theorem 30.18 Cauchy: the stress tensor exists

open in the book · parts/03-classical-mechanics/13-continuum-elasticity.tex:551 · p. 1013

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theorem 30.18: Cauchy: the stress tensor exists30.18definition 30.17: Traction30.17definition 13.5: Tensor under orthogonal transformations13.5definition 30.24: The elasticity tensor30.24definition 31.1: Fluid31.1proposition 30.19: The stress tensor is symmetric30.19proposition 30.74: The maximum shear stress, and its indifference to pressure30.74remark 30.72: Stress concentration30.72theorem A.695: Boussinesq's point-force solution, quotedA.695theorem 30.21: Cauchy's equation of motion30.21proof : ch:13-continuum-elasticity@proof-7proofdefinition 7.126: Line and surface integrals7.126definition 30.2: Representative volume element; continuum field30.2definition 13.4: Orthogonal coordinate transformation13.4definition 19.42: Inertia tensor19.42definition 29.13: Inertia tensor, continuum form29.13lemma 30.26: Isotropic Cartesian tensors of rank four30.26notation 30.1: Strain and displacement share a letter30.1proposition 30.7: Strain is a Cartesian tensor of rank two30.7proposition 13.96: The cross product is an axial vector13.96proposition 13.6: Levi-Civita identities in three dimensions13.6proposition 19.43: The moment of inertia is a quadratic form in the axis19.43remark 13.7: What the classification is used for13.7definition 30.6: Linear strain and infinitesimal rotation30.6definition 30.37: Voigt notation30.37phenomenon 30.28: Hooke's law30.28proposition 30.25: Twenty-one constants30.25proposition 30.38: The Cauchy relations30.38remark 30.78: Anharmonicity: what the quadratic energy also suppresses30.78theorem A.675: Three constants for a cubic crystal, two for an isotropic solidA.675definition 31.21: Ideal fluid31.21definition 31.2: Knudsen number31.2definition 31.32: Newtonian fluid; dynamic and kinematic viscosity31.32proposition 31.16: Hydrostatic balance31.16definition 30.20: Pressure and deviatoric stress30.20proof : ch:13-continuum-elasticity@proof-8proofphenomenon 30.73: Yield and brittle fracture30.73remark A.705: The dangerous stress is below the surfaceA.705remark 30.75: Two criteria, one uncited30.75proof : ch:13-continuum-elasticity@proof-36proofneighborhood truncated

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typedirectionnode provenancewhere
depends_on Traction declared parts/03-classical-mechanics/13-continuum-elasticity.tex:560
depends_on Tensor under orthogonal transformations declared parts/03-classical-mechanics/13-continuum-elasticity.tex:560
depends_on The elasticity tensor declared parts/03-classical-mechanics/13-continuum-elasticity.tex:778
depends_on Fluid declared parts/03-classical-mechanics/14-fluid-dynamics.tex:60
depends_on The stress tensor is symmetric declared parts/03-classical-mechanics/13-continuum-elasticity.tex:605
depends_on The maximum shear stress, and its indifference to pressure declared parts/03-classical-mechanics/13-continuum-elasticity.tex:2629
depends_on Stress concentration declared parts/03-classical-mechanics/13-continuum-elasticity.tex:2577
depends_on Boussinesq's point-force solution, quoted declared appendices/A-long-proofs.tex:33755
depends_on Cauchy's equation of motion declared parts/03-classical-mechanics/13-continuum-elasticity.tex:668
proves ch:13-continuum-elasticity@proof-7 declared parts/03-classical-mechanics/13-continuum-elasticity.tex:563