We study three “incompressibility flavors” of linearly-elastic anisotropic solids that exhibit volumetric constraints: isochoric, hydroisochoric and rigidtropic. An isochoric material deforms without volume change under any stress system. An hydroisochoric material does so under hydrostatic stress. A rigidtropic material undergoes zero deformations under a certain stress pattern. Whereas the three models coalesce for isotropic materials, important differences appear for anisotropic behavior. We find that isochoric and hydroisochoric models under certain conditions may be hampered by unstable physical behavior. Rigidtropic models can represent semistable physical materials of arbitrary anisotropy while including isochoric and hyd...
International audienceOne of the interesting features with the ellipsoidal models of anisotropy pres...
In order to avoid the numerical difficulties in locally enforcing the incompressibility constraint u...
We describe a non-linear anisotropic hyperelastic model appropriate for geomaterials, deriving the f...
We study three “incompressibility flavors” of linearly-elastic anisotropic solids that e...
We define stress and strain splittings appropriate to linearly elastic anisotropic materia...
We give conditions on the strain–energy function of nonlinear anisotropic hyperelastic materials tha...
Abstract We give conditions on the strain–energy function of nonlinear anisotropic hyperelastic mate...
We give conditions on the strain-energy function of nonlinear anisotropic hyperelastic materials tha...
The Holzapfel–Gasser–Ogden (HGO) model for anisotropic hyperelas-tic behaviour of collagen fibre rei...
In order to avoid the numerical difficulties in locally enforcing the incompressibility constraint u...
Many materials of contemporary interest, such as gels, biological tissues and elastomers, are easily...
Materials for which the stiffness under hydrostatic loads (bulk modulus) is very high compared to th...
For a given class of materials, universal deformations are those that can be maintained in the absen...
Universal deformations of an elastic solid are deformations that can be achieved for all possible st...
Incompressible nonlinearly hyperelastic materials are rarely simulated in finite element numerical e...
International audienceOne of the interesting features with the ellipsoidal models of anisotropy pres...
In order to avoid the numerical difficulties in locally enforcing the incompressibility constraint u...
We describe a non-linear anisotropic hyperelastic model appropriate for geomaterials, deriving the f...
We study three “incompressibility flavors” of linearly-elastic anisotropic solids that e...
We define stress and strain splittings appropriate to linearly elastic anisotropic materia...
We give conditions on the strain–energy function of nonlinear anisotropic hyperelastic materials tha...
Abstract We give conditions on the strain–energy function of nonlinear anisotropic hyperelastic mate...
We give conditions on the strain-energy function of nonlinear anisotropic hyperelastic materials tha...
The Holzapfel–Gasser–Ogden (HGO) model for anisotropic hyperelas-tic behaviour of collagen fibre rei...
In order to avoid the numerical difficulties in locally enforcing the incompressibility constraint u...
Many materials of contemporary interest, such as gels, biological tissues and elastomers, are easily...
Materials for which the stiffness under hydrostatic loads (bulk modulus) is very high compared to th...
For a given class of materials, universal deformations are those that can be maintained in the absen...
Universal deformations of an elastic solid are deformations that can be achieved for all possible st...
Incompressible nonlinearly hyperelastic materials are rarely simulated in finite element numerical e...
International audienceOne of the interesting features with the ellipsoidal models of anisotropy pres...
In order to avoid the numerical difficulties in locally enforcing the incompressibility constraint u...
We describe a non-linear anisotropic hyperelastic model appropriate for geomaterials, deriving the f...