EGU26-6540, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-6540
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Friday, 08 May, 08:30–10:15 (CEST), Display time Friday, 08 May, 08:30–12:30
 
Hall X3, X3.21
Towards systematic measurements of velocity profiles and sediment concentration in a wide range of laboratory debris-flow mixtures
Felix Maximilian Klein, Maximilian Ender, Georg Nagl, and Roland Kaitna
Felix Maximilian Klein et al.
  • BOKU University, Department of Landscape, Water and Infrastructure, Institute of Mountain Risk Engineering, Vienna, Austria (felix.klein@boku.ac.at)

Debris-flow dynamics are governed by the internal deformation of sediment–water mixtures. Due to the destructive potential of natural debris flows, constitutive models predicting flow velocity, impact forces, erosion, and deposition are desired. While simplified sediment–water flows are well understood, existing debris-flow models typically rely on constitutive assumptions for internal friction, sediment concentration, and solid–fluid interaction. Systematic experiments exploring the effects of grain-size distribution and fine material content on internal deformation and flow resistance are essential to better constrain and improve these models.

In this work we introduce a novel methodological setup to measure vertical velocity profiles within steady shallow (~15 cm) flows of sediment–water mixtures in a ~2.5 m diameter rotating drum. Measurements are performed in the central, most uniform flow region using an array of paired-conductivity sensors of varying geometry. Velocities are obtained via established cross-correlation methods of adjacent signals. Spectral properties of the conductivity signals are also explored as a potential complementary source of velocity information.

A low-cost capacitance probe is being developed to enable non-intrusive estimation of sediment concentration during flow. Proof-of-concept tests in air demonstrate feasibility, and further testing in water is planned to realize its use in ongoing experiments. Upcoming work will systematically investigate how grain-size distribution, particularly the fine material content and the uniformity of the coarse fraction, influence internal deformation, pore-fluid pressure, and bulk flow resistance.

How to cite: Klein, F. M., Ender, M., Nagl, G., and Kaitna, R.: Towards systematic measurements of velocity profiles and sediment concentration in a wide range of laboratory debris-flow mixtures, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-6540, https://doi.org/10.5194/egusphere-egu26-6540, 2026.