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Theory of elasticity
TLDR
The theory of the slipline field is used in this article to solve the problem of stable and non-stressed problems in plane strains in a plane-strain scenario.Abstract:
Chapter 1: Stresses and Strains Chapter 2: Foundations of Plasticity Chapter 3: Elasto-Plastic Bending and Torsion Chapter 4: Plastic Analysis of Beams and Frames Chapter 5: Further Solutions of Elasto-Plastic Problems Chapter 6: Theory of the Slipline Field Chapter 7: Steady Problems in Plane Strain Chapter 8: Non-Steady Problems in Plane Strainread more
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Topological defects in graphene: dislocations and grain boundaries
Oleg V. Yazyev,Steven G. Louie +1 more
TL;DR: In this paper, a general approach for constructing dislocations in graphene characterized by arbitrary Burgers vectors as well as grain boundaries, covering the whole range of possible misorientation angles, is introduced.
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The deformation behavior of ceramic crystals subjected to very low load (nano)indentations
TL;DR: In this article, a software-controlled hardness tester (Nanoindenter) operating in the load range 2-60 mN was used to characterize the deformation structures associated with these very small-scale hardness impressions.
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Fundamentals of flexoelectricity in solids
TL;DR: This review paper presents a critical analysis of the current knowledge on the flexoelectricity in common solids, excluding organic materials and liquid crystals.
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Viscoelastic shear properties of in vivo breast lesions measured by MR elastography
TL;DR: The in vivo results show a good separation between breast cancer and benign fibroadenoma utilizing the shear modulus and the results as obtained for theShear viscosity do not indicate to be useful for separating benign from malignant lesions.
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Northeast-southwest compressive stress in Alberta evidence from oil wells
J. S. Bell,D. I. Gough +1 more
TL;DR: In this article, Babcock et al. showed that hole elongation occurs in siltstones, sandstones, limestones, dolomites and one shale formation, and through the stratigraphic column from Devonian to Cretaceous.