Deep impact:: Working properties for the target nucleus -: Comet 9P/Tempel 1

被引:34
作者
Belton, MJ [1 ]
Meech, KJ
A'Hearn, MF
Groussin, O
Mcfadden, L
Lisse, C
Fernández, YR
Pittichová, J
Hsieh, H
Kissel, J
Klaasen, K
Lamy, P
Prialnik, D
Sunshine, J
Thomas, P
Toth, I
机构
[1] Belton Space Explorat Initiat LLC, Tucson, AZ USA
[2] Univ Hawaii, Inst Astron, Honolulu, HI 96822 USA
[3] Univ Maryland, College Pk, MD 20742 USA
[4] Max Planck Inst Sonnensystemforsch, Katlenburg Lindau, Germany
[5] Jet Prop Lab, Pasadena, CA USA
[6] CNRS, Astron Spatiale Lab, F-13012 Marseille, France
[7] Tel Aviv Univ, Dept Geophys & Planetary Sci, IL-69978 Tel Aviv, Israel
[8] Sci Applicat Int Corp, Chantilly, VA USA
[9] Cornell Univ, Ctr Radiophys & Space Res, Ithaca, NY 14853 USA
[10] Konkoly Observ Budapest, Budapest, Hungary
关键词
comets; space missions; nucleus; 9P/Tempel; 1;
D O I
10.1007/s11214-005-3389-1
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In 1998, Comet 9P/Tempel 1was chosen as the target of the Deep Impact mission ( A'Hearn, M. F., Belton, M. J. S., and Delamere, A., Space Sci. Rev., 2005) even though very little was known about its physical properties. Efforts were immediately begun to improve this situation by the Deep Impact Science Team leading to the founding of a worldwide observing campaign (Meech et al., Space Sci. Rev., 2005a). This campaign has already produced a great deal of information on the global properties of the comet's nucleus ( summarized in Table I) that is vital to the planning and the assessment of the chances of success at the impact and encounter. Since the mission was begun the successful encounters of the Deep Space 1 spacecraft at Comet 19P/Borrelly and the Stardust spacecraft at Comet 81P/Wild 2 have occurred yielding new information on the state of the nuclei of these two comets. This information, together with earlier results on the nucleus of comet 1P/Halley from the European Space Agency's Giotto, the Soviet Vega mission, and various ground-based observational and theoretical studies, is used as a basis for conjectures on the morphological, geological, mechanical, and compositional properties of the surface and subsurface that Deep Impact may find at 9P/Tempel 1. We adopt the following working values ( circa December 2004) for the nucleus parameters of prime importance to Deep Impact as follows: mean effective radius = 3.25 +/- 0.2 km, shape - irregular triaxial ellipsoid with a/b = 3.2 +/- 0.4 and overall dimensions of similar to 14.4 x 4.4 x 4.4 km, principal axis rotation with period = 41.85 +/- 0.1 hr, pole directions ( RA, Dec, J2000) = 46 +/- 10, 73 +/- 10 deg ( Pole 1) or 287 +/- 14, 16.5 +/- 10 deg ( Pole 2) ( the two poles are photometrically, but not geometrically, equivalent), Kron-Cousins (V-R) color = 0.56 +/- 0.02, V- band geometric albedo = 0.04 +/- 0.01, R-band geometric albedo = 0.05 +/- 0.01, R-band H( 1, 1, 0) = 14.441 +/- 0.067, and mass similar to 7 x 10(13) kg assuming a bulk density of 500 kg m(-3). As these are working values, i.e., based on preliminary analyses, it is expected that adjustments to their values may be made before encounter as improved estimates become available through further analysis of the large database being made available by the Deep Impact observing campaign. Given the parameters listed above the impact will occur in an environment where the local gravity is estimated at 0.027-0.04 cm s(-2) and the escape velocity between 1.4 and 2ms(-1). For both of the rotation poles found here, the Deep Impact spacecraft on approach to encounter will find the rotation axis close to the plane of the sky ( aspect angles 82.2 and 69.7 deg. for pole 1 and 2, respectively). However, until the rotation period estimate is substantially improved, it will remain uncertain whether the impactor will collide with the broadside or the ends of the nucleus.
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页码:137 / 160
页数:24
相关论文
共 64 条
[51]   IS THE NUCLEUS OF COMET HALLEY A LOW-DENSITY BODY [J].
SAGDEEV, RZ ;
ELYASBERG, PE ;
MOROZ, VI .
NATURE, 1988, 331 (6153) :240-242
[52]   LONG-TERM EVOLUTION OF ROTATIONAL STATES AND NONGRAVITATIONAL EFFECTS FOR HALLEY-LIKE COMETARY NUCLEI [J].
SAMARASINHA, NH ;
BELTON, MJS .
ICARUS, 1995, 116 (02) :340-358
[53]   Modeling the nucleus and jets of comet 81 P/Wild 2 based on the Stardust encounter data [J].
Sekanina, Z ;
Brownlee, DE ;
Economou, TE ;
Tuzzolino, AJ ;
Green, SF .
SCIENCE, 2004, 304 (5678) :1769-1774
[54]   Gas flow and dust acceleration in a cometary Knudsen layer [J].
Skorov, YV ;
Rickman, H .
PLANETARY AND SPACE SCIENCE, 1999, 47 (8-9) :935-949
[55]   PROPERTIES OF MANTLES ON COMETARY NUCLEI [J].
SMOLUCHOWSKI, R .
ASTRONOMICAL JOURNAL, 1989, 97 (01) :241-245
[56]   Short-wavelength infrared (1.3-2.6 μm) observations of the nucleus of Comet 19P/Borrelly [J].
Soderblom, LA ;
Britt, DT ;
Brown, RH ;
Buratti, BJ ;
Kirk, RL ;
Owen, TC ;
Yelle, RV .
ICARUS, 2004, 167 (01) :100-112
[57]   Imaging Borrelly [J].
Soderblom, LA ;
Boice, DC ;
Britt, DT ;
Brown, RH ;
Buratti, BJ ;
Kirk, RL ;
Lee, M ;
Nelson, RM ;
Oberst, J ;
Sandel, BR ;
Stern, SA ;
Thomas, N ;
Yelle, RV .
ICARUS, 2004, 167 (01) :4-15
[58]  
STRAZZULA G, 1991, COMETS POST HALLEY E
[59]  
SUNSHINE J, 2005, SPACE SCI REV
[60]  
TOTH I, 2001, ASTEROIDS 2001 PIAZZ, P313