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植被恢复对贵州喀斯特高原地区土壤重金属分布特征的影响。

Effects of vegetation restoration on distribution characteristics of heavy metals in soil in Karst plateau area of Guizhou.

机构信息

College of Eco-Environmental Engineering, The Institute of Karst Wetland Ecology, Guizhou Minzu University, Guiyang, Asia, China.

Department of Mechanical and Electrical and Urban Construction, Guizhou Vocational College of Agriculture, Qingzhen, Asia, China.

出版信息

PeerJ. 2023 Mar 17;11:e15044. doi: 10.7717/peerj.15044. eCollection 2023.

Abstract

In southwest China, vegetation restoration is widely used in karst rocky desertification control projects. This technology can effectively fix the easily lost soil, gradually restore the plant community and improve soil fertility. However, the change law of soil heavy metals in the restoration process remains to be further studied. Therefore, in this work, Guizhou Caohai Nature Reserve as a typical karst area was taken as the research object to investigate the influence of vegetation restoration technology on repairing soil heavy metal pollution. The spatial distribution characteristics of soil heavy metals (chromium, nickel, arsenic, zinc, lead) before and after vegetation restoration in karst area were studied by comparative analysis and linear stepwise regression analysis. The main influencing factors and spatial distribution characteristics of heavy metals in karst area were further discussed. The results showed that: (1) heavy metals in karst soils are affected by surface vegetation, root exudates, microorganisms and leaching. Only heavy metals nickel (Ni) and lead (Pb) showed the tendency of surface enrichment and bottom precipitation enrichment in non-karst soils. Path analysis suggested that non-metallic soil factors such as soil bulk density (BD), total nitrogen (TN) and ammonium nitrogen (NH -N) had direct effect on the content of heavy metals in soil. (2) The proportion of 0.25-2 mm aggregates in the surface soil of vegetation restoration belt was more than 40%, and the proportion of surface soil ≤2 mm aggregates in this increased to 83% and 88%, respectively, which could improve the soil structure and properties effectively. (3) Vegetation restoration effectively restored the nutrient elements such as carbon and nitrogen in the soil, and enhanced the soil material circulation. Furthermore the content of heavy metals in the surface soil higher than that in the 10-20 cm soil layer. Plant absorption, biosorption mechanism of microorganisms, coupling of root exudates, dissolution of soil soluble organic carbon and pH make the contents of heavy metals Cr, Ni and Pb in vegetation restoration belt slightly lower than those in karst soil. At the same time, affected by vegetation coverage, residual heavy metals in soil are further leached by surface runoff. Therefore, the content of heavy metals in soil could reduce combined heavy metal enrichment plants for extraction with remediation. This study elucidates the advantages and remedy mechanism of vegetation restoration in the remediation of heavy metal contaminated soils in Caohai area of Guizhou, and this plant activation and enrichment extraction remediation technology would be popularized and applied in the remediation of heavy metal contaminated soils in other karst areas.

摘要

在中国西南部,植被恢复广泛应用于喀斯特石漠化治理项目。该技术可以有效固定易流失的土壤,逐渐恢复植物群落,提高土壤肥力。然而,植被恢复过程中土壤重金属的变化规律仍有待进一步研究。因此,本工作以贵州草海自然保护区为典型喀斯特区为研究对象,探讨植被恢复技术对修复土壤重金属污染的影响。通过对比分析和线性逐步回归分析,研究了喀斯特区植被恢复前后土壤重金属(铬、镍、砷、锌、铅)的空间分布特征。进一步讨论了喀斯特区重金属的主要影响因素和空间分布特征。结果表明:(1)喀斯特土壤中的重金属受地表植被、根系分泌物、微生物和淋溶作用的影响。只有非喀斯特土壤中的重金属镍(Ni)和铅(Pb)表现出表面富集和底部沉淀富集的趋势。路径分析表明,土壤容重(BD)、总氮(TN)和铵态氮(NH 4 -N)等非金属土壤因素对土壤重金属含量有直接影响。(2)植被恢复带表层土壤中 0.25-2mm 团聚体的比例超过 40%,表层土壤中≤2mm 团聚体的比例分别增加到 83%和 88%,可有效改善土壤结构和性质。(3)植被恢复有效恢复了土壤中的碳、氮等养分元素,增强了土壤物质循环。此外,表层土壤中重金属的含量高于 10-20cm 土壤层。植物吸收、微生物的生物吸附机制、根系分泌物的耦合、土壤可溶性有机碳的溶解和 pH 值使植被恢复带中 Cr、Ni 和 Pb 等重金属的含量略低于喀斯特土壤。同时,受植被覆盖的影响,土壤中残留的重金属进一步被地表径流淋溶。因此,可采用种植超富集植物提取修复来降低土壤重金属的含量。本研究阐明了植被恢复在贵州草海地区重金属污染土壤修复中的优势和修复机制,这种植物激活和富集提取修复技术将在其他喀斯特地区重金属污染土壤的修复中得到推广和应用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0eef/10026723/b344cac4bd2f/peerj-11-15044-g001.jpg

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