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ABSTRACT
A procedure is developed to calculate the ratio between electrical conductivity (EC) solution (ECw) and EC of bulk soil (ECa) as a function of soil water content (
). This ratio, (F), changing nonlinearly with
, is used to calculate soil solution salinity from measurements of bulk soil electrical conductivity. Obtaining F-
relationships for intermediate and low soil moisture levels by an accurate theoretical model is impractical due to the complicated interdependence of several solid- and liquid-phase parameters. Therefore an empirical approach was adopted to obtain the complete F-
relationship by superimposing the complete suction-water retention relationship on two F-
measurements at the same
values. The experimentally determined F-
curve overlaps the theoretically calculated F-
relationship at high soil water contents and the empirically obtained F-
relationship at low soil water content. Examples are given for several soil types.
1 Contribution no. 245-E, 1980 series, from the Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel.
2 Soil Chemist, Division of Soil Physics.
Received for publication January 12, 1981. Accepted for publication March 15, 1982.
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