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Why was iron lost without significant isotope fractionation during the lateritic process in tropical environments?

Crossref DOI link: https://doi.org/10.1016/j.geoderma.2016.12.003

Published Print: 2017-03

Update policy: https://doi.org/10.1016/elsevier_cm_policy

Authors

Li, Miao

He, Yong-Sheng

Kang, Jin-Ting

Yang, Xiao-Yong

He, Zhi-Wei

Yu, Hui-Min

Huang, Fang https://orcid.org/0000-0003-1885-3311
Funding

Funding for this research was provided by:

National Science Foundation of China (41571130052)

National Science Foundation of China (41325011)

National Science Foundation of China (41503001)

111 Project

Fundamental Research Funds for the Central Universities
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Text and Data Mining valid from 2017-03-01

Text and Data Mining valid from 2017-03-01

Accepted Manuscript valid from 2017-12-21
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This article is maintained by: Elsevier

Article Title: Why was iron lost without significant isotope fractionation during the lateritic process in tropical environments?

Journal Title: Geoderma

CrossRef DOI link to publisher maintained version: https://doi.org/10.1016/j.geoderma.2016.12.003

Content Type: article

Copyright: © 2016 Elsevier B.V. All rights reserved.