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Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids
Ya-wei Xie,
Michael G. Edwards
Computational Geosciences
Swansea University Author: Michael G. Edwards
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DOI (Published version): 10.1007/s10596-017-9669-5
Abstract
Novel cell-centred finite-volume formulations are presented for incompressible and immiscible two-phase flow with both gravity and capillary pressure effects on structured and unstructured grids. The Darcy-flux is approximated by a control-volume distributed multipoint flux approximation (CVD-MPFA)...
Published in: | Computational Geosciences |
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ISSN: | 1420-0597 1573-1499 |
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2017
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URI: | https://cronfa.swan.ac.uk/Record/cronfa34232 |
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2017-10-03T16:17:42.3733254 v2 34232 2017-06-12 Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids 8903caf3d43fca03602a72ed31d17c59 Michael G. Edwards Michael G. Edwards true false 2017-06-12 FGSEN Novel cell-centred finite-volume formulations are presented for incompressible and immiscible two-phase flow with both gravity and capillary pressure effects on structured and unstructured grids. The Darcy-flux is approximated by a control-volume distributed multipoint flux approximation (CVD-MPFA) coupled with a higher resolution approximation for convective transport. The CVD-MPFA method is used for Darcy-flux approximation involving pressure, gravity, and capillary pressure flux operators. Two IMPES formulations for coupling the pressure equation with fluid transport are presented. The first is based on the classical total velocity Vt fractional flow (Buckley Leverett) formulation, and the second is based on a more recent Va formulation. The CVD-MPFA method is employed for both Vt and Va formulations. The advantages of both coupled formulations are contrasted. The methods are tested on a range of structured and unstructured quadrilateral and triangular grids. The tests show that the resulting methods are found to be comparable for a number of classical cases, including channel flow problems. However, when gravity is present, flow regimes are identified where the Va formulation becomes locally unstable, in contrast to the total velocity formulation. The test cases also show the advantages of the higher resolution method compared to standard first-order single-point upstream weighting. Journal Article Computational Geosciences 1420-0597 1573-1499 Cell-centred finite-volume, Higher resolution method, Two-phase flow, Gravity, Capillary pressure, Vt and Va formulations, CVD, MPFA 31 12 2017 2017-12-31 10.1007/s10596-017-9669-5 COLLEGE NANME Science and Engineering - Faculty COLLEGE CODE FGSEN Swansea University 2017-10-03T16:17:42.3733254 2017-06-12T08:30:58.2653386 Faculty of Science and Engineering School of Engineering and Applied Sciences - Uncategorised Ya-wei Xie 1 Michael G. Edwards 2 0034232-07092017140945.pdf xie2017(2).pdf 2017-09-07T14:09:45.9500000 Output 7292263 application/pdf Version of Record true 2017-09-07T00:00:00.0000000 true eng |
title |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
spellingShingle |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids Michael G. Edwards |
title_short |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
title_full |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
title_fullStr |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
title_full_unstemmed |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
title_sort |
Higher resolution total velocity Vt and Va finite-volume formulations on cell-centred structured and unstructured grids |
author_id_str_mv |
8903caf3d43fca03602a72ed31d17c59 |
author_id_fullname_str_mv |
8903caf3d43fca03602a72ed31d17c59_***_Michael G. Edwards |
author |
Michael G. Edwards |
author2 |
Ya-wei Xie Michael G. Edwards |
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Journal article |
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Computational Geosciences |
publishDate |
2017 |
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Swansea University |
issn |
1420-0597 1573-1499 |
doi_str_mv |
10.1007/s10596-017-9669-5 |
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Faculty of Science and Engineering |
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Faculty of Science and Engineering |
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facultyofscienceandengineering |
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Faculty of Science and Engineering |
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School of Engineering and Applied Sciences - Uncategorised{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Engineering and Applied Sciences - Uncategorised |
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description |
Novel cell-centred finite-volume formulations are presented for incompressible and immiscible two-phase flow with both gravity and capillary pressure effects on structured and unstructured grids. The Darcy-flux is approximated by a control-volume distributed multipoint flux approximation (CVD-MPFA) coupled with a higher resolution approximation for convective transport. The CVD-MPFA method is used for Darcy-flux approximation involving pressure, gravity, and capillary pressure flux operators. Two IMPES formulations for coupling the pressure equation with fluid transport are presented. The first is based on the classical total velocity Vt fractional flow (Buckley Leverett) formulation, and the second is based on a more recent Va formulation. The CVD-MPFA method is employed for both Vt and Va formulations. The advantages of both coupled formulations are contrasted. The methods are tested on a range of structured and unstructured quadrilateral and triangular grids. The tests show that the resulting methods are found to be comparable for a number of classical cases, including channel flow problems. However, when gravity is present, flow regimes are identified where the Va formulation becomes locally unstable, in contrast to the total velocity formulation. The test cases also show the advantages of the higher resolution method compared to standard first-order single-point upstream weighting. |
published_date |
2017-12-31T03:42:27Z |
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1763751963108835328 |
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11.037056 |