SeisSol is verified for a wide range of dynamic rupture problems (Pelties et al. 2014): it is possible to use branched faults, dipping fault geometries and laboratory-derived constitutive laws such as the rate-and-state friction law.
The following definitions regarding fault and stress orientation are conventions. The initial stresses need to be given in the global coordinate system. The Matlab script ‘/preprocessing/science/stressrotation3D’ is available for correct rotation of initial stress values on arbitrary orientated faults.
- Traction = (normal vector)* (stress tensor)
- Shear traction in strike direction right (left) lateral: positive (negative)
- Shear traction along dip (anti-dip) direction: positive (negative)
- Normal stress = negative in compression
- Cohesion = negative (acts on shear stress components, encapsulates the effect of pore pressurization)
- Reference point = defines dip direction, starting point of the normal vector n pointing towards the fault, at +y
- Note: SCEC benchmark descriptions define normal stress as positive in compression, opposite to SeisSol 3D convention.
The right-handed coordinate system is required. Please, make sure to follow this convention during model/mesh generation!
- Arbitrary fault orientation possible, except a fault in the xy-plane, i.e. parallel to the free surface
- Fault Output is in fault coordinate system
- n = ( nx, ny, nz ).T normal vector, from + y → - y
- s = ( ny, - nx, 0).T * sqrt ( nx^2 + ny^2) along-strike vector
- d = (-sy*nz, sx*nz, synx-nysx).T / || d || along-dip vector, pointing in -z direction (downwards)
Example 1: Initial stresses for a 60° dipping fault¶
Following the SCEC benchmark description of TPV10 we need to transfer the following initial stresses given in fault coordinates in global coordinates for SeisSol:
INPUT (from tpv10)
normal stress = - 7378 Pa/m * (meter downdip-distance) shear stress = 0.55 * (normal stress) = + 4057.9 Pa/m * (meter downdip-distance)
Assuming the fault plane in xz-plane, dipping 60° in -y-direction we can use the script ‘/preprocessing/science/stressrotation3D’ to rotate the stresses 30° clockwise at the x-axis (considering we look towards +x) to get the full stress tensor in global coordinates:
OUTPUT (to be used in SeisSol’s parameter file)
s_yy = - 2019.26 Pa/m * (meter downdip-distance) s_zz = - 5358.74 Pa/m * (meter downdip-distance) s_yz = + 5223.72 Pa/m * (meter downdip-distance) s_xx = s_xy = s_xz = 0.0 Pa
Example 2: Initial stresses for a branched fault¶
Normal and shear stresses in fault coordinate system for strike-slip fault aligned with the x- or y-axis are already in the global coordinates. But if we have additional branches the initial stresses need to be rotated again. Following for example the SCEC benchmark description for [TPV14] (http://scecdata.usc.edu/cvws/download/TPV14_15_Description_v08.pdf), the stresses for the right-lateral strike-slip fault in xz-plane are:
s_yy = - 120 MPa s_xy = + 70 MPa s_xy (nucleation patch) = + 81.6 MPa s_xx = s_zz = s_xz = s_yz = 0.0 Pa
For the 30° branch in -y direction we rotate the given stresses (in that case, they are the same as on the main fault) by 330° counterclockwise (or 30° clockwise) around the z-axis using the script ‘/preprocessing/science/stressrotation3D’.
