Abstract
The present research focuses on the calculation of the bearing capacity of low-density volcanic Pyroclasts. First, the theoretical basis that define an adequate failure criterion for collapsible rocks based on the parameters that characterize them are developed here. Second, a mathematical characteristic lines method is proposed to resolve the ultimate load of shallow foundation rocks with collapsible failure criterion. This method leads to an analytical solution that differentiates two possible rupture mechanisms depending on the rock parameters and external confining load: (a) plastic failure wedge; (b) failure due to destructuring. The analytical solution is also represented in design abacuses to make it easy and quick. Finally, the proposed formulation is validated using numerical models by implementing the collapse criterion as a model defined by the user in a finite difference code. The result is a satisfactory comparison of bearing capacity values and the analytical rupture mechanisms.
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Abbreviations
- a, k :
-
Parameters dependent on the frictional parameter M of the collapse criterion curve
- E :
-
Friction function
- F :
-
Energy consumption function
- \(f_{1}\),\(f_{2}\) :
-
Dimensionless distributed load on to boundary 1 and 2
- I (ρ):
-
Engineering Riemann’s invariant
- \(M\) :
-
Frictional parameter of the collapse criterion curve
- \(M_{x}\), \(M_{y}\) :
-
Components of the mass forces
- \(N_{\rm col}\) :
-
Bearing capacity factor of the collapse criterion curve
- \(P_{\rm c}^{*}\) :
-
Isotropic compressive strength
- \(P_{\rm co}^{*}\) :
-
Pressure module
- P h :
-
Ultimate bearing capacity
- \(p_{\rm cri}\) :
-
Destructuring limit pressure in canonical variables
- \(p_{{\rm cri},{\rm T}}\) :
-
Tensile destructuring limit pressure in canonical variables
- \(p_{{\rm cri},{\rm C}}\) :
-
Compression destructuring limit pressure in canonical variables
- \(p_{\rm e}\) :
-
Load perpendicular to boundary 1 in physical variables
- \(p_{{\rm e},{\rm cri}}\) :
-
Critical external pressure in physical variables
- \(p_{\rm Kcri}\) :
-
Destructuring limit pressure in Cambridge variables
- q, p :
-
Canonical Hill–Lambe stresses
- \(q^{*}\), \(p^{*}\) :
-
Physical Hill–Lambe stresses
- \(q_{\rm R}\), \(p_{\rm R}\) :
-
Dimensionless real Hill–Lambe stresses
- \(q_{\rm R}^{*}\), \(p_{\rm R}^{*}\) :
-
Real Hill–Lambe stresses
- \(q_{\rm K}\), \(p_{\rm K}\) :
-
Canonical Cambridge stresses
- \(q_{\rm K}^{*}\), \(p_{\rm K}^{*}\) :
-
Physical Cambridge stresses
- \(q_{\rm KR}\), \(p_{\rm KR}\) :
-
Dimensionless real Cambridge stresses
- \(q_{\rm KR}^{*}\), \(p_{\rm KR}^{*}\) :
-
Real Cambridge stresses
- r, θ :
-
Polar coordinates of a point of the characteristic line
- R :
-
Energy consumption rate
- \(R_{\rm c}\) :
-
Energy consumption rate due to cohesion
- \(R_{\rm f}\) :
-
Energy consumption rate produced by friction
- SC:
-
External load on boundary 1
- \(t^{*}\) :
-
Isotropic tensile strength
- \(W^{\rm p}\) :
-
Physical work in the plastic failure
- x, y :
-
Cartesian coordinates of a point of the characteristic line
- α :
-
Inclination with respect to the horizontal of the boundary 2
- β :
-
Inclination with the horizontal of the unstructured wedge under the foundation
- \(\dot{\gamma }^{\rm p}\) :
-
Angular distortion rate
- \(\delta_{\rm o}\) :
-
Slope for the beginning of the collapse curve in Canonical Hill–Lambe stresses
- \(\delta_{\rm f}\) :
-
Slope for the end of the collapse curve in Canonical Hill–Lambe stresses
- \(\dot{\varepsilon }_{1}^{\rm p} ,\) \(\dot{\varepsilon }_{3}^{\rm p}\) :
-
Principal plastic strains rate
- \(\zeta\) :
-
Tensile coefficient
- \(\eta\) :
-
Obliquity
- \(\lambda\) :
-
Mathematical adjustment parameter of the collapse criterion curve
- \(\mu\) :
-
Angle between the direction of principal stress and the characteristic line
- \(\dot{v}^{\rm p}\) :
-
Volumetric plastic strain rate
- \(\chi\) :
-
Dilatancy
- \(\Psi\) :
-
