Influence of Slip Flow at Fluid-solid Interface upon Permeability of Natural Rock

Shiwani Singh, Fei Jiang, Takeshi Tsuji

Research output: Contribution to journalConference article

Abstract

The flows involving CO2 sequestration encounters pores of very small size usually in micro-meter range. At this scale, various small-scale flow effects associated with the fluid-solid interaction governs the hydrological properties. Hence, realizing the importance of appropriate boundary condition when dealing with the small scale flow is of extreme importance. One such effect is the occurrence of slip at the fluid-solid interface. The implementation of slip boundary condition, in lattice Boltzmann framework, is discussed in the present study. The effect of slippage on the bulk properties is obtained in channel flow using the slip boundary condition. Further, a homogeneous porous media is considered to show the effect of slip flow on bulk as well as local flow properties.

Original languageEnglish
Pages (from-to)3572-3577
Number of pages6
JournalEnergy Procedia
Volume114
DOIs
Publication statusPublished - Jan 1 2017
Event13th International Conference on Greenhouse Gas Control Technologies, GHGT 2016 - Lausanne, Switzerland
Duration: Nov 14 2016Nov 18 2016

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Rocks
Boundary conditions
Fluids
Channel flow
Porous materials

All Science Journal Classification (ASJC) codes

  • Energy(all)

Cite this

Influence of Slip Flow at Fluid-solid Interface upon Permeability of Natural Rock. / Singh, Shiwani; Jiang, Fei; Tsuji, Takeshi.

In: Energy Procedia, Vol. 114, 01.01.2017, p. 3572-3577.

Research output: Contribution to journalConference article

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