Biogeosciences
Biogeosciences
BG
Articles | Volume 22, issue 7
Articles | Volume 22, issue 7
https://doi.org/10.5194/bg-22-1907-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-22-1907-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 22, issue 7
Research article
 | 
17 Apr 2025
Research article |  | 17 Apr 2025

Modelling the effect of climate–substrate interactions on soil organic matter decomposition with the Jena Soil Model

Marleen Pallandt, Marion Schrumpf, Holger Lange, Markus Reichstein, Lin Yu, and Bernhard Ahrens

Viewed

Total article views: 787 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
590 163 34 787 29 32
  • HTML: 590
  • PDF: 163
  • XML: 34
  • Total: 787
  • BibTeX: 29
  • EndNote: 32
Views and downloads (calculated since 29 Jan 2024)
Cumulative views and downloads (calculated since 29 Jan 2024)

Viewed (geographical distribution)

Total article views: 787 (including HTML, PDF, and XML) Thereof 773 with geography defined and 14 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 18 Apr 2025
Download
Short summary
As soils warm due to climate change, soil organic carbon (SOC) decomposes faster due to increased microbial activity, given sufficient available moisture. We modelled the microbial decomposition of plant litter and residue at different depths and found that deep soil layers are more sensitive than topsoils. Warming causes SOC loss, but its extent depends on the litter type and its temperature sensitivity, which can either counteract or amplify losses. Droughts may also counteract warming-induced SOC losses.
Read more
Share
Altmetrics
Final-revised paper
Preprint