Environ. Sci. Technol. 1997, 31,3180-3187

²²² Rn as a Partitioning Tracer To Detect Diesel Fuel Contamination in Aquifers: Laboratory Study and Field Observations

DANIEL HUNKELER, ⁺ EDUARD HOEHN, ^{++ *} PATRICK HOEHENER, ⁺ AND JOSEF ZEYER ⁺
Swiss Federal Institute of Technology (ETH), Institute of Terrestrial Ecology, Soil Biology, CH-8952 Schlieren, Switzerland, and EAWAG, Swiss Federal Institute for Environmental Science and Technology, CH-8600 Duebendorf, Switzerland

The Use of ²²² Rn, a naturally occurring radioactive isotope, was investigated as a partitioning tracer to detect and quantify the amount of non-aqueous-phase liquids (NAPLS) in contaminated aquifers. Diesel fuel was chosen as a model NAPL. The diesel fuel-water partition coefficient for ²²² Rn was 40 ± 2.3, in bottles containing diesel fuel and water at 12° C. In water-saturated quartzsand contaminated with diesel fuel, the ²²² Rn emanating from the sand partitioned between diesel fuel and water as expected based on this partition coefficient. In a column containing uncontaminated quartz sand, the ²²² Rn activity in infiltrated water increased from <0.2 to 4.9 kBq m ^-3 , and in a subsequent column containing diesel fuel-contaminated quartz sand, the ²²² Rn activity in the water phase decreased to 3.3 kBq m ^-3 . This decrease corresponds to what has been predicted using a mathematical model. At a contaminated field site, the ²²² Rn activity of groundwater decreased by about 40% between monitoring wells upgradient of the contaminated zone and monitoring wells within the contami nated zone. On the basis of this decrease, the average diesel fuel saturation was estimated using the mathematical model. The calculated diesel fuel saturation was in the range of that found in excavated aquifer material.

* Corresponding author phone: +41-1-823-5525; fax +41-823- 5210; e-mail address: hoehn@eawag.ch.
⁺ ETH.
⁺⁺ EAWAG.