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Soil electrical conductivity (EC a ) by the four electrode method was studied in the laboratory as a function of soil water electrical conductivity (EC w ) and water content in six soil types. A linear relationship between EC a and EC w was valid only at salinities > 4 mmho/cm. At very low salinity levels the contribution of the surface conductance was not constant and had a higher contribution than EC w to measured EC a . A method for calculating the partial contribution of surface conductance to EC a as a function of EC w and clay content is applied including a correction for dependence on the soil water content.
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Nadler et al. (1980) studied this question.
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