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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Cited
12 citations as recorded by crossref.
- Linking soil organic carbon mineralization to soil physicochemical properties and bacterial alpha diversity at different depths following land use changes J. Guo et al. 10.1186/s13717-023-00450-z
- Soil organic carbon accumulation in dry tropical mountainous zone of Cameroon M. Atourakai et al. 10.1007/s12517-023-11248-w
- Exploring the Influence of Natural and Agricultural Land Use Systems on the Different Lability Organic Carbon Compounds in Eutric Endocalcaric Arenosol L. Tripolskaja et al. 10.3390/su16135403
- Soil textural control on moisture distribution at the microscale and its effect on added particulate organic matter mineralization H. Li et al. 10.1016/j.soilbio.2022.108777
- Interaction between POM and pore structure during straw decomposition in two soils with contrasting texture T. Ding et al. 10.1016/j.still.2024.106288
- Quantifying and visualizing soil macroaggregate pore structure and particulate organic matter in a Vertisol under various straw return practices using X-ray computed tomography Z. Guo et al. 10.1016/j.geoderma.2024.117105
- Management impacts on whole soil warming responses of CO2 production and efflux in temperate climate M. Khan et al. 10.1016/j.geoderma.2023.116725
- Microhabitat properties explain variations in soil nematode communities across climate conditions in cropland, but not in grassland M. Wu et al. 10.1016/j.soilbio.2024.109657
- The divergent accumulation mechanisms of microbial necromass C in paddy soil under different long-term fertilization regimes L. Xiong et al. 10.1016/j.geoderma.2023.116688
- The role of soil pore structure on nitrate release from soil organic matter and applied fertilizer under three fertilization regimes R. Ruan et al. 10.1016/j.still.2024.106396
- Organic farming systems affect carbon stocks but not soil structure and associated physical properties in a long-term farming trial on Chernozem S. Schlüter et al. 10.1016/j.geoderma.2023.116619
- Spring rest-grazing time affected soil organic carbon stability and storage in subalpine meadows of Carex Y. Jing et al. 10.1016/j.ecoleng.2024.107195
12 citations as recorded by crossref.
- Linking soil organic carbon mineralization to soil physicochemical properties and bacterial alpha diversity at different depths following land use changes J. Guo et al. 10.1186/s13717-023-00450-z
- Soil organic carbon accumulation in dry tropical mountainous zone of Cameroon M. Atourakai et al. 10.1007/s12517-023-11248-w
- Exploring the Influence of Natural and Agricultural Land Use Systems on the Different Lability Organic Carbon Compounds in Eutric Endocalcaric Arenosol L. Tripolskaja et al. 10.3390/su16135403
- Soil textural control on moisture distribution at the microscale and its effect on added particulate organic matter mineralization H. Li et al. 10.1016/j.soilbio.2022.108777
- Interaction between POM and pore structure during straw decomposition in two soils with contrasting texture T. Ding et al. 10.1016/j.still.2024.106288
- Quantifying and visualizing soil macroaggregate pore structure and particulate organic matter in a Vertisol under various straw return practices using X-ray computed tomography Z. Guo et al. 10.1016/j.geoderma.2024.117105
- Management impacts on whole soil warming responses of CO2 production and efflux in temperate climate M. Khan et al. 10.1016/j.geoderma.2023.116725
- Microhabitat properties explain variations in soil nematode communities across climate conditions in cropland, but not in grassland M. Wu et al. 10.1016/j.soilbio.2024.109657
- The divergent accumulation mechanisms of microbial necromass C in paddy soil under different long-term fertilization regimes L. Xiong et al. 10.1016/j.geoderma.2023.116688
- The role of soil pore structure on nitrate release from soil organic matter and applied fertilizer under three fertilization regimes R. Ruan et al. 10.1016/j.still.2024.106396
- Organic farming systems affect carbon stocks but not soil structure and associated physical properties in a long-term farming trial on Chernozem S. Schlüter et al. 10.1016/j.geoderma.2023.116619
- Spring rest-grazing time affected soil organic carbon stability and storage in subalpine meadows of Carex Y. Jing et al. 10.1016/j.ecoleng.2024.107195
Latest update: 30 Jan 2025
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...