this case, a vulnerability assessment was conducted base on standard DRASTIC method and its modification DRASTIC MINE (DRASTICM) method. In order to take into account, the impact of mining activities, a new parameter was added which defined the impact of coal seams on the rock mass above, including the degree of its drainage and the range of its impact. In the standard DRASTIC method, the results indicate that groundwater vulnerability with high (38.6%) and very high occurrence classes (16.9% of the area), mostly covers the central part of the cast mine. In contrast, the reclaimed area of the excavation is a low-class area. The DRASTICM method increased the vulnerability index from 3 to 24 on 95% of the area, so a new vulnerability class of extremely high was delineated, which occurred in 1.6% of the area. This indicates areas that should be treated as a priority in order to avoid pollution, and in the final stage to plan activities in the field of the reclamation of mining areas. The results showed that groundwater vulnerability assessment in coal mining areas can be significantly improved.
Źródło:
Geology, Geophysics and Environment; 2023, 49, 4; 313--334
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Portal mapowy jako źródło informacji o terenie pogórniczym na przykładzie Zagłębia Wałbrzyskiego
Geoportal as the source of geographical information about post-mining area based on the example of the Wałbrzych Coal Basin
Autorzy:
Olejnik, K.
Powiązania:
https://bibliotekanauki.pl/articles/122249.pdf
Data publikacji:
2015
Wydawca:
Politechnika Wrocławska. Wydział Geoinżynierii, Górnictwa i Geologii. Instytut Górnictwa
Tematy:
Zagłębie Wałbrzyskie
teren pogórniczy
GIS
portal mapowy
open source
Wałbrzych Coal Basin
post-mining area
Web Mapping
Opis:
Portal mapowy jest doskonałą formą wizualizacji wszystkich elementów z obszaru dawnego Zagłębia Wałbrzyskiego pozostałych po przemyśle wydobywczym. Dane wykorzystane do przygotowania opracowania pochodziły głównie z map topograficznych i archiwalnych opracowań górniczych. Realizacja omawianego portalu opiera się na tak zwanej architekturze trójwarstwowej. Proces budowy rozpoczęto od przygotowania danych wektorowych w postaci warstw tematycznych. Następnie, według zastosowanego schematu, stworzono strukturę składającą się z bazy danych oraz serwera sieciowego, który umożliwił wyświetlanie obiektów w aplikacji, przeznaczonej dla użytkownika. Całość wykorzystanego oprogramowania jest dystrybuowana na licencjach typu open source.
The post-mining area of Wałbrzych Coal Basin is still undergoing revitalization and contains traces of many mining activities. Web mapping process presented in this paper is a fine way of visualization of all surface objects of the mining industry. Data used in the project has been collected from various sources like topographic maps and mining documentations. Implementation of the geoportal was based on three-tier architecture. The whole process started from preparing spatial data which occurs in vector layer form. The key step was the construction of three connected layers which are: database, server application and presentation trier designed for clients. All of the software used is distributed on open source licenses.
Źródło:
Hereditas Minariorum; 2015, 2; 161-174
2391-9450
2450-4114
Pojawia się w:
Hereditas Minariorum
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Model późnojurajsko-wczesnomioceńskiej ewolucji tektonicznej zachodnich Karpat zewnętrznych
Model of late Jurassic to early Miocene tectonic evolution of the Western Outer Carpathians
Autorzy:
Poprawa, P.
Malata, T.
