Use of electrical conductivity to estimate effects of competing ions on radionuclide distribution coefficients

The distribution coefficient (K _d) between the soil solid phase and the liquid phase is a commonly used parameter to evaluate radionuclide behavior in soil. For reliable evaluation, the variability of the K _ddue to changes of environmental conditions should be clarified. In the present study, applicability of electrical conductivity (EC) to estimate effects of competing ions on K _dwas examined in batch experiments. The K _dof five radionuclides (⁶⁰Co, ⁵⁴Mn, ⁸⁵Sr, ¹³⁷Cs, ⁶⁵Zn) were found to be in inverse proportion to the supernatant EC. The K _dof ⁶⁰Co and ⁵⁴Mn were increasing at 7 days and no stable K _dcould be determined. For ⁸⁵Sr, ¹³⁷Cs, and ⁶³Zn, the regression equations obtained between the K _dof the equilibrium state and the supernatant EC were validated in another experiment; it is expected that their K _ds can be determined accurately using the EC. Because of its simplicity in measurements, using EC should be very practical for estimating effects of competing ions on K _dof selected radionuclides.