Articles | Volume 8, issue 1
https://doi.org/10.5194/soil-8-253-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-8-253-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Land use impact on carbon mineralization in well aerated soils is mainly explained by variations of particulate organic matter rather than of soil structure
Steffen Schlüter
CORRESPONDING AUTHOR
Department of Soil System Sciences, Helmholtz Centre for Environmental
Research – UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Tim Roussety
Department of Soil System Sciences, Helmholtz Centre for Environmental
Research – UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Lena Rohe
Department of Soil System Sciences, Helmholtz Centre for Environmental
Research – UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Vusal Guliyev
Department of Soil Ecology, Helmholtz Centre for Environmental Research
– UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Evgenia Blagodatskaya
Department of Soil Ecology, Helmholtz Centre for Environmental Research
– UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Thomas Reitz
Department of Soil System Sciences, Helmholtz Centre for Environmental
Research – UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
Department of Soil Ecology, Helmholtz Centre for Environmental Research
– UFZ, Theodor-Lieser-Str. 4, 06120 Halle (Saale), Germany
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The microstructure of permafrost soils contains clues to its formation and its preconditioning to future change. We used X-ray computed tomography (CT) to measure the composition of a permafrost drill core from Siberia. By combining CT with laboratory measurements, we determined the the proportions of pore ice, excess ice, minerals, organic matter, and gas contained in the core at an unprecedented resolution. Our work demonstrates the potential of CT to study permafrost properties and processes.
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Freezing and thawing cycles are an important agent of soil structural transformation during the winter season in the mid-latitudes. This study shows that it promotes a well-connected pore system, fragments dense soil clods, and, hence, increases the unsaturated conductivity by a factor of 3. The results are important for predicting the structure formation and hydraulic properties of soils, with the prospect of milder winters due to climate change, and for farmers preparing the seedbed in spring.
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Short summary
Total denitrification, i.e. N2O and (N2O + N2) fluxes, of repacked soil cores were analysed for different combinations of soils and water contents. Prediction accuracy of (N2O + N2) fluxes was highest with combined proxies for oxygen demand (CO2 flux) and oxygen supply (anaerobic soil volume fraction). Knowledge of denitrification completeness (product ratio) improved N2O predictions. Substitutions with cheaper proxies (soil organic matter, empirical diffusivity) reduced prediction accuracy.
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Short summary
We combined microstructure analysis via X-ray CT with carbon mineralization analysis via respirometry of intact soil cores from different land uses. We found that the amount of particulate organic matter (POM) exerted a dominant control on carbon mineralization in well-aerated topsoils, whereas soil moisture and macroporosity did not play role. This is because carbon mineralization mainly occurs in microbial hotspots around degrading POM, where it is decoupled from conditions of the bulk soil.
We combined microstructure analysis via X-ray CT with carbon mineralization analysis via...