Articles | Volume 14, issue 1
https://doi.org/10.5194/esurf-14-141-2026
https://doi.org/10.5194/esurf-14-141-2026
Research article
 | 
13 Feb 2026
Research article |  | 13 Feb 2026

A numerical model for duricrust formation by laterisation

Caroline Fenske, Jean Braun, Cécile Robin, and François Guillocheau

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This preprint is open for discussion and under review for Earth Surface Dynamics (ESurf).
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Cited articles

Allard, T., Gautheron, C., Riffel, S. B., Balan, E., Soares, B. F., Pinna-Jamme, R., Derycke, A., Morin, G., Bueno, G. T., and do Nascimento, N.: Combined dating of goethites and kaolinites from ferruginous duricrusts. Deciphering the Late Neogene erosion history of Central Amazonia, Chem. Geol., 479, 136–150, https://doi.org/10.1016/j.chemgeo.2018.01.004, 2018. a, b
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Alonso-Zarza, A. M.: Palaeoenvironmental significance of palustrine carbonates and calcretes in the geological record, Earth-Sci. Rev., 60, 261–298, https://doi.org/10.1016/s0012-8252(02)00106-x, 2003. a, b, c
Anand, R. R.: Weathering History, landscape evolution and implications for exploration, Ore Geol. Rev.,, 16, 167–183, https://doi.org/10.1016/s0169-1368(99)00029-3, 2005. a, b
Anand, R. R. and Paine, M.: Regolith geology of the Yilgarn Craton, Western Australia: implications for exploration, Aust. J. Earth Sci., 49, 3–162, https://doi.org/10.1046/j.1440-0952.2002.00912.x, 2002. a
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Short summary
Duricrusts have contributed valuable insight to the evolving field of regolith science over the past two centuries. These mineral-rich layers occur in diverse settings, from hilltops to valley floors, and are thought to form through two main processes. In 2025, we introduced the first numerical model for the hydrological hypothesis; now, we present a complementary model based on laterisation. This framework simulates both the development of duricrusts and their impact on landscape evolution.
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