Articles | Volume 17, issue 3
https://doi.org/10.5194/bg-17-683-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-683-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High-pH and anoxic conditions during soil organic matter extraction increases its electron-exchange capacity and ability to stimulate microbial Fe(III) reduction by electron shuttling
Yuge Bai
Geomicrobiology, Center of Applied Geosciences, University of
Tübingen, Tübingen, 72074, Germany
Edisson Subdiaga
Environmental Mineralogy and Chemistry, Center of Applied Geosciences,
University of Tübingen, Tübingen, 72074, Germany
Stefan B. Haderlein
Environmental Mineralogy and Chemistry, Center of Applied Geosciences,
University of Tübingen, Tübingen, 72074, Germany
Heike Knicker
Instituto de Recursos Naturales y Agrobiología de Sevilla,
Consejo Superior de Investigaciones Científicas (IRNAS-CSIC), Seville,
41012, Spain
Andreas Kappler
CORRESPONDING AUTHOR
Geomicrobiology, Center of Applied Geosciences, University of
Tübingen, Tübingen, 72074, Germany
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Latest update: 20 Nov 2024
Short summary
Biogeochemical processes of SOM are key for greenhouse gas emission and water quality. We extracted SOM by water or by NaOH–HCl under oxic–anoxic conditions. Chemical and anoxic extractions lead to higher SOM electron exchange capacities, resulting in stimulation of microbial Fe(III) reduction. Therefore, aqueous pH-neutral SOM extracts should be used to reflect environmental SOM redox processes, and artifacts of chemical extractions need to be considered when evaluating SOM redox processes.
Biogeochemical processes of SOM are key for greenhouse gas emission and water quality. We...
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