A multiscale poroelastic damage model for fracturing in permeable rocks

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Jianxiong Yang
  • Jianfeng Liu
  • Wenfeng Li
  • Jingjing Dai
  • Fujun Xue
  • Xiaoying Zhuang

Organisationseinheiten

Externe Organisationen

  • Sichuan University
  • Los Alamos National Laboratory
  • Tongji University
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Aufsatznummer105676
Seitenumfang21
FachzeitschriftInternational Journal of Rock Mechanics and Mining Sciences
Jahrgang175
Frühes Online-Datum24 Feb. 2024
PublikationsstatusVeröffentlicht - März 2024

Abstract

A new poroelastic damage model is developed in the paper to describe the macroscopic failure of rock materials due to microcrack nucleation and propagation based on a multiscale framework. The model is deduced from locally periodic microstructure with dynamically evolved microcracks in heterogeneous rock body. The homogenization method based on asymptotic expansions gives rise to the damage evolution law coupled with the poroelastic fracture system, which includes the fracture opening induced permeability change. The obtained model takes into account the complex coupling between fluid pressure-deformation and hydro-mechanical (HM) properties at the microscale, leading to the nonlinear anisotropic mechanical behavior, degradation of both elastic stiffness and poroelastic properties at the macroscale, which is fundamental to describe the complex fracturing behavior influenced by microcrack distribution. The homogenized coefficients are illustrated in detail for a given set of initial material parameters, with dependence on the normalized damage variable. Results of numerical simulations well reproduce specific experimental observations where fracturing in heterogeneous rocks is shown to be a multiscale phenomenon that initiates from the microcrack nucleation and propagation, while the fracture propagation direction is shown to be influenced by both external loadings and microcrack distribution. The easy implementation in finite element framework and revealed micro-mechanism for macroscopic failure under strict mathematical formulations make the wide application of model in rock mechanics problems.

ASJC Scopus Sachgebiete

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A multiscale poroelastic damage model for fracturing in permeable rocks. / Yang, Jianxiong; Liu, Jianfeng; Li, Wenfeng et al.
in: International Journal of Rock Mechanics and Mining Sciences, Jahrgang 175, 105676, 03.2024.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Yang J, Liu J, Li W, Dai J, Xue F, Zhuang X. A multiscale poroelastic damage model for fracturing in permeable rocks. International Journal of Rock Mechanics and Mining Sciences. 2024 Mär;175:105676. Epub 2024 Feb 24. doi: 10.1016/j.ijrmms.2024.105676
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abstract = "A new poroelastic damage model is developed in the paper to describe the macroscopic failure of rock materials due to microcrack nucleation and propagation based on a multiscale framework. The model is deduced from locally periodic microstructure with dynamically evolved microcracks in heterogeneous rock body. The homogenization method based on asymptotic expansions gives rise to the damage evolution law coupled with the poroelastic fracture system, which includes the fracture opening induced permeability change. The obtained model takes into account the complex coupling between fluid pressure-deformation and hydro-mechanical (HM) properties at the microscale, leading to the nonlinear anisotropic mechanical behavior, degradation of both elastic stiffness and poroelastic properties at the macroscale, which is fundamental to describe the complex fracturing behavior influenced by microcrack distribution. The homogenized coefficients are illustrated in detail for a given set of initial material parameters, with dependence on the normalized damage variable. Results of numerical simulations well reproduce specific experimental observations where fracturing in heterogeneous rocks is shown to be a multiscale phenomenon that initiates from the microcrack nucleation and propagation, while the fracture propagation direction is shown to be influenced by both external loadings and microcrack distribution. The easy implementation in finite element framework and revealed micro-mechanism for macroscopic failure under strict mathematical formulations make the wide application of model in rock mechanics problems.",
keywords = "Damage law, Heterogeneous rock, Homogenization, Microcrack, Multiscale fracturing",
author = "Jianxiong Yang and Jianfeng Liu and Wenfeng Li and Jingjing Dai and Fujun Xue and Xiaoying Zhuang",
note = "Funding Information: This research was financially supported by the National Natural Science Foundation of China (Grant No. 12302503 , U20A20266 ) and the Scientific and technological research projects in Sichuan province (Grant No. 2023ZYD0154 , 2024GJHZ0035 ). ",
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T1 - A multiscale poroelastic damage model for fracturing in permeable rocks

AU - Yang, Jianxiong

AU - Liu, Jianfeng

AU - Li, Wenfeng

AU - Dai, Jingjing

AU - Xue, Fujun

AU - Zhuang, Xiaoying

N1 - Funding Information: This research was financially supported by the National Natural Science Foundation of China (Grant No. 12302503 , U20A20266 ) and the Scientific and technological research projects in Sichuan province (Grant No. 2023ZYD0154 , 2024GJHZ0035 ).

PY - 2024/3

Y1 - 2024/3

N2 - A new poroelastic damage model is developed in the paper to describe the macroscopic failure of rock materials due to microcrack nucleation and propagation based on a multiscale framework. The model is deduced from locally periodic microstructure with dynamically evolved microcracks in heterogeneous rock body. The homogenization method based on asymptotic expansions gives rise to the damage evolution law coupled with the poroelastic fracture system, which includes the fracture opening induced permeability change. The obtained model takes into account the complex coupling between fluid pressure-deformation and hydro-mechanical (HM) properties at the microscale, leading to the nonlinear anisotropic mechanical behavior, degradation of both elastic stiffness and poroelastic properties at the macroscale, which is fundamental to describe the complex fracturing behavior influenced by microcrack distribution. The homogenized coefficients are illustrated in detail for a given set of initial material parameters, with dependence on the normalized damage variable. Results of numerical simulations well reproduce specific experimental observations where fracturing in heterogeneous rocks is shown to be a multiscale phenomenon that initiates from the microcrack nucleation and propagation, while the fracture propagation direction is shown to be influenced by both external loadings and microcrack distribution. The easy implementation in finite element framework and revealed micro-mechanism for macroscopic failure under strict mathematical formulations make the wide application of model in rock mechanics problems.

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KW - Homogenization

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