A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media

A novel boundary-type meshless method for modeling geofluid flow in heterogeneous geological media was developed. The numerical solutions of geofluid flow are approximated by a set of particular solutions of the subsurface flow equation which are expressed in terms of sources located outside the dom...

Full description

Saved in:
Bibliographic Details
Main Authors: Jing-En Xiao, Cheng-Yu Ku, Chih-Yu Liu, Wei-Chung Yeih
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2018/9804291
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849305923959390208
author Jing-En Xiao
Cheng-Yu Ku
Chih-Yu Liu
Wei-Chung Yeih
author_facet Jing-En Xiao
Cheng-Yu Ku
Chih-Yu Liu
Wei-Chung Yeih
author_sort Jing-En Xiao
collection DOAJ
description A novel boundary-type meshless method for modeling geofluid flow in heterogeneous geological media was developed. The numerical solutions of geofluid flow are approximated by a set of particular solutions of the subsurface flow equation which are expressed in terms of sources located outside the domain of the problem. This pioneering study is based on the collocation Trefftz method and provides a promising solution which integrates the T-Trefftz method and F-Trefftz method. To deal with the subsurface flow problems of heterogeneous geological media, the domain decomposition method was adopted so that flux conservation and the continuity of pressure potential at the interface between two consecutive layers can be considered in the numerical model. The validity of the model is established for a number of test problems. Application examples of subsurface flow problems with free surface in homogenous and layered heterogeneous geological media were also carried out. Numerical results demonstrate that the proposed method is highly accurate and computationally efficient. The results also reveal that it has great numerical stability for solving subsurface flow with nonlinear free surface in layered heterogeneous geological media even with large contrasts in the hydraulic conductivity.
format Article
id doaj-art-2c5417a14e9f4e9aaadfa9ed88340bb4
institution Kabale University
issn 1468-8115
1468-8123
language English
publishDate 2018-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-2c5417a14e9f4e9aaadfa9ed88340bb42025-08-20T03:55:16ZengWileyGeofluids1468-81151468-81232018-01-01201810.1155/2018/98042919804291A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological MediaJing-En Xiao0Cheng-Yu Ku1Chih-Yu Liu2Wei-Chung Yeih3Department of Harbor and River Engineering, National Taiwan Ocean University, Keelung, TaiwanDepartment of Harbor and River Engineering, National Taiwan Ocean University, Keelung, TaiwanDepartment of Harbor and River Engineering, National Taiwan Ocean University, Keelung, TaiwanDepartment of Harbor and River Engineering, National Taiwan Ocean University, Keelung, TaiwanA novel boundary-type meshless method for modeling geofluid flow in heterogeneous geological media was developed. The numerical solutions of geofluid flow are approximated by a set of particular solutions of the subsurface flow equation which are expressed in terms of sources located outside the domain of the problem. This pioneering study is based on the collocation Trefftz method and provides a promising solution which integrates the T-Trefftz method and F-Trefftz method. To deal with the subsurface flow problems of heterogeneous geological media, the domain decomposition method was adopted so that flux conservation and the continuity of pressure potential at the interface between two consecutive layers can be considered in the numerical model. The validity of the model is established for a number of test problems. Application examples of subsurface flow problems with free surface in homogenous and layered heterogeneous geological media were also carried out. Numerical results demonstrate that the proposed method is highly accurate and computationally efficient. The results also reveal that it has great numerical stability for solving subsurface flow with nonlinear free surface in layered heterogeneous geological media even with large contrasts in the hydraulic conductivity.http://dx.doi.org/10.1155/2018/9804291
spellingShingle Jing-En Xiao
Cheng-Yu Ku
Chih-Yu Liu
Wei-Chung Yeih
A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
Geofluids
title A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
title_full A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
title_fullStr A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
title_full_unstemmed A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
title_short A Novel Boundary-Type Meshless Method for Modeling Geofluid Flow in Heterogeneous Geological Media
title_sort novel boundary type meshless method for modeling geofluid flow in heterogeneous geological media
url http://dx.doi.org/10.1155/2018/9804291
work_keys_str_mv AT jingenxiao anovelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT chengyuku anovelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT chihyuliu anovelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT weichungyeih anovelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT jingenxiao novelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT chengyuku novelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT chihyuliu novelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia
AT weichungyeih novelboundarytypemeshlessmethodformodelinggeofluidflowinheterogeneousgeologicalmedia