4.7 Article

The Influence of Temperature on Time-Dependent Deformation and Failure in Granite: A Mesoscale Modeling Approach

Journal

ROCK MECHANICS AND ROCK ENGINEERING
Volume 50, Issue 9, Pages 2345-2364

Publisher

SPRINGER WIEN
DOI: 10.1007/s00603-017-1228-9

Keywords

Brittle creep; Temperature; Creep strain rate; Damage evolution; Numerical simulation

Funding

  1. National Basic Research Program (973) of China [2013CB227902, 2014CB047100]
  2. Natural Science Foundation of China [41672301, 51474051, 41172265, 51574059, 51404067]
  3. Partenariats Hubert Curien (PHC) Cai Yuanpei grant [36605ZB]
  4. Fundamental Research Funds for the Central Universities of China [N150102002]
  5. French Agence Nationale de la Recherche (ANR) [ANR-ANR-15-CE06-0014-01]
  6. LABEX grant [ANR-11-LABX-0050]
  7. Agence National de la Recherche (ANR)
  8. Agence Nationale de la Recherche (ANR) [ANR-11-LABX-0050] Funding Source: Agence Nationale de la Recherche (ANR)

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An understanding of the influence of temperature on brittle creep in granite is important for the management and optimization of granitic nuclear waste repositories and geothermal resources. We propose here a two-dimensional, thermo-mechanical numerical model that describes the time-dependent brittle deformation (brittle creep) of low-porosity granite under different constant temperatures and confining pressures. The mesoscale model accounts for material heterogeneity through a stochastic local failure stress field, and local material degradation using an exponential material softening law. Importantly, the model introduces the concept of a mesoscopic renormalization to capture the co-operative interaction between microcracks in the transition from distributed to localized damage. The mesoscale physico-mechanical parameters for the model were first determined using a trial-and-error method (until the modeled output accurately captured mechanical data from constant strain rate experiments on low-porosity granite at three different confining pressures). The thermo-physical parameters required for the model, such as specific heat capacity, coefficient of linear thermal expansion, and thermal conductivity, were then determined from brittle creep experiments performed on the same low-porosity granite at temperatures of 23, 50, and 90 A degrees C. The good agreement between the modeled output and the experimental data, using a unique set of thermo-physico-mechanical parameters, lends confidence to our numerical approach. Using these parameters, we then explore the influence of temperature, differential stress, confining pressure, and sample homogeneity on brittle creep in low-porosity granite. Our simulations show that increases in temperature and differential stress increase the creep strain rate and therefore reduce time-to-failure, while increases in confining pressure and sample homogeneity decrease creep strain rate and increase time-to-failure. We anticipate that the modeling presented herein will assist in the management and optimization of geotechnical engineering projects within granite.

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