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Traction fields and stress matrices of the continuum model, with units and sign conventions

Physical scope

The model's contact-force quantity: a traction field assigning to each point and unit normal the force per unit area exerted across a surface, its dimensions, and the stress matrix representing it when one exists; the sign convention identifying compressive normal traction with negative scalar stress, the component reading, and the distinction from body-force densities. Existence of a representing stress matrix, its continuity and its symmetry are not asserted here; they are conditional conclusions of the balance items of this page. No measured force is asserted.

Definition

Fix body data (B,O,I) and a motion χ of the model with current regions Ωt=χt(B) and U={(s,x):s∈I, x∈χs(O)}. Let U⊆U be open and contain the swept closure {(s,x):s∈J0‾, x∈χs(B‾)}, where J0 is an open interval with compact closure in I (Adopted continuum kinematic model: body data, smooth motions as families of label worldlines, the continuum idealization and frame covariance, Continuum motions, spatial velocity, material acceleration and swept regions). Use on U the restriction of the positive C1 density slot ρ:U→(0,∞) of Continuum body data, the fixed inertial frame and the dimensions of the fields, and denote that restriction again by ρ. Let S2={n∈R3:∥n∥2=1} be the unit sphere.

A traction field of the model is a map

t:U×S2⟶R3,

read with the convention of Traction fields and stress matrices representing them: t(s,x,n) is the force per unit area exerted by the material on the side towards which n points upon the material on the other side, at the point x of a surface whose unit normal is n, at time s. Its dimension is that of force per area, [t]=μℓ−1τ−2, read in N m−2 (Dimensions and SI unit conventions of the non-relativistic classical mechanics framework).

A C1 field of matrices σ:U→M3(R) represents the traction field when

t(s,x,n)=σ(s,x) nfor every (s,x,n)∈U×S2,

the product being matrix-vector multiplication. The existence of such a σ for a given traction field is not asserted here: it is a conditional conclusion of the balance items of this page. When it exists, σ(s,x) is the stress matrix of the model at that event, and its entries read σij=(t(s,x,ej))i: the i-th component of the traction across the surface with normal ej.

The isotropic matrix −λI3 with λ∈R represents the normal traction t(n)=−λn: under the convention above, positive λ is a compressive normal traction and λ is called the pressure in this sign convention. Within this isotropic family, λ=0 gives the zero stress matrix, a pressure-free unstressed state. The body force per unit mass is a separate object: a continuous field b:U→R3 with the dimension of acceleration, [b]=ℓτ−2. The body-force density per unit volume is ρb:U→R3, of dimension μℓ−2τ−2. A traction field need not satisfy t(−n)=−t(n) and its representing matrix, when one exists, need not be symmetric; both properties are separate conditional conclusions.

Remarks

  • Cauchy's hypothesis is a modelling assumption. The definition lets the traction depend on the surface only through its unit normal at the point. Contact interactions that depend on the curvature of the surface, on a surface couple distribution, or on a thin boundary layer would require a richer object; the counterexample item of the companion page shows that the global symmetry t(−n)=−t(n) alone, without a balance law, does not even force the existence of a representing matrix.

  • Units and interpretation. The values of t and σ are model quantities in the fixed frame of Continuum body data, the fixed inertial frame and the dimensions of the fields. A measured force per area is related to them only through a measurement model and is not asserted by this definition; no measured stress is recorded on this page.

  • Sign convention. The convention is the one of Traction fields and stress matrices representing them: t(n) acts on the material on the side opposite to that towards which n points. With this convention a fluid whose total stress is assumed to lie in the isotropic family defined above has σ=−pI3, so positive p gives compression in the direction −n. Positive pressure alone does not impose this isotropic stress assumption.

Depends on

Dependency tree · 2 levels

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