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ISRN Soil Science
Saturated hydraulic conductivity (Ks), among other soil hydraulic properties, is important and necessary in water and mass transport models and irrigation and drainage studies. Although this property can be measured directly, its measurement is difficult and very variable in space and time. Thus pedotransfer functions (PTFs) provide an alternative way to predict the Ks from easily available soil data. This study was done to predict the Ks in Khuzestan province, southwest Iran. Threedoi:10.1155/2013/308159 fatcat:f2smyjmhxfaqpnrgg52kuwtiva