Web Release Date: February 5,
Lead Sorption onto Ferrihydrite. 1. A Macroscopic and Spectroscopic Assessment

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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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