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Basics of Thermomechanics and Inelasticity
Abstract Rock salt can undergo large inelastic deformations over extended periods of time. Many analyses, however, refer to time intervals and mechanical loads that cause deformations for which the small-strain assumption remains valid. Here, we restrict ourselves to such small-strain settings and postpone analyses under finite deformations to a follow-up contribution (compare also Fig. 2.1).
Basics of Thermomechanics and Inelasticity
Abstract Rock salt can undergo large inelastic deformations over extended periods of time. Many analyses, however, refer to time intervals and mechanical loads that cause deformations for which the small-strain assumption remains valid. Here, we restrict ourselves to such small-strain settings and postpone analyses under finite deformations to a follow-up contribution (compare also Fig. 2.1).
Basics of Thermomechanics and Inelasticity
Nagel, Thomas (author) / Böttcher, Norbert (author) / Görke, Uwe-Jens (author) / Kolditz, Olaf (author)
2017-01-01
16 pages
Article/Chapter (Book)
Electronic Resource
English
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