Dynamic rock fragmentation: thresholds for long runout rock avalanches

The dynamic fragmentation of rock within rock avalanches is examined using the fragmentation concepts introduced by Grady and co-workers. The analyses use typical material values for weak chalk and limestone in order to determine theoretical strain rate thresholds for dynamic fragmentation and res...

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Main Author: E.T. Bowman
Format: Article
Language:English
Published: Gruppo Italiano Frattura 2014-10-01
Series:Fracture and Structural Integrity
Subjects:
Online Access:http://www.gruppofrattura.it/pdf/rivista/numero30/numero_30_art_2.pdf
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author E.T. Bowman
author_facet E.T. Bowman
author_sort E.T. Bowman
collection DOAJ
description The dynamic fragmentation of rock within rock avalanches is examined using the fragmentation concepts introduced by Grady and co-workers. The analyses use typical material values for weak chalk and limestone in order to determine theoretical strain rate thresholds for dynamic fragmentation and resulting fragment sizes. These are found to compare favourably with data obtained from field observations of long runout rock avalanches and chalk cliff collapses in spite of the simplicity of the approach used. The results provide insight as to the energy requirements to develop long runout behaviour and hence may help to explain the observed similarities between large rock avalanches and much smaller scale chalk cliff collapses as seen in Europe.
format Article
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institution Kabale University
issn 1971-8993
1971-8993
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publishDate 2014-10-01
publisher Gruppo Italiano Frattura
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series Fracture and Structural Integrity
spelling doaj-art-295bb97a134d4f13a6f414667a29aeb82024-12-02T07:12:27ZengGruppo Italiano FratturaFracture and Structural Integrity1971-89931971-89932014-10-0183071310.3221/IGF-ESIS.30.02Dynamic rock fragmentation: thresholds for long runout rock avalanchesE.T. Bowman0University of SheffieldThe dynamic fragmentation of rock within rock avalanches is examined using the fragmentation concepts introduced by Grady and co-workers. The analyses use typical material values for weak chalk and limestone in order to determine theoretical strain rate thresholds for dynamic fragmentation and resulting fragment sizes. These are found to compare favourably with data obtained from field observations of long runout rock avalanches and chalk cliff collapses in spite of the simplicity of the approach used. The results provide insight as to the energy requirements to develop long runout behaviour and hence may help to explain the observed similarities between large rock avalanches and much smaller scale chalk cliff collapses as seen in Europe.http://www.gruppofrattura.it/pdf/rivista/numero30/numero_30_art_2.pdfFlowDynamic fragmentationRock avalancheStrain rate
spellingShingle E.T. Bowman
Dynamic rock fragmentation: thresholds for long runout rock avalanches
Fracture and Structural Integrity
Flow
Dynamic fragmentation
Rock avalanche
Strain rate
title Dynamic rock fragmentation: thresholds for long runout rock avalanches
title_full Dynamic rock fragmentation: thresholds for long runout rock avalanches
title_fullStr Dynamic rock fragmentation: thresholds for long runout rock avalanches
title_full_unstemmed Dynamic rock fragmentation: thresholds for long runout rock avalanches
title_short Dynamic rock fragmentation: thresholds for long runout rock avalanches
title_sort dynamic rock fragmentation thresholds for long runout rock avalanches
topic Flow
Dynamic fragmentation
Rock avalanche
Strain rate
url http://www.gruppofrattura.it/pdf/rivista/numero30/numero_30_art_2.pdf
work_keys_str_mv AT etbowman dynamicrockfragmentationthresholdsforlongrunoutrockavalanches