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...
Main Authors: | , , , |
---|---|
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 |
id |
doaj-87c2e9965e9e480d9eb539327ed477de |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT uraijl theformationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT abes theformationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT vangenth theformationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT hollandm theformationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT uraijl formationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT abes formationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT vangenth formationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment AT hollandm formationofopenfracturesincohesivematerialsresultsofscaledanalogueandnumericalmodellingonfaultzoneporositydevelopment |
_version_ |
1721244931101556736 |