Citation: | CAO Ruiqin, YANG Zhongfang, YU Tao. 2024. Research progress of stable isotopic geochemistry of cadmium and zinc and its harm and control in soil and other geological bodies[J]. Geology in China, 51(3): 833-864. doi: 10.12029/gc20230522001 |
This paper is the result of environmental geological survey engineering.
Cadmium(Cd) and zinc(Zn) are both important mineral resources and harmful heavy metal elements. The recent development of multi–collector inductively coupled plasma mass spectrometry (MC–ICP–MS) has improved the precision of Zn isotope composition analysis in different environments. The establishment and application of non–traditional stable isotope systems such as cadmium and zinc have raised the geochemical research of cadmium and zinc to a new level, which also have become hot topics in isotope geochemistry.
This paper reviews recent research progress on the analytical methods, fractionation mechanisms, isotopic compositions in different reservoirs, and application fields of Zn and Cd isotopes investigated in many studies.
(1) The improvement of Zn and Cd isotope analysis technology has promoted the establishment of their isotope systems. (2) The compositions of Zn isotopes in various reservoirs have been basically identified. The data for Cd isotope compositions in reservoirs and anthropogenic sources is in the period of accumulation. (3) The isotopic fractionation mechanisms of Cd and Zn mainly include mineral adsorption, biological processes, and chemical reactions, which have been applied in the indication of planetary evolution, the exploration of metallogenic mechanisms, paleoenvironmental reconstruction, and pollution source tracer. (4) The combination of multiple isotopes helps to reduce uncertainty in the analysis of heavy metal pollution sources.
The development of new isotope analysis instruments and technologies has made the research of Zn and Cd isotopes more promising. It is expected that more work should be carried out in the near future to improve the fractionation mechanisms, compositions in partial reservoirs, and application fields.
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Zn isotope fractionation during anionexchange chromatography (after Maréchal and Albaréde, 2002)
Zn isotope fractionation of different higher plantsin nutrient solutions (after Weiss et al., 2005)
Zn isotope fractionation during adsorption on different minerals (after Pokrovsky et al., 2005)
Zn isotope fractionation during adsorption on aluminum oxide (modified from Gou et al., 2018)
Zn isotope fractionation duringthe potential change process of redox reaction (after Kavner et al., 2008)
Cd isotope fractionation in samples from a smelter in British Columbia, Canada (after Shiel et al., 2010)
Isotope composition of the cadmium in the root, straw and grain of wheat (after Zhong Songxiong et al., 2021)
Cd isotope compositions between solution and solid phases as the function of Cd–adsorbed fraction during adsorption onto goethite (a), hematite (b), and 2L ferrihydrite (c) (the lines inside the graphs represent error bars; after Yan et al., 2021)
Cd isotope fractionation during adsorption and coprecipitation of iron (oxyhydr) oxides (after Yan et al., 2021)
Zn isotopic composition of meteorites (after Brugier et al., 2019)
Dissolved Zn concentrations and stable isotope ratio (δ66Zn) profiles from the SAFe station in the Northeast Pacific (30°N 140°W) (after Conway and John, 2015)
δ66Zn variations in the different types of soils (after Liang et al., 2022)
Frequency distribution of δ66Zn in the tropical soils (a) and non–tropical soils (b) (after Liang et al., 2022)
Cadmium isotopic compositions of bivalves in the different areas (after Zhong et al., 2020)
Variations of δ114Cd of carbonates in the Yangdi profile across the FFB (after Wang Weizhong et al., 2020)
Cd concentrations and Cd isotopic compositions in the soil and stream sediment samples of the Bijiang River, China (after Zhang et al., 2016)
δ66Zn vs. abundance of Zn in ureilites. The ureilite samples are designatedwith their degree of shock (after Moynier et al., 2010)
Zinc isotope vs. abundance data in the lunar samples (after Dhaliwal et al., 2018)
Correlation between Zn/Cd ratios and δ66Zn of sphalerites in the Jinding and Wusihe Zn–Pb deposits (after Li et al., 2019)
Variation of zinc isotope ratios of sphalerites as a function of sulfur isotopic compositions (after Li et al., 2019)
Schematic portrayal of the Zn isotope evolution of the post–snowball ocean and cap dolostones (after Kunzmann et al., 2013)
δ66ZnJMC and zinc concentrations measured in the peat samples at Hietajärvi Outokumpu and Harjavalta (after Weiss et al., 2007)
Processes and mechanisms of the observed isotopic variability of zinc in the peat samples at Hietajärvi Outokumpu and Harjavalta (after Weiss et al., 2007)
Soil Cd pollution index in different regions of China (after Wang Jing et al., 2023)
Principles of phytoremediation (after Shen et al., 2021)
Principles of microbial remediation (after Chang Haiwei et al., 2018)