Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model

For the problem of whether the representative elementary volume (REV) obtained in the Darcy flow is also applicable to the case of the non-Darcy flow, the study on the REV size within the non-Darcy flow is proposed tentatively. The concept of the REV in the non-Darcy flow is based on the definition...

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Main Authors: Yuan Wang, Yu-long Niu, Qiang Feng
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2018/7535927
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author Yuan Wang
Yu-long Niu
Qiang Feng
author_facet Yuan Wang
Yu-long Niu
Qiang Feng
author_sort Yuan Wang
collection DOAJ
description For the problem of whether the representative elementary volume (REV) obtained in the Darcy flow is also applicable to the case of the non-Darcy flow, the study on the REV size within the non-Darcy flow is proposed tentatively. The concept of the REV in the non-Darcy flow is based on the definition of the REV. According to the determination of the REV in the Darcy flow, the intrinsic permeability k and non-Darcy coefficient β are used simultaneously for the determination of the REV in the non-Darcy flow. The pore pressure cohesive element (PPCE) is developed with the subroutine in ABAQUS. Then the simulation method of the Darcy and non-Darcy flow in the fractured rock mass is built using the PPCE. The proposed plan is examined through the comparison with existing research results. It is validated that this technic is efficient and accurate in simulating the Darcy and non-Darcy flow in the fractured rock mass. Combined with fracture networks generated by Monte Carlo Simulation technique, the PPCE is applied to the study on the REV size. Both conditions of the Darcy and non-Darcy flow are simulated for comparison. The simulation results of this model show that the REV of the non-Darcy flow is inconsistent with the REV of the Darcy flow, and the REV of the non-Darcy flow is more significant than the REV of the Darcy flow. The intrinsic permeability k tensors obtained in the Darcy flow and the non-Darcy flow are basically the same.
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institution Kabale University
issn 1468-8115
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language English
publishDate 2018-01-01
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series Geofluids
spelling doaj-art-042c5f8c47c743d9bb4a69bb501363382025-02-03T01:26:10ZengWileyGeofluids1468-81151468-81232018-01-01201810.1155/2018/75359277535927Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity ModelYuan Wang0Yu-long Niu1Qiang Feng2Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing 210098, ChinaKey Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing 210098, ChinaKey Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing 210098, ChinaFor the problem of whether the representative elementary volume (REV) obtained in the Darcy flow is also applicable to the case of the non-Darcy flow, the study on the REV size within the non-Darcy flow is proposed tentatively. The concept of the REV in the non-Darcy flow is based on the definition of the REV. According to the determination of the REV in the Darcy flow, the intrinsic permeability k and non-Darcy coefficient β are used simultaneously for the determination of the REV in the non-Darcy flow. The pore pressure cohesive element (PPCE) is developed with the subroutine in ABAQUS. Then the simulation method of the Darcy and non-Darcy flow in the fractured rock mass is built using the PPCE. The proposed plan is examined through the comparison with existing research results. It is validated that this technic is efficient and accurate in simulating the Darcy and non-Darcy flow in the fractured rock mass. Combined with fracture networks generated by Monte Carlo Simulation technique, the PPCE is applied to the study on the REV size. Both conditions of the Darcy and non-Darcy flow are simulated for comparison. The simulation results of this model show that the REV of the non-Darcy flow is inconsistent with the REV of the Darcy flow, and the REV of the non-Darcy flow is more significant than the REV of the Darcy flow. The intrinsic permeability k tensors obtained in the Darcy flow and the non-Darcy flow are basically the same.http://dx.doi.org/10.1155/2018/7535927
spellingShingle Yuan Wang
Yu-long Niu
Qiang Feng
Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
Geofluids
title Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
title_full Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
title_fullStr Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
title_full_unstemmed Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
title_short Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model
title_sort study on the rev size of fractured rock in the non darcy flow based on the dual porosity model
url http://dx.doi.org/10.1155/2018/7535927
work_keys_str_mv AT yuanwang studyontherevsizeoffracturedrockinthenondarcyflowbasedonthedualporositymodel
AT yulongniu studyontherevsizeoffracturedrockinthenondarcyflowbasedonthedualporositymodel
AT qiangfeng studyontherevsizeoffracturedrockinthenondarcyflowbasedonthedualporositymodel