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滑坡侵蚀作用下的运动机制。

The mechanics of landslide mobility with erosion.

作者信息

Pudasaini Shiva P, Krautblatter Michael

机构信息

Technical University of Munich, Chair of Landslide Research, Arcisstrasse 21, 80333, Munich, Germany.

University of Bonn, Institute of Geosciences, Geophysics Section, Meckenheimer Allee 176, 53115, Bonn, Germany.

出版信息

Nat Commun. 2021 Nov 23;12(1):6793. doi: 10.1038/s41467-021-26959-5.

Abstract

Erosion can significantly increase the destructive power of a landslide by amplifying its volume, mobility and impact force. The threat posed by an erosive landslide is linked to its mobility. No mechanical condition has yet been presented for when, how and how much energy erosive landslides gain or lose. Here, we pioneer a mechanical model for the energy budget of erosive landslides that controls enhanced or reduced mobility. Inertia is related to an entrainment velocity, is a fundamentally new understanding. This ascertains the true inertia of erosive landslides, making a breakthrough in correctly determining the landslide mobility. Erosion velocity, which regulates the energy budget, determines the enhanced or reduced mobility. Newly developed energy generator offers the first-ever mechanical quantification of erosional energy and a precise description of mobility. This addresses the long-standing question of why many erosive landslides generate higher mobility, while others reduce mobility. We demonstrate that erosion and entrainment are different processes. Landslides gain energy and enhance mobility if the erosion velocity exceeds the entrainment velocity. Energy velocity delineates distinct excess energy regimes. Newly introduced mobility scaling and erosion number deliver the explicit measure of mobility. Presented dynamical equations correctly include erosion induced net momentum production.

摘要

侵蚀可通过增大滑坡的体积、移动性和冲击力,显著增强其破坏力。侵蚀性滑坡所构成的威胁与其移动性相关。目前尚未有关于侵蚀性滑坡在何时、如何以及获得或损失多少能量的力学条件。在此,我们开创了一个用于侵蚀性滑坡能量收支的力学模型,该模型控制着滑坡移动性的增强或减弱。惯性与夹带速度相关,这是一种全新的基本认识。这确定了侵蚀性滑坡的真正惯性,在正确确定滑坡移动性方面取得了突破。调节能量收支的侵蚀速度决定了移动性的增强或减弱。新开发的能量发生器首次对侵蚀能量进行了力学量化,并对移动性进行了精确描述。这解决了一个长期存在的问题,即为何许多侵蚀性滑坡具有更高的移动性,而其他一些则降低了移动性。我们证明侵蚀和夹带是不同的过程。如果侵蚀速度超过夹带速度,滑坡就会获得能量并增强移动性。能量速度界定了不同的过剩能量状态。新引入的移动性标度和侵蚀数给出了移动性的明确度量。所提出的动力学方程正确地包含了侵蚀引起的净动量产生。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e865/8611095/eadbf096a2c4/41467_2021_26959_Fig1_HTML.jpg

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