# Softening-Healing Mohr-Coulomb Joint Model In 3DEC

The Mohr-Coulomb joint model has the following deficiencies when used to model seismicity:

• The stress drop is instantaneous when slipping starts (shear strength drops instantaneously from a peak to a residual value). This means that all slip events are seismic (see Figure 1).
• Once slip has occurred, there is no way for the strength on the fault to recover back to the peak value. This means that stick-slip behavior is not possible.

Formulation

The Softening Healing Mohr-Coulomb model is based on the standard Mohr-Coulomb model with two additions:

1. When the joint starts slipping, the shear strength evolves from the peak value to the residual value over a user-specified critical slip distance $$D_c$$.
2. When slipping stops, the shear strength recovers instantaneously to the peak value.

There is no softening or healing for the tensile forces. The tensile strength drops instantaneously when the strength is exceeded (no softening) and the tensile strength remains at the residual value (no healing).

For a non-slipping joint, the value of cohesion and friction are the peak values. When the strength is exceeded, the strength is a function of the slip distance. When the slip distance exceeds the critical slip distance, the residual values of cohesion and friction are used. Two formulations for the evolution of shear strength are provided.

Linear

For linear softening, the shear strength is calculated by:

(1)\begin{align}\begin{aligned}S_F = S_F^{peak} = c + \sigma_n \tan\phi \; , \; u_s^p = 0\\S_F = S_F^{peak} - (S_F^{peak} - S_F^{resid}) * {u_s^p \over D_c } \; , \; 0 < u_s^p < D_c\\S_F = S_F^{resid} = c_{resid}+ \sigma_n \tan\phi_{resid} \; , \; u_s^p > D_c\end{aligned}\end{align}

where $$c$$ is the cohesion, $$\sigma_n$$ is the normal stress, $$\phi$$ is the friction angle, $$c_resid$$ is the residual cohesion, $$\phi_{resid}$$ is the residual friction angle, $$D_c$$ is the critical slip distance, and $$u_s^p$$ is the plastic shear displacement (slip) since the start of slipping. When slipping stops, the shear strength returns instantaneously to the peak value and $$u_s^p$$ is set back to 0. An example of a subcontact with no cohesion is shown in Figure 2.

Figure 2: Shear stress versus shear displacement for a slipping joint with constant normal stress. The linear softening law is used.

Non-Linear

For non-linear softening, the shear strength is calculated by:

(2)\begin{align}\begin{aligned}S_F = S_F^{peak} = c + \sigma_n \tan\phi \; , \; u_s^p = 0\\S_F = S_F^{resid} + (S_F^{peak} - S_F^{resid}) * {D_c^\alpha \over (D_c + u_s^p)^\alpha } \; , \; u_s^p > 0\end{aligned}\end{align}

where $$\alpha$$ is an exponent (> 1) that dictates the severity of the strength drop (see Figure 3).

Figure 3: Shear stress versus shear displacement for a slipping joint with constant normal stress. The non-linear softening law is used.

Dilation ($$\psi$$) behaves in the same way as cohesion or friction. If a non-zero residual dilation is specified, the dilation varies according to the following equation for $$\alpha$$ = 0 (linear):

(3)\begin{align}\begin{aligned}\tan\psi = \tan\psi_{peak} - (\tan\psi_{peak} - \tan\psi_{resid}) * {u_s^p \over D_c } \; 0 < u_s^p < D_c\\\tan\psi = \tan\psi_{resid} \; , \; u_s^p > D_c\end{aligned}\end{align}

For the non-linear case, the dilation is given by:

(4)$tan\psi = tan\psi_{resid} + (\tan\psi_{peak} - \tan\psi_{resid}) * {D_c^\alpha \over (D_c + u_s^p)^\alpha } \; , \; u_s^p > 0$

If a value of $$\psi_{resid}$$ is not provided, it defaults to $$\psi_{peak}$$

Subcontact failure state are the same as for Mohr-Coulomb Joint Model In 3DEC.

