Biogeosciences
Biogeosciences
BG
Articles | Volume 12, issue 22
Articles | Volume 12, issue 22
https://doi.org/10.5194/bg-12-6791-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-12-6791-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 12, issue 22
Research article
 | 
27 Nov 2015
Research article |  | 27 Nov 2015

Evaluating sensitivity of silicate mineral dissolution rates to physical weathering using a soil evolution model (SoilGen2.25)

E. Opolot and P. A. Finke

Viewed

Total article views: 2,546 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,163 1,077 306 2,546 115 117
  • HTML: 1,163
  • PDF: 1,077
  • XML: 306
  • Total: 2,546
  • BibTeX: 115
  • EndNote: 117
Views and downloads (calculated since 26 Aug 2015)
Cumulative views and downloads (calculated since 26 Aug 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 15 Nov 2024
Download
Short summary
This study evaluated the sensitivity of silicate mineral dissolution rates to intrinsic and extrinsic factors using a soil evolution model, SoilGen2.25. Modelling results showed a dominant role of pH and a direct effect of soil texture on dissolution rates. Clay migration and plant nutrient recycling influenced the pH and thus the dissolution rates. These results demonstrate the need to couple different soil processes in order to explain differences between lab and field dissolution rates.
Read more
Altmetrics
Final-revised paper
Preprint