Radon-222 as a tracer for nonaqueous phase liquid in the vadose zone:: Experiments and analytical model

The potential use of the naturally occurring noble gas Rn-222 as a tracer for vadose zone contamination by nonaqueous phase liquids (NAPLs) is studied experimentally and theoretically. n-Dodecane was chosen as the model NAPL. In batch experiments containing alluvial sand, a 2.9-fold decrease of the steady-state Rn-222 activity in soil gas was measured as a consequence of the increase in the volumetric NAPL content from 0 to 0.074. A one-dimensional analytical reactive transport model was developed that includes Rn-222 production, gas-phase diffusion, partitioning, and radioactive decay. Radon-222 soil gas profiles were predicted for homogeneous and heterogeneous sandy profiles where NAPL contamination was restricted to selected depth layers. The resulting depth profiles document that the position of the NAPL has great influence on the Rn-222 activity depth profile. An outdoor lysimeter experiment was performed using alluvial sand contaminated by NAPL at depths from 1 to 1.2 m. In the lysimeter experiment, a spill of 2 L m(-2) NAPL did not alter significantly the Rn-222 profile, as predicted also by model We concluded that Rn-222 can be used as a NAPL tracer in the vadose zone only at heavily polluted sites with uniform spatial Rn-222 production.