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在大型原位现场试验中进行亚硒酸盐的生物还原。

Selenate bioreduction in a large in situ field trial.

机构信息

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

Enviromin, Inc., 524 Professional Drive, Bozeman, MT 59715, USA.

出版信息

Sci Total Environ. 2024 Jul 10;933:172869. doi: 10.1016/j.scitotenv.2024.172869. Epub 2024 Apr 30.

DOI:10.1016/j.scitotenv.2024.172869
PMID:38697548
Abstract

Removing selenium (Se) from mine effluent is a common challenge. A long-term, in situ experiment was conducted to bioremediate large volumes (up to 7500 m d) of Se(VI)-contaminated water (mean 87 μg L) by injecting the water into a saturated waste rock fill (SRF) at a coal mining operation in Elk Valley, British Columbia, Canada. To stimulate/maintain biofilm growth in the SRF, labile organic carbon (methanol) and nutrients were added to the water prior to its injection. A conservative tracer (Br) was also added to track the migration of injected water across the SRF, identify wells with minimal dilution and used to quantify the extent of bioreduction. The evolution of the Se species through the SRF was monitored in time and space for 201 d. Selenium concentrations of <3.8 μg L were attained in monitoring wells located 38 m from the injection wells after 114 to 141 d of operation. Concentrations of Se species in water samples from complementary long-term (351-498 d) column experiments using influent Se(VI) concentrations of 1.0 mg L were consistent with the results of the in situ experiment. Solid samples collected at the completion of the column experiments confirmed the presence of indigenous Se-reducing bacteria and that the sequestered Se was present as insoluble Se(0), likely in Se-S ring compounds. Based on the success of this ongoing bioremediation experiment, this technology is being applied at other mine sites.

摘要

从矿山废水中去除硒 (Se) 是一个常见的挑战。在加拿大不列颠哥伦比亚省埃尔克山谷的一个采煤作业中,进行了一项长期的原位实验,通过将受 Se(VI) 污染的水(平均 87μg/L)注入饱和废石填充层(SRF)来修复大量(高达 7500 m d)的 Se(VI)-污染水。为了刺激/维持 SRF 中的生物膜生长,在注入水之前向水中添加了易生物降解的有机碳(甲醇)和营养物质。还添加了一种保守示踪剂(Br)来追踪注入水在 SRF 中的迁移,识别稀释最小的井,并用于量化生物还原的程度。在 201 天的时间内,监测了 Se 物种在 SRF 中的时空演化。在运行 114 至 141 天后,距注入井 38 米的监测井中,硒浓度达到 <3.8μg/L。使用 1.0mg/L 的 Se(VI) 进水浓度进行的补充长期(351-498d)柱实验的水样中 Se 物种浓度与原位实验结果一致。在柱实验完成时收集的固体样品证实了存在土著 Se 还原细菌,并且被固定的 Se 以不溶性 Se(0) 的形式存在,可能是在 Se-S 环化合物中。基于这项正在进行的生物修复实验的成功,该技术正在其他矿山场地应用。

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