Inclination of the major principal stress with vertical axis
- ρ :
-
Instantaneous friction angle
- \(\rho_{1} , \rho_{2}\) :
-
Instantaneous friction angle in boundary 1 and 2
- \(\rho_{1,{\rm cri}}\) :
-
Critical friction angle in boundary 1
- \(\rho_{\rm o}\) :
-
Friction angle for the beginning of the collapse criterion curve
- \(\rho_{\rm f}\) :
-
Friction angle for the end of the collapse criterion curve
- \(\sigma_{1}\), \(\sigma_{3}\) :
-
Canonical principal stresses
- \(\sigma_{1}^{*}\), \(\sigma_{3}^{*}\) :
-
Physical principal stresses
- \(\sigma_{1{\rm R}}\), \(\sigma_{3{\rm R}}\) :
-
Dimensionless real principal stresses
- \(\sigma_{1{\rm R}}^{*}\), \(\sigma_{3{\rm R}}^{*}\) :
-
Real principal stresses
- \(\sigma_{{\text{c}}}\) :
-
Simple compressive strength
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Acknowledgements
This research (Project: “Behavior study geomechanical of the pyroclasts low density canaries for your application on road works” 82-309-0-001-(IF)) was funded through the Canary Islands Government of Spain. The authors would like to thank State Research Center: CEDEX, who provided the field and laboratory tests and data of the work and allowed its publication. Finally, we would also like to thank Itasca Consultores S.L. for the technical assistance received in generating the numerical model in finite differences.
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Appendix: Theoretical bases of the failure criterion
Appendix: Theoretical bases of the failure criterion
The change in volumetric plastic deformation (\(\dot{v}^{\rm p}\)) and angular distortion (\(\dot{\gamma }^{\rm p}\)) can be expressed as a function of the major principal strain (\(\varepsilon_{1}\)) and minor principal strain (\(\varepsilon_{3}\)):
From the obliquity (\(\eta = q_{\rm KR} /p_{\rm KR}\)) and the dilatancy (\(\chi = \dot{v}^{\rm p} /\dot{\gamma }^{\rm p}\)) an energy consumption function (F) can be defined as the sum of both: \(F = \chi + \eta\), and the consumed physical work in the plastic failure (\(\dot{W}^{\rm p}\)) can be expressed by:
And therefore, with R being the consumption rate: \(R = \dot{W}^{\rm p} /\dot{\gamma }^{p}\), results \(R = F p_{\rm KR}\).
Considering Drucker's stability postulate (1964):
In a material with associated dilatancy the condition must be strictly verified, that is:
Since \(q_{\rm KR} = \eta p_{\rm KR}\), differentiating it will obtain:
Therefore:
An energy consumption law is proposed, which is an extension of the Granta Gravel model by Roscoe et al. (1963) to cohesive materials. Following these ideas, the energy consumption at failure has two addends, one (\(R_{\rm f} = M p_{\rm KR}^{2}\)) produced by friction (where M is a frictional parameter) and the second (\(R_{\rm c} = q_{i}\)) due to cohesion. In this way, and since it was deduced that \(R = F p_{\rm KR}\), it is possible to obtain:
From (A2) and (A3), the following differential equation is obtained:
The solution of this differential equation is immediate, and the solution can now be a function of the constant \(C_{1}\), resulting in:
Equation (A4) can be expressed in the previously defined physical canonical variables (\(p_{\rm KR} = p_{\rm K} - \zeta\), \(q_{\rm KR} = q_{\rm K}\)), so that:
Applying the known boundary condition (\(p_{\rm K} = 0\), \(q_{\rm K} = 0\)) in Eq. (A5), results into:
And considering in (A5) the other boundary condition (\(p_{\rm K} = 1\), \(q_{\rm K} = 0\)), obtains:
Finally, substituting (A6) and (A7) in (A5) the collapse equation that complies with what is indicated in (2) for the most common case of λ = 1 is obtained:
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Serrano, A., Galindo, R. & Perucho, Á. Ultimate Bearing Capacity of Low-Density Volcanic Pyroclasts: Application to Shallow Foundations. Rock Mech Rock Eng 54, 1647–1670 (2021). https://doi.org/10.1007/s00603-020-02341-7
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DOI: https://doi.org/10.1007/s00603-020-02341-7