The mean displacement form with its initial boundary operator #
The operator is constructed as I - J* H J + R* C R, where J is the
actual displacement primitive and R its initial trace. The boundary lower
bound is required only on the trace image, as in the source's solenoidal space.
The actual bounded operator representing kinetic, potential, and boundary terms.
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The constructed operator has exactly the intended bilinear form.
The source's two time estimates and coefficient bounds prove coercivity.
The forcing-to-derivative map constructed from the coercive mean form.
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- One or more equations did not get rendered due to their size.
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The actual weak equation follows from the constructed inverse.
Uniqueness holds in the same actual Hilbert displacement space.
The derivative bound is polynomial in the primitive norm.
Existence and uniqueness are conclusions, with no solution or inverse hypothesis.