Iron and sulfur mineral analysis methods for natural attenuation assessments

Based on electron acceptor abundance, Fe³⁺ and SO₄^2- reduction by bacteria may play a dominant role in intrinsic bioremediation of some organic contaminants in the subsurface. Both Fe³⁺ and SO₄^2- reduction processes involve mineral phases and may not be properly understood by evaluating only groundwater concentrations. Fe and S mineral analyses should be incorporated in natural attenuation studies; however, inherent problems with sample collection and analysis have discouraged such efforts. Methods are presented here for (1) sediment collection and anoxic preservation, (2) evaluation of biologically available Fe³⁺ and biogenically produced Fe²⁺ minerals, and (3) a simplified extended mineral sulfide analysis for ∼FeS and S°+FeS₂. These techniques are demonstrated to evaluate Fe³⁺ and SO₄^2- reduction at three sites where the soil or aquifer matrix had been contaminated with gasoline fuel, methane gas, or landfill leachate. It is expected that these techniques will permit Fe and S mineral analyses to become a routine part of natural attenuation assessments.