Matthews (1992) has proposed that HCN ''polymer'' is ubiquitous in the
solar system. We apply vacuum deposition and spectroscopic techniques
previously used on synthetic organic heteropolymers (tholins), keroge
ns, and meteoritic organic residues to the measurement of the optical
constants of poly-HCN in the wavelength range 0.05-40 mu m. These meas
urements allow quantitative comparison with spectrophotometry of organ
ic-rich bodies in the outer solar system. In a specific test of Matthe
ws' hypothesis, poly-HCN fails to match the optical constants of the h
aze of the Saturnian moon, Titan, in the visible and near-infrared, de
rived from astronomical observations and standard models of the Titan
atmosphere. In contrast, a tholin produced from a simulated Titan atmo
sphere matches within the probable errors. Poly-HCN is much more N-ric
h than Titan tholin.