银同位素在行星和地球科学中的研究进展

朱原峰; 董戈; 刘茜; 盛雪芬; 魏海珍

doi:10.3799/dqkx.2021.080

Volume 46 Issue 12

Dec. 2021

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Zhu Yuanfeng, Dong Ge, Liu Xi, Sheng Xuefen, Wei Haizhen, 2021. Progress of Silver Isotopes Studies in Planetary and Earth Sciences. Earth Science, 46(12): 4390-4404. doi: 10.3799/dqkx.2021.080

Citation:

Zhu Yuanfeng, Dong Ge, Liu Xi, Sheng Xuefen, Wei Haizhen, 2021. Progress of Silver Isotopes Studies in Planetary and Earth Sciences. Earth Science, 46(12): 4390-4404. doi: 10.3799/dqkx.2021.080

Zhu Yuanfeng, Dong Ge, Liu Xi, Sheng Xuefen, Wei Haizhen, 2021. Progress of Silver Isotopes Studies in Planetary and Earth Sciences. Earth Science, 46(12): 4390-4404. doi: 10.3799/dqkx.2021.080

Citation:

Zhu Yuanfeng, Dong Ge, Liu Xi, Sheng Xuefen, Wei Haizhen, 2021. Progress of Silver Isotopes Studies in Planetary and Earth Sciences. Earth Science, 46(12): 4390-4404. doi: 10.3799/dqkx.2021.080

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Progress of Silver Isotopes Studies in Planetary and Earth Sciences

doi: 10.3799/dqkx.2021.080

Zhu Yuanfeng^{1
,
,},
Dong Ge¹,
Liu Xi¹,
Sheng Xuefen²,
Wei Haizhen^{1, 3
,
,}

1.
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
2.
Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
3.
Center for Excellence in Comparative Planetology, Chinese Academy of Sciences, Hefei 230026, China

Received Date: 2021-04-15
Publish Date: 2021-12-15

Abstract

Abstract

The progresses of the radioactive Pd-Ag system in planetary sciences and the stable silver isotope in environmental sciences and ore-deposits are systematically reviewed in this paper. In the formation of solar nebula and planetary nucleus, ¹⁰⁷Ag can be produced by ¹⁰⁷Pd through β decay, and the dissipation of volatile elements will cause the early Pd/Ag differentiation, which makes the Pd-Ag system applicable to investigate various activities of the early solar system, such as defining the formation of planetary nucleus and the age of planetary formation. In the stable silver isotope system, it has been proved that the wide variation range of δ¹⁰⁹Ag is -1.0‰ to +2.3‰ in terrestrial materials. Stable silver isotope has characteristics similar to "fingerprint" in environmental materials, which makes it possible to effectively determine pollutants sources and to track migration paths of pollutants. Much wider variations of δ¹⁰⁹Ag in metallic ore-deposits have been observed, showing a great potential of silver isotope in studying the genesis and evolution mode of Au-Ag deposits. However, there are still many concerns remained to be resolved, such as the precise definition of ¹⁰⁷Pd/¹⁰⁸Pd ratio in the early solar system of radioactive Pd-Ag system, and the quantification of silver isotope fractionation in physiochemical processes (e.g., boiling/phase separation, multistage ore paragenesis, precipitation, redox, adsorption and remobilization etc.) involved in silver migration and deposition in environmental and ore-forming processes.
- silver isotope,
- radioactive Pd-Ag system,
- tracking environmental pollutant,
- Au-Ag deposit,
- geochemistry

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References(72)

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