Lithium isotope signatures of weathering in the hyper-arid climate of the western Tibetan Plateau

Abstract Biogeochemical cycling within the Critical Zone depends on the interactions between minerals and fluids controlling chemical weathering and physical erosion rates. In this study, we explore the role of water availability in controlling soil chemical weathering in semiarid climatic conditions. Weathering rates and intensities were evaluated for nine soil profiles located on convex ridge crests of three mountain ranges in the Spanish Betic Cordillera. We combine a geochemical mass balance with 10 Be cosmogenic nuclides to constrain chemical weathering intensities and long‐term denudation rates. As such, this study presents new data on chemical weathering and 10 Be‐derived denudation for understudied semiarid climate systems. In the Betic Cordillera, chemical weathering intensities are relatively low (~5 to 30% of the total denudation of the soil) and negatively correlated with the magnitude of the water deficit in soils. Chemical mass losses are inversely related to denudation rates (14–109 mm/kyr) and positively to soil thickness (14–58 cm); these results are consistent with kinetic limitation of chemical weathering rates. A worldwide compilation of chemical weathering data suggests that soil water balance may regulate the coupling between chemical weathering and physical erosion by modulating soil solute fluxes. Therefore, future landscape evolution models that seek to link chemical weathering and physical erosion should include soil water flux as an essential driver of weathering.

Denudation

Soil production function

Biogeochemical Cycle

Cosmogenic nuclide

10.1002/2015jf003626

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Competition between erosion and reaction kinetics in controlling silicate-weathering rates

Earth and Planetary Science Letters (2010)

G. E. Hilley C. Page Chamberlain Seulgi Moon Stephen Porder Sean D. Willett

Denudation

Silicate minerals

10.1016/j.epsl.2010.01.008

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Citations (143)