SOIL
SOIL
SOIL
Articles | Volume 10, issue 1
Articles | Volume 10, issue 1
https://doi.org/10.5194/soil-10-275-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-10-275-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 10, issue 1
SOIL Letters
 | Highlight paper
 | 
15 Apr 2024
SOIL Letters | Highlight paper |  | 15 Apr 2024

The six rights of how and when to test for soil C saturation

Johan Six, Sebastian Doetterl, Moritz Laub, Claude R. Müller, and Marijn Van de Broek

Viewed

Total article views: 3,563 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,842 645 76 3,563 51 62
  • HTML: 2,842
  • PDF: 645
  • XML: 76
  • Total: 3,563
  • BibTeX: 51
  • EndNote: 62
Views and downloads (calculated since 07 Nov 2023)
Cumulative views and downloads (calculated since 07 Nov 2023)

Viewed (geographical distribution)

Total article views: 3,563 (including HTML, PDF, and XML) Thereof 3,415 with geography defined and 148 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Executive editor
This manuscript is published as SOIL Letters publication as it provides a timely and important contribution, formulating six fundamental principles for the robust study of soil carbon saturation. This is an important topic in research on soil carbon and its role in climate change mitigation which should be of interest to the wider geoscience community.
Read more
Short summary
Soil C saturation has been tested in several recent studies and led to a debate about its existence. We argue that, to test C saturation, one should pay attention to six fundamental principles: the right measures, the right units, the right dispersive energy and application, the right soil type, the right clay type, and the right saturation level. Once we take care of those six rights across studies, we find support for a maximum of C stabilized by minerals and thus soil C saturation.
Read more