Original paper
Uranium reduction and isotopic fractionation in reducing sediments: Insights from reactive transport modeling
Abstract
Uranium concentrations and isotopic ratios (238U/235U, denoted as δ238U) have been used to provide quantitative information about the degree of oxygenation and de-oxygenation of past oceans. The potential to constrain changes in global redox conditions, in contrast to many other proxies that reflect local conditions, is a particular strength of the uranium isotope approach. Because uranium reduction primarily occurs in sediments underlying...
Paper Details
Title
Uranium reduction and isotopic fractionation in reducing sediments: Insights from reactive transport modeling
Published Date
Oct 1, 2020
Volume
287
Pages
65 - 92
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Notes
History