Articles | Volume 13, issue 6
https://doi.org/10.5194/esurf-13-1205-2025
https://doi.org/10.5194/esurf-13-1205-2025
Research article
 | 
17 Nov 2025
Research article |  | 17 Nov 2025

Spatial assessment of sediment production in a badland catchment using repeat LiDAR surveys, Draix, Alpes de Haute-Provence, France

Yassine Boukhari, Antoine Lucas, Caroline Le Bouteiller, Sébastien Klotz, Gabrielle Chabaud, and Stéphane Jacquemoud

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Cited articles

Alberti, S., Leshchinsky, B., Roering, J., Perkins, J., and Olsen, M. J.: Inversions of landslide strength as a proxy for subsurface weathering, Nature Communications, 13, 6049, https://doi.org/10.1038/s41467-022-33798-5, 2022. a
Antoine, P., Giraud, A., Meunier, M., and Van Asch, T.: Geological and geotechnical properties of the “Terres Noires” in southeastern France: Weathering, erosion, solid transport and instability, Engineering Geology, 40, 223–234, https://doi.org/10.1016/0013-7952(95)00053-4, 1995. a
Ariagno, C., Le Bouteiller, C., van der Beek, P., and Klotz, S.: Sediment export in marly badland catchments modulated by frost-cracking intensity, Draix–Bléone Critical Zone Observatory, SE France, Earth Surf. Dynam., 10, 81–96, https://doi.org/10.5194/esurf-10-81-2022, 2022. a, b, c, d, e
Ariagno, C., Pasquet, S., Le Bouteiller, C., van der Beek, P., and Klotz, S.: Seasonal dynamics of marly badlands illustrated by field records of hillslope regolith properties, Draix–Bléone Critical Zone Observatory, South‐East France, Earth Surface Processes and Landforms, 48, 1526–1539, https://doi.org/10.1002/esp.5564, 2023. a, b, c, d
Badoux, A., Turowski, J. M., Mao, L., Mathys, N., and Rickenmann, D.: Rainfall intensity–duration thresholds for bedload transport initiation in small Alpine watersheds, Nat. Hazards Earth Syst. Sci., 12, 3091–3108, https://doi.org/10.5194/nhess-12-3091-2012, 2012. a
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Short summary
We combine aerial and drone Light Detection and Ranging surveys with sediment export and density measurements to assess catchment-scale mass balance in a badland environment. Landslides and crest failures are found to contribute 15 % of total mass export while affecting only 1 % of bare surfaces. Flood-condition drainage reconstruction shows low-drainage areas export 3.5 times more sediment than other slopes.
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