The effect of pH and natural microbial phosphatase activity on the speciation of uranium in subsurface soils

被引:67
作者
Beazley, Melanie J. [1 ]
Martinez, Robert J. [2 ]
Webb, Samuel M. [3 ]
Sobecky, Patricia A. [2 ]
Taillefert, Martial [1 ]
机构
[1] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
[2] Univ Alabama, Dept Biol Sci, Tuscaloosa, AL 35487 USA
[3] Stanford Synchrotron Radiat Lightsource, Menlo Pk, CA 94025 USA
基金
美国国家卫生研究院;
关键词
HIGHLY CONTAMINATED AQUIFER; SURFACE COMPLEXATION MODEL; METAL-REDUCING BACTERIUM; IN-SITU BIOREDUCTION; GOETHITE-COATED SAND; MULTIPLE-SCATTERING; CITROBACTER SP; SHEWANELLA-PUTREFACIENS; ALKALINE-PHOSPHATASE; U(VI) REDUCTION;
D O I
10.1016/j.gca.2011.07.006
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The biomineralization of U(VI) phosphate as a result of microbial phosphatase activity is a promising new bioremediation approach to immobilize uranium in both aerobic and anaerobic conditions. In contrast to reduced uranium minerals such as uraninite, uranium phosphate precipitates are not susceptible to changes in oxidation conditions and may represent a long-term sink for uranium in contaminated environments. So far, the biomineralization of U(VI) phosphate has been demonstrated with pure cultures only. In this study, two uranium contaminated soils from the Department of Energy Oak Ridge Field Research Center (ORFRC) were amended with glycerol phosphate as model organophosphate source in small flow-through columns under aerobic conditions to determine whether natural phosphatase activity of indigenous soil bacteria was able to promote the precipitation of uranium(VI) at pH 5.5 and 7.0. High concentrations of phosphate (1-3 mM) were detected in the effluent of these columns at both pH compared to control columns amended with U(VI) only, suggesting that phosphatase-liberating microorganisms were readily stimulated by the organophosphate substrate. Net phosphate production rates were higher in the low pH soil (0.73 +/- 0.17 mM d(-1)) compared to the circumneutral pH soil (0.43 +/- 0.31 mM d(-1)), suggesting that non-specific acid phosphatase activity was expressed constitutively in these soils. A sequential solid-phase extraction scheme and X-ray absorption spectroscopy measurements were combined to demonstrate that U(VI) was primarily precipitated as uranyl phosphate minerals at low pH, whereas it was mainly adsorbed to iron oxides and partially precipitated as uranyl phosphate at circumneutral pH. These findings suggest that, in the presence of organophosphates, microbial phosphatase activity can contribute to uranium immobilization in both low and circumneutral pH soils through the formation of stable uranyl phosphate minerals. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:5648 / 5663
页数:16
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