Application of magnetic susceptibility measurement for mapping and assessment of ecological quality in urban topsoils

A. Vasiliev, Mikhail Razinsky, Svetlana S. Gorokhova
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引用次数: 1

Abstract

The article presents the results of geostatistical mapping of the magnetic susceptibility of the urban top soil. Soil magnetometry is well suited for rapid monitoring of pollution in urban areas due to its high sensitivity, ease of measurement, rapidity, high reproducibility of analysis, and low cost. This method allows obtaining large datasets with high resolution. The purpose of the study: spatial modeling of magnetic susceptibility and ecological-geochemical assessment of the top soil of Kudymkar city. The research area covers a section of the city with a total area of 32 km². Spatial modeling was carried out by the geostatistical method based on 51 soil samples. The background magnetic susceptibility of the soils of the city is 3–4 times higher than the magnetic susceptibility of the soils of the non-contaminated regional background. Soils with high and very high magnetic susceptibility occupy more than 30 % of the city area. Anomalous zones of soil magnetic pollution or magnetic “hot spots” formed near industrial facilities, heating boilers, on roadside soils with heavy traffic. A scale for the volumetric magnetic susceptibility of soils was developed on the centile analysis of the data. Strongly magnetic soils contain elevated concentrations of Zn, Cu, and Ni. The concentrations and names of pollutant metals in urban soils depend on the techno-geochemical specialization of cities. It can be recommended that the Environmental Services of cities use measurements of the magnetic susceptibility to monitor the ecological and geochemical state of soils and identify areas of city soils contaminated with heavy metals.
磁化率测量在城市表土生态质量制图与评价中的应用
本文介绍了城市表层土壤磁化率的地质统计填图结果。土壤磁强计具有灵敏度高、测量方便、快速、分析重现性强、成本低等特点,非常适合城市污染的快速监测。这种方法可以获得高分辨率的大型数据集。研究目的:库迪姆卡尔市表层土壤磁化率空间模拟及生态地球化学评价。研究区域覆盖了城市的一部分,总面积为32平方公里。利用地统计学方法对51个土壤样品进行空间建模。城市土壤的本底磁化率是未受污染区域本底土壤磁化率的3 ~ 4倍。高、极高磁化率土壤占城市面积的30%以上。在工业设施、采暖锅炉附近、交通繁忙的路边土壤上形成土壤磁污染异常区或磁“热点”。在对资料进行百分位分析的基础上,建立了土壤体积磁化率的标度。强磁性土壤含有高浓度的锌、铜和镍。城市土壤中污染金属的浓度和名称取决于城市的技术-地球化学专业化。建议城市环境服务部门利用磁化率测量来监测土壤的生态和地球化学状态,并确定城市土壤受重金属污染的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
0.90
自引率
0.00%
发文量
2
审稿时长
8 weeks
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