Variational modeling of hydromechanical fracture in saturated porous media: A micromechanics-based phase-field approach

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autorschaft

  • Jacinto Ulloa
  • Nima Noii
  • Roberto Alessi
  • Fadi Aldakheel
  • Geert Degrande
  • Stijn François

Organisationseinheiten

Externe Organisationen

  • KU Leuven
  • California Institute of Technology (Caltech)
  • University of Pisa
  • Swansea University
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Details

OriginalspracheEnglisch
Aufsatznummer115084
FachzeitschriftComputer Methods in Applied Mechanics and Engineering
Jahrgang396
Frühes Online-Datum21 Mai 2022
PublikationsstatusVeröffentlicht - 1 Juni 2022

Abstract

This paper presents a novel variational phase-field model for different fracture processes in fully saturated porous media. As a key feature, the model employs a micromechanics-based theory for the description of brittle-tensile and compressive–ductile fracture. As such, the field variables are linked to physical mechanisms at the microcrack level, with damage emerging as the consequence of microcrack growth. Similarly, plasticity emerges as a consequence of the frictional sliding of closed microcracks. In this way, the evolution of opening microcracks in tension leads to (mode I) brittle fracture, while the evolution of closed microcracks in compression/shear leads to (mode II) ductile fracture. These failure mechanisms are coupled to fluid flow, resulting in a Darcy–Biot–type hydromechanical model. Therein, in the tensile regime, plasticity naturally vanishes, while damage is driven by poroelastic energy, accounting for the pressure in fluid-filled opening microcracks. On the other hand, in the compressive/shear regime, the plastic driving force naturally follows as a Terzaghi-type effective stress in terms of the local stress field acting on the microcrack surfaces, while damage is solely driven by the frictionally blocked free energy. As another important feature, the model includes a non-associative frictional plasticity law. Nevertheless, a thermodynamically consistent variational framework is employed, for which different energetic principles are discussed. Finally, the numerical simulations show that the model captures relevant hydromechanical coupling effects in benchmark problems, including mechanically induced shear fracture and hydraulically induced tensile fracture.

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Variational modeling of hydromechanical fracture in saturated porous media: A micromechanics-based phase-field approach. / Ulloa, Jacinto; Noii, Nima; Alessi, Roberto et al.
in: Computer Methods in Applied Mechanics and Engineering, Jahrgang 396, 115084, 01.06.2022.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Ulloa J, Noii N, Alessi R, Aldakheel F, Degrande G, François S. Variational modeling of hydromechanical fracture in saturated porous media: A micromechanics-based phase-field approach. Computer Methods in Applied Mechanics and Engineering. 2022 Jun 1;396:115084. Epub 2022 Mai 21. doi: 10.1016/j.cma.2022.115084
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title = "Variational modeling of hydromechanical fracture in saturated porous media: A micromechanics-based phase-field approach",
abstract = "This paper presents a novel variational phase-field model for different fracture processes in fully saturated porous media. As a key feature, the model employs a micromechanics-based theory for the description of brittle-tensile and compressive–ductile fracture. As such, the field variables are linked to physical mechanisms at the microcrack level, with damage emerging as the consequence of microcrack growth. Similarly, plasticity emerges as a consequence of the frictional sliding of closed microcracks. In this way, the evolution of opening microcracks in tension leads to (mode I) brittle fracture, while the evolution of closed microcracks in compression/shear leads to (mode II) ductile fracture. These failure mechanisms are coupled to fluid flow, resulting in a Darcy–Biot–type hydromechanical model. Therein, in the tensile regime, plasticity naturally vanishes, while damage is driven by poroelastic energy, accounting for the pressure in fluid-filled opening microcracks. On the other hand, in the compressive/shear regime, the plastic driving force naturally follows as a Terzaghi-type effective stress in terms of the local stress field acting on the microcrack surfaces, while damage is solely driven by the frictionally blocked free energy. As another important feature, the model includes a non-associative frictional plasticity law. Nevertheless, a thermodynamically consistent variational framework is employed, for which different energetic principles are discussed. Finally, the numerical simulations show that the model captures relevant hydromechanical coupling effects in benchmark problems, including mechanically induced shear fracture and hydraulically induced tensile fracture.",
keywords = "Hydraulic fracture, Micromechanics, Non-associative plasticity, Phase-field models, Porous media, Variational formulation",
author = "Jacinto Ulloa and Nima Noii and Roberto Alessi and Fadi Aldakheel and Geert Degrande and Stijn Fran{\c c}ois",
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Download

