Evaluation of infiltration rates within the Vistula River valley, central Poland

• Autorzy: Krogulec E.
• Języki publikacji: EN

Abstrakty

EN

The Vistula river valley groundwater system has a strong hydraulic connectivity with the surface waters of the Vistula River. Typically, it is dominated by infiltration, and may at the same time represent a transitional system, in which lateral baseflow discharge takes place from surrounding units (e.g. plateau) to the river valley. A relatively simple mechanism of infiltration represents one of the elements of a complex water circulation system in the valley unit. The recognition of the entire recharge mechanism in a valley unit allows indicating a variable but significant role of infiltration. Evaluation of the value of infiltration on a regional scale has been made for the Vistula River valley in the Kampinoski National Park (KNP) area. Data on the spatial distribution of infiltration, averaged for a particular time interval, are indispensable e.g. for balance calculations as well as for evaluation of groundwater vulnerability to contamination. Evaluation of infiltration into the groundwater system of the KNP area was made using the following methods: meteorological and empirical methods, water table fluctuation (WTF), runoff hydrograph sub-division (BFI), and numerical simulations.

Słowa kluczowe

EN

groundwater recharge; infiltration; Kampinoski National Park; river valley; Vistula river

PL

dolina rzeki; infiltracja; Kampinowski Park Narodowy; odnawialność wód podziemnych; Wisła

• Wydawca: Faculty of Geology of the University of Warsaw ; Komitet Nauk Geologicznych PAN
• Czasopismo: Acta Geologica Polonica
• Rocznik: 2010
• Tom: Vol. 60, no. 4
• Strony: 617--628
• Opis fizyczny: Bibliogr. 26 poz.,

Twórcy

autor

Krogulec E.

• University of Warsaw, Faculty of Geology, Institute of Hydrogeology and Engineering Geology, Żwirki and Wigury 93, 02-089 Warsaw, Poland,

