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    Wyświetlanie 1-6 z 6
    Tytuł:
    Strukturalne właściwości drewna sosny zwyczajnej (Pinus sylvestris L.) w zależności od strony świata - wstępne wyniki badań
    Structural properties of Scots pine wood (Pinus sylvestris L.) in relation to the cardinal directions - preliminary results
    Autorzy:
    Rola, P.
    Staniszewski, P.
    Tomusiak, R.
    Sekrecki, P.
    Wysocka, N.
    Powiązania:
    https://bibliotekanauki.pl/articles/881330.pdf
    Data publikacji:
    2014
    Wydawca:
    Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Leśny Zakład Doświadczalny. Centrum Edukacji Przyrodniczo-Leśnej w Rogowie
    Tematy:
    drzewa
    polozenie w stosunku do stron swiata
    sosna zwyczajna
    Pinus sylvestris
    drewno sosnowe
    drewno pozne
    sloje przyrostu rocznego
    wlasciwosci strukturalne
    szerokosc
    Źródło:
    Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej; 2014, 16, 3[40]
    1509-1414
    Pojawia się w:
    Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Porównanie efektów usuwania ortofosforanów ze ścieków metodą elektrokoagulacji i metodą roztwarzania metali
    Comparison of the results of orthophosphates removal from sewage using electrocoagulation method and metal digestion method
    Autorzy:
    Wysocka, I.
    Giza, M. N.
    Powiązania:
    https://bibliotekanauki.pl/articles/1819439.pdf
    Data publikacji:
    2011
    Wydawca:
    Politechnika Koszalińska. Wydawnictwo Uczelniane
    Tematy:
    ortofosforanty
    roztwarzanie metali
    elektrokoagulacja
    orthophosphates
    dissolution of metals
    electrocoagulation
    Opis:
    Celem niniejszych badań było porównanie efektów usuwania związków fosforu (ortofosforanów) z wód z dodatkiem ortofosforanów, z wykorzystaniem dwóch metod: metody elektrokoagulacji (z wykorzystaniem procesów elektrochemicznych z użyciem prądu stałego) i metody roztwarzania metali (z wykorzystaniem procesów korozyjnych).
    There is a search in progress for some efficient methods of removing biogenic compounds from the treated sewage. Unquestionably, effective methods of phosphorus compounds removal include precipitation methods. The most common is the chemical precipitation method based on applying iron, aluminium or calcium salt to the solution and electrocoagulation. These methods utilise low solubility of metal phosphates and their sorption on the surfaces of the forming agglomerates. The real mechanism is quite complicated and consists of transforming phosphorus compounds into insoluble forms, and then separating them from the sewage by flotation, sedimentation, filtration. The method of iron solution should also be accounted into similar physical and chemical methods. The main difference between the aforementioned methods lies in the way of applying the precipitation agent to the solution. The method of iron solution is based on similar premises as the electrocoagulation method, however, metal ions here are dissolved into the solution as a result of spontaneous corrosion processes and, due to the further transformations in the sewage environment, they are to be responsible for phosphorus removal. The article presents comparative tests on a laboratory scale. The electrocoagulation method and metal digestion method were compared with regard to the effectiveness of orthophosphates removal from synthetic sewage. The comparison of both methods suggests that they can bring similar results of removing phosphorus (ortophosphates) from sewage. The process of reduction of concentration of orthophosphates in sewage occurs faster when the electrocoagulation method is used. However, with a longer test duration, better results are achieved using the metal digestion method. It was also noted that both methods introduce different amounts of iron into the solution. The methods differ with regard to the amount of iron remaining in the sewage in a suspended form. This indicates a better use of iron ions in the metal digestion method and it slightly limits the problem of an excessive amount of sludge.
    Źródło:
    Rocznik Ochrona Środowiska; 2011, Tom 13; 1915-1925
    1506-218X
    Pojawia się w:
    Rocznik Ochrona Środowiska
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Własności bakteriobójcze osocza i granulocytów u osób nadużywających alkoholu
    Baktericidnye svojjstva plazmy i granulocitov u lic zloupotrebljajushhikh spirtnymi napitkami
    Bactericidal properties of plasma and granulocytes in subjects abusing alkohol
    Autorzy:
    Wysocka, J.
    Wołosowicz, N.
    Sidun, Z.
    Powiązania:
    https://bibliotekanauki.pl/articles/2187853.pdf
    Data publikacji:
    1986
    Wydawca:
    Polskie Towarzystwo Diagnostyki Laboratoryjnej
    Źródło:
    Diagnostyka Laboratoryjna; 1986, 22, 1; 35-38
    0867-4043
    Pojawia się w:
    Diagnostyka Laboratoryjna
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Sedimentary petrology characteristics and their implications for provenance of Hoanh Bo Basin Neogene system in Quang Ninh province, north-eastern Vietnam
    Autorzy:
    Tha, H.V.
    Wysocka, A.
    Cuong, N. Q.
    Pha, P.D.
    Ziółkowski, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/184381.pdf
    Data publikacji:
    2017
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    conglomerate
    sandstone
    petrography
    Hoanh Bo Basin
    Neogene
    Vietnam
    Opis:
    The Hoanh Bo Basin has developed over multiple periods since the Miocene period in association with the tectonic activity of the Chi Linh-Hon Gai and Trung Luong Faults. The basin is filled with Neogene continental sediments, comprising mainly polymictic conglomerates, sandstones, siltstones, claystones, and shales. Coarser-grained polymictic deposits predominate along the northern and western margins of the basin, whereas different types of siltstones, claystones, and sandstones occur in its centre, as well as along its southern and eastern parts, toward the Ha Long Bay. The conglomerates and sandstones are composed mainly of quartz and sedimentary rock fragments, and a small amount of mica. Cement is mainly built of iron-oxide, clay or carbonate mud. The source area for the Hoanh Bo Basin sediments was located in the close vicinity of the basin. It was built of strongly weathered rocks of the Hon Gai, Ha Coi, Cat Ba Formations.
