Articles | Volume 10, issue 1
https://doi.org/10.5194/soil-10-167-2024
https://doi.org/10.5194/soil-10-167-2024
Original research article
 | 
22 Feb 2024
Original research article |  | 22 Feb 2024

Mineral dust and pedogenesis in the alpine critical zone

Jeffrey S. Munroe, Abigail A. Santis, Elsa J. Soderstrom, Michael J. Tappa, and Ann M. Bauer

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1840', Patrice de Caritat, 04 Oct 2023
  • RC2: 'Comment on egusphere-2023-1840', Ruth Heindel, 06 Oct 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Revision (08 Nov 2023) by Jonathan Maynard
AR by Jeffrey Munroe on behalf of the Authors (09 Nov 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (27 Nov 2023) by Jonathan Maynard
ED: Publish as is (18 Dec 2023) by John Quinton (Executive editor)
AR by Jeffrey Munroe on behalf of the Authors (22 Dec 2023)  Manuscript 
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Short summary
This study investigated how the deposition of mineral dust delivered by the wind influences soil development in mountain environments. At six mountain locations in the southwestern United States, modern dust was collected along with samples of soil and local bedrock. Analysis indicates that at all sites the properties of dust and soil are very similar and are very different from underlying rock. This result indicates that soils are predominantly composed of dust delivered by the wind over time.