omega_0
plain-language theorem explainer
The reference spectral peak sets the silicate baseline frequency to unity in RS-native units. Materials engineers cite it when scaling phonon resonances across phi-rungs for asteroid ore classification and hydride superconductor optimization. It enters as a direct constant assignment with no additional computation.
Claim. The reference spectral peak frequency for the silicate baseline is defined to be 1.
background
The Asteroid Ore Spectroscopy module derives mineral identification from phi-ladder phonon resonances. Each ore class receives a characteristic peak frequency scaled from the silicate baseline by successive powers of phi, with seven classes ranked by rung and a discrimination floor bounded by the module falsifier on peak ratios outside the interval [1/(2 phi), 2 phi].
proof idea
The declaration is a direct definition that assigns the value 1 to the reference frequency with no lemmas or tactics applied.
why it matters
This definition anchors the frequency scaling in AsteroidOreSpectroscopyCert, which certifies positivity, successor scaling by phi, and strict monotonicity of the rung sequence. It is imported into HydrideSCOptimizationCert to support T_c optimization over finite rung ranges. It instantiates the phi fixed point from the unified forcing chain as the scaling base for the engineering track.
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