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Environmental geochemistry of calcium isotopes: Applications of a new stable isotope approach

机译:钙同位素的环境地球化学:一种新的稳定同位素方法的应用

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This paper summarizes isotope fractionation mechanism, analytical method and applications in environmental geochemistry of calcium isotopes. Calcium isotopic composition can be used to constrain material sources and study geological and environmental processes as the isotopic composition of calcium (δ~(44)Ca) and fractionation processes depend on geochemical circumstances in nature. Recently, thanks to current advances in analytical technology of calcium isotopes, calcium isotopes are broadly used in biological and geochemical studies, such as the mechanism of plants imbibing nutrients through their roots, calcium transport in the environmental ecosystem, calcium cycle in oceans and paleo-oceans and paleo-cli-mate. The elementary data show that δ ~(44)Ca values vary from -2. 88 per thousand to 0. 92 per thousand in natural samples.
机译:本文概述了钙同位素的同位素分馏机理,分析方法及其在环境地球化学中的应用。钙同位素组成可用于限制物质来源并研究地质和环境过程,因为钙的同位素组成(δ〜(44)Ca)和分馏过程取决于自然界中的地球化学环境。最近,由于钙同位素分析技术的最新进展,钙同位素被广泛用于生物和地球化学研究,例如植物通过根吸收养分的机制,环境生态系统中的钙运输,海洋中的钙循环和古土壤的钙化。海洋和古气候。基本数据表明δ〜(44)Ca值在-2范围内变化。天然样品中的百分含量为88到0。92。

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