锂同位素在环境地球化学研究中的新进展
NEW PROGRESS IN LITHIUM ISOTOPE ENVIRONMENTAL GEOCHEMISTRY
查看参考文献40篇
文摘
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锂的两个稳定同位素(^6Li和^7Li)相对质量差较大,因此易产生明显的同位素分馏。业已查明,自然界中δ^2Li值的变化在-40‰和+50‰之间。其中较小的δ^7Li值见于海相生物碳酸盐样品,较大的δ^7Li值见于某些盐湖卤水以及有孔虫的样品。由于明显的同位素分馏和不同地质体中截然不同的δ^7Li值,锂同位素应用十分广泛,且在壳-幔演化、陆壳风化、卤水和污染水体示踪等研究领域取得显著成效。 |
其他语种文摘
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Relatively great mass difference between two stable isotopes of lithium results in distinct isotope fractionation. Due to the improvement of analytical technology, rapid progress has been made in the study of lithium isotope geochemistry. The δ^7Li values of natural samples vary from -40‰ to + 50‰. Saline water and foraminifer are enriched in ^7Li, and marine biogenetic carbonates are depleted in ^7Li. Larger isotope fractionation and different lithium isotopic values in geological reservoirs make Li fred extensive applications in environmental geochemistry, such as upper continental crust weathering, brine and polluted water tracing, etc. |
来源
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矿物学报
,2006,26(2):196-202 【核心库】
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关键词
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锂同位素
;
地表风化
;
卤水
;
污染
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地址
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中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵州, 贵阳, 550002
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语种
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中文 |
文献类型
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研究性论文 |
ISSN
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1000-4734 |
学科
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地质学;环境科学基础理论 |
基金
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国家自然科学基金面上项目
;
中国科学院知识创新工程重要方向项目
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文献收藏号
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CSCD:2510426
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40
共2页
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