Abstract
The physical and chemical characteristics of karst springs are not a sole function of flow path in the carbonatic rock mass. A number of other parameters, including the type of precipitation, soil cover, morphology of the exposed area, and the hydrochemistry of the infiltrating water into the karst system also have their own contribution. In the present study, the Gar and Barm-Firooz mountains are chosen to determine some of the governing factors of the physical and hydrochemical characteristics of karst springs. The following measurements were carried out: The results indicate that if the physical and chemical characteristics of a karst spring are going to be used to determine the characteristics of corresponding aquifer, first the effect of external factors on the outflow should be accounted for, and then the characteristics of the karst aquifer be determined.
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