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Okay, this seems to be a valid point. You do hear people describe a
slow leak as a quasi-static process.
On the other hand, you also
hear people offer the opinion that, in a quasi-static process, "the
system" remains at or near thermodynamic equilibrium.
Clearly, if
"the system" consists of all gas on either side of the porous plug,
then "the system" is nowhere near thermodynamic equilibrium. Maybe
we need to alter the definition to allow systems that are in
piecewise thermodynamic equilibrium? Not completely sure how you'd
do that.
So I wonder if anything important would be lost if we refined these
ideas to say that the gases on either side of the porous plug undergo
quasi-static processes, but that the gas as a whole doesn't.
I do recognize that this raises an important question about "where"
the dissipation is taking place and I'm not particularly comfortable
saying that it happens in or "near" the porous plug.