- mechanics_functions.general_geotech_funcs.calc_Jaky_at_rest(phi_prime)¶
Calculate at rest earth pressure coefficient (k_{0}) using Jaky relationship.
- Parameters:
phi_prime (float) – Effective friction angle [degrees].
- Returns:
Coefficient of At Rest Lateral Earth Pressure
- Return type:
float
Notes
The coefficient of at rest lateral earth pressure is calculated using the equation:
\[\]- where:
\(k_{0}\) : Coefficient of At Rest Lateral Earth Pressure
:math:phi_prime` : Effective friction angle
- mechanics_functions.general_geotech_funcs.calc_cambridge_mean_eff_stress(sigma_1, sigma_2, sigma_3)¶
Calculate the Cambridge mean effective stress (p’).
- Parameters:
sigma_1 (float) – Effective stress 1.
sigma_2 (float) – Effective stress 2.
sigma_3 (float) – Effective stress 3.
- Returns:
Cambridge mean effective stress (p’).
- Return type:
float
Notes
The Cambridge mean effective stress is calculated using the equation:
\[p' = \frac{{\sigma'_{1} + \sigma'_{2} + \sigma'_{3}}}{{3}}\]- where:
\(p'\) : Cambridge mean effective stress.
\(\sigma'_{1}\) : Effective stress 1.
\(\sigma'_{3}\) : Effective stress 3.
\(\sigma'_{2}\) : Effective stress 2.
- mechanics_functions.general_geotech_funcs.calc_consolidation_coeff(diameter, t_50, T_50=0.6)¶
Calculate the consolidation coefficient (c_h).
This function computes the consolidation coefficient based on the given diameter, time to 50% pore pressure dissipation, and a dimensionless time factor.
- Parameters:
diameter (float) – Diameter of the penetrating object [m].
t_50 (float) – Time to 50% of pore pressure dissipation [s].
T_50 (float, optional) – Dimensionless time factor (default is 0.6).
- Returns:
Consolidation coefficient [m^2/s].
- Return type:
float
Notes
The consolidation coefficient is calculated using the following equation:
\[c_{h} = \frac{D^{2} T_{50}}{t_{50}}\]- where:
\(D\) is the diameter of the penetrating object.
\(t_{50}\) is the time to 50% of pore pressure dissipation.
\(T_{50}\) is the dimensionless time factor.
Reference¶
White, D. J., et al. “Free fall penetrometer tests in sand: Determining the equivalent static resistance.”
- mechanics_functions.general_geotech_funcs.calc_dimensionless_velocity(v, D, coeff_consolidation)¶
Calculate the dimensionless velocity (V).
- Parameters:
v (float) – Probe velocity [m/s].
D (float) – Diameter of the probe [m].
coeff_consolidation (float) – Consolidation coefficient (c_{h}).
- Returns:
Dimensionless velocity (V).
- Return type:
float
Notes
The dimensionless velocity is calculated using the equation:
\[V = \frac{v \cdot D}{c_{h}}\]where:
\(V\) : Dimensionless velocity.
\(v\) : Probe velocity.
\(D\) : Diameter of the probe.
\(c_{h}\) : Consolidation coefficient.
- mechanics_functions.general_geotech_funcs.calc_mohr_coulomb_su(failure_mean_eff_stress, phi_cv=32)¶
Calculate the undrained strength (s_{u}) assuming a Mohr-Coulomb failure envelope.
- Parameters:
failure_mean_eff_stress (float) – Mean effective stress at failure [kPa].
phi_cv (float) – Friction angle at constant volume [degrees].
- Returns:
Undrained strength (s_{u}) [kPa].
- Return type:
float
Notes
The undrained strength is calculated using the equation:
\[s_{u} = \frac{1}{2} p'_{f} \frac{6 \sin(\phi_{cv})}{3 - \sin(\phi_{cv})}\]- where:
\(s_{u}\) : Undrained strength.
\(p'_{f}\) : Mean effective stress at failure.
:math:phi_{cv}` : Friction angle at constant volume (in degrees).
- mechanics_functions.general_geotech_funcs.calc_white_failure_mean_eff_stress(relative_density, Q=10)¶
Calculate the mean effective stress at failure (p’_{f}).
- Parameters:
Q (float) – Crushing strength parameter. Commonly taken as 10.
relative_density (float) – Relative density.
- Returns:
Mean effective stress at failure (p’_{f}) [kPa].
- Return type:
float
Notes
The mean effective stress at failure is calculated using the equation:
\[p'_{f} = e^{Q - \frac{1}{I_{D}}}\]- where:
\(p'_{f}\) : Mean effective stress at failure.
\(Q\) : Crushing strength parameter.
\(I_{D}\) : Relative density.
Note that the equation derivation assumes zero relative dilatancy (I_{R} = 0) at undrained failure.