A general two-phase debris flow model

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A mechanical erosion model for two-phase mass flows (2016, methodology): “(2) These solid and fluid momentum equations are rigorously derived (Pudasaini, 2012) and include the solid and fluid momentum production terms, second terms on the right hand sides.”
The hypermobility of huge landslides and avalanches (2013, background): “However, Λ can be mathematically analogous to the fluid volume fraction (Pudasaini et al., 2005; Pudasaini, 2012), or any other possible mechanism (see, Section 1) that reduces the basal shear resistance such as dynamic fragmentation (McSaveney”
r.avaflow v1, an advanced open-source computational framework for the propagation and interaction of two-phase mass flows (2016, unknown): “…detail Full handling of the evolution of the basal topography within the TVD-NOC scheme is not straightforward and could also produce some diffusion Therefore, as entrainment is not included in the original Pudasaini (2012) model, entrainment is treated as a complementary function in a ﬁrst step .”