TY - JOUR
T1 - Partitioned Time Stepping Method for a Dual-Porosity-Stokes Model
AU - Shan, Li
AU - Hou, Jiangyong
AU - Yan, Wenjing
AU - Chen, Jie
N1 - Publisher Copyright:
© 2018, Springer Science+Business Media, LLC, part of Springer Nature.
PY - 2019/4/1
Y1 - 2019/4/1
N2 - In this report, we study a partitioned time stepping algorithm for a dual-porosity-Stokes model, which consists of dual-porosity media and macrofractures/conduits in the coupled system. More specifically, the dual-porosity-Stokes model uses two pressures, the matrix pressure and the fracture pressure, to couple with the Stokes equations. There are four physically valid interface conditions to couple the two models on the interface, including a no-exchange condition, a mass balance condition, a force balance condition, and the Beavers–Joseph condition. To decouple the complex model into three simple sub-problems and solve them separately, we propose a partitioned time stepping method. It solves one, uncoupled matrix pressure equation, microfracture pressure equation and Stokes equation per time step. Under a modest time step restriction of the form ▵t≤ C(depending on physical parameters) , we prove the stability of the method. We also derive its optimal error estimates. Numerical tests verify the theoretical results.
AB - In this report, we study a partitioned time stepping algorithm for a dual-porosity-Stokes model, which consists of dual-porosity media and macrofractures/conduits in the coupled system. More specifically, the dual-porosity-Stokes model uses two pressures, the matrix pressure and the fracture pressure, to couple with the Stokes equations. There are four physically valid interface conditions to couple the two models on the interface, including a no-exchange condition, a mass balance condition, a force balance condition, and the Beavers–Joseph condition. To decouple the complex model into three simple sub-problems and solve them separately, we propose a partitioned time stepping method. It solves one, uncoupled matrix pressure equation, microfracture pressure equation and Stokes equation per time step. Under a modest time step restriction of the form ▵t≤ C(depending on physical parameters) , we prove the stability of the method. We also derive its optimal error estimates. Numerical tests verify the theoretical results.
KW - Beavers–Joseph interface condition
KW - Dual-porosity-Stokes model
KW - Error estimate
KW - Partitioned time stepping method
UR - http://www.scopus.com/inward/record.url?scp=85058062404&partnerID=8YFLogxK
U2 - 10.1007/s10915-018-0879-3
DO - 10.1007/s10915-018-0879-3
M3 - Article
AN - SCOPUS:85058062404
SN - 0885-7474
VL - 79
SP - 389
EP - 413
JO - Journal of Scientific Computing
JF - Journal of Scientific Computing
IS - 1
ER -