Iron behavior in a northern estuary: Large pools of non-sulfidized Fe(II) associated with organic matter

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Iron behavior in a northern estuary: Large pools of non-sulfidized Fe(II) associated with organic matter

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作者：Changxun Yu^a ; ^{changxun.yu@lnu.se" class="auth_mail" title="E-mail the corresponding author} ; ^{yuchangxun2006@163.com" class="auth_mail" title="E-mail the corresponding author} ; Joonas J. Virtasalo^b ; Torbjö ; rn Karlsson^c ; Pasi Peltola^a ; Peter Ö ; sterholm^d ; Edward D. Burton^e ; Laura Arppe^f ; Johan K. Hogmalm^g ; Antti E.K. Ojala^b ; Mats E. Å ; strö ; m^a
关键词：Iron diagenesis ; X-ray absorption spectroscopy (XAS) ; Sulfidization ; Gulf of Bothnia ; Sediments ; Non-sulfidized reactive Fe pools
刊名：Chemical Geology
出版年：2015
出版时间：15 October 2015
年：2015
卷：413
期：Complete
页码：73-85
全文大小：1984 K

文摘

•: The estuaries in the Boreal zone receive an abundance of organically complexed and hydroxide bound Fe(III)
•: In the sediment, the organically complexed Fe(III) is to a limited extent sulfidized due to comparatively little sulfate
•: Pyritization is low due to chemical and physical characteristics of the sediment
•: Organically complexed Fe(II) dominates the abundant non-sulfidized Fe pool in the sediment

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