Changes of grounwater levels of the Turonian aquifer in the "Certovy zdi" region in the Bohemian Cretaceous Basin on the base of a longterm monitoring

Abstract

Longterm time series of the Turonian groundwater level in many monitoring boreholes in this region show significant changes, mostly its fall. Probable cause: water supply pumping in Dolanky, and interaquifer overflowing between Turonian and Cenomanian aquifer through old boreholes that were wrongly cementated.

Keywords

• groundwater
• Bohemian Cretaceous Basin
• Certovy zdi
• groundwater monitoring
• Dolanky