Hydrogen sulfide clathrate hydrate FTIR spectroscopy: A help gas for clathrate formation in the Solar System?

Icarus ◽  
2012 ◽  
Vol 220 (2) ◽  
pp. 427-434 ◽  
Author(s):  
E. Dartois ◽  
Ph. Duret ◽  
U. Marboeuf ◽  
B. Schmitt
Keyword(s):  
Hydrogen Sulfide ◽  
Solar System ◽  
Ftir Spectroscopy ◽  
Clathrate Hydrate ◽  
Clathrate Formation

scholarly journals Clathrate hydrate FTIR spectroscopy - infrared signatures, astrophysical significance

2014 ◽  
Vol 2 ◽  
pp. 03005 ◽  
Author(s):  
E. Dartois ◽  
M. Bouzit ◽  
Ph. Duret ◽  
B. Schmitt
Keyword(s):  
Ftir Spectroscopy ◽  
Clathrate Hydrate ◽  
Astrophysical Significance

Clathrate Formation in the Water–Tetraisoamylammonium Propionate System: X-ray Structural Analysis of the Clathrate Hydrate (i-C5H11)4NC2H5CO2·36H2O

2006 ◽  
Vol 56 (3-4) ◽  
pp. 331-335 ◽  
Author(s):  
Kinga Suwinska ◽  
Janusz S. Lipkowski ◽  
Yuri A. Dyadin ◽  
V.Yu. Komarov ◽  
Irina S. Terekhova ◽  
...  
Keyword(s):  
Structural Analysis ◽  
Clathrate Hydrate ◽  
Clathrate Formation ◽  
X Ray

Uranus after Voyager 2 and the Origin of the Solar System

1986 ◽  
Vol 6 (4) ◽  
pp. 394-402 ◽  
Author(s):  
A. J. R. Prentice
Keyword(s):  
Solar System ◽  
Clathrate Hydrate ◽  
Turbulence Parameter ◽  
Convective Turbulence ◽  
Satellite Systems ◽  
Equatorial Radius ◽  
Voyager 2 ◽  
Uranian Satellites

AbstractThe discoveries made by the Voyager 2 spacecraft at Uranus in January 1986 are discussed in the light of the modern Laplacian theory for the formation of the solar system. Various accounts of this theory, which has as its basis the concept of supersonic convective turbulence, have been presented at previous meetings of the ASA (Prentice 1977, 1979, 1981a). The most important confirmation by Voyager was the discovery of 2 new satellite groups near orbital radii 2½ RUand 3½ RU(RU= Uranus’ equatorial radius = 26, 200 km), as first predicted in 1977. The discovery that the densities of the Uranian satellites are consistent with these bodies having condensed in a single compositional class, consisting of anhydrous rock, NH3ice and CH4.6H2O clathrate hydrate in normal solar proportions, confirms the hypothesis that the chemistry of all planetary/regular satellite systems are accounted for by a single choice of the turbulence parameter, namely β = 0.107 ±0.001. The implication of the Voyager data for the origin of comets is also discussed.

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