中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Lithium isotopic composition of soil pore water: Responses to evapotranspiration

文献类型:期刊论文

作者Xu, Zhewen5; Li, Tao5; Li, Gaojun3,4,5; Hedding, David W.2; Wang, Yunqiang1; Gou, Long-Fei3; Zhao, Liang5; Chen, Jun5
刊名GEOLOGY
出版日期2022-02-01
卷号50期号:2页码:194-198
ISSN号0091-7613
DOI10.1130/G49366.1
通讯作者Li, Gaojun(ligaojun@nju.edu.cn)
英文摘要Lithium isotopes show great potential to trace Earth surface processes due to the large mass discrimination between Li-6 and Li-7 associated with clay uptake. However, factors controlling the Li isotopic composition (delta Li-7) of river water, especially those with a water-bedrock delta Li-7 difference higher than that of the equilibrium fractionation associated with clay formation (Delta(W-C)), have not yet been fully resolved. Traditional interpretation involves the Rayleigh distillation, but it unrealistically separates the stage of clay formation from that of silicate dissolution using fractionation factors that are much lower than laboratories can constrain. We propose an in situ mechanism that simulates high delta Li-7 by evapotranspiration. A model with coupled mineral dissolution and clay precipitation shows that evaporative enrichment of pore-water Li progressively increases the incorporation of Li into clays with light delta Li-7, resulting in higher delta Li-7 values in the residual water than Delta(W-C). We also provide evidence from the Chinese Loess Plateau, where an evaporative effect readily explains the observed delta Li-7. The influence of evapotranspiration on riverine delta Li-7 implies that changes in aridity may partly explain the variations of seawater delta Li-7. The same principle may also apply to other stable isotopic systems whereby incorporation into secondary precipitates controls the isotopic fractionation.
WOS关键词WEATHERING PROCESSES ; LI ; FRACTIONATION ; BEHAVIOR ; RIVERS ; LOESS ; CYCLE
资助项目National Natural Science Foundation of China[41991321] ; National Natural Science Foundation of China[41877351] ; National Natural Science Foundation of China[41730101] ; National Natural Science Foundation of China[42061130212] ; National Natural Science Foundation of China[42002198] ; Royal Society Newton Advanced Fellowship[NA201244] ; Fundamental Research Funds for the Central Universities[0206-14380124] ; Second Tibetan Plateau Scientific Expedition and Research program[2019QZKK0707]
WOS研究方向Geology
语种英语
WOS记录号WOS:000749789600013
出版者GEOLOGICAL SOC AMER, INC
资助机构National Natural Science Foundation of China ; Royal Society Newton Advanced Fellowship ; Fundamental Research Funds for the Central Universities ; Second Tibetan Plateau Scientific Expedition and Research program
源URL[http://ir.ieecas.cn/handle/361006/17413]  
专题地球环境研究所_生态环境研究室
通讯作者Li, Gaojun
作者单位1.Chinese Acad Sci, Inst Earth Environm, SKLLQG, Xian 710061, Peoples R China
2.Univ South Africa, Dept Geog, ZA-1710 Florida, South Africa
3.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
4.Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing 210023, Peoples R China
5.Nanjing Univ, Dept Earth & Planetary Sci, Minist Educ, Key Lab Surficial Geochem, Nanjing 210023, Peoples R China
推荐引用方式
GB/T 7714
Xu, Zhewen,Li, Tao,Li, Gaojun,et al. Lithium isotopic composition of soil pore water: Responses to evapotranspiration[J]. GEOLOGY,2022,50(2):194-198.
APA Xu, Zhewen.,Li, Tao.,Li, Gaojun.,Hedding, David W..,Wang, Yunqiang.,...&Chen, Jun.(2022).Lithium isotopic composition of soil pore water: Responses to evapotranspiration.GEOLOGY,50(2),194-198.
MLA Xu, Zhewen,et al."Lithium isotopic composition of soil pore water: Responses to evapotranspiration".GEOLOGY 50.2(2022):194-198.

入库方式: OAI收割

来源:地球环境研究所

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