Abstract
This article derives the effective poroelastic properties of N-layered composite assemblage. The derivation is based on the Hashin composite sphere assemblage (CSA) model and the linear elastic solution of n-layer coated inclusion-reinforced materials proposed by Hervé and Zaoui. The contribution of this study consists in the consideration of the poromechanical coupling to derive not only the bulk and shear drained moduli but also the Biot coefficient and the solid Biot modulus. The theoretical solutions are used for studying the oolitic limestone from Bourgogne (France), in which the microstructure exhibits generally an assemblage of oolite grains surrounded by a matrix. They are linked via interphase where most of the macropores locate. A two-step homogenisation scheme is proposed. The first step consists in upscaling the mesoscopic poroelastic properties of each porous phase by using the differential self-consistent scheme. In the second step, the three different porous constituents (oolite, ITZ and matrix) are homogenised using the CSA model. Results are validated against the data collected from the open literature.
Appendix. Poroelastic properties resulted from the four-phase CSA model
A1. Bulk modulus ![](//:0)
![](//:0)
with
(A2)
(A2)
A2. Shear modulus ![](//:0)
![](//:0)
The overall shear modulus is the root of the following equation:
(A3)
(A3)
in which,
is only appear in 4 components a31, a32; a41 and a42:
(A4)
(A4)
Other components of the matrix in EquationEquation (A3)
(A3)
(A3) depends only on properties of three phases:
(58)
(58)
A3. Biot coefficient ![](//:0)
![](//:0)
where
(A6)
(A6)
A4. Biot modulus of solid skeleton ![](//:0)
![](//:0)
with
(A8)
(A8)
and
(A9)
(A9)