Engineering Papers⌕ Search

Engineering topics

Knacke, R. F.

Publications and source records attributed to Knacke, R. F..

47 records · Page 3

Infrared spectra of carbonaceous chondrites and the composition of interstellar grains

Infrared spectra (7 to 40 microns) of the Cold Bokkeveld, Murray, and Orgueil carbonaceous chondrites are compared with phyllosilicate-mineral and interstellar-grain spectra. Similarities in the position and shape of the silicate feature near 9.8 microns suggest that similar silicate minerals are present in primitive meteorites and the interstellar dust.

Zaikowski, A.↗

On the presence of phyllosilicate minerals in the interstellar grains

The composition of the interstellar silicate dust is investigated. Condensation or alteration of silicate grains at temperatures of a few hundred degrees, in the presence of H2O, would result in hydrous or phyllosilicates, the silicate type most abundant in the type I carbonaceous chondrites. Infrared spectra of small particles (about 0.1 microns) of the high temperature condensates, olivine and pyroxene, at 300 K and 4 K do not give a good match to the interstellar absorption band near 9.8 microns. Laboratory spectra of several phyllosilicates give better agreement as does the spectrum of a carbonaceous chondrite. We propose that the silicates in the interstellar grains are predominantly phyllosilicates and suggest additional spectral tests for this hypothesis.

Zaikowski, A.↗

Infrared observations of the surface and atmosphere of Titan

Infrared photometry of Titan, Saturn, and Saturn's Rings at 3.5, 4.9, 17.8, and 18.4 microns is reported. Comparison of the albedo of Titan in the 4.9 micron 'window' with the albedo of the rings and with laboratory spectra suggests that frost, possibly water ice, could be a major constituent. If thick clouds are present they must be very dark at 4.9 microns. The 17.8 and 18.4 micron data are not consistent with a clear, dense molecular hydrogen atmosphere.

Knacke, R. F.↗

An upper limit on the 4.9-micron flux from Titan.

Discussion of the limits on surface temperature (under 190 K) and reflectivity (under 0.5) corresponding to an upper limit set on the 4.9-micron flux from Titan. Special attention is given to the possibility of the presence of an opaque cloud layer or some gaseous absorber on Titan and to the subsequent implications.

Joyce, R. R.↗