LocalizedSplitMass #
Ported from scottnarmstrong/Superdiffusion at 7f20476385d4af418f110303085ad0740c9eba46. Module imports, support namespace and local option directives adapted for Lean Pool.
The Agmon mass estimate with a split antisymmetric part #
The drift term produced by the smooth antisymmetric part carries the divergence of that part and the gradient of the exponential weight. Both contributions are paid for here: the part carried by the gradient of the localization is absorbed by half of the mass, and the part carried by the gradient of the phase is proportional to the rate, so it is absorbed by the same budget that fixes the rate.
Main results #
The drift term #
The coordinate gradient of a squared weight.
The drift term of the smooth antisymmetric part. The drift produced by integrating the smooth part by parts carries no gradient of the solution: it is split between a part absorbed by an eighth of the mass and a layer part proportional to the squared divergence bound and to the squared gradient of the weight. The size of the divergence is needed only on the layer that carries the weight.
The split-skew mass argument after admissibility, energy and drift witnesses are supplied. The logarithmic weight is arbitrary, and no trace or domain regularity is required here.
The Agmon mass estimate with a split antisymmetric part #
The Agmon weighted mass estimate with a split antisymmetric part. The
rough part contributes its size on the layer and the smooth part its
divergence on the layer; the admissibility of the rate is the single budget
inequality hadmiss.
The effective upper constant #
The effective upper ellipticity constant of the localized estimate: the size of the rough part on the layer, together with the divergence of the smooth part measured against the mass.
Equations
Instances For
Normalize an Agmon mass estimate at the effective constant and its rate budget.
The uniformly elliptic shape at the effective constant #
The localized Agmon mass estimate at the effective constant. With the
effective upper constant the estimate takes exactly the form of the uniformly
elliptic one, at lower constant nu, and so does its admissibility
hypothesis.
The Caccioppoli gradient bound with a split antisymmetric part #
The Caccioppoli gradient bound with a split antisymmetric part. The mass term is retained and absorbs the part of the drift carried by the gradient of the localization, so the constant depends only on the size of the rough part and the divergence of the smooth part on the layer.
The Caccioppoli gradient bound at the effective constant. With the
effective upper constant the bound takes exactly the form of the uniformly
elliptic one, at lower constant nu.