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laws:solnl1

SOLNL1

Description

Constitutive law of flow and deformation in porous media for a pipe element

The model

Elasto-plastic nonlinear analysis of coupled seepage and compaction in porous media. This law is used for one-dimensional problems

Files

Prepro: LSONL1.F
Lagamine: SOLNL1.F

Availability

Plane stress stateYES
Plane strain state YES
Axisymmetric stateNO
3D state NO
Generalized plane stateNO

Input file

Parameters defining the type of constitutive law

Line 1 (2I5, 60A1)
ILLaw number
ITYPE 260
COMMENT Any comment (up to 60 characters) that will be reproduced on the output listing.

Integer parameters

Line 1 (I5)
KPERM 0 $\rightarrow$ loi NISHIDA (K=exp($\alpha e + \beta$))
1 $\rightarrow$ loi TERZAGMI (K = $\alpha (e-\beta )^{\delta} \cdot (1+e$))

Real parameters

Line 1 (9G10.0)
A elasticity logarithm modulus
C elastoplasticity logarithm modulus
GAMA = $\gamma$ fluid specific weight
$\alpha$ 1st flow parameter
$\beta$ 2nd flow parameter
$\delta$ 3rd flow parameter
$\Omega$ section
$e_0$ initial void ratio
$\sigma_{p’}$ initial preconsolidation stress

Note: Y axis is vertical directed from bottom to top. Gravity same direction, other sense.

Stresses

Number of stresses

4

Meaning

SIG(1)axial effective stress
SIG(2) fluid flow in the pipe
SIG(3) fluid flow accumulated as a consequence of the evolution of soil porosity = strain rate
SIG(4) axial total stress

State variables

Number of state variables

4

List of state variables

QA(1) A
cross-section
QA(2)e
void ratio = $v_v/v_m$
QA(3) $\sigma_{p’r}$
yield stress
preconsolidation stress
QB(4) yield
yield indicator
laws/solnl1.txt · Last modified: 2020/08/25 15:46 (external edit)