Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
It has been shown that reactive soil minerals, specifically iron(III) (oxyhydr)oxides, can trap organic carbon in soils overlying intact permafrost, and may limit carbon mobilization and degradation as it is observed in other environments. However, the use of iron(III)-bearing minerals as terminal e...
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Bibliographic Details
Published in: | Nature Communications |
Main Authors: |
Patzner, Monique S.,
Mueller, Carsten W.,
Malusova, Miroslava,
Baur, Moritz,
Nikeleit, Verena,
Scholten, Thomas Univ. of Tubingen . Chair of Soil Science and Geomorphology,
Hoeschen, Carmen Technische Univ. Munchen, Freising . Chair of Soil Science,
Byrne, James M. Univ. of Tubingen . Center for Applied Geosciences. Geomicrobiology; Bristol Univ. . School of Earth Sciences,
Borch, Thomas Colorado State Univ., Fort Collins, CO . Dept. of Soil & Crop Sciences. Dept. of Chemistry,
Kappler, Andreas Univ. of Tubingen . Center for Applied Geosciences. Geomicrobiology,
Bryce, Casey Univ. of Tubingen . Center for Applied Geosciences. Geomicrobiology; Bristol Univ. . School of Earth Sciences |
Language: | unknown |
Published: |
2022
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Subjects: |
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Online Access: | http://www.osti.gov/servlets/purl/1816797
https://www.osti.gov/biblio/1816797
https://doi.org/10.1038/s41467-020-20102-6
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