Take the trace of the constitutive relation at zero stress. It gives . With the observed stress-free volume strain this requires
This is the bulk modulus. A stable solid resists uniform compression, so ; equivalently the elastic energy of a nonzero pure dilation is positive. The thermal strain is isotropic, , because here is the volumetric, not linear, thermal expansion coefficient.
Let . Using , stress divergence is
Zero body force and equilibrium therefore give
For an applied body force per unit volume , equilibrium is , so its right-hand side becomes . Consequently
cancels the effective thermal forcing in the displacement equation. Per unit mass the force is . This sign follows from the divergence of the thermal stress , which is . Cancelling that divergence is distinct from removing the stress tensor itself: boundary tractions and thermal compatibility still matter.
For spatially uniform heating with the entire boundary fixed, is the unique equilibrium displacement in a stable elastic solid, and
The stress is compressive hydrostatic stress for a temperature rise. The fixed boundary supplies the tractions that prevent thermal expansion. If varies spatially and no compensating body force is imposed, fixing the boundary alone does not generally force the interior displacement to vanish: one must solve the displayed forced Navier-Cauchy equation with on the boundary, then recover the stress. The simple uniform hydrostatic expression should not be asserted for arbitrary temperature fields. This is uniform thermal stress in a fully constrained solid.
The in-plane equilibrium equations are and . On a simply connected patch, each divergence-free row has a streamfunction: write , , . Symmetry gives , so another potential exists with , . Hence
If two such Airy stress functions give the same stress, their difference has zero Hessian and is therefore an arbitrary affine function on a connected domain. This is the full nonuniqueness for a fixed stress. The existence argument is local, or global on a simply connected domain; domains that are multiply connected regions require the associated force and moment period conditions for a single-valued global potential. Equilibrium alone should not silently erase that topological qualification.
For plane strain put . The constitutive equation gives . Consequently
The displacement Saint-Venant compatibility equations then becomes
For stable elastic moduli the coefficient is nonzero, so . If is bounded and smooth and on its boundary, integrating twice by parts gives . Thus is harmonic with zero boundary value and by uniqueness of the Dirichlet problem. The normal-derivative condition is what removes the extra fourth-order boundary terms.
For the pressurized annulus, substituting the radial constitutive equations into equilibrium gives , so . The stresses are
Using gauge stresses relative to ambient, the boundaries are , . Therefore
and
The maximum occurs at the bore. Once the chosen yield criterion is reached, Hooke's law cannot describe the total strain alone: write total strain as elastic plus plastic strain and supplement the elastic stress law with a yield condition, a plastic flow rule and any required work hardening law. A plastic region starts near the bore and must be matched to the remaining elastic region. The exact conversion between a principal-stress difference and the quoted yield stress depends on whether the material criterion is Tresca or von Mises. This is the elastic stress concentration in a pressurized thick cylinder.

Pinned article: Introduction to the OurBigBook Project

Welcome to the OurBigBook Project! Our goal is to create the perfect publishing platform for STEM subjects, and get university-level students to write the best free STEM tutorials ever.
Everyone is welcome to create an account and play with the site: ourbigbook.com/go/register. We belive that students themselves can write amazing tutorials, but teachers are welcome too. You can write about anything you want, it doesn't have to be STEM or even educational. Silly test content is very welcome and you won't be penalized in any way. Just keep it legal!
We have two killer features:
  1. topics: topics group articles by different users with the same title, e.g. here is the topic for the "Fundamental Theorem of Calculus" ourbigbook.com/go/topic/fundamental-theorem-of-calculus
    Articles of different users are sorted by upvote within each article page. This feature is a bit like:
    • a Wikipedia where each user can have their own version of each article
    • a Q&A website like Stack Overflow, where multiple people can give their views on a given topic, and the best ones are sorted by upvote. Except you don't need to wait for someone to ask first, and any topic goes, no matter how narrow or broad
    This feature makes it possible for readers to find better explanations of any topic created by other writers. And it allows writers to create an explanation in a place that readers might actually find it.
    Figure 1.
    Screenshot of the "Derivative" topic page
    . View it live at: ourbigbook.com/go/topic/derivative
  2. local editing: you can store all your personal knowledge base content locally in a plaintext markup format that can be edited locally and published either:
    This way you can be sure that even if OurBigBook.com were to go down one day (which we have no plans to do as it is quite cheap to host!), your content will still be perfectly readable as a static site.
    Figure 5. . You can also edit articles on the Web editor without installing anything locally.
    Video 3.
    Edit locally and publish demo
    . Source. This shows editing OurBigBook Markup and publishing it using the Visual Studio Code extension.
  3. https://raw.githubusercontent.com/ourbigbook/ourbigbook-media/master/feature/x/hilbert-space-arrow.png
  4. Infinitely deep tables of contents:
    Figure 6.
    Dynamic article tree with infinitely deep table of contents
    .
    Descendant pages can also show up as toplevel e.g.: ourbigbook.com/cirosantilli/chordate-subclade
All our software is open source and hosted at: github.com/ourbigbook/ourbigbook
Further documentation can be found at: docs.ourbigbook.com
Feel free to reach our to us for any help or suggestions: docs.ourbigbook.com/#contact