2020
DOI: 10.1051/e3sconf/202020513014
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A thermomechanical model for argillaceous rocks

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Cited by 3 publications
(2 citation statements)
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“…10)As 𝑑𝜑 = 𝑑𝜑(𝑑 𝜀 𝑒𝑞 𝑝 , 𝑑 𝑇) and 𝑑𝑐 = 𝑑𝑐(𝑑 𝜀 𝑒𝑞 𝑝 , 𝑑 𝑇) the plastic multiplier 𝜆, which controls the amount of the plastic strain rate, is affected by the change in 𝜑 and c(Tourchi et al, 2020): strain increment is affected by the thermal variation of internal friction and cohesion, as long as 𝜎 ′ ≠ 0. Otherwise, this dependence disappears, as for both forms of the yield locus 𝜕𝜑 𝜕𝑇 ⁄…”
mentioning
confidence: 99%
“…10)As 𝑑𝜑 = 𝑑𝜑(𝑑 𝜀 𝑒𝑞 𝑝 , 𝑑 𝑇) and 𝑑𝑐 = 𝑑𝑐(𝑑 𝜀 𝑒𝑞 𝑝 , 𝑑 𝑇) the plastic multiplier 𝜆, which controls the amount of the plastic strain rate, is affected by the change in 𝜑 and c(Tourchi et al, 2020): strain increment is affected by the thermal variation of internal friction and cohesion, as long as 𝜎 ′ ≠ 0. Otherwise, this dependence disappears, as for both forms of the yield locus 𝜕𝜑 𝜕𝑇 ⁄…”
mentioning
confidence: 99%
“…Figure12: Model geometry, boundary conditions and finite element mesh employed(Tourchi et al, 2020).…”
mentioning
confidence: 99%