Solubility product of chromate analogue of hydrogarnet (Ca3Al2[CrO4]0.12[O4H4]2.88(s)) at 25 °C

被引:1
|
作者
Bhattacharya, Mainak [1 ,2 ,3 ]
Bandyopadhyay, Tathagata [1 ,2 ,4 ]
Shriwastav, Amritanshu [1 ,2 ,5 ]
Mohapatra, Ashwini Kumar [1 ,2 ]
Singh, Abhas [1 ,2 ]
机构
[1] Indian Inst Technol Kanpur, Dept Civil Engn, Kanpur 208016, Uttar Pradesh, India
[2] Indian Inst Technol Kanpur, Ctr Environm Sci & Engn, Environm Geochem Lab, Kanpur 208016, Uttar Pradesh, India
[3] Indian Inst Technol Delhi, Civil Engn Dept, New Delhi 110016, India
[4] ERM India Pvt Ltd, Ahmadabad 380054, Gujarat, India
[5] Indian Inst Technol, Environm Sci & Engn Dept, Mumbai 400076, Maharashtra, India
关键词
Chromium hydrogarnet; Solubility product; COPR; Dissolution; Precipitation; ORE PROCESSING RESIDUE; CEMENT; CR(VI); PH; 180-DEGREES-C; GROUNDWATER; SPECIATION; PHASES; MODEL; WATER;
D O I
10.1016/j.apgeochem.2023.105805
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
Chromium (Cr)-hydrogarnet (Ca3Al2 [CrO4](0.12)[O4H4](2.88(s))) is a critical host of hexavalent chromium [Cr(VI)] in cementitious and alkaline solids such as chromium ore processing residue (COPR). Leaching from COPR often results in Cr(VI) contamination of soil and groundwater. Although Cr-hydrogarnet has been synthesized and characterized previously, its solubility product (K-sp) is poorly constrained. Accurate determination of this thermodynamic parameter is critical to quantify the extent of Cr(VI) dissolution from COPR in water. In this contribution, the K-sp of Cr-hydrogarnet was determined by (i) hydrothermal synthesis of the solid at 150 degrees C in alkaline conditions in two batches; and (ii) batch equilibration experiments over 745 d from undersaturation and over 60 d from supersaturation. For each synthesized batch of solids, Cr-hydrogarnet solubility in ultrapure water at 25 degrees C in triplicate reactors was measured. Time-dependent aqueous samples were collected, and concentrations of Cr(VI) and co-solutes and pH were measured until a steady state was attained from undersaturation, after which the state was perturbed by the addition of 7x Cr(VI) to trigger the supersaturation experiment. X-ray diffraction and SEM-EDS analyses on the reacted solids confirmed the presence of Cr-hydrogarnet and its constituent elements, respectively. In addition, calcite and aluminum oxyhydroxides were formed as minor secondary phases. The log ion activity products at steady states attained from undersaturation and supersaturation were 72.36 +/- 0.86 and 72.75 +/- 0.14, respectively. A mean log K-sp of 72.55 +/- 0.87 at 25 degrees C for the reaction Ca3Al2 [CrO4](0.12)[O4H4](2.88(s)) + 11.52H(+) <-> 3Ca(2+) + 2Al(3+) + 0.12CrO(4)(2-) + 11.52H(2)O was proposed. Furthermore, the new thermodynamic constant was used to analyze data from two previous COPR equilibration studies in water and identify the governing mechanisms of Cr(VI) release.
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页数:11
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