Lithium isotopic records of anthropogenic activity in the Xiaoqing River basin, eastern China.

Yang-Yang Wang, Hongqiong Wan, Yilin Xiao, Liping Qin, Xiaoqing He, He Sun
Author Information
  1. Yang-Yang Wang: State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
  2. Hongqiong Wan: State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
  3. Yilin Xiao: State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; CAS Center for Excellence in Comparative Planetology, Hefei 230026, China. Electronic address: ylxiao@ustc.edu.cn.
  4. Liping Qin: State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; CAS Center for Excellence in Comparative Planetology, Hefei 230026, China.
  5. Xiaoqing He: State Key Laboratory of Lithospheric and Environmental Coevolution, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; School of Carbon Neutrality Science and Engineering, Anhui University of Science and Technology, Hefei 231131, China.
  6. He Sun: School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China.

Abstract

The environmental impact of the discharge of lithium (Li) by anthropogenic activity has been overlooked. By analyzing Li concentrations and isotope compositions (��Li) of water and sediment samples, this study evaluates the influence of anthropogenic Li discharge on the Xiaoqing River and Laizhou Bay, which are heavily polluted areas in China. High Li concentrations of the river water (up to 7.8 ��mol/L) should be linked to anthropogenic Li discharge. However, no profound ��Li anomalies were observed, preventing identification of the exact discharge sources. In the river sediments, Li concentrations (19.0-45.0 ��g/g) were weakly correlated with Zn, Cu, and Cr concentrations, whereas ��Li values ranged from 0.6 ��� to 13.9 ��� with high values being accompanied by high contents of total organic carbon and heavy Cr isotope compositions (��Cr). All these point to significant influence of anthropogenic activity on the Li budget of river sediments. A simple mass balance calculation indicates that smelters, Li-bearing therapeutic drugs, and secondary Li-ion batteries are the main anthropogenic Li sources. In contrast to river sediments, marine sediments in the Laizhou Bay were broadly homogeneous at both spatial and temporal scales, indicating no significant influence of anthropogenic Li discharge. Overall, our data indicate that Li isotope systematics in river sediments, especially sediments near intense anthropogenic activity, are effective at tracing potential Li pollution and can help obtain accurate results for environmental inspection.

Keywords

Word Cloud

Similar Articles

Cited By