Articles | Volume 13, issue 3
https://doi.org/10.5194/gmd-13-1399-2020
© 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/gmd-13-1399-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
23 Mar 2020
Development and technical paper |
| 23 Mar 2020
| 23 Mar 2020
Dynamic upscaling of decomposition kinetics for carbon cycling models
Arjun Chakrawal
CORRESPONDING AUTHOR
Department of Physical Geography, Stockholm University, Svante Arrhenius väg 8C, Frescati, 106 91 Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Anke M. Herrmann
Department of Soil & Environment, Swedish University of Agricultural Sciences, P.O. Box 7014, 75007 Uppsala, Sweden
John Koestel
Department of Soil & Environment, Swedish University of Agricultural Sciences, P.O. Box 7014, 75007 Uppsala, Sweden
Jerker Jarsjö
Department of Physical Geography, Stockholm University, Svante Arrhenius väg 8C, Frescati, 106 91 Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Naoise Nunan
Institute of Ecology and Environmental Sciences – Paris, Sorbonne Université-CNRS-IRD-INRA-P7-UPEC, 4 place Jussieu, 75005 Paris, France
Thomas Kätterer
Department of Ecology, Swedish University of Agricultural Sciences, P.O. Box 7044, 75007 Uppsala, Sweden
Stefano Manzoni
Department of Physical Geography, Stockholm University, Svante Arrhenius väg 8C, Frescati, 106 91 Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
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- Storage of soil carbon is not sequestration: Straightforward graphical visualization of their basic differences P. Baveye et al. 10.1111/ejss.13380
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- Spatial Control of Microbial Pesticide Degradation in Soil: A Model-Based Scenario Analysis E. Schwarz et al. 10.1021/acs.est.2c03397
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- Linking Soil Structure, Hydraulic Properties, and Organic Carbon Dynamics: A Holistic Framework to Study the Impact of Climate Change and Land Management A. Jha et al. 10.1029/2023JG007389
- Chemodiversity controls microbial assimilation of soil organic carbon: A theoretical model J. Weverka et al. 10.1016/j.soilbio.2023.109161
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- Micro on a macroscale: relating microbial-scale soil processes to global ecosystem function D. Smercina et al. 10.1093/femsec/fiab091
- Microbial evolution—An under‐appreciated driver of soil carbon cycling E. Abs et al. 10.1111/gcb.17268
- How to adequately represent biological processes in modeling multifunctionality of arable soils H. Vogel et al. 10.1007/s00374-024-01802-3
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- Coupling scales in process‐based soil organic carbon modeling including dynamic aggregation S. Zech et al. 10.1002/jpln.202300080
- Accounting for soil architecture and microbial dynamics in microscale models: Current practices in soil science and the path ahead V. Pot et al. 10.1111/ejss.13142
- A framework for modelling soil structure dynamics induced by biological activity K. Meurer et al. 10.1111/gcb.15289
- Denitrification‐Driven Transcription and Enzyme Production at the River‐Groundwater Interface: Insights From Reactive‐Transport Modeling A. Störiko et al. 10.1029/2021WR031584
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- Comparing an exponential respiration model to alternative models for soil respiration components in a Canadian wildfire chronosequence (FireResp v1.0) J. Zobitz et al. 10.5194/gmd-14-6605-2021
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Latest update: 23 Apr 2024
Short summary
Soils are heterogeneous, which results in a nonuniform spatial distribution of substrates and the microorganisms feeding on them. Our results show that the variability in the spatial distribution of substrates and microorganisms at the pore scale is crucial because it affects how fast substrates are used by microorganisms and thus the decomposition rate observed at the soil core scale. This work provides a methodology to include microscale heterogeneity in soil carbon cycling models.
Soils are heterogeneous, which results in a nonuniform spatial distribution of substrates and...
