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ORIGINAL RESEARCH

Radon-222 as a Tracer for Nonaqueous Phase Liquid in the Vadose Zone

Experiments and Analytical Model

^a Swiss Federal Institute of Technology (EPFL), ENAC-ISTE-LPE, CH-1015 Lausanne, Switzerland
^b University of Neuchâtel, Center for Hydrogeology (CHYN), Rue Emile Argand 11, CH-2007 Neuchâtel, Switzerland
^* Corresponding author: (patrick.hoehener{at}epfl.ch)

Received 20 November 2003.

The potential use of the naturally occurring noble gas ²²²Rn 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 unsaturated alluvial sand, a 2.9-fold decrease of the steady-state ²²²Rn 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 ²²²Rn 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 ²²²Rn activity depth profile. An outdoor lysimeter experiment was performed using unsaturated 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 ²²²Rn profile, as predicted also by model calculations. We concluded that ²²²Rn can be used as a NAPL tracer in the vadose zone only at heavily polluted sites with uniform spatial ²²²Rn production.

Abbreviations: NAPL, nonaqueous phase liquid • TDR, time domain reflectometry • VOC, volatile organic compound