The actual bounded solution and Volterra inverse #
The Duhamel integral is a bounded linear map in the forcing and initial data. It gives a two-sided inverse for the continuous-path Volterra operator. This unweighted inverse is used only for qualitative parameter regularity; source quantitative estimates use the original relative propagator bound directly.
The actual zero-initial-data forcing operator.
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The actual homogeneous initial-data operator.
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The bounded forcing operator is exactly the Duhamel construction.
Splitting the actual forced solution into its two bounded data maps.
The original relative propagator bound controls the actual forcing map.
The homogeneous initial-data map has the same profile and propagator constant.
The forced path satisfies the actual integral equation.
The ordinary continuous-path Volterra operator.
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Duhamel's formula gives an actual inverse on every continuous input.
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The Volterra operator followed by the constructed inverse is the identity.
The homogeneous Volterra equation has only its zero solution.
The constructed inverse is also a left inverse.
The actual two-sided Volterra equivalence.