Bibliografia

• 1. Anderson, M. and Woessner, W. 1992. Applied Groundwater Modeling, 381 pp. Academic Press Inc.; London.
• 2. Centre Naturopa, 1998. The paneuropean ecological network. Questions and answers, 4, 43 pp.
• 3. Civita, M.V. 1993. Ground Water Vulnerability Maps: A Review. Proc. IX Symp. Pesticide Chemistry “Mobility and Degradation of Xenobiotics”, Piacenza, 587–631.
• 4. Cygański, K. and Woźniak, E. 1997. Mapa hydrogeologiczna Polski w skali 1:50 000, arkusz Błonie. [Hydrogeological Map of Poland in scale 1:50,000, Sheet Blonie]. Państwowy Instytut Geologiczny; Warszawa.
• 5. Healy, R.W. and Cook, P.G. 2002. Using ground water levels to estimate recharge. Hydrogeology Journal, 10, 91–109.
• 6. Harbaugh, A.W., Banta, E.R., Hill, M.C. and McDonald, M.G. 2000. MODFLOW-2000. the U.S. Geological Survey Modular Ground-Water Model - User guide to modularization concepts and the ground-water flow process: U.S. Geological Survey Open-File Report 00-92, 121 pp.
• 7. Krogulec, E. 1997. Numeryczna analiza struktury strumienia filtracji w strefie krawędziowej poziomu błońskiego. Wydawnictwa Uniwersytetu Warszawskiego, Warszawa. [Numerical analysis of filtration stream in the margin zone of blonski level], 97 pp.
• 8. Krogulec, E. 2001. Monitoring shallow groundwater within protected areas – an example of local groundwater monitoring network in Kampinos National Park (Poland). Conference “Hydrogeochemia 2001”, Bratislava, 117–123.
• 9. Krogulec, E. 2003. Hydrogeological conditions of the Kampinos National Park (KNP) region. Ecohydrology and Hydrobiology, 3, 257–266.
• 10. Krogulec, E. 2004. Ocena podatności wód podziemnych na zanieczyszczenia w dolinie rzecznej na podstawie przesłanek hydrodynamicznych. Wydawnictwa Uniwersytetu Warszawskiego; Warszawa [Assessment of groundwater vulnerability to contamination in the River valley on the basis of hydrodynamical indications], 116 pp.
• 11. Krogulec, E. and Andrzejewska, A. 2005. Zastosowanie automatycznych pomiarów stanów wód podziemnych w lokalnym systemie monitoringowym. [Electronic groundwater level observation in local monitoring system]. Współczesne problemy hydrogeologii, 12, 397–405.
• 12. Learner, D.N. 1997. Groundwater recharge. In: Geochemical processes, weathering and groundwater recharge in catchments, pp. 109–150. AA Balkema; Rotterdam.
• 13. Learner, D.N. Issar, A.S. and Simmers, I. 1998. Groundwater. A Guide to Understanding and Estimating Natural Recharge, Volume 8, 345 pp. Verlag Heinz Heise.
• 14. Liro, A. (Ed.). 1998. Koncepcja krajowej sieci ekologicznej ECONET – Polska. Fundacja ICUN Poland; Warszawa. 1–205 pp. [The concept of ecological net-work EECONET]
• 15. Magnuszewski, A. 1990. Zautomatyzowany sposób obliczania charakterystyk niżówkowych [Automatized way of low water characteristics estimation]. Przegląd Geofizyczny, 1-2, 79–83.
• 16. Małecki, J. 1998. Rola strefy aeracji w kształtowaniu składu chemicznego płytkich wód podziemnych wybranych środowisk hydrogeologicznych. Biuletyn Państwowego Instytutu Geologicznego, 381. [Role of aeration zone in forming of chemical composition of shallow groundwater of chosen hydrogeological environments], 1–156 pp.
• 17. McDonald, M.G. and Harbaugh, A.W. 1988, A modular threedimensional finite-difference ground-water flow model: Techniques of Water-Resources Investigations of the United States Geological Survey, Book 6, Chapter A1, 586 pp.
• 18. Paczyński, B. (Ed.). 1995. Atlas hydrogeologiczny Polski, skala 1:500 000, część II. [Polish Hydrogeological atlas, scale 1:500 000, part II], Państwowy Instytut Geologiczny; Warszawa.
• 19. Pazdro, Z. 1983. Hydrogeologia ogólna. [General hydrogeology], 506 pp. Wydawnictwa Geologiczne; Warszawa.
• 20. Rudzińska-Zapaśnik, T. 2000. Mapa hydrogeologiczna Polski w skali 1:50 000, arkusz Sochaczew. [Hydrogeological map of Poland in scale 1:50,000, Sheet Sochaczew]. Państwowy Instytut Geologiczny, Warszawa.
• 21. Scanlon, B.R. Healy, R.W. and Cook, P.G. 2002. Choosing appropriate techniques for quantifying groundwater recharge. Hydrogeology Journal, 10, 18–39.
• 22. Simmers, I. 1990. Aridity, groundwater recharge and water resources management. In: A guide to understanding and estimating natural recharge. IAH, 9, 1–20. Verlag Heinz Heise.
• 23. Soczyńska, U. Gutry-Korycka, M. Pokojska, P. and Mikos, D. 2003. Water balance as base for proper water management in the Lasica catchment (Kampinoski National Park). Ecohydrology and Hydrobiology, 3, 291–309.
• 24. Somorowska, U. 2003. Risk assessment of the occurrence of extreme groundwater levels, discharge and soil moisture stages. Ecohydrology and Hydrobiology, 3, 311–321.
• 25. Stephens, D.B. 1996. Estimation of infiltration and recharge for environmental site assessment. API Publ 4643. 143 pp. Health and Environmental Science Department, Albuquerque; New Mexico.
• 26. Tomaszewski, E. 1998. Zastosowanie zmodyfikowanego algorytmu FRIEND do oceny wielkości podziemnego zasilania rzek. In: Magnuszewski, A. and Soczyńska, U. (Eds), Hydrologia u progu XXI wieku. Komisja Hydrologiczna PTG, Wydawnictwa Uniwersytetu Warszawskiego; Warszawa. [Applying of modified FIEND formula for supply of baseflow evaluation], 285–293.