The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development

We compare analogue and numerical models of dilatational fractures at low confining stress. These structures form an effective conduit for fluid flow in the field, but are difficult to model since they form in cohesive materials at low stresses. We use a truly cohesive powder for the analogue mod...

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Main Authors: Urai J.L., Abe S., van Gent H, Holland M.
Format: Article
Language:English
Published: EDP Sciences 2010-06-01
Series:EPJ Web of Conferences
Online Access:http://dx.doi.org/10.1051/epjconf/20100622016
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spelling doaj-87c2e9965e9e480d9eb539327ed477de2021-08-02T01:13:40ZengEDP SciencesEPJ Web of Conferences2100-014X2010-06-0162201610.1051/epjconf/20100622016The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity developmentUrai J.L.Abe S.van Gent HHolland M.We compare analogue and numerical models of dilatational fractures at low confining stress. These structures form an effective conduit for fluid flow in the field, but are difficult to model since they form in cohesive materials at low stresses. We use a truly cohesive powder for the analogue models and a Discrete Element Model (DEM) with brittle-elastic bonds for the numerical modelling. We show that despite variations in the model type, small differences in the location of initial fractures and the way these structures link-up to control the evolution of the model, the observed structures are robust. Three structural zones develop where different fault types dominate. In 3D numerical models we show an increase of the porosity on the fault zone with increasing deformation. The progradation direction is shown to be controlled by the position of the fracture. The combination of analogue models with cohesive powder and DEMs with internal cohesion is an excellent tool to study the evolution of open fractures. http://dx.doi.org/10.1051/epjconf/20100622016
collection DOAJ
language English
format Article
sources DOAJ
author Urai J.L.
Abe S.
van Gent H
Holland M.
spellingShingle Urai J.L.
Abe S.
van Gent H
Holland M.
The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
EPJ Web of Conferences
author_facet Urai J.L.
Abe S.
van Gent H
Holland M.
author_sort Urai J.L.
title The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
title_short The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
title_full The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
title_fullStr The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
title_full_unstemmed The formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
title_sort formation of open fractures in cohesive materials, results of scaled analogue and numerical modelling on fault zone porosity development
publisher EDP Sciences
series EPJ Web of Conferences
issn 2100-014X
publishDate 2010-06-01
description We compare analogue and numerical models of dilatational fractures at low confining stress. These structures form an effective conduit for fluid flow in the field, but are difficult to model since they form in cohesive materials at low stresses. We use a truly cohesive powder for the analogue models and a Discrete Element Model (DEM) with brittle-elastic bonds for the numerical modelling. We show that despite variations in the model type, small differences in the location of initial fractures and the way these structures link-up to control the evolution of the model, the observed structures are robust. Three structural zones develop where different fault types dominate. In 3D numerical models we show an increase of the porosity on the fault zone with increasing deformation. The progradation direction is shown to be controlled by the position of the fracture. The combination of analogue models with cohesive powder and DEMs with internal cohesion is an excellent tool to study the evolution of open fractures.
url http://dx.doi.org/10.1051/epjconf/20100622016
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