## Example

To view this examples in 3DEC, use the menu command Help ► Examples…. Choose “3DEC/ Constitutive_Models/ SHMohr_Model” and select “shmohr.prj” to load. The data files used are shown at the end of this example.

A spring-slider problem is simulated with three blocks as shown in Figure 4. A normal stress of 1 MPa was applied to the top surface of the slider block. A velocity of 1 mm/s was applied to the right side of the system. The model was then run until one or more slip events occurred.

The test is a simulation of a direct shear test, which consists of a single horizontal joint that is first subjected to a normal confining stress, and then to a unidirectional shear displacement. Figure 5 shows the model; the joint is defined by one contact that is composed of 10 sub-contacts.

The following strength properties were assigned to the sliding joint:

Peak friction, $$\phi$$ = 25 degrees Residual friction, $$\phi_{resid}$$ = 20 degrees Critical slip distance, $$D_c = 1x10^{-4} , 1x10^{-5}$$ Alpha exponent, $$\alpha$$ = 0 (linear)

Figure 4: 3DEC Block configuration in the spring-slider test.

Plots of friction on the joint, and shear velocity versus shear displacement are shown for the different values of $$D_c$$ in Figure 5 to Figure 8. Velocities are plotted with the same maximum in each plot to ease comparisons. The effect of the softening is clear, and the higher velocities observed in the model with the lower value of $$D_c$$ suggests a possible criterion for differentiating seismic and aseismic slip events.

Figure 5: Average shear stress versus shear displacement in the Softening-Healing-Mohr-Coulomb joint model with $$D_c$$ = 1e-5.

Figure 6: Shear velocity versus shear displacement in the Softening-Healing-Mohr-Coulomb joint model with $$D_c$$ = 1e-5.

Figure 7: Average shear stress versus shear displacement in the Softening-Healing-Mohr-Coulomb joint model with $$D_c$$ = 1e-4.

Figure 8: Shear velocity versus shear displacement in the Softening-Healing-Mohr-Coulomb joint model with $$D_c$$ = 1e-4.

To test changing dilation, the test was run three more times: with a constant dilation of 10 degrees, with a constant dilation of 2 degrees and with dilation evolving from 10 to 2 over a critical slip distance of $$D_c$$ of 1e-4. Graphs of normal displacement versus shear displacement for the three cases are shown in Figure 9.

Figure 9: Normal displacement versus shear displacement for constant dilation angle of 10 degrees, constant dilation angle of 2 degrees, and a dilation angle evolving from 10 to 2 degrees.

Data Files

spring-slider.dat

model new
model random 10000
model config energy
model large-strain off

; slider brick
block create brick -1 1 -1 1 -1 1

; spring brick
block create brick 1 3 -1 1 -1 1

; base brick
block create brick -1.5 3.5 -1.5 1.5 -1.5 -1

block zone gen edgelength 0.5

block zone cmodel assign el
block zone prop dens 2000 bulk 1e11 shear 0.6e11

; spring
block contact jmodel assign el
block contact prop stiffness-normal 1e9 stiffness-shear 1e9

;slider-base contact - mohr-coulomb with 0 friction
block hide range pos-x -1 1 pos-z -1 1
block contact jmodel assign mohr
block contact prop stiffness-normal 1e11 stiffness-shear 1e11
block hide off

; sliding contacts
block hide range pos-x 1 3 pos-z -1 1
block contact jmodel assign softening-mohr

; joint properties
block contact prop stiffness-normal 1e11 stiffness-shear 1e11 friction 25 friction-res 20 tens 1e12 dc 1e-4

block hide off

block insitu stress 0 0 -1e6 0 0 0
block face apply stress-zz -1e6 range pos-z 1
block fix range pos-z -1.5 -1
model solve

model save 'blocks'

