Colluvial deposits as  a possible weathering reservoir in uplifting mountains

Carretier, Sébastien; Goddéris, Yves; Martinez, Javier; Reich, Martin; Martinod, Pierre

doi:https://doi.org/10.5194/esurf-6-217-2018

Articles | Volume 6, issue 1

https://doi.org/10.5194/esurf-6-217-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/esurf-6-217-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 6, issue 1

Research article

| Highlight paper

|

21 Mar 2018

Research article | Highlight paper |

| 21 Mar 2018

Colluvial deposits as a possible weathering reservoir in uplifting mountains

Sébastien Carretier, Yves Goddéris, Javier Martinez, Martin Reich, and Pierre Martinod

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Dec 2022	59	11	1	71
Jan 2023	51	18	3	72
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Jun 2024	305	13	5	323
Jul 2024	64	7	2	73
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Cumulative views and downloads (calculated since 28 Aug 2017)

Month	HTML	PDF	XML	Total
Aug 2017	110	37	4	151
Sep 2017	72	21	0	93
Oct 2017	72	12	1	85
Nov 2017	57	6	0	63
Dec 2017	26	5	0	31
Jan 2018	39	6	0	45
Feb 2018	39	6	10	55
Mar 2018	276	82	7	365
Apr 2018	208	48	4	260
May 2018	100	28	6	134
Jun 2018	79	23	0	102
Jul 2018	43	12	2	57
Aug 2018	70	14	2	86
Sep 2018	49	9	0	58
Oct 2018	65	23	1	89
Nov 2018	53	30	1	84
Dec 2018	45	13	2	60
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Jun 2020	84	30	2	116
Jul 2020	83	57	17	157
Aug 2020	55	7	2	64
Sep 2020	68	26	0	94
Oct 2020	65	13	2	80
Nov 2020	38	10	1	49
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Jul 2023	13	6	0	19
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Apr 2024	53	21	4	78
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Short summary

The role of mountain uplift and associated silicate weathering in the global climate over geological times is controversial. Previous soil column models suggest that weathering falls at a high denudation rate. We present the results of a 3-D model that couples erosion and weathering, a CO₂ consumer during mountain uplift. Our model suggests that the weathering of temporarily stocked colluvium may contribute significantly to the mountain weathering outflux at high denudation rates.