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受矿山影响的湿地沉积物中胶体相关金属迁移性的实验研究。

Experimental investigations of colloid-associated metal mobility in mine-impacted wetland sediment.

作者信息

Harper Colleen O, Amos Richard T

机构信息

Department of Earth Sciences, Carleton University, 1125 Colonel By Dr, Ottawa, ON, K1S 5B6, Canada.

出版信息

Heliyon. 2024 Dec 13;11(1):e41223. doi: 10.1016/j.heliyon.2024.e41223. eCollection 2025 Jan 15.

DOI:10.1016/j.heliyon.2024.e41223
PMID:39801966
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11719310/
Abstract

Metal mining operations can release toxic metals to surrounding environments where site-specific conditions control the movement of contaminants. Colloid-facilitated transport, the transport of contaminants with small, mobile particles, has been recognized as a potential contaminant transport vector in groundwater, but it remains unclear under what conditions it is important and whether neutral, metal-rich mine drainage from legacy mining impacts this transport vector. This work presents a set of laboratory column experiments that study the effect of colloids on metal mobility in saturated, wetland sediment that has been receiving neutral mine drainage for nearly a century, using mixed and single metal input solutions at neutral pH. Results indicate that colloid-facilitated transport is only important when small (<0.01 μm) colloids, most likely formed from organic matter, are present. Larger particles were found to be generally immobile, so could aid in the immobilization of metal contaminants. These findings imply that colloid-facilitated transport is an important transport vector in mine-impacted wetland sediment and should be considered when remediating mine sites.

摘要

金属采矿作业会将有毒金属释放到周围环境中,而特定场地条件会控制污染物的迁移。胶体促进迁移,即污染物随小的可移动颗粒迁移,已被认为是地下水中一种潜在的污染物迁移载体,但目前尚不清楚在何种条件下它很重要,以及来自遗留采矿的中性、富含金属的矿井排水是否会影响这种迁移载体。这项工作展示了一组实验室柱实验,研究了胶体对饱和湿地沉积物中金属迁移率的影响,该湿地沉积物近一个世纪以来一直接收中性矿井排水,实验使用了中性pH值的混合和单一金属输入溶液。结果表明,只有当存在可能由有机物形成的小(<0.01μm)胶体时,胶体促进迁移才很重要。发现较大颗粒通常是不可移动的,因此有助于固定金属污染物。这些发现表明,胶体促进迁移是受采矿影响的湿地沉积物中的一种重要迁移载体,在修复矿场时应予以考虑。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/5e67ccdeca0c/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/6e31db757ecb/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/d94b0a738340/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/1fe372d99bf5/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/4cecf3bbf0df/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/b4f7609b4f14/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/62f17bca8de4/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/5e67ccdeca0c/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/6e31db757ecb/ga1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/d94b0a738340/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/1fe372d99bf5/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/4cecf3bbf0df/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/b4f7609b4f14/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/62f17bca8de4/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28f6/11719310/5e67ccdeca0c/gr6.jpg

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