T162 Debris Flow, Landslide, and Rockfall: Initiation, Prediction, and Warning
Tuesday, 30 October 2007
1:30 PM - 5:30 PM
THE VELOCITIES AND IMPACT FORCES OF DIFFERENT SIZE PARTICLES WITHIN DEBRIS FLOWS
Paper number: T162-8
Program: Technical Sessions
Time: 3:40 PM – 3:55 PM
Authors
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Paul M. SantiColorado School of Mines, Golden, CO
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Jerry D. HigginsColorado School of Mines, Golden, CO
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Susan H. CannonU.S. Geological Survey, Denver, CO
Abstract
Particle velocity was found to decrease with increasing particle size on the surface of granular flows where no matrix material was present between boulders and for fluid flows where few large-particle interactions occurred. No trend was found between particle velocity and particle size for flows that contained a high concentration of boulders within a viscous matrix.
For all analyzed flows, calculated impact forces were found to increase with increasing particle size. However, maximum impact forces commonly resulted from particles whose sizes were 60 to 90 percent of the largest particle within the flow.