TY - JOUR

T1 - Variational modeling of hydromechanical fracture in saturated porous media

T2 - A micromechanics-based phase-field approach

AU - Ulloa, Jacinto

AU - Noii, Nima

AU - Alessi, Roberto

AU - Aldakheel, Fadi

AU - Degrande, Geert

AU - François, Stijn

N1 - Funding Information: F. Aldakheel and N. Noii were funded by the Priority Program DFG-SPP 2020 (project number: 353757395).

PY - 2022/6/1

Y1 - 2022/6/1

N2 - This paper presents a novel variational phase-field model for different fracture processes in fully saturated porous media. As a key feature, the model employs a micromechanics-based theory for the description of brittle-tensile and compressive–ductile fracture. As such, the field variables are linked to physical mechanisms at the microcrack level, with damage emerging as the consequence of microcrack growth. Similarly, plasticity emerges as a consequence of the frictional sliding of closed microcracks. In this way, the evolution of opening microcracks in tension leads to (mode I) brittle fracture, while the evolution of closed microcracks in compression/shear leads to (mode II) ductile fracture. These failure mechanisms are coupled to fluid flow, resulting in a Darcy–Biot–type hydromechanical model. Therein, in the tensile regime, plasticity naturally vanishes, while damage is driven by poroelastic energy, accounting for the pressure in fluid-filled opening microcracks. On the other hand, in the compressive/shear regime, the plastic driving force naturally follows as a Terzaghi-type effective stress in terms of the local stress field acting on the microcrack surfaces, while damage is solely driven by the frictionally blocked free energy. As another important feature, the model includes a non-associative frictional plasticity law. Nevertheless, a thermodynamically consistent variational framework is employed, for which different energetic principles are discussed. Finally, the numerical simulations show that the model captures relevant hydromechanical coupling effects in benchmark problems, including mechanically induced shear fracture and hydraulically induced tensile fracture.

AB - This paper presents a novel variational phase-field model for different fracture processes in fully saturated porous media. As a key feature, the model employs a micromechanics-based theory for the description of brittle-tensile and compressive–ductile fracture. As such, the field variables are linked to physical mechanisms at the microcrack level, with damage emerging as the consequence of microcrack growth. Similarly, plasticity emerges as a consequence of the frictional sliding of closed microcracks. In this way, the evolution of opening microcracks in tension leads to (mode I) brittle fracture, while the evolution of closed microcracks in compression/shear leads to (mode II) ductile fracture. These failure mechanisms are coupled to fluid flow, resulting in a Darcy–Biot–type hydromechanical model. Therein, in the tensile regime, plasticity naturally vanishes, while damage is driven by poroelastic energy, accounting for the pressure in fluid-filled opening microcracks. On the other hand, in the compressive/shear regime, the plastic driving force naturally follows as a Terzaghi-type effective stress in terms of the local stress field acting on the microcrack surfaces, while damage is solely driven by the frictionally blocked free energy. As another important feature, the model includes a non-associative frictional plasticity law. Nevertheless, a thermodynamically consistent variational framework is employed, for which different energetic principles are discussed. Finally, the numerical simulations show that the model captures relevant hydromechanical coupling effects in benchmark problems, including mechanically induced shear fracture and hydraulically induced tensile fracture.

KW - Hydraulic fracture

KW - Micromechanics

KW - Non-associative plasticity

KW - Phase-field models

KW - Porous media

KW - Variational formulation

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U2 - 10.1016/j.cma.2022.115084

DO - 10.1016/j.cma.2022.115084

M3 - Article

AN - SCOPUS:85133895493

VL - 396

JO - Computer Methods in Applied Mechanics and Engineering

JF - Computer Methods in Applied Mechanics and Engineering

SN - 0045-7825

M1 - 115084

ER -