Collisions, cosmic radiation and the colors of the Trojan asteroids
The Trojan asteroids orbit about the Lagrangian points of Jupiter and the residence times about their present location are very long for most of them. If these bodies originated in the outer Solar System, they should be mainly composed of water ice, but, in contrast with comets, all the volatiles cl...
Guardado en:
Publicado: |
2009
|
---|---|
Materias: | |
Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v203_n1_p134_Melita http://hdl.handle.net/20.500.12110/paper_00191035_v203_n1_p134_Melita |
Aporte de: |
id |
paper:paper_00191035_v203_n1_p134_Melita |
---|---|
record_format |
dspace |
spelling |
paper:paper_00191035_v203_n1_p134_Melita2023-06-08T14:40:15Z Collisions, cosmic radiation and the colors of the Trojan asteroids Asteroids Comets Origin Solar System Surfaces Trojan asteroids The Trojan asteroids orbit about the Lagrangian points of Jupiter and the residence times about their present location are very long for most of them. If these bodies originated in the outer Solar System, they should be mainly composed of water ice, but, in contrast with comets, all the volatiles close to the surface would have been lost long ago. Irrespective of the rotation period, and hence the surface temperature and ice sublimation rate, a dust layer exists always on the surface. We show that the timescale for resurfacing the entire surface of the Trojan asteroids is similar to that of the flattening of the red spectrum of the new dust by solar-proton irradiation. This, if the cut-off radius of the size distribution of the impacting objects is between 1 mm and 1 m and its slope is -3, for the entire size range. Therefore, the surfaces of most Trojan asteroids should be composed mainly of unirradiated dust. © 2009 Elsevier Inc. All rights reserved. 2009 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v203_n1_p134_Melita http://hdl.handle.net/20.500.12110/paper_00191035_v203_n1_p134_Melita |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Asteroids Comets Origin Solar System Surfaces Trojan asteroids |
spellingShingle |
Asteroids Comets Origin Solar System Surfaces Trojan asteroids Collisions, cosmic radiation and the colors of the Trojan asteroids |
topic_facet |
Asteroids Comets Origin Solar System Surfaces Trojan asteroids |
description |
The Trojan asteroids orbit about the Lagrangian points of Jupiter and the residence times about their present location are very long for most of them. If these bodies originated in the outer Solar System, they should be mainly composed of water ice, but, in contrast with comets, all the volatiles close to the surface would have been lost long ago. Irrespective of the rotation period, and hence the surface temperature and ice sublimation rate, a dust layer exists always on the surface. We show that the timescale for resurfacing the entire surface of the Trojan asteroids is similar to that of the flattening of the red spectrum of the new dust by solar-proton irradiation. This, if the cut-off radius of the size distribution of the impacting objects is between 1 mm and 1 m and its slope is -3, for the entire size range. Therefore, the surfaces of most Trojan asteroids should be composed mainly of unirradiated dust. © 2009 Elsevier Inc. All rights reserved. |
title |
Collisions, cosmic radiation and the colors of the Trojan asteroids |
title_short |
Collisions, cosmic radiation and the colors of the Trojan asteroids |
title_full |
Collisions, cosmic radiation and the colors of the Trojan asteroids |
title_fullStr |
Collisions, cosmic radiation and the colors of the Trojan asteroids |
title_full_unstemmed |
Collisions, cosmic radiation and the colors of the Trojan asteroids |
title_sort |
collisions, cosmic radiation and the colors of the trojan asteroids |
publishDate |
2009 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v203_n1_p134_Melita http://hdl.handle.net/20.500.12110/paper_00191035_v203_n1_p134_Melita |
_version_ |
1768541735738146816 |