13 citations as recorded by crossref.

1. Mean velocity estimation of viscous debris flows H. Yang et al. https://doi.org/10.1007/s12583-014-0465-z
2. Development of a mechanistic model of granular flow on vibrating screens O. Ogunmodimu et al. https://doi.org/10.1016/j.mineng.2020.106771
3. Overview: Documentation and monitoring of landslides and debris flows for mathematical modelling and design of mitigation measures – outcomes of the EGU 2011, NH session L. Franzi et al. https://doi.org/10.5194/nhess-13-2013-2013
4. Sedankinsky Dol (Sredinny Range, Kamchatka): K–Ar Isotopic Age of Volcanoes, Relationship of Volcanic and Glacial Relief Forms M. Pevzner et al. https://doi.org/10.1134/S0742046321040035
5. Propagation and deposition of stony debris flows at channel confluences L. Stancanelli et al. https://doi.org/10.1002/2015WR017116
6. Influence of Pore Fluid on Grain‐Scale Interactions and Mobility of Granular Flows of Differing Volume A. Taylor‐Noonan et al. https://doi.org/10.1029/2022JF006622
7. Physical modelling to map the rheological and morphological dynamics along with entrainment mechanics of debris flow: a comprehensive review of the state of the art M. Bilal & R. Kumar https://doi.org/10.1186/s40677-025-00349-1
8. Influence of fine sediment on the fluidity of debris flows N. Hotta et al. https://doi.org/10.1007/s11629-013-2522-y
9. An Approach to Predict Debris Flow Average Velocity C. Cao et al. https://doi.org/10.3390/w9030205
10. Laboratory investigation of the effects of grain size on the dynamics of debris flows: Measurement of pore fluid pressure in an open channel Y. Sakai et al. https://doi.org/10.1051/e3sconf/202341501022
11. The Effects of Particle Segregation on Debris Flow Fluidity Over a Rigid Bed N. Hotta et al. https://doi.org/10.2113/EEG-D-20-00106
12. The role of the phase shift of fine particles on debris flow behavior: an numerical simulation for a debris flow in Illgraben, Switzerland T. Uchida et al. https://doi.org/10.1139/cgj-2019-0452
13. Field monitoring of pore water pressure in fully and partly saturated debris flows at Ohya landslide scar, Japan S. Oya et al. https://doi.org/10.5194/esurf-12-67-2024