Articles | Volume 6, issue 1
https://doi.org/10.5194/soil-6-231-2020
https://doi.org/10.5194/soil-6-231-2020
Original research article
 | 
03 Jun 2020
Original research article |  | 03 Jun 2020

Catchment export of base cations: improved mineral dissolution kinetics influence the role of water transit time

Martin Erlandsson Lampa, Harald U. Sverdrup, Kevin H. Bishop, Salim Belyazid, Ali Ameli, and Stephan J. Köhler

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Oct 2019) by Boris Jansen
AR by Martin Erlandsson Lampa on behalf of the Authors (30 Dec 2019)  Author's response   Manuscript 
ED: Publish as is (27 Jan 2020) by Boris Jansen
ED: Publish as is (27 Jan 2020) by Jorge Mataix-Solera (Executive editor)
AR by Martin Erlandsson Lampa on behalf of the Authors (21 Feb 2020)
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Short summary
In this study, we demonstrate how new equations describing base cation release from mineral weathering can reproduce patterns in observations from stream and soil water. This is a major step towards modeling base cation cycling on the catchment scale, which would be valuable for defining the highest sustainable rates of forest harvest and levels of acidifying deposition.