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Earth and Space Sciences · 术语表

什么是 Factor of safety, debris flow?

又称: factor of safety · debris flow

Definition 28.7 University Earth and Space Sciences — Year 2 · 第 28 章 — Geological Hazards and Risk

The factor of safety FF of a slope along a potential slip surface is the ratio of the shear strength available on the surface to the shear stress required for equilibrium. The slope is stable for F>1F > 1 and fails when FF falls to 1. A debris flow is a rapid flow of water-saturated mud, sand, gravel, boulders and wood that moves down a channel as one dense mass, the grains carrying much of its weight, and spreads on the fan at the mouth of the channel.

Left: the infinite slope, a layer of thickness z on a slip surface parallel to the ground, with a column of weight W. Right: its factor of safety against the pore-pressure ratio, for c' = 5\, kPa, ' = 35, = 19\, kN\, m-3 and z = 2\, m, at three slope angles. Rising pore pressure brings each slope to failure.
Left: the infinite slope, a layer of thickness z on a slip surface parallel to the ground, with a column of weight W. Right: its factor of safety against the pore-pressure ratio, for c' = 5\, kPa, ' = 35, = 19\, kN\, m-3 and z = 2\, m, at three slope angles. Rising pore pressure brings each slope to failure.
Left: the infinite slope, a layer of thickness zz on a slip surface parallel to the ground, with a column of weight WW. Right: its factor of safety against the pore-pressure ratio, for c′=5 kPac' = 5\,\mathrm{kPa}, φ′=35∘\varphi' = 35{}^{\circ}, γ=19 kN m−3\gamma = 19\,\mathrm{kN}\,\mathrm{m}^{-3} and z=2 mz = 2\,\mathrm{m}, at three slope angles. Rising pore pressure brings each slope to failure.
Debris-flow deposits on the fan of Caraballeda, on the coast of Venezuela, after the storm of December 1999: the flows left the main channel and buried the town under boulders. Photograph: Lawson Smith, U.S. Army Corps of Engineers (public domain).
Debris-flow deposits on the fan of Caraballeda, on the coast of Venezuela, after the storm of December 1999: the flows left the main channel and buried the town under boulders. Photograph: Lawson Smith, U.S. Army Corps of Engineers (public domain).
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