Using Zn isotopes to trace Zn sources and migration pathways in paddy soils around mining area

被引:44
作者
Liu, Yuhui [1 ,2 ]
Gao, Ting [1 ,2 ,3 ]
Xia, Yafei [1 ,2 ]
Wang, Zhengrong [4 ]
Liu, Chengshuai [1 ,3 ]
Li, Shehong [1 ]
Wu, Qiqi [3 ]
Qi, Meng [1 ,2 ]
Lv, Yiwen [3 ]
机构
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550081, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Guangdong Acad Sci, Nat Reg Joint Engn Res Ctr Soil Pollut Control &, Guangdong Key Lab Integrated Agroenvironm Pollut, Guangdong Inst Ecoenvironm Sci & Technol, Guangzhou 510650, Peoples R China
[4] CUNY, City Coll New York, Dept Earth & Atmospher Sci, New York, NY 10031 USA
基金
中国国家自然科学基金;
关键词
Heavy metal pollution; Zn isotopes; Migration processes; Fe-bearing minerals; Paddy soil; HEAVY-METAL POLLUTION; ACID-MINE DRAINAGE; DABAOSHAN MINE; SEQUENTIAL EXTRACTION; GUANGDONG PROVINCE; ZINC; FRACTIONATION; CHINA; CONTAMINATION; LEAD;
D O I
10.1016/j.envpol.2020.115616
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Paddy soils around mining areas suffer from the great threat of heavy metal pollution. The traditional source-tracing methods based on metal concentrations limit our ability to quantify the sources of heavy metals and trace their transport processes to paddy soils. In this study, Zn isotope compositions of paddy soils in Dabaoshan mine area, a typical sulfide deposit in southern China, have been systematically studied. According to a plot between 1/Zn (i.e. inverse concentration) and delta Zn-66 value, all the polluted paddy soils fall on the mixing line between acid mine drainage precipitate (AMD-precipitate) and fertilizer while the unpolluted paddy soil falls on the mixing line between fertilizer and bedrock. This indicates the mixing of Zn sources at least three end-members: the mining end-member (i.e. AMD-precipitate), the agricultural end-member (i.e. fertilizer), and bedrock whose geochemical signature is often overprinted by the former two sources around the mining area. The quantitative calculations to apportion the end-member's contributions show that the mining activity contributes most Zn in the paddy soils with an average of similar to 66.2%. The contribution of mining activities has significant spatial variations. Specifically, the mining activities have relatively low impacts on the lower reach and the deep soil. Additionally, the apparent Zn isotope fractionation between AMD and AMD-precipitate (Delta Zn-66(AMD-precipitate) - (AMD) of -0.35 to -0.08 parts per thousand) in the tailings dam suggests that Zn cations in AMD coprecipitated with the secondary Fe-bearing minerals (e.g. jarosite and goethite). After being discharged from the tailings dam, Zn is mainly carried by the Fe-oxide minerals and migrated during surface runoff. Our study highlights the contribution of human activities to the Zn pollution in the paddy soils and the key role of Fe-bearing minerals in the migration of Zn. These findings provide a scientific base for the development of policy for pollution control in mining-affected region. (C) 2020 Elsevier Ltd. All rights reserved.
引用
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页数:12
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