Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics

A method to predict the most probable flow rheology in Alpine debris flows is presented. The methods classifies outcropping rock masses in catchments on the basis of the type of resulting unconsolidated deposits. The grain size distribution of the debris material and the depositional style of past d...

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Main Authors: Davide eTiranti, Chiara eDeangeli
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-03-01
Series:Frontiers in Earth Science
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/feart.2015.00008/full
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author Davide eTiranti
Chiara eDeangeli
author_facet Davide eTiranti
Chiara eDeangeli
author_sort Davide eTiranti
collection DOAJ
description A method to predict the most probable flow rheology in Alpine debris flows is presented. The methods classifies outcropping rock masses in catchments on the basis of the type of resulting unconsolidated deposits. The grain size distribution of the debris material and the depositional style of past debris flow events are related to the dominant flow processes: viscoplastic and frictional/collisional. Three catchments in the upper Susa Valley (Western Alps), characterized by different lithologies, were selected for numerical analysis carried out with a Cellular Automata code with viscoplastic and frictional/collisional rheologies. The obtained numerical results are in good agreement with in site evidences in terms of depositional patterns, confirming the possibility of choosing the rheology of the debris flow based on the source material within the catchment.
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spelling doaj.art-7f7982f5ff81418f9325c0ba07b15cb42022-12-22T03:21:21ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632015-03-01310.3389/feart.2015.00008120019Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristicsDavide eTiranti0Chiara eDeangeli1Regional Agency for Environmental Protection of PiemontePolitecnico di TorinoA method to predict the most probable flow rheology in Alpine debris flows is presented. The methods classifies outcropping rock masses in catchments on the basis of the type of resulting unconsolidated deposits. The grain size distribution of the debris material and the depositional style of past debris flow events are related to the dominant flow processes: viscoplastic and frictional/collisional. Three catchments in the upper Susa Valley (Western Alps), characterized by different lithologies, were selected for numerical analysis carried out with a Cellular Automata code with viscoplastic and frictional/collisional rheologies. The obtained numerical results are in good agreement with in site evidences in terms of depositional patterns, confirming the possibility of choosing the rheology of the debris flow based on the source material within the catchment.http://journal.frontiersin.org/Journal/10.3389/feart.2015.00008/fullWestern AlpsCatchment lithologytorrential sedimentary processesflow rheologycellular automata model
spellingShingle Davide eTiranti
Chiara eDeangeli
Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
Frontiers in Earth Science
Western Alps
Catchment lithology
torrential sedimentary processes
flow rheology
cellular automata model
title Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
title_full Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
title_fullStr Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
title_full_unstemmed Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
title_short Modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
title_sort modeling of debris flow depositional patterns according to the catchments and sediment source areas characteristics
topic Western Alps
Catchment lithology
torrential sedimentary processes
flow rheology
cellular automata model
url http://journal.frontiersin.org/Journal/10.3389/feart.2015.00008/full
work_keys_str_mv AT davideetiranti modelingofdebrisflowdepositionalpatternsaccordingtothecatchmentsandsedimentsourceareascharacteristics
AT chiaraedeangeli modelingofdebrisflowdepositionalpatternsaccordingtothecatchmentsandsedimentsourceareascharacteristics