Scale-invariance of soil moisture variability and its implications for the frequency-size distribution of landslides

Details Scale-invariance of soil moisture variability and its implications for the frequency-size distribution of landslides Scale-invariance of soil moisture variability and its implications for the frequency-size distribution of landslides

1997-05-26

arxiv.org/abs/physics/9705035v1

Physics

Geophysics

latex file, 20 pages, 10 postscript figures

Scientific paper

Power spectral analyses of soil moisture variability are carried out from scales of 100 m to 10 km on the microwave remotely-sensed data from the Washita experimental watershed during 1992. The power spectrum S(k) has an approximately power-law dependence on wave number k with exponent -1.8. This behavior is consistent with the behavior of a stochastic differential equation for soil moisture at a point. This behavior has important consequences for the frequency-size distribution of landslides. We present the cumulative frequency-size distributions of landslides induced by precipitation in Japan and Bolivia as well as landslides triggered by the 1994 Northridge, California earthquake. Large landslides in these regions, despite being triggered by different mechanisms, have a cumulative frequency-size distribution with a power-law dependence on area with an exponent ranging from -1.5 to -2. We use a soil moisture field with the above statistics in conjunction with a slope stability analysis to model the frequency-size distribution of landslides. In our model landslides occur when a threshold shear stress dependent on cohesion, pore pressure, internal friction and slope angle is exceeded. This implies a threshold dependence on soil moisture and slope angle since these factors are primarily dependent on soil moisture. Abstract continued in paper.

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