GEOC 28 |
| Iron and phosphate are known to interact strongly in the environment. However, the incorporation of phosphate ions during the oxidation of Fe(II) has received very little attention. In our study, ferrous ions were oxidized at pH 6.0 in the presence of an excess of dissolved oxygen and increasing quantities of phosphate. The resulting precipitates were characterized by TEM, SEM, XRD, IR spectroscopy, Mössbauer spectroscopy, EXAFS, and chemical analyses. The kinetics and the stoichiometry of oxidation were also measured. Chemical analyses revealed that virtually all the phosphorus introduced was adsorbed in the precipitates up to an introduced P/Fe elemental ratio of 0.6-0.7. In the presence of an excess of phosphate, the maximal P/Fe ratio of the precipitates was found to be equal to about 0.86 ± 0.02. The properties of the precipitates, as obtained from the various techniques used, will be presented. We are now examining the reduction of these iron phosphates by bacteria. |
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Physical Chemistry of Soil and Aquifer Systems: A Symposium in Honor of Garrison Sposito
1:30 PM-5:10 PM, Sunday, 10 September 2006 Moscone Center -- Room 256, Oral
Division of Geochemistry |