Reactive Transport of U and V from Abandoned Uranium Mine Wastes.
Reactive Transport of U and V from Abandoned Uranium Mine Wastes.
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DOI:
10.1021/acs.est.7b03823
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发表时间:
2017-11-07
影响因子:
11.4
通讯作者:
Cerrato JM
中科院分区:
文献类型:
--
作者:
Avasarala S;Lichtner PC;Ali AS;González-Pinzón R;Blake JM;Cerrato JM
The reactive transport of uranium (U) and vanadium(V) from abandoned mine wastes collected from the Blue Gap/Tachee Claim-28 mine site in Arizona was investigated by integrating flow-through column experiments with reactive transport modeling, and electron microscopy. The mine wastes were sequentially reacted in flow-through columns at pH 7.9 (10 mM HCO3−) and pH 3.4 (10 mM CH3COOH) to evaluate the effect of environmentally relevant conditions encountered at Blue Gap/Tachee on the release of U and V. The reaction rate constants (km) for the dissolution of uranyl–vanadate (U–V) minerals predominant at Blue Gap/Tachee were obtained from simulations with the reactive transport software, PFLOTRAN. The estimated reaction rate constants were within 1 order of magnitude for pH 7.9 (km = 4.8 × 10−13 mol cm−2 s−1) and pH 3.4 (km = 3.2 × 10−13 mol cm−2 s−1). However, the estimated equilibrium constants (Keq) for U–V bearing minerals were more than 6 orders of magnitude different for reaction at circumneutral pH (Keq = 10−38.65) compared to acidic pH (Keq = 10−44.81). These results coupled with electron microscopy data suggest that the release of U and V is affected by water pH and the crystalline structure of U–V bearing minerals. The findings from this investigation have important implications for risk exposure assessment, remediation, and resource recovery of U and V in locations where U–V-bearing minerals are abundant.
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影响因子:
11.4
作者:
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通讯作者:
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DOI:
10.1111/rssa.12099
发表时间:
2015-10-01
影响因子:
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作者:
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