  Viscous vortex layers subject to a more general uniform strain are
considered. They include Townsend's steady solution for plane strain
(corresponding to a parameter $a = 1$) in which all the strain in the plane of
the layer goes toward vorticity stretching, as well as Migdal's recent steady
asymmetric solution for axisymmetric strain ($a = 1/2$) in which half of the
strain goes into vorticity stretching. In addition to considering asymmetric,
symmetric and antisymmetric steady solutions $\forall a \ge 0$, it is shown
that for $a < 1$, i.e., anything less than the Townsend case, the vorticity
inherently decays in time: only boundary conditions that maintain a supply of
vorticity at one or both ends lead to a non-zero steady state. For the
super-Townsend case $a > 1$, steady states have a sheath of opposite sign
vorticity. Comparison is made with homogeneous-isotropic turbulence in which
case the average vorticity in the strain eigenframe is layer-like, has wings of
opposite vorticity, and the strain configuration is found to be super-Townsend.
Only zero-integral perturbations of the $a > 1$ steady solutions are stable;
otherwise, the solution grows. Finally, the appendix shows that the average
flow in the strain eigenframe is (apart from an extra term) the
Reynolds-averaged Navier-Stokes equation.