=====================================

block gridpoint ini disp 0 0 0
block contact reset disp

; ==== FISH for histories =====
[cxi0 = block.subcontact.near(0,0,0)]
fish def sh_mu
sh_mu = block.subcontact.prop(cxi0,'friction-current')
end

block gridpoint apply vel-x 1.0e-3 range pos-x 2.9 3.1
block contact his stress-norm pos 0 0 0
block contact his stress-shear pos 0 0 0
block contact his dis-shear pos 0 0 0

; get velocity
block hide range pos-z -1.5 -1
block his vel-x pos 0 0 0
block hide off

fish history sh_mu

block his fob

model save 'initial'

================================

; dc = 1e-4
model rest 'initial'

his interval 100
model cyc 30000
his interval 10
model cyc 30000

model save 'spring-slider-dc1e-4'

===========================================

; dc 1e-5
model rest 'initial'
block hide range pos-x 1 3 pos-z -1 1
block contact prop dc 1e-5
block hide off

his interval 100
model cyc 30000
his interval 10
model cyc 25000

model save 'spring-slider-dc1e-5'

========================================


dilation.dat

; File to test changing dilation angle with slip

model rest 'blocks'

block gridpoint ini disp 0 0 0
block contact reset disp

block gridpoint apply vel-x 1.0e-3 range pos-x 2.9 3.1

block contact his stress-norm pos 0 0 0
block contact his stress-shear pos 0 0 0
block contact his dis-shear pos 0 0 0
block contact his dis-norm pos 0 0 0

; function to compute dilation
fish def get_dilation
local cx0 = block.subcontact.near(0,0,0)
local ndis = block.subcontact.dis.norm(cx0)
local sdis = math.mag(block.subcontact.dis.shear(cx0))
local status = io.out('Dilation = '+string(dilation))
end

model save 'initial'

; ========= dilation constant 10 =============

; set joint properties
block hide range pos-x 1 3 pos-z -1 1
block contact prop dilation 10
block hide off

his interval 100
model cyc 30000
his interval 10
model cyc 15000

[get_dilation]

his export '4' vs '3' table 'dilation10'
table 'dilation10' export 'dilation10.tab'

; ========= dilation constant 2 =============

model rest 'initial'

; set joint properties
block hide range pos-x 1 3 pos-z -1 1
block contact prop dilation 2
block hide off

his interval 100
model cyc 30000
his interval 10
model cyc 15000

[get_dilation]

his export '4' vs '3' table 'dilation2'
table 'dilation2' export 'dilation2.tab'

; ========= dilation changing from 10 to 2 =============

model rest 'initial'

; set joint properties
block hide range pos-x 1 3 pos-z -1 1
block contact prop dilation 10 dilation-res 2
block hide off

his interval 100
model cyc 30000
his interval 10
model cyc 15000

[get_dilation]

his export '4' vs '3' table 'dilation_10_2'
table 'dilation10' import 'dilation10.tab'
table 'dilation2' import 'dilation2.tab'


## Properties

softening-mohr
alpha f

An exponent (>= 1) that dictates the severity of friction drop. If $$alpha$$ = 0, the linear friction reduction relationship is used.

cohesion f

Joint cohesion.

cohesion-residual f

Residual joint cohesion.

dc f

Slip distance over which friction reduces from peak to residual friction.

dilation f

Joint dilation angle in degrees.

dilation-zero f

Shear displacement at which joint will cease to dilate.

friction f

Peak friction angle in degrees.

friction-current f

Current friction angle in degrees (read only).

friction-residual f

Residual joint friction angle in degrees.

healing b

If set to true, friction recovers to the peak value when slipping stops. Default is true.

slip

stiffness-normal f

Joint normal stiffness (stress / distance)

stiffness-shear f

Joint shear stiffness (stress / distance)

tension f

Tensile strength.

tension-residual f

Residual joint tensile tensile.

## References

Rice, J., 1983. “Constitutive relations for fault slip and earthquake instabilities,” Pure Appl. Geoph., 116, 790-806, 1983.