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Concentration‐discharge relationships of dissolved rhenium in Alpine catchments reveal its use as a tracer of oxidative weathering

Hilton, Robert G.; Turowski, Jens M.; Winnick, Matthew; Dellinger, Mathieu; Schleppi, Patrick; Williams, Kenneth H.; Lawrence, Corey R.; Maher, Katharine; West, Martin; Hayton, Amanda

Authors

Robert G. Hilton

Jens M. Turowski

Matthew Winnick

Mathieu Dellinger

Patrick Schleppi

Kenneth H. Williams

Corey R. Lawrence

Katharine Maher

Profile image of Martin West

Martin West m.d.west@durham.ac.uk
Senior Analytical Experimental Officer

Profile image of Amanda Hayton

Amanda Hayton a.j.hayton@durham.ac.uk
Analytical Experimental Officer



Abstract

Oxidative weathering of sedimentary rocks plays an important role in the global carbon cycle. Rhenium (Re) has been proposed as a tracer of rock organic carbon (OCpetro) oxidation. However, the sources of Re and its mobilization by hydrological processes remain poorly constrained. Here, we examine dissolved Re as a function of water discharge, using samples collected from three alpine catchments that drain sedimentary rocks in Switzerland (Erlenbach and Vogelbach) and Colorado, USA (East River). The Swiss catchments reveal a higher dissolved Re flux in the catchment with higher erosion rates, but have similar [Re]/[Na+] and [Re]/[SO42−] ratios, which indicate a dominance of Re from OCpetro. Despite differences in rock type and hydro-climatic setting, the three catchments have a positive correlation between river water [Re]/[Na+] and [Re]/[SO42−] and water discharge. We propose that this reflects preferential routing of Re from a near-surface, oxidative weathering zone. The observations support the use of Re as a proxy to trace rock-organic carbon oxidation, and suggest it may be a hydrological tracer of vadose zone processes. We apply the Re proxy and estimate CO2 release by OCpetro oxidation of 5.7 +6.6/−2.0 tC km−2 yr−1 for the Erlenbach. The overall weathering intensity was ∼40%, meaning that the corresponding export of unweathered OCpetro in river sediments is large, and the findings call for more measurements of OCpetro oxidation in mountains and rivers as they cross floodplains.

Citation

Hilton, R. G., Turowski, J. M., Winnick, M., Dellinger, M., Schleppi, P., Williams, K. H., Lawrence, C. R., Maher, K., West, M., & Hayton, A. (2021). Concentration‐discharge relationships of dissolved rhenium in Alpine catchments reveal its use as a tracer of oxidative weathering. Water Resources Research, 57(11), Article e2021WR029844. https://doi.org/10.1029/2021wr029844

Journal Article Type Article
Acceptance Date Oct 26, 2021
Online Publication Date Nov 23, 2021
Publication Date Nov 23, 2021
Deposit Date Nov 16, 2021
Publicly Available Date Jan 31, 2022
Journal Water Resources Research
Print ISSN 0043-1397
Electronic ISSN 1944-7973
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 57
Issue 11
Article Number e2021WR029844
DOI https://doi.org/10.1029/2021wr029844
Public URL https://durham-repository.worktribe.com/output/1222820

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