Publications Details
How the K(d) Approach Undermines Groundwater Cleanup
Environmental scientists have long appreciated that the distribution coefficient (the ''K{sub d}'' or ''constant K{sub d}'') approach predicts the partitioning of heavy metals between sediment and groundwater inaccurately; nonetheless, transport models applied to problems of environmental protection and groundwater remediation almost invariably employ this technique. To examine the consequences of this practice, we consider transport in one dimension of Pb and other heavy metals through an aquifer containing hydrous ferric oxide, onto which heavy metals sorb strongly. We compare the predictions of models calculated using the K{sub d} approach to those given by surface complexation theory, which is more realistic physically and chemically. The two modeling techniques give qualitatively differing results that lead to divergent cleanup strategies. The results for surface complexation theory show that water flushing is ineffective at displacing significant amounts of Pb from the sorbing surface. The effluent from such treatment contains a ''tail'' of small but significant levels of contamination that persists indefinitely. Subsurface zones of Pb contamination, furthermore, are largely immobile in flowing groundwater. These results stand in sharp contrast to the predictions of models constructed using the k{sub d} approach, yet are consistent with experience in the laboratory and field.