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Unsaturated Zone Calculations

Unsaturated Zone Calculations section under Strength tab provides extension to the conventional geomechanical constitutive models to accommodate for the unsaturated soil behavior. RS3 provides two approaches, including Unsaturated Shear Strength and Single Effective Stress. In short, the Unsaturated Shear Strength provides direct control over how shear strength evolves with changes in pore pressure, whereas Single Effective Stress approach modifies the effective stress formulation by applying a suction (or degree of saturation)-related coefficient to the pore pressure term. Barcelona Basic model (Strength > Failure Criterion > Softening / Hardening > Barcelona Basic) is a constitutive model based on the Cam-Clay type effective stress model for the behavior of unsaturated clay-type soils.

  1. Unsaturated Zone Calculations option is only effective for Finite Element seepage analysis methods (Steady state and Transient)
  2. For detailed information about the underlying theory and formulations RS3 to accommodate the unsaturated soil mechanics, see the linked topic.

Unsaturated Shear Strength

The Unsaturated Shear Strength models, including Fredlund (1978) and Vanapalli (1996), are provided under Unsaturated Zone Calculation section. These models are extensions of the Mohr–Coulomb criterion, enhancing its ability to represent the development of shear strength in relation to soil moisture conditions. They are only accessible when the Mohr–Coulomb criterion is selected and the Material Type is set to Plastic.

  1. As described in sections below, the pore water pressure parameter is inherited in the shear strength formulations of the two models. To avoid twofold effect of matric suction in both effective stress calculation, as well as the shear strength calculation, the Maximum Negative Pore Water Pressure defined under Hydraulics tab is automatically set to 0 pressure unit when Unsaturated Shear Strength model is enabled.
  2. By convention, the term matric suction implies the POSITIVE, or absolute value of the negative pore pressures calculated in the unsaturated zone

Fredlund (1978)

Suggested by Fredlund et al (1978), the unsaturated shear strength is calculated as:

fredlund method_1
whereeffective cohesion of saturated soil_cprimeis the effective saturated cohesion,total stressis the total stress,net normal stress on the plane of failure at failureis the net normal stress on the plane of failure at failure,wherematric suction_eqnis the matric suction,pore air pressureis the pore-air pressure,pore water pressureis the pore water pressure,effective saturated angle of frictionis the effective saturated angle of friction, andangle of friction with respect to matric suctionis the angle of friction accounting for matric suction contribution to shear strength. Note that the Unsaturated Shear Strength Angle is usually not a well-known quantity. To obtain an appreciation of its importance, a parametric study can be carried out, in which the Unsaturated Shear Strength Angle is varied between 0 and the Friction Angle of the material.

Air Entry Value

Air Entry value is defined in Fredlund and Rahardjo (1993) as the matric suction value that must be exceeded before air recedes into the soil pores. The Air Entry Value is also referred to as the "displacement pressure" in petroleum engineering or the "bubbling pressure" in ceramics engineering.

In terms of strength, it is the point at which the strength of the soil deviates from its saturated effective Mohr-Coulomb behavior. If matric suction exceeds the air entry value, the strength is assumed to follow a linear envelope with angle of friction with respect to matric suction as the friction angle. Thus RS3 uses a bilinear strength envelope where:

  • effective cohesion of saturated soil_cprime and effective saturated angle of friction are used with positive pore pressures, and with negative pore pressures (matric suction) up to the air entry value
  • angle of friction with respect to matric suction is used when negative pore pressure exceeds the air entry value.

The following figure (after Fredlund (2000) ) illustrates the effect of the air entry value. For matric suction less than the air entry value, the saturated effective stress friction angle is used. For matric suction greater than the air entry value, the unsaturated shear strength angle, angle of friction with respect to matric suction is used.

Effect of air entry value (aev) on unsaturated shear strength envelopes
Effect of air entry value (aev) on unsaturated shear strength envelopes

Maximum Negative Pore Water Pressure for Unsaturated Shear Strength

This is an optional parameter to set the threshold impact of suction for the effective stress calculation of soil above the water table. The essence of this parameter is different from the one under Hydraulics tab or Project Settings > Groundwater tab. The one under Hydraulics tab is the limitation applying to the pore water pressure in effective stress principle (total stress' = total stress - pore water pressure) and the one under Fredlund (1978) model sets the limitation to the same parameter in shear strength formula (fredlund method_1).

Vanapalli (1996)

Proposed by Vanapalli et al (1996), the unsaturated shear strength can be represented using either the degree of saturation or the water content.

With degree of saturation,

Vanapalli degree of saturation
whereresidual degree of saturationis the residual degree of saturation anddegree of saturationis degree of saturation.

With water content,

Vanapalli water content
wherewater contentis the water content,residual water contentis the residual water content, andsaturated water contentis the saturated water content. The water content or degree of saturation values are to be inputted on the Hydraulic tab of the Define Material Properties dialog.

Single Effective Stress

The Single Effective Stress calculation approach is available for all failure criteria models except for the Barcelona model. According to Bishop (1959), the single effective stress for unsaturated soils is written as:

single effective stress_eqn

Where effe stress is the effective stress, total stress is the total stress, chiis the surface fraction coefficient, pore air pressureis the pore-air pressure, and pore water pressure is the pore water pressure. In practice, pore air pressure is omitted from the equation, thus the effective stress will be calculated as:

single effective stress_eqn_calc

where suction is the suction, and unit matrix is the unit matrix.
In RS3, the value ofchican be determined by nine different methods. Note thatchi=1 for saturated soils when the Unsaturated Zone Calculations is off. For more information, see the “Soil Behaviors in Unsaturated Zones” theory manual for explanation on each method below:
  1. Bishop (1959)
  2. Tabular Values – with respect to suction
    • Users define a table ofchivs. matric suction values.
  3. Tabular Values – with respect to degree of saturation
    • Users define a table ofchivs. degree of saturation ( degree of saturation) values.
  4. Tabular Values – with respect to effective degree of saturation
    • Users define a table of chivs. effective degree of saturation (effective degree of saturation_se) values.
  5. Gudehus (1995)
  6. Khalili (2004)
  7. Bolzon (1996)
  8. Aitchison (1961)
  9. Kohgo (1993)

Use Cutoff

The Use Cutoff option is subjected to the Single Effective Stress approach only, intended for limiting the suction (suction). In the calculation based on the equation above, an upper limit cutoff value can be set for the termsingle effective stress_suction term. The default input is -100 kPa.

This Use Cutoff option is applicable exclusively to the Single Effective Stress approach. It is independent from the Maximum Negative Pore Water Pressure.

Barcelona Basic

The Barcelona Basic model is based on the Cam-Clay type effective stress model for the behavior of unsaturated clay-type soils. This constitutive model can be adopted for a material property by selecting Failure Criterion > Softening/Hardening > Barcelona Basic under Strength tab. Alternative to single effective stress, the effect of suction on mechanical behaviors can be directly interpreted through this constitutive model that account for the matric suction.

In such cases, the effective stress for fully saturated zone will be calculated as usual, however, in the unsaturated zone, the total stress will be employed (total stress) and the unsaturated behavior will be considered in the constitutive model.
In alignment with Unsaturated Shear Strength models, the Maximum Negative Pore Water Pressure of the material under Hydraulics tab is automatically set to 0 pressure unit when Unsaturated Shear Strength model is enabled.
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