In hyperuniform active fluids, nucleation is governed by a nonequilibrium quasi-potential with nucleation probability not separating into surface and volume terms, while capillary waves exhibit breakdown of detailed balance from nonreciprocal dynamics.
We recall that: ζ(r, t)ζ(r ′, t′) =δ(t−t ′)δ(r−r ′).(A16) Symbolic manipulations lead to: ⟨ψα, ζ⟩(t)⟨ψβ, ζ⟩(t′) =⟨ψ α, ψβ⟩δ(t−t ′).(A17) Using the mean field surface tension Eq
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Hyperuniformity in active fluids reshapes nucleation and capillary-wave dynamics
In hyperuniform active fluids, nucleation is governed by a nonequilibrium quasi-potential with nucleation probability not separating into surface and volume terms, while capillary waves exhibit breakdown of detailed balance from nonreciprocal dynamics.