====== EP-ROCK ====== ===== Description ===== Constitutive law for layered rocks at constant temperature ==== The model ==== This law is only used for elasto‑plastic constitutive law for mechanical analysis of layered rocks, with only one family of parallel joints. Rocks are elastic and joints have a COULOMB rigid plastic behaviour. ==== Files ==== Prepro: LROCK.F \\ Lagamine: ELP1.F (2D), ELP3DT.F (3D) ===== Availability ===== |Plane stress state| NO | |Plane strain state| YES | |Axisymmetric state| NO | |3D state| YES (?) | |Generalized plane state| NO | ===== Input file ===== ==== Parameters defining the type of constitutive law ==== ^ Line 1 (2I5, 60A1)^^ |IL|Law number| |ITYPE| 10 | |COMMENT| Any comment (up to 60 characters) that will be reproduced on the output listing| ==== Integer parameters ==== ^ Line 1 (I5) ^^ |NINTV|number of sub‑steps used to integrate numerically the constitutive equation in a time step.| ==== Real parameters ==== ^Line 1 (6G10.0)^^ |E|Young's elastic modulus| |ANU|Poisson's ratio| |CO|material cohesion between layers| |FI|friction angle (in degrees) between layers| |ST|stratigraphy angle (in degrees), that is the angle of the layers with respect to an horizontal plane| |PSI|dilatancy angle (in degrees)| ===== Stresses ===== ==== Number of stresses ==== = 6 for the 3-D state \\ = 4 for the other cases. ==== Meaning ==== The stresses are the components of CAUCHY stress tensor in global (X, Y, Z) coordinates. For the 3-D state : |SIG(1)|$\sigma_{xx}$| |SIG(2)|$\sigma_{yy}$| |SIG(3)|$\sigma_{zz}$| |SIG(4)|$\sigma_{xy}$| |SIG(5)|$\sigma_{xz}$| |SIG(6)|$\sigma_{yz}$| For the other cases : |SIG(1)|$\sigma_{xx}$| |SIG(2)|$\sigma_{yy}$| |SIG(3)|$\sigma_{xy}$| |SIG(4)|$\sigma_{zz}$| ===== State variables ===== ==== Number of state variables ==== 2 ==== List of state variables ==== |Q(1)|= element thickness (t) in plane stress state| |:::|= 1 in plane strain state| |:::|= circumferential strain rate ($\dot{\varepsilon}_\theta$) in axisymmetrical state| |:::|= 0 in 3‑D state| |:::|= element thickness (t) in generalized plane state.| |Q(2)|= 0 if the current state is elastic| |:::|= 1 if the current state in elasto‑plastic (i.e., sliding between joints has occurred)|