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定量源解析揭示了历史汞矿区周边农田土壤中潜在有毒元素的强降雨洪水和大气沉降的主要贡献。

Dominant roles of torrential floods and atmospheric deposition revealed by quantitative source apportionment of potentially toxic elements in agricultural soils around a historical mercury mine, Southwest China.

机构信息

CAS Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China; University of Chinese Academy of Sciences, Beijing 100049, China.

CAS Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.

出版信息

Ecotoxicol Environ Saf. 2022 Sep 1;242:113854. doi: 10.1016/j.ecoenv.2022.113854. Epub 2022 Jul 8.

Abstract

Hg pollution in soils surrounding the Wanshan mercury mine (WMM), once the largest Hg-producing center in China, has been confirmed, neglecting other potential toxic elements (PTEs). Better understanding of the sources and transport pathways of soil PTEs remains insufficient. To response these limitations, eight soil PTEs (As, Cd, Cr, Cu, Hg, Ni, Pb and Zn) at two typical agricultural sites, namely AZ and WW that are located near and far from the WMM, respectively, were systemically investigated. The results showed that AZ exhibited significantly higher concentrations of all the PTEs in the surface soil than WW (p < 0.01). Hg and Cd were recognized as the priority control PTEs, with their average concentrations of 21.54 and 1.21 mg kg at AZ, and 15.79 and 0.48 mg kg at WW. Those affected PTEs tended to enrich in near-river areas. Atmospheric deposition contributed more to soil Hg than did regular irrigation, but these two sources could not explain the considerable soil Hg accumulation. Three sources, including natural sources, hydraulic transport (torrential floods and regular irrigation) and atmospheric deposition, were identified and quantified based on the positive matrix factorization model, statistical methods and various auxiliary information. Hydraulic transport (mainly torrential floods) dominated the soil Hg input, which could explain 83.8% and 69.8% of the soil Hg input at AZ and WW, respectively. Atmospheric deposition dominated the soil Cd input, explaining 44.3% and 59.9% of the soil Cd input at AZ and WW, respectively. More attention should be given to the safe utilization of agricultural land and long-term monitoring of atmospheric deposition of Hg and Cd. This study could provide insights to prevent PTE diffusion along the above dominant transportation pathways while developing similar mine regions.

摘要

万山汞矿(WMM)周围土壤中的汞污染已得到确认,但其他潜在有毒元素(PTEs)却被忽视了。对于土壤 PTEs 的来源和迁移途径的了解仍然不足。为了应对这些限制,在距离 WMM 较近的 AZ 和较远的 WW 两个典型农业区系统地调查了 8 种土壤 PTEs(As、Cd、Cr、Cu、Hg、Ni、Pb 和 Zn)。结果表明,AZ 表层土壤中所有 PTEs 的浓度均显著高于 WW(p<0.01)。Hg 和 Cd 被认为是优先控制的 PTEs,其在 AZ 的平均浓度分别为 21.54 和 1.21mgkg,在 WW 的平均浓度分别为 15.79 和 0.48mgkg。受影响的 PTEs 倾向于在河流附近地区富集。大气沉降对土壤 Hg 的贡献大于常规灌溉,但这两个来源并不能解释土壤 Hg 的大量积累。基于正矩阵因子分解模型、统计方法和各种辅助信息,确定并量化了包括自然源、水力传输(暴雨和常规灌溉)和大气沉降在内的三个来源。水力传输(主要是暴雨)主导着土壤 Hg 的输入,分别解释了 AZ 和 WW 土壤 Hg 输入的 83.8%和 69.8%。大气沉降主导着土壤 Cd 的输入,分别解释了 AZ 和 WW 土壤 Cd 输入的 44.3%和 59.9%。应更加关注农业用地的安全利用和大气沉降中 Hg 和 Cd 的长期监测。本研究可为防止 PTEs 沿上述主要传输途径扩散提供参考,同时为开发类似的矿区提供参考。

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