Literature DB >> 17783829

Infrared observations of the saturnian system from voyager 1.

R Hanel, B Conrath, F M Flasar, V Kunde, W Maguire, J Pearl, J Pirraglia, R Samuelson, L Herath, M Allison, D Cruikshank, D Gautier, P Gierasch, L Horn, R Koppany, C Ponnamperuma.   

Abstract

During the passage of Voyager 1 through the Saturn system, the infrared instrument acquired spectral and radiometric data on Saturn, the rings, and Titan and other satellites. Infrared spectra of Saturn indicate the presence of H(2), CH(4), NH(3), PH(3), C(2)H(2), C(2)H(6), and possibly C(3)H(4) and C(3)H(8). A hydrogen mole fraction of 0.94 is inferred with an uncertainty of a few percent, implying a depletion of helium in the atmosphere of Saturn relative to that of Jupiter. The atmospheric thermal structure of Saturn shows hemisphere asymmetries that are consistent with a response to the seasonally varying insolation. Extensive small-scale latitudinal structure is also observed. On Titan, positive identifications of infrared spectral features are made for CH(4), C(2)H(2), C(2)H(4), C(2)H(6), and HCN; tentative identifications are made for C(3)H(4) and C(3)H(8). The infrared continuum opacity on Titan appears to be quite small between 500 and 600 cm(-1), implying that the solid surface is a major contributor to the observed emission over this spectral range; between 500 and 200 cm(-1) theopacity increases with decreasing wave number, attaining an optical thickness in excess of 2 at 200 cm(-1). Temperatures near the 1-millibar level are independent of longitude and local time but show a decrease of approximately 20 K between the equator and north pole, which suggests a seasonally dependent cyclostrophic zonal flow in the stratosphere of approximately 100 meters per second. Measurements of the C ring of Saturn yield a temperature of 85 +/- 1 K and an infrared optical depth of 0.09 +/- 0.01. Radiometer observations of sunlight transmitted through the ring system indicate an optical depth of 10(-1.3 +/-0.3) for the Cassini division. A phase integral of 1.02 +/- 0.06 is inferred for Rhea, which agrees with values for other icy bodies in the solar system. Rhea eclipse observations indicate the presence of surface materials with both high and low thermal inertias, the former most likely a blocky component and the latter a frost.

Entities:  

Year:  1981        PMID: 17783829     DOI: 10.1126/science.212.4491.192

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  17 in total

1.  Accelerated high-resolution differential ion mobility separations using hydrogen.

Authors:  Alexandre A Shvartsburg; Richard D Smith
Journal:  Anal Chem       Date:  2011-11-10       Impact factor: 6.986

2.  The cold origin of life: B. Implications based on pyrimidines and purines produced from frozen ammonium cyanide solutions.

Authors:  Shin Miyakawa; H James Cleaves; Stanley L Miller
Journal:  Orig Life Evol Biosph       Date:  2002-06       Impact factor: 1.950

3.  Organic environments on Saturn's moon, Titan: simulating chemical reactions and analyzing products by FT-ICR and ion-trap mass spectrometry.

Authors:  Arpad Somogyi; Chu-Ha Oh; Mark A Smith; Jonathan I Lunine
Journal:  J Am Soc Mass Spectrom       Date:  2005-03-29       Impact factor: 3.109

Review 4.  The search for life in the solar system.

Authors:  Donald A Gurnett
Journal:  Trans Am Clin Climatol Assoc       Date:  2009

5.  Possibility of production of amino acids by impact reaction using a light-gas gun as a simulation of asteroid impacts.

Authors:  Kazuki Okochi; Tetsu Mieno; Kazuhiko Kondo; Sunao Hasegawa; Kosuke Kurosawa
Journal:  Orig Life Evol Biosph       Date:  2015-03-22       Impact factor: 1.950

6.  Formation of amino acids and nucleotide bases in a Titan atmosphere simulation experiment.

Authors:  S M Hörst; R V Yelle; A Buch; N Carrasco; G Cernogora; O Dutuit; E Quirico; E Sciamma-O'Brien; M A Smith; A Somogyi; C Szopa; R Thissen; V Vuitton
Journal:  Astrobiology       Date:  2012-08-23       Impact factor: 4.335

7.  Heteropolypeptides on Titan?

Authors:  C N Matthews
Journal:  Orig Life       Date:  1982-09

8.  Organic syntheses from CH4-N2 atmospheres: implications for Titan.

Authors:  F Raulin; D Mourey; G Toupance
Journal:  Orig Life       Date:  1982-09

9.  The atmosphere of Titan.

Authors:  T Owen
Journal:  J Mol Evol       Date:  1982       Impact factor: 2.395

10.  Acetylene as a substrate in the development of primordial bacterial communities.

Authors:  C W Culbertson; F E Strohmaier; R S Oremland
Journal:  Orig Life Evol Biosph       Date:  1988       Impact factor: 1.950

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