Investigation of unsaturated water flow in a deep vadose zone by applying quasi-partition law to 222Rn

This paper describes an application of the quasi-partition law of radon-222 (222Rn) to a deep unsaturated vadose zone in a field. 222Rn is a very useful tracer to investigate not only saturated but also unsaturated water flows in vadose zones. Concentrations of 222Rn in water in unsaturated soils are, based on the quasi-partition law, lower than those in saturated soils. However, no study has previously applied quasi-partition law of 222Rn to analyze saturated and unsaturated water flows in vadose zones. In this study, we observed the applicability of existing theoretical equations of quasi-partition law of 222Rn experimentally. After confirming the validity of the theoretical equation, we applied this equation to estimate the unsaturated water flow in an actual vadose zone. By comparing the estimated degree of saturation from 222Rn measurement with that from a neutron moisture meter measurement, we obtained a beautiful agreement between them.