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If rapid leaching does occur, the reduced concentration of carbofiiran at 1 to 5ftdepths implies the stability of carbofiiran is lower below the surface than at the surface. Because of the effects of wind and sun, the surface sand has a lower moisture content than that below 1 ft. This higher moisture content at depth encourages hydrolysis and may support a unique coastal-marine microbial consortium effective at degrading carbofiiran. The lack of significant contamination below the surface also suggests that there is not a buried source continuously releasing carbofiiran to the site as has been previously speculated (1,2).
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