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A periodic Q1/Q1 checkerboard pressure mode is invisible to divergence
Example
Take the periodic square with a unit-square Q1 mesh. At the grid node , for , set and identify opposite boundaries periodically. Assume on every cell. These nodal values define a nonzero mean-zero Q1 pressure. It is invisible to the ordinary velocity-divergence coupling, although its PSPG pressure-gradient term is strictly positive.
Facts & Assumptions
Given: The periodic Q1 mesh, equal-order Q1 velocity and pressure, strictly positive cell parameters , and the PSPG residual term from Residual PSPG and grad-div terms for equal-order flow spaces.
Residual PSPG and grad-div terms for equal-order flow spaces: PSPG adds ; for the Stokes specialization and , , , the residual is .
Verification
On a cell with local coordinates , the corner values are with . Q1 interpolation therefore gives . Its integral on every cell is zero, so its global mean is zero, and it is nonzero at every mesh node.
For any Q1 velocity component , on a cell is affine in and independent of . Since , . Similarly, is independent of and , so . Summing cells gives for every Q1 velocity.
On each unit cell, . Thus by the strict positivity in Given. By [F1], the PSPG term detects this mode, while the unstabilized divergence equation does not. This finite mode check proves neither a mesh-uniform inf-sup bound nor general PSPG accuracy.
Depends on
Used by
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Sources
- Felipe Galarce and Douglas R. Q. Pacheco, Fully consistent lowest-order finite element methods for generalised Stokes flows with variable viscosity, arXiv:2411.02100v1 (standard reference, not scraped)
- Thomas J. R. Hughes, Multiscale and Stabilized Methods (standard reference, not scraped)