土(古典元素)
同位素
地质学
稳定同位素比值
天体生物学
地球表面
地球科学
物理
核物理学
数学物理
作者
Isabelle Basile-Doelsch
标识
DOI:10.1016/j.gexplo.2005.08.050
摘要
Abstract Silicon (Si) is the second most abundant element on Earth after oxygen. Only few studies have attempted to use stable isotopes of Si as proxies for understanding the Si cycle and its variations in the past. By using three different methods (IRMS, MC–ICP–MS and SIMS), the overall measurements show that the isotopic composition (δ30Si) of terrestrial samples ranges from − 5.7‰ to + 3.4‰. Dissolved Si in rivers and seawater is 30Si-enriched (− 0.8‰
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