Lj. Huang et P. Mora, THE PHONONIC LATTICE SOLID WITH FLUIDS FOR MODELING NONLINEAR SOLID-FLUID INTERACTIONS, Geophysical journal international, 117(2), 1994, pp. 529-538
The phononic lattice solid has been developed recently as a possible a
pproach for modelling compressional waves in complex solids at the mic
roscopic scale. Rather than directly modelling the wave equation, the
microdynamics of quasi-particles is simulated on a discrete lattice. I
t is comparable with the lattice gas approach to model idealized gas p
articles but differs fundamentally in that lattice solid particles car
ry pressure rather than mass and propagate through a heterogeneous med
ium. Their speed may be space and direction dependent while the speed
of lattice gas particles is constant. Furthermore, they may be scatter
ed by medium heterogeneities. Lattice sites in the phononic lattice so
lid approach are considered to be fixed in space for all time. Lattice
site movements (i.e. deformations) induced by the passage of a macros
copic wave are particularly important for a fluid-filled porous medium
considering that non-linear solid-fluid interactions are thought to p
lay a role in attenuation mechanisms. We take lattice site movements i
nto account in the phononic lattice solid and name the approach 'the p
hononic lattice solid with fluids (PLSF)' because it could lead to an
improved understanding of the effect of solid-fluid interactions in wa
ve propagation problems. The macroscopic limit of the Boltzmann equati
on for the PLSF yields the acoustic wave equation for heterogeneous me
dia modified by shear and bulk viscosity terms as well as the second-o
rder term in macroscopic velocity (for the PLS) and additional non-lin
ear terms due to the lattice site movements. It is hoped that PLSF num
erical simulation studies of waves through digitized rock matrices may
lead to an improved understanding of attenuation mechanisms of waves
in porous rocks.