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Numerical model of the catchments of the Oziąbel and Wołczyński Strumień rivers - Wołczyn municipality

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EN
Abstrakty
EN
The article presents a numerical model designed for determining groundwater dynamics and water balance of the catchments of the Oziąbel (Czarna Woda) river and the Wołczyński Strumień river in Wołczyn region. Hydrogeological mapping and modelling research covered the area of 238.9 km 2 . As a result of measurements performed in 2008-2009, flows were determined in major rivers and water table positions were measured at 26 points. In the major part of the area described, the water table, lying at the depth of 1.5-18.7 m, has unconfined character, and the aquifer is built of Neogene (Quaternary) sands and gravels. In the area under study, groundwaters are drawn from 6 wells with total withdrawal of 6133 m 3 /d. The numerical modelling was performed with the use of Visual Modflow 3.1.0 software. The area was partitioned by a discretization grid with a step size l = 250 m. The conceptual model of the hydrogeological system is based on hydrological data gathered over a period of one year, data from HYDRO bank database, cross-sections and maps. The boundaries of the modelled hydrogeological system were established on the watersheds of the Wołczyński Strumień river and the Oziąbel river, apart from the areas where they run together. The modelled area was extended (271.5 km 2 ) around the Wołczyński Strumień river catchment to achieve a more effective mapping of the anthropogenic impact on its balance and the hydrodynamic system of the catchment area. The structure is characterised by the occurrence of one or rarely two aquifers separated by a pack of Quaternary clays. The investigation produced a detailed water balance and its components.
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Rocznik
Strony
73--89
Opis fizyczny
Bibliogr. 10 poz., tab., rys., wykr.
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autor
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Bibliografia
  • [1] ANDERSON M.P., WOESSNER W.W., Applied Groundwater Modeling, Academic Press, Inc., London 1992.
  • [2] DĄBROWSKI S., The Prosna valley evolution. The lithology and stratigraphy of Quaternary formations, Wydawnictwo UAM, Poznań 1991, (in Polish).
  • [3] DZIEDZIAK J., A hydrogeological map of Poland, scale 1:50 000, Rychtal sheet, Wydawnictwo PIG, Warszawa 2000.
  • [4] GURWIN J., POPRAWSKI L., Assessment of regional groundwater resources by means of numerical modelling methods, [in:] Współczesne Problemy Hydrogeologii X, tom 2, Wyd. Sudety, Wrocław 2001 (in Polish).
  • [5] GÓRNIK M., A hydrogeological map of Poland, scale 1:50 000, Wołczyn sheet with explanation. Państwowy Instytut Geologiczny, Warszawa 1998 (in Polish).
  • [6] KLECZKOWSKI A.S., Hydrogeology of areas surrounding Poland, Wyd. Geol., Warszawa 1979 (in Polish).
  • [7] McDONALD M.G., HARBAUGH A.W., A modular three dimensional finite-difference ground-water flow model, US Geol. Surv. Technical of water resources investigations book 6, chap A1, USGS. Washington, DC, 1988.
  • [8] WĄSIK M., Infiltration capacity of near-surface formations and groundwater recharging, [in:] Acta Universitatis Wratislaviensis (Hydrogeologia), No 2591, 2003, (in Polish).
  • [9] WANG H.X., ZHANG L., DAWES W.R., LIU C.M., Improving water use efficiency of irrigated crops in the North China Plain – measurements and modelling, Agricultural Water Management, 2001, 48, 151–167.
  • [10] WOUDT van’t B.D., NICOLLE K., Flow processes below a gravelly riverbed, Journal of Hydrology, 1978, Vol. 17, No. 2, 103–120.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BPW8-0022-0013
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