Arsenic and iron speciation in uranium mine tailings using X-ray absorption spectroscopy

被引:32
|
作者
Essilfie-Dughan, Joseph [1 ]
Hendry, M. Jim [1 ]
Warner, Jeff [2 ]
Kotzer, Tom [1 ,3 ]
机构
[1] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada
[2] Univ Saskatchewan, Canadian Light Source Inc, Saskatoon, SK S7N 0X4, Canada
[3] Cameco Corp, Saskatoon, SK S7M 1J3, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
MINERALOGICAL CHARACTERIZATION; 2-LINE FERRIHYDRITE; MILL TAILINGS; FE; GEOCHEMISTRY; CHEMISTRY; EXAFS; PH; TRANSFORMATION; SASKATCHEWAN;
D O I
10.1016/j.apgeochem.2012.10.022
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
In northern Saskatchewan, Canada, high-grade U ores and the resulting tailings can contain high levels of As. An environmental concern in the U mining industry is the long-term stability of As within tailings management facilities (TMFs) and its potential transfer to the surrounding groundwater. To mitigate this problem, U mill effluents are neutralized with lime to reduce the aqueous concentration of As. This results in the formation of predominantly Fe3+-As5+ secondary mineral phases, which act as solubility controls on the As in the tailings discharged to the TMF. Because the speciation of As in natural systems is critical for determining its long-term environmental fate, characterization of As-bearing mineral phases and complexes within the deposited tailings is required to evaluate its potential transformation, solubility, and long-term stability within the tailings mass. In this study, synchrotron-based bulk X-ray absorption spectroscopy (XAS) was used to study the speciation of As and Fe in mine tailings samples obtained from the Deilmann TMF at Key Lake, Saskatchewan. Comparisons of K-edge X-ray absorption spectra of tailings samples and reference compounds indicate the dominant oxidation states of As and Fe in the mine tailings samples are +5 and +3, respectively, largely reflecting their generation in a highly oxic mill process, deposition in an oxidized environment, and complexation within stable oxic phases. Linear combination fit analyses of the K-edges for the Fe X-ray absorption near edge spectra (XANES) to reference compounds suggest Fe is predominantly present as ferrihydrite with some amount of the primary minerals pyrite (8-15% in some samples) and chalcopyrite (5-15% in some samples). Extended Xray absorption fine structure (EXAFS) analysis of As K-edge spectra indicates that As5+ (arsenate) present in tailings samples is adsorbed to the ferrihydrite though an inner-sphere bidentate linkage. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:11 / 18
页数:8
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