    Źródło:
    Geology, Geophysics and Environment; 2017, 43, 1; 69-87
    2299-8004
    2353-0790
    Pojawia się w:
    Geology, Geophysics and Environment
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    New data on the continental deposits from the Cao Bang Basin (Cao Bang-Tien Yen Fault Zone, NE Vietnam) - biostratigraphy, provenance and faciespattern
    Autorzy:
    Wysocka, A.
    Pha, D. P.
    Durska, E.
    Czarniecka, U.
    Thang, D. V.
    Filipek, A.
    Cuong, N. Q.
    Tuan, D. M.
    Huyen, N. X.
    Tha, H.V.
    Powiązania:
    https://bibliotekanauki.pl/articles/138599.pdf
    Data publikacji:
    2018
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    continental environments
    pollen
    spores
    provenance
    Palaeogene
    Cao Bang
    Vietnam
    środowisko lądowe
    pyłek
    zarodniki
    proweniencja
    paleogen
    Wietnam
    Opis:
    The Cao Bang Basin is the northernmost of the basins related to the Cao Bang-Tien Yen Fault Zone in northern Vietnam. The basin is filled with a thick series of continental deposits. However, the exact age of the sedimentary basin infill has been under discussion for a long time. Because of new published data, the authors have decided to revisit this basin. Palynological data has allowed us to assign the Cao Bang Basin infill to the Lower Oligocene PC1 complex of the Shangcun Fm. (southern China). Among the saccate grains of gymnosperms, the domination of Cathaya and Pinus was observed, whereas angiosperms are represented by Carya, Celtis, Hammamelidaceae, Ulmus and also Pterocarya, Quercus, the Castanea–Castanopsis–Lithocarpus group, and the Loranthaceae. Among pteridophytes occur Laevigatosporites, Osmundaceae, and Pteris. The sedimentological features of the Cao Bang Basin are distinct from those of other basins from the Cao Bang-Tien Yen Fault Zone. The basin is filled with a wide variety of clastic deposits, from some of coarse-grained, alluvial-fan origin, through sandy beds of fluvial origin up to fine, organic-rich lacustrine deposits. The coarse-grained lithofacies are built of clasts derived mainly from local sources. The sandstones from the basin equally are submature or immature. They contain a lot of lithoclasts, the composition of which depends on the sample location within the basin. The potential source area is composed of older sedimentary units and of granitic rocks. The geochemical samples studied reflect the geochemical composition of silicic source rocks with only a minor contribution of basic components. The succession that fills the basin is interpreted as a typical fill for relatively long-lasting evolving half-graben or strike-slip basins. Moreover, the basin is partly occupied by a subsequent present-day sedimentary basin of Quaternary age.
    Źródło:
    Acta Geologica Polonica; 2018, 68, 4; 689-709
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ewolucja utworów mioceńskich zapadliska przedkarpackiego w rejonie Rzeszowa (obszar zdjęcia sejsmicznego 3D Sokołów-Smolarzyny)
    Evolution of the Miocene deposits of the Carpathian Foredeep in the vicinity of Rzeszów (the Sokołów-Smolarzyny 3D seismic survey area)
    Autorzy:
    Krzywiec, P.
    Wysocka, A.
    Oszczypko, N.
    Mastalerz, K.
    Papiernik, B.
    Wróbel, G.
    Oszczypko-Clowes, M.
    Aleksandrowski, P.
    Madej, K
    Kijewska, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074574.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    zapadlisko przedkarpackie
    miocen
    zdjęcie sejsmiczne 3D
    Carpathian foredeep
    Miocene
    3D seismic data
    Opis:
    The Miocene Carpathian foredeep basin in Poland (CFB) developed in front of the Outer Carpathian fold-and-thrust belt, at the junction of the East European craton and the Palaeozoic platform. 3D seismic data, cores and well logs from Sokołów area (vicinity of Rzeszów) were used in order to construct new depositional model of the Miocene succession of the Carpathian foredeep. The gas-bearing Miocene infill of the CFB is characterized by a shallowing-upward trend of sedimentation and consists of hemipelagic, turbiditic and deltaic and nearshore-to-estuarine facies associations. Lowermost part of the Miocene infill seems to has been deposited from the North. Such direction of sediment supply was related to influence of existing relief of the pre-Miocene basement, where very deep (up to 1,5 km) erosional valleys cut into the pre-Miocene (Precambrian) basement due to inversion and uplift of the SE segment of theMid-Polish Trough are located. Upper part of theMiocene infill reflects sediment progradation from the South, from the Carpathian area into the foredeep basin. In the Rzeszów area existence of the so-called anhydrite-less island, i.e. relatively large area devoid of the Badenian evaporitic cover caused by the post-Badenian uplift and widespread erosion of evaporites,has been postulated for many years. Interpretation of 3D seismic data showed that such model should be abandoned. In the studied part of the CFB, Late Badenian evaporitic sedimentation was restricted to the axial parts of deep paleovalleys. Evaporites deposited in these valleys have been rarely encountered by exploration wells as such wells were almost exclusively located above basement highs separating erosional paleovalleys, hence giving incorrect assumption regarding regional lack of evaporitic cover. It is possible that in axial parts of these valleys important gas accumulations might exist, charged from the South and sealed by the Badenian evaporites.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 3; 232-232
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-6 z 6

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