Abstract

Isotopic ratios were used to identify the source of Lead (Pb) contamination in rural soils from Southeast China. Enrichment of Pb in surface soils was detected from three sampling locations, with the 206Pb/207Pb ratio indicating recent anthropogenic input. The 206Pb/207Pb ratio from deeper soil profiles reflected the ratio from parent basalt. Mass fractions of anthropogenic-derived Pb for soil samples in the upper profiles was as high as 50%, implying that surface soils in the current study were impacted by anthropogenic activity. The 206Pb/207Pb and 208Pb/206Pb ratios were similar to anthropogenic sources including the combustion of coal, which has been common practice in the region for 2500 years. Considering the relatively short history of petroleum use in this area and the rural location of soils, anthropogenic Pb source from coal burning was considered to be the main cause of lead pollution.

Highlights

  • Isotopic ratios were used to identify the source of Lead (Pb) contamination in rural soils from Southeast China

  • The objective of this study was to analyze Pb concentrations and isotopic compositions of three subtropical soils in Southeast China to examine the isotopic composition of Pb through the soil profile, identify likely sources for the contamination, and to calculate the relative contribution of natural and anthropogenic Pb sources

  • The results clearly demonstrate an enrichment of surface soil Pb concentrations

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Summary

Introduction

Isotopic ratios were used to identify the source of Lead (Pb) contamination in rural soils from Southeast China. Considering the relatively short history of petroleum use in this area and the rural location of soils, anthropogenic Pb source from coal burning was considered to be the main cause of lead pollution. Heavy metals, such as Cu, Zn, Ni, Cd, Cr and Pb, can be major contaminants in the soil e­ nvironment[1,2,3,4,5,6,7]. The objective of this study was to analyze Pb concentrations and isotopic compositions of three subtropical soils in Southeast China to examine the isotopic composition of Pb through the soil profile, identify likely sources for the contamination, and to calculate the relative contribution of natural and anthropogenic Pb sources

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