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23. Simple Soil Models
This chapter describes the background theory for the Hardin-Drnevich and
Ramberg-Osgood soil models. Both models are elastic models with a nonlinear
shear stress-shear strain relationship. The contents of this chapter are
based on Jenning [53], Konder [56], and
Hardin & Drnevich [37].
In a three-dimensional isotropic linear-elastic material model, the stress-strain
relationship can be characterised as:
where the parameters c1
, c2
, and c3
are constant. In the
Hardin-Drnevich and Ramberg-Osgood models, the parameter c3
is
dependent on the shear strain
as described in
§23.1 and §23.2. The parameters
c1
and c2
are dependent on the Poisson's ratio
, and on either
the initial Young's modulus E
or the current shear state. In a bulk
modulus formulation this reads, respectively
K =  |
(23.2) |
or
K = . |
(23.3) |
The models should behave according to the so-called extended Masing
rules:
- For the initial loading, the stress-strain relationship is
prescribed by a skeleton curve (or backbone curve).
- When reloading or unloading from the initial loading occurs, the
stress-strain relationship forms a loop, which is obtained by scaling
the skeleton curve by a factor two.
- If the previous maximum shear strain is exceeded, the
stress-strain relationship again follows the skeleton curve.
- If the hysteresis loop intersects a previous loading or unloading
curve, the stress-strain relationship follows that previous curve.
Subsections
Next: 23.1 Hardin-Drnevich Model
Up: IV. Background Theory
Previous: 22.5.2 Decay of Shear
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DIANA-9.3 User's Manual - Material Library
First ed.
Copyright (c) 2008 by TNO DIANA BV.