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汞-铊矿区暴露砂质泥岩风化过程中重金属的迁移特征。

Migration characteristics of heavy metals in the weathering process of exposed argillaceous sandstone in a mercury-thallium mining area.

机构信息

College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025, China.

College of Resource and Environmental Engineering, Guizhou University, Guiyang 550025, China; Guizhou Karst Environmental Ecosystem Observation and Research Station, Ministry of Education, Guizhou University, Guiyang 550025, China; Institute of Applied Ecology, Guizhou University, Guiyang 550025, Guizhou, China.

出版信息

Ecotoxicol Environ Saf. 2021 Jan 15;208:111751. doi: 10.1016/j.ecoenv.2020.111751. Epub 2020 Dec 8.

Abstract

Lanmuchang mercury-thallium mine, a typical polymetallic mine is located in southwestern Guizhou, China, is the most serious and typical area resulted from multi-metal contamination (Tl, Hg, As, and Sb). After the mercury-thallium mining, a large area of surrounding rocks such as argillaceous sandstone with high contents of Tl, Hg, As, and Sb is exposed to air. Weathering caused the argillaceous sandstone to form different weathering layers, including the grey-black external layer, the brown-yellow middle layer and the gray-white inner layer, and the external layer was enriched with higher heavy metals. However, the reason of heavy metal migration and transformation in argillaceous sandstone caused by weathering is unclear. The objective of this paper was to investigate the migration, transformation and release characteristics of Tl, Hg, As, and Sb in argillaceous sandstone during the weathering. The results indicated that weathering not only promoted an acidic oxidation environment in argillaceous sandstone, but also increased its specific surface area, pore volume and hydrophilicity, which are beneficial to the permeability of oxygen and etching liquids during the process of weathering and leaching. Meanwhile, weathering led to the transformation or decomposition of hydrophilic groups, such as -OH and -C˭O in the grey-black external layer of argillaceous sandstone, resulting in the further release of heavy metals bound to these groups. The concentration of Tl, Hg, As, and Sb in the leaching solution of argillaceous sandstone represented a positive correlation with that of Fe, Ca, Mg at different levels, indicating that Tl, Hg, As, and Sb were released with the dissolution of Fe, Ca and Mg during weathering and leaching. In summary, these results indicated that weathering caused the dissolution and migration of heavy metals in the argillaceous sandstone. Tl, Hg, As, and Sb migrated from the grey-white inner layer to the grey-black external layer and partially adsorbed by free alumina (Al), jarosite and Ca-bearing minerals, showing enrichment phenomena, partially released into the environment, causing environmental pollution.

摘要

滥木厂汞锑矿是中国西南地区一个典型的多金属矿,是受多金属污染(Tl、Hg、As 和 Sb)最严重和典型的地区。汞锑矿开采后,大量高 Tl、Hg、As 和 Sb 含量的泥质砂岩等围岩暴露于空气中。风化作用导致泥质砂岩形成不同的风化层,包括灰黑色外带、棕黄色中带和灰白色内带,外带富含更高的重金属。然而,风化作用导致泥质砂岩中重金属迁移和转化的原因尚不清楚。本文旨在研究风化过程中 Tl、Hg、As 和 Sb 在泥质砂岩中的迁移、转化和释放特征。结果表明,风化不仅促进了泥质砂岩中酸性氧化环境的形成,而且增加了其比表面积、孔体积和亲水性,有利于风化和浸出过程中氧气和蚀刻液的渗透。同时,风化导致灰黑色外带中亲水基团如-OH 和-C˭O 的转化或分解,导致与这些基团结合的重金属进一步释放。泥质砂岩浸出液中 Tl、Hg、As 和 Sb 的浓度与 Fe、Ca、Mg 的浓度呈正相关,表明在风化和浸出过程中,Tl、Hg、As 和 Sb 随 Fe、Ca 和 Mg 的溶解而释放。综上所述,这些结果表明风化导致了泥质砂岩中重金属的溶解和迁移。Tl、Hg、As 和 Sb 从灰白色内带迁移到灰黑色外带,并部分被游离氧化铝(Al)、黄钾铁矾和含钙矿物吸附,表现出富集现象,部分释放到环境中,造成环境污染。

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