Название | Computational Geomechanics |
---|---|
Автор произведения | Manuel Pastor |
Жанр | Физика |
Серия | |
Издательство | Физика |
Год выпуска | 0 |
isbn | 9781118535301 |
To keep this mapping continuous and bijective at all times, the determinant of the Jacobian of this transformation must not equal zero and must be strictly positive, since it is equal to the determinant of the deformation gradient tensor Fπ
(2.56)
where Uπ is the right stretch tensor, Vπ the left stretch tensor, and the skew‐symmetric tensor Rπ gives the rigid body rotation. Differentiation with respect to the appropriate coordinates of the reference or actual configuration is respectively denoted by comma or slash, i.e.
(2.57)
Because of the non‐singularity of the Lagrangian relationship (2.55), its inverse can be written and the Eulerian or spatial description of motion follows
(2.58)
The material time derivative of any differentiable function fπ(X, t) given in its spatial description and referred to a moving particle of the π phase is
If superscript α is used for
2.5.2 Microscopic Balance Equations
In the hybrid mixture theories, the microscopic situation of any π phase is first described by the classical equations of continuum mechanics. At the interfaces to other constituents, the material properties and thermodynamic quantities may present step discontinuities. As throughout the book, the effects of the interfaces are here not taken into account explicitly. These are introduced, e.g. in Schrefler (2002) and Gray and Schrefler (2001, 2007).
For a thermodynamic property ψ, the conservation equation within the π phase may be written as
where
Table 2.2 Thermodynamic properties for the microscopic mass balance equations.
Sources: Adapted from Hassanizadeh and Gray (1980, 1990), and Schrefler (1995).
Quantity | ψ | i | g | G |
---|---|---|---|---|
Mass | 1 | 0 | 0 | 0 |
Momentum |
|
t m | g | 0 |
Energy |
|
|
|
0 |
Entropy | Λ | Φ | S | φ |
2.5.3 Macroscopic Balance Equations
For isothermal conditions, as here assumed, the macroscopic