Spectral studies of asteroids 21 lutetia and 4 vesta as objects of space missions

被引:8
作者
Busarev, V. V. [1 ]
机构
[1] Moscow MV Lomonosov State Univ, Sternberg Astron Inst, Moscow 119992, Russia
基金
俄罗斯基础研究基金会;
关键词
ROTATIONALLY-RESOLVED SPECTROSCOPY; REFLECTANCE SPECTRA; PHASE-II; S-TYPE; SURFACE; METEORITE; BODIES; BELT; EXCITATION; 21-LUTETIA;
D O I
10.1134/S0038094610060043
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Asteroid 21 Lutetia is one of the objects of the Rosetta mission carried out by the European Space Agency (ESA). The Rosetta spacecraft launched in 2004 is to approach Lutetia in July 2010, and then it will be directed to the comet Churyumov-Gerasimenko. Asteroid 4 Vesta is planned to be investigated in 2011 from the Dawn spacecraft launched by the National Aeronautics and Space Administration (NASA) in 2007 (its second object is the largest asteroid, 1 Ceres). The observed characteristics of Lutetia and Vesta are different and even contradictory. In spite of the intense and versatile ground-based studies, the origin and evolution of these minor planets remain obscure or not completely clear. The types of Lutetia and Vesta (M and V, respectively) determined from their spectra correspond to the high-temperature mineralogy, which agrees with their albedo estimated from the Infrared Astronomical Satellite (IRAS) observations. However, according to the opinion of some researchers, Lutetia is of the C type, and, therefore, its mineralogy is of the lowtemperature type. In turn, hydrosilicate formations have been found in some places on the surface of Vesta. Our observations also testify that at some relative phases of rotation (RP), the reflectance spectra of Lutetia and Vesta demonstrate features confirming the presence of hydrosilicates in the surface material. However, this fact can be reconciled with the magmatic nature of Lutetia and Vesta if the hydrated material was delivered to their surfaces by falling primitive bodies. Such small bodies are probably present everywhere in the main asteroid belt and can be the relicts of silicate-icy planetesimals from Jupiter's formation zone or the fragments of primitive-type asteroids. When interpreting the reflectance spectra of Lutetia and Vesta, we discuss the spectral classification by Tholen (1984) from the standpoint of its general importance for the estimation of the mineralogical type of the asteroids and the study of their origin and evolution.
引用
收藏
页码:507 / 519
页数:13
相关论文
共 87 条
  • [1] Adams J.B., 1975, INFRARED RAMAN SPECT, P91
  • [2] VISIBLE AND NEAR-INFRARED DIFFUSE REFLECTANCE SPECTRA OF PYROXENES AS APPLIED TO REMOTE-SENSING OF SOLID OBJECTS IN SOLAR-SYSTEM
    ADAMS, JB
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1974, 79 (32): : 4829 - 4836
  • [3] ADAMS JB, 1970, P APOLLO 11 LUNAR SC, V3, P1937
  • [4] [Anonymous], 1993, Mineralogical Applications of Crystal Field Theory
  • [5] Asphaug E, 1997, METEORIT PLANET SCI, V32, pA9
  • [6] Bakhtin A.I., 1985, Rock-Forming Silicates: Optical Spectra, Crystal Chemistry, Color Patterns, Typomorphism
  • [7] Asteroids 2867 Steins and 21 Lutetia: surface composition from far infrared observations with the Spitzer space telescope
    Barucci, M. A.
    Fornasier, S.
    Dotto, E.
    Lamy, P. L.
    Jorda, L.
    Groussin, O.
    Brucato, J. R.
    Carvano, J.
    Alvarez-Candal, A.
    Cruikshank, D.
    Fulchignoni, A.
    [J]. ASTRONOMY & ASTROPHYSICS, 2008, 477 (02) : 665 - 670
  • [8] BATRAKOV YV, 2000, EFEMERIDY MALYKH PLA, P244
  • [9] Bell J.F., 1989, ASTEROIDS, P921
  • [10] CHIPS OFF OF ASTEROID-4 VESTA - EVIDENCE FOR THE PARENT BODY OF BASALTIC ACHONDRITE METEORITES
    BINZEL, RP
    XU, S
    [J]. SCIENCE, 1993, 260 (5105) : 186 - 191