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离子型稀土矿区及周边土壤中稀土、重金属元素的地球化学特征
引用本文:徐春丽,刘斯文,魏吉鑫,黄园英,马嘉宝,曾普胜,李旭光.离子型稀土矿区及周边土壤中稀土、重金属元素的地球化学特征[J].矿产保护与利用,2021,41(4):1-11.
作者姓名:徐春丽  刘斯文  魏吉鑫  黄园英  马嘉宝  曾普胜  李旭光
作者单位:1.国家地质实验测试中心, 北京 100037
基金项目:中国地质调查局地质调查项目(DD20190703)
摘    要:20世纪60年代末中国离子型稀土矿在江西赣州首次发现并开采,在长期开采过程中对矿区及周边水土的生态环境问题产生了持续影响,本文选择赣南足洞离子型稀土矿及其周边地区进行了系统的土壤地球化学调查和风险评价。结果表明,土壤中重稀土含量明显高于轻稀土,其中Y含量是全国背景值(22.90 μg/g)的7.2倍,占比最高;地累积指数评价Igeo均值显示HREE和Sm分别有77.44%和99.55%为无污染至中等污染,95.92%的LREE为无污染;重金属除Pb处于轻度-中等污染水平外,As、Cd、Cr、Cu、Hg、Zn、Ni元素均为无污染,与农用地污染风险筛选值相比,样品中重金属的超标率为7.35%,区内土壤重金属生态风险低。统计结果显示稀土含量与重金属污染具有较好的相关性,花岗岩风化壳地质背景对稀土、重金属Pb的控制占主导地位,意味着重稀土含量越高,Pb污染可能越大,因此,在矿山土壤修复中需重视Pb元素的地球化学特征与分布,采用合理的修复技术和手段。 

关 键 词:离子型稀土矿    重金属    地累积指数    赣州    地球化学特征
收稿时间:2021-07-02

Geochemical Characteristics of Rare Earth and Heavy Metal Elements in Ion-type Rare Earth Mining Area and Surrounding Soil
XU Chunli,LIU Siwen,WEI Jixin,HUANG Yuanying,MA Jiabao,ZENG Pusheng,LI Xuguang.Geochemical Characteristics of Rare Earth and Heavy Metal Elements in Ion-type Rare Earth Mining Area and Surrounding Soil[J].Conservation and Utilization of Mineral Resources,2021,41(4):1-11.
Authors:XU Chunli  LIU Siwen  WEI Jixin  HUANG Yuanying  MA Jiabao  ZENG Pusheng  LI Xuguang
Affiliation:1.National Research Center for Geoanalysis, Beijing 100037, China2.China University of Geosciences(Beijing), Beijing 100083, China3.Key Laboratory of Ministry of Natural Resources for Eco-geochemistry, Beijing 100037, China4.Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, Liaoning, China
Abstract:In the late 1960s, China's ion-type rare earth ore was first discovered and mined in Ganzhou, Jiangxi Province. In the long-term mining process, it has a continuous impact on the ecological environment of the mining area and the surrounding water and soil. In this paper, the soil geochemical survey and risk assessment of the ion-type rare earth ore in Southern Jiangxi Province and its surrounding areas were carried out.The results showed that the content of heavy rare earth in soil was significantly higher than that of light rare earth, and the content of Y was 7.2 times of the national background value (22.90 μg/g), accounting for the highest proportion.The Igeo mean of geo-accumulation index evaluation showed that 77.44% of HREE and 99.55% of Sm were non-pollution to medium pollution, and 95.92% of LREE was non-pollution.Except for Pb at mild to moderate pollution levels, As, Cd, Cr, Cu, Hg, Zn and Ni were all non-polluting. Compared with the pollution risk screening value of agricultural land, the exceeding rate of heavy metals in the samples was 7.35%, and the ecological risk of heavy metals in the soil was low.The statistical results show that there is a good correlation between rare earth content and heavy metal pollution. The geological background of granite weathering crust dominates the control of rare earth and heavy metal Pb, which means that the higher the content of heavy rare earth is, the greater the Pb pollution may be. Therefore, it is necessary to pay attention to the geochemical characteristics and distribution of Pb elements in mine soil remediation, and adopt reasonable remediation technologies and means. 
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