Exact solutions for flow through porous media with the Klinkenberg effect
Source abstract
Abstract
The effect of gas compressibility during flow through a porous medium modifies the governing equation for pressure, and for low pressures, this leads to the so-called Klinkenberg effect. Darcy’s law remains unchanged, and accounting for the equation of state leads to a parabolic governing equation for pressure. The increased flow rate at low pressure modifies the nonlinearity of this governing equation. We present two broad approaches for constructing exact solutions to the steady state problem. First, geometric reduction is employed to construct exact solutions in Cartesian and polar coordinates. Next, the governing equation is interpreted so that a stream function exists for the flow, and this is used to demonstrate that solutions can only be found when the flow is irrotational. A second, rather broad, class of exact solutions is thus constructed from potential flows and their generalization for variable permeability cases. The latter leads to a non-constant coefficient problem, and we provide both an algorithm illustrating how to use an existing linear numerical solver to solve the nonlinear problem and an explicit exact solution for an annular domain.
Source: crossref · Quality: baseline
Research context
OpenAlex topics: Heat and Mass Transfer in Porous Media · Hydraulic Fracturing and Reservoir Analysis · Groundwater flow and contamination studies
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
Department of Applied Mathematics, University of Waterloo , Waterloo, Ontario N2L 3G1, Canada
Funding
Ontario Ministry of Research and Innovation
References (27)
Show source-provided references
1. Towards the ultimate regime in Rayleigh–Darcy convection10.1017/jfm.2020.1178 ↗
2. Strong Rayleigh–Darcy convection regime in three-dimensional porous media10.1017/jfm.2022.461 ↗
3. The Diavik Waste Rock Project: Implications of wind-induced gas transport10.1016/j.apgeochem.2012.10.015 ↗
4. Multiphase transfer processes in waste rock piles producing acid mine drainage: 1: Conceptual model and system characterization10.1016/s0169-7722(01)00156-5 ↗
5. Waste-rock hydrogeology and geochemistry10.1016/j.apgeochem.2014.06.020 ↗
6. A generalized framework model for the simulation of gas production in unconventional gas reservoirs10.2118/163609-pa ↗
7. Physics and modeling of gas flow in shale reservoirs
8. Experimental and numerical investigations on the flow around and through the fractal soft rocks with water vapor absorption10.1016/j.ijheatmasstransfer.2016.01.025 ↗
9. Relative-permeability measurements: An overview10.2118/18565-pa ↗
10. Does Klinkenberg’s law survive upscaling?10.1023/b:tipm.0000021759.02545.d3 ↗
11. Flow of gas through porous materials10.1063/1.1744983 ↗
12. Studies on the flow of gaseous mixtures through capillaries. II. The molecular flow of gaseous mixtures10.1246/bcsj.12.285 ↗
13. Nanoscale gas flow in shale gas sediments10.2118/07-10-06 ↗
14. The permeability of porous media to liquids and gases10.5510/OGP20120200114 ↗
15. Pore networks and fluid flow in gas shales
16. Gas flow in porous media with Klinkenberg effects10.1023/a:1006535211684 ↗
17. An updated model of induced airflow in the unsaturated zone10.1029/94wr02423 ↗
18. Nonlinear pressure diffusion in a porous medium: Approximate solutions with applications to permeability measurements using transient pulse decay method10.1029/2000jb900344 ↗
19. Evaluation of unsaturated zone air permeability through pneumatic tests10.1029/91wr01655 ↗
20. 1856
21. Flow in porous media I: A theoretical derivation of Darcy’s law10.1007/bf01036523 ↗
22. Numerical simulations of flow through a variable permeability circular cylinder10.1063/5.0066415 ↗
23. 2008
24. 2012
25. Knudsen’s permeability correction for tight porous media10.1007/s11242-011-9842-6 ↗
26. Gas slippage effect on microscale porous flow using the lattice Boltzmann method10.1103/PhysRevE.72.056301 ↗
27. Effective correlation of apparent gas permeability in tight porous media10.1007/s11242-009-9432-z ↗