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Wyświetlanie 1-2 z 2
Tytuł:
Geochemical analyses of recent sediments from Lake Morzycko against selected physiographic parameters of the Słubia River catchment (Western Poland)
Autorzy:
Adamek, Anna
Mareczka, Paulina
Jucha, Witold
Musielak, Stanisław
Okupny, Daniel
Powiązania:
https://bibliotekanauki.pl/articles/2037025.pdf
Data publikacji:
2021-12-23
Wydawca:
Łódzkie Towarzystwo Naukowe
Tematy:
lake sediments
geochemistry
grain-size composition
land-cover photointerpretation
Myślibórz Lakeland
Opis:
This paper presents the results of a study on the content of lithogeochemical components (organic matter, Na, K, Mg, Ca, Mn, Fe, Cu and Zn) and grain-size composition of mineral matter in the bottom sediments of Morzycko Lake (Myślibórz Lakeland, NW Poland). This lake is large (342.7 ha) and deep (69 m). The catchment has a typical forested character (mainly in the middle part of the Słubia River valley) with agricultural area (mainly in the upland areas north of the lake). The diversity of concentrations of metals was analysed based on 44 samples from 22 representative sites, including surface sediments and sediments from 5 cm below the current lake bed. The results showed that the chemical composition and granulometry of bottom sediments depends on contemporary morphogenetic processes in the catchment of the Słubia River. Geochemical and grain-size indices varied due to changes in biological productivity, intensity of weathering of postglacial material making up the catchment, and potential for migration of metals to the lake with surface or underground runoff. An important aspect in assessing the degree of enrichment of the sediments in trace elements is the location of shallow parts of the lake near the tourist districts of Moryń.
Źródło:
Acta Geographica Lodziensia; 2021, 111; 71-87
0065-1249
Pojawia się w:
Acta Geographica Lodziensia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Warunki hydrogeologiczne Pojezierza Myśliborskiego i obszarów sąsiednich w granicach jednolitej części wód podziemnych nr 23
Hydrogeological conditions in the Myoelibórz Lakeland and adjacent areas within the borders of Groundwater Body No. 23
Autorzy:
Wiśniowski, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2074807.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
warunki hydrogeologiczne
Pojezierze Myśliborskie
wody podziemne
główne zbiorniki wód podziemnych
odnawialne zasoby wód podziemnych
dyspozycyjne zasoby wód podziemnych
hydrogeological conditions
Myślibórz Lakeland
groundwater body (GWB)
main groundwater reservoirs (GZWP)
groundwater renewable resources
groundwater disposable resources
Opis:
The area of the GWB (groundwater body) No. 23 is a part of West Pomeranian and Lubusz Voivodeships and the water region of the Lower Odra and Przymorze Zachodnie. It includes districts: gryfiński, myśliborski, pyrzycki and gorzowski. The geological conditions of the study area are visibly corresponding to the deep tectonic structures of Szczecin basin and Gorzów block. Fresh groundwater is occurring here in porous sediments of the Quaternary, Neogene and Paleogene and fissured-porous rocks of the Upper Cretaceous. In the area of Szczecin basin, structures of Cretaceous aquifers are associated with Mesozoic secondary anticlines. In the Odra valley the aquifers are constituted from shallow laying Quaternary sediments (depth: 10 to 50 m). Thickness of Upper Cretaceous marbles leading fresh water does not exceed 30 m. The primal structures of the youngest sediments of Neogene- Miocene (-50 to -80 m above sea level) were disrupted during the earlier glaciations. During this geological period many of the geomorphological forms - egzaration depressions and glacitectonic extrusions formed from the Paleogene and Neogene sediments, and also elevations built from xenoliths coming from deeper rock bed, were formed by the complex of different geomorphological processes. The sediments of Neogene-Miocene have variable thickness, from a few meters within the deep erosion structures, up to 200 m within the Tertiary elevations. The Quaternary aquifers occur in multilayer system of groundwater layers constituted by fluvioglacial and fluvial sedimentation (sand and gravel) during successive glaciations and interglacials. Aquifers are often divided in multiple different layers, isolated by low-permeable layers of clays or glacial silts and proglacial clays. There are selected few regional aquifers: four Quaternary aquifers - first unconfined; upper, interior and lower intertill aquifers; two Miocene - upper and lower aquifers and one Cretaceous aquifer. The thickness of individual aquifer is variable; it's locally up to 50 m. The GWB No. 23 aquifers were aggregated to 3 levels (hydrogeological zones) belonging to different systems of groundwater flow: I level - first unconfined and upper intertill aquifer (locally Cretaceous aquifer); II level - interior intertill aquifer; III - lower intertill aquifer and upper Miocene aquifer. Because of the multilayer character, the GWB No. 23 groundwater system is very rich in water.
Źródło:
Przegląd Geologiczny; 2010, 58, 8; 704-711
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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