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硒酸盐与重晶石共沉淀的特征及其环境意义。

Characterization and environmental implications of selenate co-precipitation with barite.

机构信息

Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada.

Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK S7N 5E2, Canada.

出版信息

Environ Res. 2020 Jul;186:109607. doi: 10.1016/j.envres.2020.109607. Epub 2020 Apr 27.

Abstract

This study investigated the sequestration of dissolved selenate (SeO) via co-precipitation in barite for a range of SeO concentrations (0-~8650 mg/L), as well as its release at near neutral pH conditions (pH = ~5.5-6.5). Solid precipitates were characterized via X-ray diffraction and subsequent Rietveld refinements, Raman spectroscopy, Brunauer-Emmett-Teller surface area analyses, scanning electron microscopy, electron probe microanalyses (EPMA), inductively coupled plasma optical emission spectroscopy (ICP-OES), and X-ray absorption spectroscopy (XAS). ICP-OES results suggested barite efficiently removed >99% of SeO from the test solutions during all co-precipitation experiments. EPMA results showed the SeO was sequestered from the aqueous phase via co-precipitation with barite. XAS analyses indicated the SeO tetrahedron is incorporated into the barite structure by substituting for sulfate (SO) and bonding to Ba atoms through bidentate mononuclear and bidentate binuclear complexes. Dissolution data showed the release of SeO sequestered in barite to the aqueous phase is unlikely due to the low solubility and stability of the barite phase. As such, co-precipitation of SeO with barite could be effective for removing SeO from waters affected by mining and metallurgical operations.

摘要

本研究考察了在重晶石中通过共沉淀将溶解的硒酸盐(SeO )固定的过程,研究了一系列 SeO 浓度(0-8650mg/L)下的固定作用,以及在接近中性 pH 值条件(pH=5.5-6.5)下的释放过程。通过 X 射线衍射和随后的 Rietveld 精修、拉曼光谱、Brunauer-Emmett-Teller 表面积分析、扫描电子显微镜、电子探针微分析(EPMA)、电感耦合等离子体发射光谱(ICP-OES)和 X 射线吸收光谱(XAS)对固体沉淀物进行了表征。ICP-OES 结果表明,在所有共沉淀实验中,重晶石有效地从测试溶液中去除了>99%的 SeO 。EPMA 结果表明,SeO 是通过与重晶石共沉淀从水相向固相转移的。XAS 分析表明,SeO 四面体通过与 Ba 原子的桥联单核和桥联双核配合物取代硫酸盐(SO )而结合到重晶石结构中。溶解数据表明,由于重晶石相的低溶解度和稳定性,SeO 被固定在重晶石中的释放到水相中的可能性不大。因此,SeO 与重晶石的共沉淀可有效去除受采矿和冶金作业影响的水中的 SeO 。

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