干旱区生态环境知识资源中心

In this study, natural and anthropogenic factors affecting the spatial distribution of topsoil mass magnetic susceptibility (chi lf) were investigated in an arid region in Isfahan province, central Iran. A total of 100 surface (0-5cm) soil samples were collected, and the chi lf value of the soil samples was measured. High values of chi lf in the east and northeast parts of the area indicated the occurrence of hilly igneous rocks and pediment geomorphic surface, enriched by ferrimagnetic minerals. In order to investigate the effects of human activities, multivariate geostatistics was applied to the results on the concentrations of eight heavy metals in surface soil samples. The results indicated that the spatial variability of second factor extracted by factor analysis, with high contribution of Zn, Pb and Cu, was well in agreement with the distribution of urban and industrial sites. This implied that magnetic particles accompanying the heavy metal emissions have increased chi lf in the topsoil of the west of the area studied. Multiple linear regression analysis of chi lf with studied factors revealed that the developed model explained about 64% of total variability in chi lf in the studied area; and geology was identified as the most important controlling factor.