Abstract
1 Sturzstroms are a rare category of rock avalanche that travel
vast horizontal distances with only a comparatively small vertical
drop in height. Their extraordinary mobility appears to be a consequence
of sustained fluid-like behavior during motion, which persists even
for driving stresses well below those normally associated with granular
flows. One mechanism that may explain this temporary increase in
the mobility of rock debris is acoustic fluidization; where transient,
high-frequency pressure fluctuations, generated during the initial
collapse and subsequent flow of a mass of rock debris, may locally
relieve overburden stresses in the rock mass and thus reduce the
frictional resistance to slip between fragments. In this paper we
develop the acoustic fluidization model for the mechanics of sturzstroms
and discuss the conditions under which this process may sustain fluid-like
flow of large rock avalanches at low driving stresses.
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