Influence of rainfall on fluctuation of the water table in wells in the village of Bratkowice, Podkarpackie Province

• Autorzy: Stanek-Tarkowska Jadwiga , Słowik Klaudia

Identyfikatory

DOI

10.12911/22998993/196723

• Języki publikacji: EN

Abstrakty

EN

The purpose of the study was to determine whether the aquifer in the 15 wells shows a rapid response to increased recharge after precipitation or lack thereof during dry months. The 15 wells located in Świlcza village were selected for monitoring. The average depth of the well was 4.7 m. The deepest was 7 m deep, and the shallowest was 3.1 m deep. Of the 15 wells, only two were in use. Water intake has not changed the position of the water table. The greatest fluctuations in the water table were recorded in shallow wells up to 0.8 m deep during the dry months. The greatest lowering of the water table in the dry months was recorded in well No. 13 by 0.72 m from the highest state (water was taken for watering plants) and in well No. 5 by 0.80 m from the highest state. From well No. 5 water was not drawn.

Słowa kluczowe

EN

wells dug; groundwater table fluctuation; rainfall

• Wydawca: Polskie Towarzystwo Inżynierii Ekologicznej ; Lublin University of Technology
• Czasopismo: Journal of Ecological Engineering
• Rocznik: 2025
• Tom: Vol. 26, nr 2
• Strony: 162--168
• Opis fizyczny: Bibliogr. 23 poz., rys. tab.

Twórcy

autor

Stanek-Tarkowska Jadwiga

• Department of Soil Science, Environmental Chemistry, and Hydrology, University of Rzeszow, ul. Zelwerowicza 8B, 35-601 Rzeszów, Poland

• https://orcid.org/0000-0003-1664-2625

autor

Słowik Klaudia

• Department of Soil Science, Environmental Chemistry, and Hydrology, University of Rzeszow, ul. Zelwerowicza 8B, 35-601 Rzeszów, Poland

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