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Computational Geomechanics. Manuel Pastor
Читать онлайн.Название Computational Geomechanics
Год выпуска 0
isbn 9781118535301
Автор произведения Manuel Pastor
Жанр Физика
Издательство John Wiley & Sons Limited
3.2.4.3 The Consolidation Equation
In the standard treatment of consolidation equation (see, for instance, Lewis and Schrefler 1998), the acceleration terms are generally omitted a priori. However, as explained above, there is no disadvantage in writing the full dynamic formulation for solving such a problem. The procedure simply reduces the multiplier of the mass matrix M to a negligible value without influencing in any way the numerical stability, provided, of course, that an implicit integration scheme is used.
3.2.4.4 Static Problems – Undrained and Fully Drained Behavior
Steady state (static) conditions will only be reached under the extremes of undrained or fully drained behavior. This can be deduced by rewriting the two, discrete, governing Equations (3.23) and (3.28) omitting terms involving time derivatives. The equations now become:
and
with the effective stresses given by (3.27) and are defined incrementally as
First, we observe that the equations are uncoupled and that the second of these, i.e. (3.56) can be solved independently of the first for the water pressures. Indeed, in this solution, the negative pressure zones and, hence, the partially saturated regions can be readily determined following the procedures outlined in the previous chapter.
With
(3.58)
the first Equation (3.55) coupled with the appropriate constitutive law (3.57) can be solved once the history of the load applied has been specified.
The solution so obtained is, of course, the well‐known, drained, behavior.
The case of undrained behavior is somewhat more complex. We note that with k = 0, i.e. with totally impermeable behavior
(3.59)
But on re‐examining Equation (3.28), we find that it becomes
(3.60)
which, on integration, establishes a unique relationship between
assuming that the initial condition of
Equation (3.61) now has to be solved together with (3.55). If S = 0, i.e. no compressibility is admitted, then we have the problem already discussed in the previous Section 3.2.3 in which only certain
Solving (3.61) for