2018
DOI: 10.1016/j.ijrmms.2018.07.004
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A new approach to quantify the anisotropy of hydromechanical strains in clay-rock at the gallery scale

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Cited by 5 publications
(9 citation statements)
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“…The set of pictures and the H-DIC algorithm have demonstrated the anisotropy of hydric strains along the directions parallel and perpendicular to the stratification and the presence of subhorizontal and subvertical cracks with intervals of 34.97 to 69.4 mm between subhorizontal cracks. 10 These observations and Figure 1 confirm the presence of mixed-mode I-mode III fractures in the argillaceous rock submitted to natural variations in hygrometry. Figure 7 presents, on a state close to an extreme state (ΔRH = 73.71%, ΔT = 7.22 C), the jump maps (o, s) and α-map calculated using the H-DIC algorithm.…”
Section: Applications To a Real Casesupporting
confidence: 72%
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“…The set of pictures and the H-DIC algorithm have demonstrated the anisotropy of hydric strains along the directions parallel and perpendicular to the stratification and the presence of subhorizontal and subvertical cracks with intervals of 34.97 to 69.4 mm between subhorizontal cracks. 10 These observations and Figure 1 confirm the presence of mixed-mode I-mode III fractures in the argillaceous rock submitted to natural variations in hygrometry. Figure 7 presents, on a state close to an extreme state (ΔRH = 73.71%, ΔT = 7.22 C), the jump maps (o, s) and α-map calculated using the H-DIC algorithm.…”
Section: Applications To a Real Casesupporting
confidence: 72%
“…According to the results of Hedan et al 10 regarding the variability of the anisotropy ratio of argillaceous rock submitted to a natural annual cycle, the scheme of principle ( Figure 1a) confirms that the spatial heterogeneity of strains induces opening and shear modes along the boundaries of blocks 1 and 2 ( Figure 1b). The opening value o _imp is constant and equal to 0.645, and in the shear mode, s _imp evolves slightly but linearly in the range of −0.615 to −0.625.…”
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confidence: 60%
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