Cadmium isotopic fractionation in lead-zinc smelting process and signatures in fluvial sediments.

Cd isotopes Cd pollution Isotopic fractionation Sediment Source tracer

Journal

Journal of hazardous materials
ISSN: 1873-3336
Titre abrégé: J Hazard Mater
Pays: Netherlands
ID NLM: 9422688

Informations de publication

Date de publication:
05 06 2021
Historique:
received: 14 10 2020
revised: 28 12 2020
accepted: 29 12 2020
pubmed: 15 1 2021
medline: 15 1 2021
entrez: 14 1 2021
Statut: ppublish

Résumé

Cadmium (Cd) is a toxic heavy metal pollutant. Various industrial activities, especially metal smelting, are the main sources of Cd pollution. Cd isotopes have exhibited the ability to be excellent source tracers and can be used to assess the pollution contributions from different sources. Herein, in a typical lead-zinc smelter, Shaoguan, China, significant Cd isotopic fractionation was found during the high temperature smelting process and followed a Rayleigh distillation model. The heavier Cd isotopes were concentrated in the slag, while the lighter Cd isotopes were concentrated in the dust. In the downstream sediment profile of the smelter, sediments have extremely high Cd concentrations that far exceed the Chinese background sediment, indicating severe pollution levels. The ε

Identifiants

pubmed: 33445048
pii: S0304-3894(20)33006-5
doi: 10.1016/j.jhazmat.2020.125015
pii:
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

125015

Informations de copyright

Copyright © 2021 Elsevier B.V. All rights reserved.

Auteurs

Qiaohui Zhong (Q)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China; Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510405, China.

Meiling Yin (M)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China.

Qiong Zhang (Q)

Department of Earth Sciences, University of Oxford, Oxford, UK.

Jingzi Beiyuan (J)

School of Environment and Chemical Engineering, Foshan University, Foshan, Guangdong, China.

Juan Liu (J)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China; Department of Earth Sciences, University of Oxford, Oxford, UK. Electronic address: liujuan858585@163.com.

Xiao Yang (X)

Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

Jin Wang (J)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China. Electronic address: wangjin@gzhu.edu.cn.

Lulu Wang (L)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China.

Yanjun Jiang (Y)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China.

Tangfu Xiao (T)

Key Laboratory of Water Quality and Conservation in the Pearl River Delta, Ministry of Education, School of Environmental Science and Engineering, Guangzhou University, Guangzhou, China.

Zhaofeng Zhang (Z)

Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510405, China.

Classifications MeSH