On dielectric models of interstellar grains
Dielectric models of interstellar grains from calculations for smooth particles of homogeneous materials
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Dielectric models of interstellar grains from calculations for smooth particles of homogeneous materials
Compositional zoning in pyroxenes from grained Apollo 11 microgabbros, implying supercooled magma origin
Metallic fe grains in Apollo 12 igneous rocks, discussing Ni and Co abundances
H II region dust grains thermal emission, examining effect on diffuse nebulae
Electron microprobe analysis of fine-grained igneous rocks from lunar sample 10022 from Sea of Tranquillity
Nondestructive test technique developed for large solid propellant grains
Satellite stability and interstellar dust grain studies
Interstellar molecular hydrogen formation by physical adsorption on grains, determining H atoms adsorptive potentials on silicates, graphite, solid hydrogen and ice
Interstellar grain formation relation with stellar evolution in terms of density wave theory of spiral structure origin
Soft galactic X rays role in interstellar grains alignment
Meteoritic graphite, silicon carbide and silicates to explain observed interstellar grains properties
Hydrogen recombination and molecule formation by nonactivated chemisorption on iron grains surfaces
Interstellar grain temperatures, determining shape effects on emissivities
Galactic nucleus thermal emission due to dirty ice or silicate grains, explaining far IR radiation power output and spectral dependence
Methane, ammonia and silicate effects on 3.07 micron ice absorption in interstellar grains, using cesium iodide window deposited sample measurements
Elastic seismic waves attenuation in polycrystalline ceramics and rocks by grain boundary relaxation, noting strong frequency dependence of earth mantle internal friction
Petrography, mineral composition and grain size distribution of Apollo 12 lunar fines
Radiation at IR wavelengths from circumstellar grains surrounding R CrB has been observed for approximately three years. Variations of flux with time have been larger at a wavelength of 3.5 microns than at 11 microns. Observations at IR and visual wavelengths of R CrB are presented in a graph. Another graph shows the change in the shape of the excess radiaton between two observations spaced by a period of about one year.