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中国中部武汉土壤中微量元素的浓度、分布、来源及生态风险评估。

Concentrations, Distribution, Sources and Ecological Risk Assessment of Trace Elements in Soils from Wuhan, Central China.

机构信息

Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China.

Sino-Africa Joint Research Center, Chinese Academy of Sciences, Wuhan 430074, China.

出版信息

Int J Environ Res Public Health. 2018 Dec 14;15(12):2873. doi: 10.3390/ijerph15122873.

Abstract

This study aimed to determine the concentration levels, potential sources and ecological risks of eleven trace elements, namely Cr, Fe, Co, Ni, Cu, As, Sb, Cd, Zn, Hg and Pb, in the soil from Huangpi district, Wuhan, Central China. Soil samples were collected from eighteen sites at soil depths of 1⁻10 and 10⁻20 cm and analyzed using Inductively Coupled Plasma-Mass Spectrometer ICP-MS (Thermo X SERIES 2, Scientific and Innovative Technology Co. Ltd., Beijing, China). The recorded mean concentration of the elements were in a decreasing order of Fe > Co > Cr > Ni > Pb > Cu > As > Cd > Sb > Zn > Hg. The mean concentration of trace elements, soil pH and total organic carbon (TOC) were higher at a soil depth of 1⁻10 cm. The obtained mean concentration of Cr, Co, As, Cd, Ni, Cu, Hg and Pb were above the soil background values of Wuhan and Hubei Province. The mean concentration values of Co, Ni and Cd, exceeded the recommended FAO (Food and Agriculture Organization)/ISRIC (International Soil Reference and Information Centre) (2004) and WHO/FAO (2001) values. Pearson's correlation analysis illustrated that there was a strong and significant correlation between trace elements, whereas, a weak positive and negative correlation between elements and soil properties (pH and TOC). The principal component analysis (PCA) and cluster analysis (CA) result indicated that the concentration of trace elements in Huangpi soil were originated from anthropogenic sources. Potential ecological risk index (RI) of this study revealed that there is a high ecological risk of trace elements in the soil. Enrichment factor (EF) and geo-accumulation index () of trace elements for this study indicated that the study area is strongly contaminated with Cd and Co. Generally, the finding of this research showed that Huangpi soil is contaminated.

摘要

本研究旨在测定华中武汉市黄陂区土壤中 11 种微量元素(Cr、Fe、Co、Ni、Cu、As、Sb、Cd、Zn、Hg 和 Pb)的浓度水平、潜在来源和生态风险。从土壤深度为 1-10cm 和 10-20cm 的 18 个地点采集土壤样本,使用电感耦合等离子体质谱仪(ICP-MS)(Thermo X SERIES 2,北京赛谱锐思科技有限公司)进行分析。记录的元素平均浓度依次为 Fe>Co>Cr>Ni>Pb>Cu>As>Cd>Sb>Zn>Hg。在土壤深度为 1-10cm 处,微量元素、土壤 pH 值和总有机碳(TOC)的平均浓度较高。研究区 Cr、Co、As、Cd、Ni、Cu、Hg 和 Pb 的平均浓度高于武汉和湖北省的土壤背景值。Co、Ni 和 Cd 的平均浓度值超过了粮农组织/国际土壤参考和信息中心(2004 年)和世卫组织/粮农组织(2001 年)推荐值。Pearson 相关分析表明,微量元素之间存在很强且显著的相关性,而元素与土壤性质(pH 值和 TOC)之间存在弱正相关和负相关。主成分分析(PCA)和聚类分析(CA)结果表明,黄陂土壤中微量元素的浓度来源于人为来源。本研究的潜在生态风险指数(RI)表明,土壤中微量元素具有高生态风险。本研究中微量元素的富集因子(EF)和地质累积指数(Igeo)表明,研究区受到 Cd 和 Co 的强烈污染。总的来说,本研究的结果表明黄陂土壤受到了污染。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bb9b/6313746/59092dc6a6bc/ijerph-15-02873-g001.jpg

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