Temat: zasoby odnawialne wód podziemnych - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Ocena zasobów odnawialnych wód podziemnych Pomorza Zachodniego na podstawie modelu symulacyjnego WETSPASS
Assessment of renewable groundwater resources in Western Pomerania based on the WetSpass simulation model
Autorzy:: Kajewska-Szkudlarek, J.
Kubicz, J.
Kajewski, I.
Dąbek, P.
Powiązania:: https://bibliotekanauki.pl/articles/2075750.pdf
Data publikacji:: 2017
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: bilans wodny
model WetSpass
Pomorze Zachodnie
zasoby odnawialne wód podziemnych
zmiany klimatu
water balance
WetSpass model
Western Pomerania
renewable groundwater resources
climate change
Opis:: The aim of the study was to the assess Western Pomeranian renewable groundwater resources in relation to climate change. The objective was accomplished by simulating the water balance components in two periods of 1971-2000 and 1981-2010, differing in terms of climatic parameters (precipitation, evaporation, air temperature and wind speed). The results of the simulation calculations allowed to assess the impact of climate change on the water balance structure of Western Pomerania and particularly on groundwater recharge. The data for the simulation calculations in the WetSpass model were included 8 numerical maps (raster), representing the basic elements of the climate, land use, types of soil (due to soil texture), depth of the groundwater table and terrain slopes. As a result of the simulation calculations, raster maps of the spatial distribution ofparticular elements of the water balance were obtained sub-divided into the summer and winter seasons and for the whole year.
Źródło:: Przegląd Geologiczny; 2017, 65, 11/1; 1080--1084
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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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

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