Influence of environmental factors on changes in the speciation of Pb and Cr in sediments of Wuliangsuhai Lake, during the ice-covered period

• Published in: Environmental geochemistry and health 2024-04, Vol.46 (4), p.116-116, Article 116
• Main Authors: Zhao, Yunxi, Zhao, Shengnan, Shi, Xiaohong, Lu, Junping, Cui, Zhimou, Yu, Haifeng, Ye, Bowen, Li, Xingyue
• Format: Article
• Language: English
• Subjects: China; Chromium; Contamination; Earth and Environmental Science; Ecological effects; Environment; Environmental Chemistry; Environmental factors; Environmental Health; Environmental Monitoring - methods; Geochemistry; Geologic Sediments; Heavy metals; Ice; Ice cover; Lake ice; Lakes; Lead; Manganese; Metals; Metals, Heavy - analysis; Organic matter; Original Paper; Pollution; Public Health; Risk Assessment; Salinity; Salinity effects; Sediment; Sediments; Soil Science & Conservation; Speciation; Sulfides; Sulphides; Terrestrial Pollution; Water; Water circulation; Water column; Water Pollutants, Chemical - analysis; Water temperature
• ISSN: 0269-4042; 1573-2983
• DOI: 10.1007/s10653-023-01842-y

Ecological pollution caused by heavy metals released from sediments is a worldwide concern. However, the effect of changes in sediment speciation on their release of heavy metals has not been adequately reported. In this study, the research focused on Pb and Cr in the ice period of Wuliangsuhai. This study analyzed changes in the sediment speciation of Pb and Cr before and after a release experiment using four risk assessment methods while varying the temperature, pH, and salinity of the water column. The results indicated that the total concentration of Pb ranged from 11.17 to 24.25 mg/kg, while for Cr it ranged from 42.26 to 69.68 mg/kg. Both elements exhibited mild contamination. The release of Pb and Cr from sediments increases with increasing water temperature, mainly due to the conversion of the residual fraction of Pb to the Fe–Mn oxide fraction and Cr converting more residual fraction to the organic matter and sulfide fraction. The release of sediment Pb and Cr decreased with increasing pH, with Pb converting more acid extractable fraction to the residual fraction and Cr converting more organic matter and sulfide fraction to the residual fraction. In contrast, the release of Pb and Cr increased and then decreased with increasing salinity. For Pb, the acid extractable fraction was more susceptible to conversion to the residual fraction by environmental influences, whereas for Cr, the organic matter and sulfide fraction were susceptible to conversion to the residual fraction.