OUTPUT (to be used in SeisSol’s parameter file)
s_xx = + 30.62 MPa s_yy = - 150.62 MPa s_xy = - 16.96 MPa s_zz = s_xz = s_yz = 0.0 Pa
In case of a left-lateral strike slip fault (for example TPV15) the stresses on the main fault are:
s_yy = - 120 MPa s_xy = - 70 MPa s_xy (nucleation patch) = - 81.6 MPa s_xx = s_zz = s_xz = s_yz = 0.0 Pa
Projected linear slip-weakening¶
A sudden decrease of slip rate to very small values, as for example occurring at a rupture front about to be arrested, may cause numerical issues and pollute the solution - in the worst case even leading to re-activation of rupture. Such numerical issues are easy to diagnose in the fault output visualization: a checkerboard pattern with unphysical values for the slip rate and slip in the affected region will be visible. This is a sign of mesh resolution (h-refinement) being locally not sufficient. SeisSol mitigates such artifacts (currently only for linear slip-weakening friction) by projecting the slip increment on the 2D fault interface basis function after evaluation of the friction law. This implementation lowers the required h-refinement for linear-slip weakening friction across the fault in comparison to earlier implementations (cf. Pelties et al. , JGR 2012; GMD 2014) Note, that the corresponding implementation for rate-and-state friction laws is currently pending - thus, a sudden decrease to small slip rates may cause numerical artifacts.
Visualisation: SlipRateOutputType (default =1)¶
By default, the fault output will be showing regions affected by numerical problems. However, the user may choose to smooth out such artifacts for visualization purposes. Switching
SlipRateOutputType in the
DynamicRupture namelist from the default value to 0, will evaluate the slip-rate from the difference between the velocity on both sides of the fault, rather than evaluating the slip-rate from the fault tractions and the failure criterion directly.
Note that this fix only applies to the output, but does not suppress numerical problems in the simulation.
Also note that that
SlipRateOutputType=0 is slightly less accurate than the default
SlipRateOutputType=1 without numerical problems.
Seissol can account for thermal pressurization (TP) of pore fluids.
As deformation occurs within the fault gauge, frictional heating increases the temperature of the rock matrix and pore fluids.
The pore fluids then pressurize, which weakens the fault.
The evolution of the pore fluid pressure and temperature is governed by the diffusion of heat and fluid.
TP can be activated using
thermalPress in the
The TP parameters for which no spatial dependence has been implemented are defined directly in the
&DynamicRupture thermalPress = 1 ! Thermal pressurization 0: inactive; 1: active IniTemp = 483.15 ! Initial temperature [K] IniPressure = -80.0e6 ! Initial pore pressure; have to be added to normal stress in your initial stress yaml file [Pa] alpha_th = 1.0e-6 ! Thermal diffusivity [m^2/s] rho_c = 2.7e6 ! Specific heat [Pa/K] TP_lambda = 0.1e6 ! Pore pressure change per unit temperature [Pa/K]
Two additional thermal pressurization parameters are space-dependent and therefore have to be specified in the dynamic rupture yaml file:
!ConstantMap map: alpha_hy: 1e-4 ! Hydraulic diffusivity [m^2/s] TP_half_width_shear_zone: 0.01 ! Half width of shearing zone [m]
TP generates 2 additional on-fault outputs: Pore pressure and temperature (see fault output).
Slip-rate imposed on a DR boundary condition¶
This friction law allows imposing slip-rate on a dynamic rupture boundary (potentially any kinematic models, but the current implementation is limited, see below). The FL id for this friction law is 33. The advantage of this approach compared to a multi point-sources representation is that the fault slip is not condensed to points. Therefore the discontinuity of the displacement across the fault can be accurately accounted for, and more generally the wavefield is accurate in the near-field.
The current implementation allows imposing a slip distribution on the DR Boundary using the same arbitrary smooth-step SR function everywhere on the fault.
The slip distribution is imposed simultaneously everywhere on the fault, smoothly over a time
t_0 is a parameter of the
This is an expensive way of getting the final stress distribution from a given slip distribution.
The slip distribution is defined using easi by the
Warning: the direction of positive
dip_slip is based on the convention of Seissol (e.g. positive strike_slip for right-lateral faulting).
Below is an example of an input file for defining the slip distribution:
!Switch [strike_slip, dip_slip]: !Any components: - !AxisAlignedCuboidalDomainFilter limits: x: [-1000, 0] y: [-1e10, 1e10] z: [-5000, -3000] components: !ConstantMap map: strike_slip: 0.01 dip_slip: 0.1 - !ConstantMap map: strike_slip: 0.05 dip_slip: 0.05