Powiązania:
https://bibliotekanauki.pl/articles/2074481.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
basen sedymentacyjny
obszar źródłowy
tektonika
Karpaty zewnętrzne
miocen
jura
Outer Carpathians
Mesozoic
Cainozoic
sedimentary basin
source area
tectonics
Opis:
At the end of the Jurassic and beginning of the Cretaceous in the Western Outer Carpathians (WOC) rift-related extension led to development of: the deep marine grabens with flysch and pelagic sedimentation, the zones of shallow marine carbonate sedimentation, and the elevated horsts, supplying the basins with sediments. Transition to the Early Cretaceous and Cenomanian post-rift thermal sag stage was responsible for a general ceasing of tectonic activity in the source areas and unification of the previous sub-basins. In Barremian–Albian time, the northern, external sources for sediments were uplifted due to compression, presumably caused by the orogenic collision in the Middle and Outer Dacides and/or collision related to subduction of the Penninic Ocean. The Silesian Ridge, rapidly elevated and eroded during Late Cretaceous and Paleocene, is interpreted here as an active thick-skinned thrust belt. Nappe stacking in that area and stress transmission towards foreland caused flexural subsidence of the proximal zone (the inner Silesian Basin) and uplift in the distal zone (including: the outer Silesian Basin, the Subsilesian facies zone, the Skole Basin and the northern sediment source areas). The Eocene alternating shallow marine deposition in the Silesian Ridge and its exposition for erosion is interpreted as controlled by both eustatic sea level changes and episodic tectonic activity. At this time new thick-skinned thrust belt developed south of the Magura Basin, which supplied vast amount of detritus for the Magura Beds. The Eocene tectonic shortening and deformations in the Southern Magura Ridge and development of the accretionary prism caused flexural bending of its broad foreland, subsidence and relative facies unification of the basins and decrease of activity of the source areas located north of the Magura Basin. The Oligocene progress of plates/microplates convergence and relocation of the zone of tectonic shortening towards the north led to compressional uplift of the source areas located both to the north of the WOC basins and to the south of the Silesian facies zone, the later composed of crystalline basement, as well as sediments of the Magura Unit. That sources supplied with detritus the Upper Oligocene–Llower Miocene Krosno Beds, being a diachronic continuation of synorogenic deposition of the Magura Beds. During the Late Cretaceous–Paleogene–Early Miocene, an important tectonic shortening across the WOC took place, accommodated mainly in the source areas. This indicates that the palaeogeographic relationships between the Silesian Basin, the Magura Basin and the Central Carpathian Paleogene Basin were changing during the Cretaceous and Cainozoic. In the time span of Albian to Oligocene in the zone palaeogeographically located between the Magura Basin and the Central Carpathians three separate source areas were active, each characterized by a different geological setting. These sources were replacing each other in time, suggesting significant collisional and/or strike slip reorganisation of the zone during that period. The collision of the WOC evolved in time from thick-skinned mode during the Late Cretaceous–Paleogene to thin-skinned one during the Middle Miocene.
Źródło:
Przegląd Geologiczny; 2006, 54, 12; 1066-1080
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Horizontal and vertical distribution of lignin in surface sediments of the Gdańsk Basin
Autorzy:
Staniszewski, A.
Lejman, A.
Pempkowiak, J.
Powiązania:
https://bibliotekanauki.pl/articles/47928.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
oxidation provenience
organic matter
surface sediment
vertical distribution
accumulation area
Baltic Sea
Vistula River
Gdansk Basin
horizontal distribution
lignin
Opis:
The aim of this study was to identify and quantify lignin transported from the River Vistula to the accumulation area in the Gdańsk Basin. Sediment samples collected along the Vistula mouth –Gdańsk Deep transect were analysed for lignin. Lignin was characterised by oxidative degradation, cupric oxide being chosen as the most suitable oxidising agent. The polar functional groups of the oxidation products were silylated and the derivatives analysed by capillary gas chromatography on fused capillary silica columns with flame ionisation detection. Lignin-derived oxidation products were quantified in the range from 3 to 20 μg g−1 dry wt. for phenolic acids and from 6 to 12 μg g−1 dry wt. for phenolic aldehydes. Differences in oxidation products contents are assigned to different lignin sources in the marine environment. The horizontal and vertical gradients of these compounds in the sediments of the Gdańsk Basin are documented. The results are discussed in terms of the origin and fate of organic matter in the Gdańsk Basin. The measured differences in quality and quantity of the identified oxidation products provide insight into diagenetic processes in the surface marine sediments.
Źródło:
Oceanologia; 2001, 43, 4
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł

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