Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a
<p>Mass movements such as debris flows and landslides differ in behaviour due to their material properties and internal forces. Models employ generalized multi-phase flow equations to adaptively describe these complex flow types. Such models commonly assume unstructured and fragmented flow, wh...
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doaj-04cb1843cf6b47dab958ef95b18928152021-04-06T10:44:21ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032021-04-01141841186410.5194/gmd-14-1841-2021Towards a model for structured mass movements: the OpenLISEM hazard model 2.0aB. van den Bout0T. van Asch1W. Hu2C. X. Tang3O. Mavrouli4V. G. Jetten5C. J. van Westen6Faculty of Geo-Information Science and Earth Observation, University of Twente, Enschede, the NetherlandsState Key Laboratory of Geohazard Prevention and Geo-Environment Protection, Chengdu University of Technology, Chengdu, ChinaState Key Laboratory of Geohazard Prevention and Geo-Environment Protection, Chengdu University of Technology, Chengdu, ChinaInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, ChinaFaculty of Geo-Information Science and Earth Observation, University of Twente, Enschede, the NetherlandsFaculty of Geo-Information Science and Earth Observation, University of Twente, Enschede, the NetherlandsFaculty of Geo-Information Science and Earth Observation, University of Twente, Enschede, the Netherlands<p>Mass movements such as debris flows and landslides differ in behaviour due to their material properties and internal forces. Models employ generalized multi-phase flow equations to adaptively describe these complex flow types. Such models commonly assume unstructured and fragmented flow, where internal cohesive strength is insignificant. In this work, existing work on two-phase mass movement equations are extended to include a full stress–strain relationship that allows for runout of (semi-)structured fluid–solid masses. The work provides both the three-dimensional equations and depth-averaged simplifications. The equations are implemented in a hybrid material point method (MPM), which allows for efficient simulation of stress–strain relationships on discrete smooth particles. Using this framework, the developed model is compared to several flume experiments of clay blocks impacting fixed obstacles. Here, both final deposit patterns and fractures compare well to simulations. Additionally, numerical tests are performed to showcase the range of dynamical behaviour produced by the model. Important processes such as fracturing, fragmentation and fluid release are captured by the model. While this provides an important step towards complete mass movement models, several new opportunities arise, such as application to fragmenting mass movements and block slides.</p>https://gmd.copernicus.org/articles/14/1841/2021/gmd-14-1841-2021.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
B. van den Bout T. van Asch W. Hu C. X. Tang O. Mavrouli V. G. Jetten C. J. van Westen |
spellingShingle |
B. van den Bout T. van Asch W. Hu C. X. Tang O. Mavrouli V. G. Jetten C. J. van Westen Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a Geoscientific Model Development |
author_facet |
B. van den Bout T. van Asch W. Hu C. X. Tang O. Mavrouli V. G. Jetten C. J. van Westen |
author_sort |
B. van den Bout |
title |
Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a |
title_short |
Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a |
title_full |
Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a |
title_fullStr |
Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a |
title_full_unstemmed |
Towards a model for structured mass movements: the OpenLISEM hazard model 2.0a |
title_sort |
towards a model for structured mass movements: the openlisem hazard model 2.0a |
publisher |
Copernicus Publications |
series |
Geoscientific Model Development |
issn |
1991-959X 1991-9603 |
publishDate |
2021-04-01 |
description |
<p>Mass movements such as debris flows and landslides differ in behaviour due to
their material properties and internal forces. Models employ generalized
multi-phase flow equations to adaptively describe these complex flow types.
Such models commonly assume unstructured and fragmented flow, where internal
cohesive strength is insignificant. In this work, existing work on two-phase
mass movement equations are extended to include a full stress–strain
relationship that allows for runout of (semi-)structured fluid–solid
masses. The work provides both the three-dimensional equations and
depth-averaged simplifications. The equations are implemented in a hybrid
material point method (MPM), which allows for efficient simulation of
stress–strain relationships on discrete smooth particles. Using this
framework, the developed model is compared to several flume experiments of
clay blocks impacting fixed obstacles. Here, both final deposit patterns and
fractures compare well to simulations. Additionally, numerical tests are
performed to showcase the range of dynamical behaviour produced by the model.
Important processes such as fracturing, fragmentation and fluid release are
captured by the model. While this provides an important step towards
complete mass movement models, several new opportunities arise, such as
application to fragmenting mass movements and block slides.</p> |
url |
https://gmd.copernicus.org/articles/14/1841/2021/gmd-14-1841-2021.pdf |
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