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典型铅锌矿流域土壤重金属累积与分布的影响因素分析
摘要点击 2824  全文点击 841  投稿时间:2022-12-27  修订日期:2023-02-04
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中文关键词  铅锌矿流域  土壤重金属  累积与分布  主控因素  全量  形态
英文关键词  lead-zinc mine watershed  soil heavy metal  accumulation and distribution  main controlling factors  total amount  fractional
作者单位E-mail
潘泳兴 桂林理工大学环境科学与工程学院, 桂林 541004 pan15277479634@163.com 
陈盟 桂林理工大学环境科学与工程学院, 桂林 541004
广西岩溶地区水污染控制与用水安全保障协同创新中心, 桂林 541004 
cattlepen@163.com 
王櫹橦 桂林理工大学地球科学学院, 桂林 541004  
中文摘要
      以桂北地区阳朔铅锌矿流域为研究对象,对其流域内表层土壤中9种重金属元素(Zn、Pb、Cd、Fe、Mn、Cu、Cr、Sb和As)的全量和形态,以及5种土壤性质指标(pH、电导率、阳离子交换量、有机质和粒径)进行分析测定.综合运用相关性分析、冗余分析(RDA)和地理探测器揭示土壤重金属累积与分布的主控因素.在土壤样本分析数据中,As、Cd、Fe、Cu、Mn、Pb和Zn含量平均值均超过背景值,其中Cd、Mn、Pb和Zn分别是背景值的4.01、3.15、5.53和9.72倍,表明其在表层土壤中明显富集;在分布上具有较为明显的空间差异,在冲洪积扇堆积区(1~6号)高于其他区域(7~9号).Pb和Mn可利用态占比(K)分别为48.8%和57.2%,生物可利用性较大,潜在迁移能力一般(PMI分别为0.015~0.068和0.036~0.082);Zn和Cu可利用态占比(K)分别为30.9%和16.8%,且中等利用态占比(Z)分别为10.9%和13.6%,有一定生物可利用性,但Zn迁移能力较强(PMI为0.160~0.203),Cu潜在迁移能力一般(PMI为0.017~0.084);Fe和Cr难利用态占比(N)均大于95%,生物可利用性较低,迁移能力弱(PMI<0.005).影响累积和分布的主控因素分析结果表明,Cr受阳离子交换量(CEC)和黏粒(clay)控制,Fe受砂粒(sand)控制,As受电导率(EC)和pH控制,Cu、Zn、Cd和Sb则主要受pH和clay控制,Pb累积的主控因素为pH和有机质(SOM),Mn的主控因素为pH.研究定量解析影响土壤重金属累积和分布的主控因素,可为土壤重金属污染防治提供科学决策依据.
英文摘要
      Taking a typical lead-zinc mining area watershed in northern Guangxi as the research object, the total amount and morphology of nine heavy metals(Zn, Pb, Cd, Fe, Mn, Cu, Cr, Sb, and As) and fine soil property indicators(pH, conductivity, cation exchange, organic matter, and particle size) in the surface soils of the Yangshuo lead-zinc mine were analyzed and determined. The accumulation and distribution of soil heavy metals and their main controlling factors were revealed using correlation, redundancy(RDA), and GeoDetector analyses. In the analytical data of soil samples, the mean values of As, Cd, Fe, Cu, Mn, Pb, and Zn exceeded the background values, in which Cd, Mn, Pb, and Zn were 4.01, 3.15, 5.53, and 9.72 times higher than the background values, respectively, indicating that they were significantly enriched in the surface soil. There were more noticeable spatial differences in distribution, which were higher in the alluvial floodplain accumulation area(1-6) than those in the other areas(7-9). The available states(K) of Pb and Mn were 48.8% and 57.2%, respectively, with high bioavailability and average potential migration capacity(PMI 0.015-0.068 and 0.036-0.082, respectively). The Zn and Cu had some bioavailability degree, with available states(K) of 30.9% and 16.8% and moderately available states of 10.9% and 13.6%, respectively. The difference was that Zn had a strong migration capacity(PMI 0.160-0.203), and Cu had an average potential migration capacity(PMI 0.017-0.084). Fe and Cr had a difficult-to-use state(N)>95%, low bioavailability, and weak migration capacity(PMI<0.005). The results of the analysis of the main controlling factors affecting accumulation and distribution showed that Cr was controlled by cation exchange capacity(CEC) and clay; Fe was controlled by sand; As was controlled by electrical conductivity(EC) and pH; Cu, Zn, Cd, and Sb were controlled by pH and clay; Pb accumulation was controlled by pH and soil organic matter(SOM); Mn was controlled by pH. This study quantified the main controlling factors affecting the accumulation and distribution of soil heavy metals, which can provide a scientific basis for decision making in the prevention and control of soil heavy metal pollution.

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