The mean inverse with the source's actual nonlocal boundary operator. The boundary lower bound is proved from the spatial hypotheses (5), not an input.
The concrete boundary lower bound used in the mean time-variational solve.
The source localization estimate for the constructed nonlocal boundary operator.
Boundary localization C1, given by 36 * (2 + 4 * weakHarmonicSmallBallConstant).
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Boundary localization C2, given by 4 * weakHarmonicSmallBallConstant.
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The literal local mass estimate (8), with fixed dimensional constants.
The same estimate directly in terms of the actual boundary quadratic form.
Integrating the source's different lower bounds inside and outside the core.
The actual localized boundary operator compensates for the core's negative gradient.
The exact cutoff and physical-label core from source (7)–(8).
Effective negative bound, given by Be + boundaryLocalizationC2 * Bc * r^3.
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- EulerMeanSourceInverse.effectiveNegativeBound Be Bc r = Be + EulerMeanHarmonic.boundaryLocalizationC2 * Bc * r ^ 3
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This is the actual Lax–Milgram mean inverse, with spatial coercivity discharged.
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- One or more equations did not get rendered due to their size.
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The literal mean weak equation, retaining both original initial boundary terms.
Existence and uniqueness from the actual source spatial and time assumptions.