Environ. Sci. Technol., 37 (5), 908 -914, 2003. 10.1021/es0257927 S0013-936X(02)05792-9
Web Release Date: February 5, 2003

Copyright © 2003 American Chemical Society

Lead Sorption onto Ferrihydrite. 1. A Macroscopic and Spectroscopic Assessment

Paras Trivedi,* James A. Dyer, and Donald L. Sparks

Department of Plant and Soil Sciences, University of Delaware, Newark, Delaware 19717, and DuPont Engineering Technology, Brandywine Building, Wilmington, Delaware 19898

Received for review May 15, 2002

Revised manuscript received December 9, 2002

Accepted December 13, 2002

Abstract:

In this research, traditional macroscopic studies were complemented with XAS analyses to elucidate the mechanisms controlling Pb(II) sorption onto ferrihydrite as a function of pH, ionic strength, and adsorbate concentra tions. Analyses of XANES and XAFS studies demonstrate that Pb(II) ions predominantly sorb onto ferrihydrite via inner-sphere complexation, not retaining their primary hydration shell upon sorption. At higher pH values (pH 5.0), edge-sharing bidentate complexes are mainly formed on the oxide surface with two Fe atoms located at approximately 3.34 Å. In contrast, XAS studies on Pb(II) sorption onto ferrihydrite, at pH 4.5, reveal two distinct Pb-Fe bond average radial distances of 3.34 and 3.89 Å, suggestive of a mixture of monodentate and bidentate sorption complexes present at the oxide surface. Interestingly, at constant pH, the configuration of the sorption complex is independent of the adsorbate concentration. Hence, Pb(II) sorption to a highly disordered adsorbent such as ferrihydrite can be described by one average type of mechanism. Overall, this information will aid scientists and engineers in improving the current models that predict and manage the fate of toxic metals, such as Pb(II), in the aquatic and soil environments.


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