出版社：geodynamics Research International Bulletin Online
摘要：Considering water storage and specific yield, rocks and sediments have different characteristics. The possibility of forming groundwater reservoirs and specific yield of each reservoir initially deponds on the physical features and the geology of the porous media. Thus, in groundwaters studies, investigating aquifer characters is very important. In this study, the relation between hydrulic parameters of aquifer and its electrical resistivity is investigated. This relationship is studied over an alluvial aquifer in Gerehbygun - Zahedan Fasa plain in Fars province. In this regards, electrical resistivity of the alluvial aquifer layers was computed from 149 electrical soundings which have been measured by Schlumberger array. Using empirical formulas porosity and hydraulic conductivity in different areas of studied area were estimated. From Hubert equation, hydraulic conductivity of 59 meter per day and of the Archie equation, the average porosity of 25 % in plain were estimated. The results show, compatibility of areas having high hydraulic conductivity and porosity with location of the discharge operating wells with more than 15 liters per second in the plain, is acceptable.
