欢迎访问《生态学杂志》官方网站,今天是 分享到:

生态学杂志 ›› 2025, Vol. 44 ›› Issue (10): 3436-3446.doi: 10.13292/j.1000-4890.202510.032

• 研究报告 • 上一篇    下一篇

地质背景制约西南喀斯特地区土壤重金属空间分布及生态风险:以兴义市西南地区三个乡镇为例

吴义昭1,汪花2,王世杰2,刘秀明2*   

  1. 1中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳 550081; 2中国科学院大学, 北京 100049; 3中国科学院普定喀斯特生态系统观测研究站, 贵州普定 562100)
  • 出版日期:2025-10-10 发布日期:2025-10-14

The spatial distribution and ecological risk of soil heavy metals in southwest China karst region constrained by geological background: A case of three townships in the southwest of Xinyi City, Guizhou Province.

WU Yizhao1, WANG Hua2, WANG Shijie2, LIU Xiuming2*   

  1. (1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3Puding Karst Ecosystem Observation and Research Station, Chinese Academy of Sciences, Puding 562100, Guizhou, China).

  • Online:2025-10-10 Published:2025-10-14

摘要: 为探究不同地质背景下土壤重金属含量、空间分布特征及生态风险状况,本文选择贵州兴义市具有土壤重金属高背景值的3个乡镇作为研究区域,并将其分为3个地质背景区(碳酸盐岩区、碳酸盐岩夹碎屑岩区和碎屑岩区)。基于187个土壤样品,分析不同地质背景区土壤重金属As、Cd、Cr、Cu、Ni、Pb、Zn的含量、空间分布特征,采用污染指数法和潜在生态风险指数法对不同地质背景区土壤污染水平、生态风险进行评价。结果显示:(1)与贵州省土壤背景值相比,碳酸盐岩地区7种重金属均显示富集,尤其As和Cd富集最为显著;碳酸盐岩夹碎屑岩区除Cd和Pb贫化外,As、Cr、Cu、Ni和Zn均富集;碎屑岩地区7种土壤重金属均显示贫化。(2)土壤重金属的空间分布除了受地质背景的制约,矿区的影响亦不可忽略。As、Cd、Pb和Zn空间分布格局相似,含量显示碳酸盐岩地区>碳酸盐岩夹碎屑岩地区>碎屑岩地区,主要受地质背景差异控制;Cr、Cu和Ni分布也相似,显示碳酸盐岩夹碎屑岩地区>碳酸盐岩地区>碎屑岩地区,其空间分布主要受七舍镇西北部大际山铀多金属成矿区影响。(3)污染指数和生态风险评价显示,研究区以Cd、As为首要污染,且对3个地质背景区生态风险都有很高的贡献率,重金属污染程度和潜在生态风险均呈现碳酸盐岩地区>碳酸盐岩夹碎屑岩地区>碎屑岩地区。从空间分布看,重金属污染严重和较强以上风险区域主要分布于猪场坪镇南部的碳酸盐岩地区。


关键词: 地质高背景, 重金属污染, 分布特征, 潜在生态风险指数

Abstract: To investigate the content, spatial distribution characteristics, and ecological risk status of soil heavy metals in different geological backgrounds, we selected three townships in Xingyi City, Guizhou Province, which have high background values of soil heavy metals, as the study area, and divided them into three geological background zones (carbonatite zone, carbonatite interspersed with clastic rock zone, and clastic rock zone). We analyzed the contents and spatial distributions of soil heavy metals As, Cd, Cr, Cu, Ni, Pb, and Zn in 187 soil samples from different geological background areas. The pollution index and potential ecological risk index were used to evaluate the level of soil pollution and ecological risks. The results showed that: (1) compared with the soil background values in Guizhou Province, all seven heavy metals were enriched in the carbonatite zone, especially for As and Cd. As, Cr, Cu, Ni and Zn were enriched in the carbonatite interbedded with clastic rock zone except for the depletion of Cd and Pb. All the seven heavy metals in the soil in the clastic rock zone showed depletion. (2) The spatial distribution of soil heavy metals was constrained by the geological background as well as the mining area. The spatial distribution pattern of As, Cd, Pb and Zn was similar, with their contents showing the carbonatite zone > carbonatite interbedded with clastic rock zone > clastic zone, which was mainly controlled by geological background. The spatial distribution of Cr, Cu and Ni was also similar, showing the carbonatite with clastic rock zone > carbonatite zone > clastic zone, which was mainly affected by Daji Mountain uranium polymetallic mining area in the northwest of Qishe Town. (3) The results of pollution index and ecological risk evaluations revealed Cd and As were the primary pollutants, which had a high contribution to the ecological risk of the three geological background zones. Overall, the degree of heavy metal pollution and potential ecological risk exhibited a pattern of carbonatite zone > carbonatite interbedded with clastic rock zone > clastic zone. Spatially, the areas with serious heavy metal pollution and strong risk were mainly distributed in the carbonatite zone in the south of Zhuchangping Town.

Key words: geological background, heavy metal pollution, distribution characteristics, potential ecological risk index