Sunden CH010.tex 10/9/2010 15: 22 Page 411
SPH – a versatile multiphysics modeling tool 411
where, <v> and P are the volume averaged (superficial) velocity and the pressure
of the fluid (bold text denotes vector or tensor); K is the permeability tensor of the
porous medium; and µ is the dynamic viscosity of the fluid.
Darcy’s law is a macroscopic phenomenological model, which is largely based
on experimental observations. In this law, the complex interactions between fluid
and microscopic porous structures are all lumped in a macroscopic physical
quantity – the permeability tensor, K. As the permeability tensor is of paramount
importance to the fluid flow in porous media, numerous research efforts [42–45]
were devoted to establish theoretical relations between the permeability and other
characteristic material properties with the purpose of avoiding time-consuming
physical experiments.These theoreticalmodels are generally based on the analysis
of the microscopic porous structure of the medium and the subsequent extraction
of the desired macroscopic information. The complicated, diverse pore structures
in reality present a major challenge to pure (or semiempirical) theoretical models
because they are all constructed on the basis of artificially simple, regular pore
arrangements.
Obviously, the modeling of fluid flow in fibrous porous media directly from
the mesoscopic pore structure level provides refined fluid flow information and
it does not resort to Darcy’s law. Moreover, the simulated fluid field is amenable
to the determination of K as well. Over the last few decades, rapid advances in
computer capabilities andcomputational algorithms enabled thiskind of modeling
work. For example, the lattice-gas-automaton (LGA) or lattice Boltzmann method
(LBM) [46], based upon a micro- or mesoscopic model of kinetic formulations
or the Boltzmann equation, respectively, can bridge the gap between microscopic
structuresandmacroscopicphenomena.Thesemodelshavetheadvantageofallow-
ing parallelism in a straightforward manner for large-scale numerical calculations,
and they have the attractive feature of nonslip bounce-back solid boundar y treat-
ment for the simulation of fluid flow in porous media. The simulations based on
LGA [47, 48] and LBM [49–51] have demonstrated that Darcy’s law can be repro-
duced by these methods. The simulated porous media in the work by Koponen et
al. [49] describe three-dimensional (3-D) random fiber webs that closely resemble
fibrous sheetssuch as paper andnon-woven fabrics.The computed permeability of
these webs presents an exponential dependence on the porosity over a large range
of porosity and is in good agreement with experimental data [52, 53]. Spaid and
Phelan [51] investigated the resin injection process encountered in RTM. The cell
permeability obtained for transverse flow through regularly arranged porous tows
of circular or elliptical cross-section agrees well with the semi-analytical solution.
In contrast to LBM or LGA, SPH is a meshless particle-based method and offers
more freedomin dealingwith complicated geometries.Application of SPHto fluid
flow in porous media has the potential of providing a mesoscopic/microscopic
pore-scale insight into the relevant physics [54–57]. In the present work, SPH
is employed to construct a mesoscopic pore-scale model for fluid flow in porous
media,inparticular,forthetransversefluidflowinrandomlyalignedfibrousporous
media.