山坡风化表层碎石爬行机理研究
THE STUDY OF CRUSHED STONE CRAWL MECHANISM ON HILLSLOPES OF WEATHERED SURFACE
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摘要: 山坡风化表层碎石爬行运动是存在于自然界、受多种环境因素影响的一种地表缓慢地质变形现象。本文在介绍有关现场试验测量方法的基础上,通过对测量数据和实地观察结果的分析研究,初步描述了这一自然现象的运动机理和存在的运动形式,并提出了对这一自然现象进行可能的力学、数学模拟研究的初步设想和尝试。Abstract: The Ccrawl movement of crushed stone on hillslopes of weathered surface is a natural and dependent varied environmental slow geological deformation.This paper described the movement mechanism of this natural phenomenon and its movementform,besed on the study of surveying data and observation from a seious of in - site trialsurveying methods.Thisalso posed the preliminaly assumptions and trials of the possible mechanical and mathematical models for this natural phenomenon.
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