Stress Density Material
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This command is used to construct a multi-dimensional stress density material object for modeling sand behaviour following the work of Cubrinovski and Ishihara (1998a,b).
nDMaterial StressDensityModel $matTag $mDen $eNot $A $n $nu $a1 $b1 $a2 $b2 $a3 $b3 $fd $muNot $muCyc $sc $M $patm <$ssl1 $ssl2 $ssl3 $ssl4 $ssl5 $ssl6 $ssl7 $ssl8 $ssl9 $ssl10 $hsl $p1 $p2 $p3 $p4 $p5 $p6 $p7 $p8 $p9 $p10> |
$matTag | integer tag identifying material |
$mDen | mass density |
$eNot | initial void ratio |
$A | constant for elastic shear modulus |
$n | pressure dependency exponent for elastic shear modulus |
$nu | Poisson's ratio |
$a1 | peak stress ratio coefficient (etaMax = a1 + b1*Is) |
$b1 | peak stress ratio coefficient (etaMax = a1 + b1*Is) |
$a2 | max shear modulus coefficient (Gn_max = a2 + b2*Is) |
$b2 | max shear modulus coefficient (Gn_max = a2 + b2*Is) |
$a3 | min shear modulus coefficient (Gn_min = a3 + b3*Is) |
$b3 | min shear modulus coefficient (Gn_min = a3 + b3*Is) |
$fd | degradation constant |
$muNot | dilatancy coefficient (monotonic loading) |
$muCyc | dilatancy coefficient (cyclic loading) |
$sc | dilatancy strain |
$M | critical state stress ratio |
$patm | atmospheric pressure (in appropriate units) |
Optional steady state line parameters (default values shown for each, be careful with units)
<$ssl1> | void ratio of quasi steady state (QSS-line) at pressure $p1 (default = 0.877) |
<$ssl2> | void ratio of quasi steady state (QSS-line) at pressure $p2 (default = 0.877) |
<$ssl3> | void ratio of quasi steady state (QSS-line) at pressure $p3 (default = 0.873) |
<$ssl4> | void ratio of quasi steady state (QSS-line) at pressure $p4 (default = 0.870) |
<$ssl5> | void ratio of quasi steady state (QSS-line) at pressure $p5 (default = 0.860) |
<$ssl6> | void ratio of quasi steady state (QSS-line) at pressure $p6 (default = 0.850) |
<$ssl7> | void ratio of quasi steady state (QSS-line) at pressure $p7 (default = 0.833) |
<$ssl8> | void ratio of quasi steady state (QSS-line) at pressure $p8 (default = 0.833) |
<$ssl9> | void ratio of quasi steady state (QSS-line) at pressure $p9 (default = 0.833) |
<$ssl10> | void ratio of quasi steady state (QSS-line) at pressure $p10 (default = 0.833) |
<$hsl> | void ratio of upper reference state (UR-line) for all pressures (default = 0.895) |
<$p1> | pressure corresponding to $ssl1 (default = 1.0 kPa) |
<$p2> | pressure corresponding to $ssl1 (default = 10.0 kPa) |
<$p3> | pressure corresponding to $ssl1 (default = 30.0 kPa) |
<$p4> | pressure corresponding to $ssl1 (default = 50.0 kPa) |
<$p5> | pressure corresponding to $ssl1 (default = 100.0 kPa) |
<$p6> | pressure corresponding to $ssl1 (default = 200.0 kPa) |
<$p7> | pressure corresponding to $ssl1 (default = 400.0 kPa) |
<$p8> | pressure corresponding to $ssl1 (default = 400.0 kPa) |
<$p9> | pressure corresponding to $ssl1 (default = 400.0 kPa) |
<$p10> | pressure corresponding to $ssl1 (default = 400.0 kPa) |
The material formulations for the StressDensity object are "ThreeDimensional" and "PlaneStrain"
Code Developed by Saumyashuchi Das, University of Canterbury. Maintained by Chris McGann
General Information
This nDMaterial object provides the
Notes
Usage Examples
The following usage example provides the input parameters for dry pluviated Toyura sand (with initial void ratio e = 0.73) after Cubrinovski and Ishihara (1998b). The units of this analysis are Mg, kN, s, and m.
# mass density set mDen 1.8 # atmospheric pressure set patm 98.1 # stress density model parameters set eNot 0.730 set A 250.0 set n 0.60 set a1 0.58 set b1 0.023 set a2 230.0 set b2 65.0 set a3 79.0 set b3 16.0 set fd 4.0 set muNot 0.22 set muCyc 0.0 set sc 0.0055 set M 0.607 nDMaterial StressDensityModel 1 $mDen $eNot $A $n $nu $a1 $b1 $a2 $b2 $a3 $b3 $fd $muNot $ muCyc $sc $M $patm
References
Cubrinovski, M. and Ishihara K. (1998a) 'Modelling of sand behaviour based on state concept,' Soils and Foundations, 38(3), 115-127.
Cubrinovski, M. and Ishihara K. (1998b) 'State concept and modified elastoplasticity for sand modelling,' Soils and Foundations, 38(4), 213-225.