Release characteristics of arsenic from sediments and its source or sink competition with phosphorus: A case of a great lake with grass-algae alternation

• Published in: Journal of environmental sciences (China) 2025-03, Vol.149, p.278-287
• Main Authors: Wang, Shuhang, Chang, Yongsheng, Huang, Wei, Yang, Dianhai, Che, Feifei
• Format: Article
• Language: English
• Subjects: Arsenic; Arsenic - analysis; China; Contribution; Environmental Monitoring; Geologic Sediments - chemistry; Lakes - chemistry; Phosphorus; Phosphorus - analysis; Poaceae; Sediment; Source and sink; Water Pollutants, Chemical - analysis
• ISSN: 1001-0742
• DOI: 10.1016/j.jes.2024.01.031

•The sediments from algae-type areas acted as source role of As.•The external conditions could influence the As release characteristic in sediments.•The intense source or sink competition of As and P existed with area alternation.•The surface sediments from algae-type areas had the high As release risk.•The bottom sediments from grass-type areas had the high As release risk. The arsenic (As) release from sediments in great lakes is affected by various factors. In this study, the characteristics of As release from sediments was investigated, and the As sources and sinks with the strengths in sediments from different areas (grass-type, algae-type, and grass-algae alternation areas) in great shallow lakes (Taihu Lake, China) were analyzed, and the influence of P competition in the process of As release was also studied. The results showed that changing trend of the values of equilibrium As concentration in sediments were consistent with the regional changes (0 to 28.12 µg/L), and the sediments from algae-type areas had the higher values. The sediments from western lake and northwest lake bay were a strong As and a weak P source, and the north lake bay had the opposite trend of these two regions. Intense P source competition with As from the sediments occurred in algae-type areas. The grass-type areas had strong As and P retention capacities, indicating a sink role of sediment with high As and P sorption capacities. The degree of As and P saturation had similar trend in sediments, and the grass-type areas had the higher values, 18.3%-21.4% and 15.31%-20.34%, respectively. Contribution analysis results showed that most of As release contribution was from the bottom (30-50 cm) sediments, and the surface (0-10 cm) sediments from algae-type areas contributed more to the overlying water than other region. [Display omitted]