ON THE INFLUENCE OF TURBULENCE ON THE INITIATION OF SEDIMENT MOTION

By U. Zanke. 2003

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Role of instantaneous force magnitude and duration on particle entrainment (2010, background): “…1949; Sutherland, 1967; Nelson et al., 1995; Cheng and Chiew, 1998; Sechet and Le Guennec, 1999; Schmeeckle and Nelson, 2003; Sumer et al., 2003; Zanke, 2003; Hofland et al., 2005; Smart and Habersack, 2007], here the role of duration of force is analytically and experimentally demonstrated to…”
Flow discharge and sediment transport models for estimating a minimum timescale of hydrological activity and channel and delta formation on Mars (2005, unknown): “Various criteria for incipient motion are given to demonstrate the limited variability (fit through the original Shields data and Soulsby [1997] and Zanke [2003]).”
Seamless cross-scale modeling with SCHISM (2016, background): “2012), SED2D (Dodet 2013), and TIMOR (Zanke 2003)), 2 biological/ecological models (EcoSIM 86 (Rodrigues et al.”
Double-Averaged Open-Channel Flows with Small Relative Submergence (2007, background): “Such results have important consequences in other contexts, such as the prediction of grain entrainment in sediment transport, where they show that for lower relative submergences the critical shear stress must be higher than for higher submergences Zanke 2003 .”