Biogeosciences
Biogeosciences
BG
Articles | Volume 20, issue 3
Articles | Volume 20, issue 3
https://doi.org/10.5194/bg-20-635-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-635-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 3
BG Letters
 | Highlight paper
 | 
16 Feb 2023
BG Letters | Highlight paper |  | 16 Feb 2023

Reconciling the paradox of soil organic carbon erosion by water

Kristof Van Oost and Johan Six

Viewed

Total article views: 4,622 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,570 998 54 4,622 37 56
  • HTML: 3,570
  • PDF: 998
  • XML: 54
  • Total: 4,622
  • BibTeX: 37
  • EndNote: 56
Views and downloads (calculated since 14 Jan 2022)
Cumulative views and downloads (calculated since 14 Jan 2022)

Viewed (geographical distribution)

Total article views: 4,622 (including HTML, PDF, and XML) Thereof 4,477 with geography defined and 145 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 19 Apr 2024
Download
Co-editor-in-chief
Application for BG Letter format accepted.
Short summary
The direction and magnitude of the net erosion-induced land–atmosphere C exchange have been the topic of a big scientific debate for more than a decade now. Many have assumed that erosion leads to a loss of soil carbon to the atmosphere, whereas others have shown that erosion ultimately leads to a carbon sink. Here, we show that the soil carbon erosion source–sink paradox is reconciled when the broad range of temporal and spatial scales at which the underlying processes operate are considered.
Read more
Altmetrics
Final-revised paper
Preprint