The Movement of Small Particulate Matter in the Early Solar System and the Formation of Satellites

1974 ◽  
pp. 483-485
Author(s):  
T. Gold
1974 ◽  
Vol 3 ◽  
pp. 483-485
Author(s):  
T. Gold

Satellites are a common feature in the solar system, and all planets on which satellite orbits would be stable possess them. (For Mercury the solar perturbation is too large, and the retrograde spin of Venus would cause satellites to spiral in to the planet through tidal friction.) An explanation of the formation of satellites must hence be one which makes the phenomenon exceedingly probable at some stage in the solar system formation processes, and very improbable processes like a capture cannot be the answer in most cases.Small particulate matter must have been very abundant in the early solar nebula. Such particulate matter must have existed both from the first condensation of the low vapor pressure components of the gas in the first round, and it must also have been composed of material scattered from impacts after some major bodies had begun to form, frequently finding themselves no doubt on collision orbits.


Author(s):  
D.E. Brownlee ◽  
A.L. Albee

Comets are primitive, kilometer-sized bodies that formed in the outer regions of the solar system. Composed of ice and dust, comets are generally believed to be relic building blocks of the outer solar system that have been preserved at cryogenic temperatures since the formation of the Sun and planets. The analysis of cometary material is particularly important because the properties of cometary material provide direct information on the processes and environments that formed and influenced solid matter both in the early solar system and in the interstellar environments that preceded it.The first direct analyses of proven comet dust were made during the Soviet and European spacecraft encounters with Comet Halley in 1986. These missions carried time-of-flight mass spectrometers that measured mass spectra of individual micron and smaller particles. The Halley measurements were semi-quantitative but they showed that comet dust is a complex fine-grained mixture of silicates and organic material. A full understanding of comet dust will require detailed morphological, mineralogical, elemental and isotopic analysis at the finest possible scale. Electron microscopy and related microbeam techniques will play key roles in the analysis. The present and future of electron microscopy of comet samples involves laboratory study of micrometeorites collected in the stratosphere, in-situ SEM analysis of particles collected at a comet and laboratory study of samples collected from a comet and returned to the Earth for detailed study.


2016 ◽  
Vol 50 (1) ◽  
pp. 1-2 ◽  
Author(s):  
Tomohiro Usui ◽  
Audrey Bouvier ◽  
Justin I. Simon ◽  
Noriko Kita

Nature ◽  
2019 ◽  
Vol 569 (7754) ◽  
pp. 85-88 ◽  
Author(s):  
Imre Bartos ◽  
Szabolcs Marka

2021 ◽  
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Author(s):  
Dante S. Lauretta ◽  
Heather L. Enos ◽  
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Heather L. Roper ◽  
Catherine W.V. Wolner

2008 ◽  
Author(s):  
S. Itoh ◽  
H. Yurimoto ◽  
Takuma Suda ◽  
Takaya Nozawa ◽  
Akira Ohnishi ◽  
...  

2014 ◽  
Vol 127 ◽  
pp. 57-66 ◽  
Author(s):  
Thomas Mueller ◽  
E. Bruce Watson ◽  
Dustin Trail ◽  
Michael Wiedenbeck ◽  
James Van Orman ◽  
...  

2006 ◽  
Vol 70 (18) ◽  
pp. A29
Author(s):  
J.A. Baker ◽  
M. Bizzarro

2006 ◽  
Vol 777 ◽  
pp. 5-69 ◽  
Author(s):  
G.J. Wasserburg ◽  
M. Busso ◽  
R. Gallino ◽  
K.M. Nollett

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