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Iron-mediated organic matter decomposition in humid soils can counteract protection

Open access
Chen, Chunmei, Hall, Steven J., Coward, Elizabeth, Thompson, Aaron·2020·Nature Communications

Abstract

Soil organic matter (SOM) is correlated with reactive iron (Fe) in humid soils, but Fe also promotes SOM decomposition when oxygen (O 2) becomes limited. Here we quantify Fe-mediated OM protection vs. decomposition by adding 13 C dissolved organic matter (DOM) and 57 Fe II to soil slurries incubated under static or fluctuating O 2. We find Fe uniformly protects OM only under static oxic conditions, and only when Fe and DOM are added together: de novo reactive Fe III phases suppress DOM and SOM mineralization by 35 and 47%, respectively. Conversely, adding 57 Fe II alone increases SOM mineralization by 8% following oxidation to 57 Fe III. Under O 2 limitation, de novo reactive 57 Fe III phases are preferentially reduced, increasing anaerobic mineralization of DOM and SOM by 74% and 32‒41%, respectively. Periodic O 2 limitation is common in humid soils, so Fe does not intrinsically protect OM; rather reactive Fe phases require their own physiochemical protection to contribute to OM persistence.

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Metadata

Authors
Chen, C., Hall, S. J., Coward, E., & Thompson, A.
Venue
Nature Communications
Published
2020-05-07
Volume
11
Issue
1
Pages
2255-2255
ISSN
2041-1723 (ISSN-L)
OpenAlex
W3022072646
Cited by
583
References
4
FWCI
35.88
Type
journal article
Language
en
Open access
gold

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CoChat. (2026). Citation check: Iron-mediated organic matter decomposition in humid soils can counteract protection. https://app.cochat.ai/papers/10.1038/s41467-020-16071-5
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Chen, C., Hall, S. J., Coward, E., & Thompson, A. (2020). Iron-mediated organic matter decomposition in humid soils can counteract protection. Nature Communications. https://doi.org/10.1038/s41467-020-16071-5

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