The actual forcing in the ordered flux calculus.
theorem
AVenhance.Infra.Section4.amnr_temperatureFlux_contDiffOn
{β : ℝ}
(I : Ingredients β)
{Φ : ℕ → ℝ → Homogenization.Vec 2 → ℝ}
(hΦ : IsStreamSeq I Φ)
{m : ℕ}
(hm : 1 ≤ m)
{κm κprev : ℝ}
(hκm : 0 < κm)
{b : ℝ → Homogenization.Vec 2 → Homogenization.Vec 2}
{F u : ℝ → Homogenization.Vec 2 → ℝ}
{u₀ : Homogenization.Vec 2 → ℝ}
(hu : IsClassicalSol b κprev F u₀ u)
(j : Fin 2)
:
ContDiffOn ℝ (↑(Nstar β)) (amnrTemperatureFlux I hΦ m κm κprev u j) (Set.Ioi 0 ×ˢ Set.univ)
Flux regularity uses only the proved finite Kmat order and actual classical temperature regularity on the positive-time domain.
theorem
AVenhance.Infra.Section4.amnr_temperatureForcing_eq_flux_divergence
{β : ℝ}
(I : Ingredients β)
{Φ : ℕ → ℝ → Homogenization.Vec 2 → ℝ}
(hΦ : IsStreamSeq I Φ)
{m : ℕ}
(hm : 1 ≤ m)
{κm κprev : ℝ}
(hκm : 0 < κm)
{b : ℝ → Homogenization.Vec 2 → Homogenization.Vec 2}
{F u : ℝ → Homogenization.Vec 2 → ℝ}
{u₀ : Homogenization.Vec 2 → ℝ}
(hu : IsClassicalSol b κprev F u₀ u)
(B : AmnrSpace → Homogenization.Vec 2)
:
The matrix divergence equals the ordered coordinate divergence of its actual flux, with no forcing estimate or evolution equation assumed.