摘要
Mixing processes are universal in the genesis of thermal waters from Xinzhou basin. Chemical and isotopic (δD-δ18O,34S/32S,87Sr/86Sr,T) data are comprehensively used to dis cern the geochemical and hydrodynamic environments of these waters. Based on a two-year hydrochemical monitoring on thermal waters from the well XD1 in Duncun geothermal field . a series of changes in quality have been observed , which are attributed to the change in the proportion of end members making up the thermal waters being withdrawn .
Mixing processes are universal in the genesis of thermal waters from Xinzhou basin. Chemical and isotopic (δD-δ18O,34S/32S,87Sr/86Sr,T) data are comprehensively used to dis cern the geochemical and hydrodynamic environments of these waters. Based on a two-year hydrochemical monitoring on thermal waters from the well XD1 in Duncun geothermal field . a series of changes in quality have been observed , which are attributed to the change in the proportion of end members making up the thermal waters being withdrawn .
基金
The research is supported by the IET Education Foundation
