The Estimation of Groundwater Recharge from Water Level and Precipitation Data

The amount of precipitation that reaches the zone of saturation depends upon several factors. Because of these factors, determining the recharge to aquifers is a difficult problem in all water resources studies. A study for determining quantitative groundwater recharge is illustrated by the analysis of water level fluctuations in Kütahya-Çavdarhisar plain in Turkiye. The recharge of the groundwater in the study area is from precipitation.