The phenomena of Cs sorption in soil as well as the main factors affec
ting K-d value were investigated in this study. Ion exchange/chemical
sorption dominated the Cs sorption in soil components, and the reactio
n was found to be exothermic. Cesium could be desorbed by ion exchange
in soil, but it is not easily desorbed in deionized water. The pH ran
ge of groundwater did not affect the sorption on soil components. The
K-d value would increase slightly with a higher liquid-solid ratio. In
equilibrium, the Cs concentration in soil solution is a function of t
he liquid-solid ratio.