Physical changes due to a deforming porous media - a finite element solution
This paper discusses a finite element solution to investigate the physical changes due to the deforming porous media. The mathematical model was derived based on Biot's self-consistent theory, which describes a fully compled governing equation system for a multiphase flow in a three dimensional...
| Main Authors: | , , |
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| Format: | Conference or Workshop Item |
| Language: | English |
| Published: |
2004
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| Subjects: | |
| Online Access: | http://eprints.utm.my/3582/ http://eprints.utm.my/3582/1/SKMBT_60007052215400.pdf |
| _version_ | 1848890604303417344 |
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| author | Sukirman, Yahya Ismail, Raihan Samsuri, Ariffin |
| author_facet | Sukirman, Yahya Ismail, Raihan Samsuri, Ariffin |
| author_sort | Sukirman, Yahya |
| building | UTeM Institutional Repository |
| collection | Online Access |
| description | This paper discusses a finite element solution to investigate the physical changes due to the deforming porous media. The mathematical model was derived based on Biot's self-consistent theory, which describes a fully compled governing equation system for a multiphase flow in a three dimensional reservoir system. It consists of the equilibrium and continuity equations for oil, gas and water-phases. An elastoplastic reservoir rock model based on the Mohr Coulomb yield criteria was used for simulating the deformation behaviour of the reservoir. The compressibility factors are calculated based on the unknowns solved in each time step. Finally, the recent values of porosity and permeability are calculated for various types of reservoir rocks. |
| first_indexed | 2025-11-15T20:44:43Z |
| format | Conference or Workshop Item |
| id | utm-3582 |
| institution | Universiti Teknologi Malaysia |
| institution_category | Local University |
| language | English |
| last_indexed | 2025-11-15T20:44:43Z |
| publishDate | 2004 |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | utm-35822017-09-06T06:58:41Z http://eprints.utm.my/3582/ Physical changes due to a deforming porous media - a finite element solution Sukirman, Yahya Ismail, Raihan Samsuri, Ariffin TP Chemical technology This paper discusses a finite element solution to investigate the physical changes due to the deforming porous media. The mathematical model was derived based on Biot's self-consistent theory, which describes a fully compled governing equation system for a multiphase flow in a three dimensional reservoir system. It consists of the equilibrium and continuity equations for oil, gas and water-phases. An elastoplastic reservoir rock model based on the Mohr Coulomb yield criteria was used for simulating the deformation behaviour of the reservoir. The compressibility factors are calculated based on the unknowns solved in each time step. Finally, the recent values of porosity and permeability are calculated for various types of reservoir rocks. 2004 Conference or Workshop Item PeerReviewed application/pdf en http://eprints.utm.my/3582/1/SKMBT_60007052215400.pdf Sukirman, Yahya and Ismail, Raihan and Samsuri, Ariffin (2004) Physical changes due to a deforming porous media - a finite element solution. In: Conference. |
| spellingShingle | TP Chemical technology Sukirman, Yahya Ismail, Raihan Samsuri, Ariffin Physical changes due to a deforming porous media - a finite element solution |
| title | Physical changes due to a deforming porous media - a finite element solution |
| title_full | Physical changes due to a deforming porous media - a finite element solution |
| title_fullStr | Physical changes due to a deforming porous media - a finite element solution |
| title_full_unstemmed | Physical changes due to a deforming porous media - a finite element solution |
| title_short | Physical changes due to a deforming porous media - a finite element solution |
| title_sort | physical changes due to a deforming porous media - a finite element solution |
| topic | TP Chemical technology |
| url | http://eprints.utm.my/3582/ http://eprints.utm.my/3582/1/SKMBT_60007052215400.pdf |