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The role of pore pressures on the mechanics of mudslides

机译:孔隙压力对泥石流力学的作用

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摘要

Mudslides are complex phenomena whose mechanics has not yet been completely clarified. According to some Authors, mudslide initiation has to be associated with undrained stress conditions which establish at the onset of failure; probably undrained conditions are continuously renewed during following movements as a consequence of further total stress changes. The analysis of the results of long-lasting investigations and monitoring of a number of mudslides in Southern Italy seem to confirm previous hypotheses.
机译:泥石流是复杂现象,其机理尚未完全阐明。一些作者认为,泥石流的发生必须与不排水的应力条件相关联,而应力条件是在破坏开始时就建立的。由于进一步的总应力变化,在随后的运动中不排水的状况可能会不断更新。对意大利南部的长期泥石流进行长期调查和监测的结果的分析似乎证实了先前的假设。

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