Synthesis of the morphological description of cometary dust at comet 67P/Churyumov-Gerasimenko

被引:109
|
作者
Guettler, C. [1 ]
Mannel, T. [2 ,3 ]
Rotundi, A. [4 ,5 ]
Merouane, S. [1 ]
Fulle, M. [6 ]
Bockelee-Morvan, D. [7 ]
Lasue, J. [8 ]
Levasseur-Regourd, A. C. [9 ]
Blum, J. [10 ]
Naletto, G. [11 ,12 ,13 ]
Sierks, H. [1 ]
Hilchenbach, M. [1 ]
Tubiana, C. [1 ]
Capaccioni, F. [4 ]
Paquette, J. A. [1 ]
Flandes, A. [14 ]
Moreno, F. [15 ]
Agarwal, J. [1 ]
Bodewits, D. [20 ]
Bertini, I [16 ]
Tozzi, G. P. [17 ]
Hornung, K. [18 ]
Langevin, Y. [19 ]
Krueger, H. [1 ]
Longobardo, A. [4 ]
Della Corte, V [4 ]
Toth, I [21 ]
Filacchione, G. [4 ]
Ivanovski, S. L. [6 ]
Mottola, S. [22 ]
Rinaldi, G. [4 ]
机构
[1] Max Planck Inst Solar Syst Res, Justus von Liebig Weg 3, D-37077 Gottingen, Germany
[2] Austrian Acad Sci, Space Res Inst, Schmiedlstr 6, A-8042 Graz, Austria
[3] Karl Franzens Univ Graz, Phys Inst, Univ Pl 5, A-8010 Graz, Austria
[4] INAF, Ist Astrofis & Planetol Spaziali, Via Fosso del Cavaliere 100, I-00133 Rome, Italy
[5] Univ Napoli Parthenope, CDN IC4, Dipartimento Sci & Tecnol, I-80143 Naples, Italy
[6] INAF, Osservatorio Astron, Via Tiepolo 11, I-34143 Trieste, Italy
[7] Sorbonne Univ, Sorbonne Paris Cite, Univ Paris Diderot, LESIA,Observ Paris,Univ PSL,CNRS, 5 Pl J Janssen, F-92195 Meudon, France
[8] Univ Toulouse, UPS, CNRS, CNES,IRAP, Toulouse, France
[9] Sorbonne Univ, LATMOS, CNRS, UVSQ, Campus Pierre & Marie Curie,BC 102,4 Pl Jussieu, F-75005 Paris, France
[10] Tech Univ Carolo Wilhelmina Braunschweig, Inst Geophys & Extraterr Phys, Mendelssohnstr 3, D-38106 Braunschweig, Germany
[11] Univ Padua, Dept Phys & Astron Galileo Galilei, Via Marzolo 8, I-35131 Padua, Italy
[12] Univ Padua, Ctr Studies & Act Space CISAS G Colombo, Via Venezia 15, I-35131 Padua, Italy
[13] CNR IFN UOS Padova LUXOR, Via Trasea 7, I-35131 Padua, Italy
[14] Univ Nacl Autonoma Mexico, Inst Geofis, Ciencias Espaciales, Mexico City 04510, DF, Mexico
[15] CSIC, Inst Astrofis Andalucia, C Glorieta Astron S-N, Granada 18008, Spain
[16] Univ Padua, Dept Phys & Astron Galileo Galilei, Vicolo Osservatorio 3, I-35122 Padua, Italy
[17] INAF, Osservatorio Astrofis Arcetri, Florence, Italy
[18] Univ Bundeswehr Munchen, LRT 7, D-85577 Neubiberg, Germany
[19] Univ Paris Sud, CNRS, Inst Astrophys Spatiale, F-91405 Orsay, France
[20] Auburn Univ, Phys Dept, 206 Allison Lab, Auburn, AL 36849 USA
[21] Konkoly Observ Budapest, POB 67, H-1525 Budapest, Hungary
[22] Deutsch Zentrum Luft & Raumfahrt DLR, Inst Planetenforsch, Rutherfordstr 2, D-12489 Berlin, Germany
来源
ASTRONOMY & ASTROPHYSICS | 2019年 / 630卷
关键词
comets: general; comets: individual: 67P/Churyumov-Gerasimenko; space vehicles: instruments; COSIMA MASS-SPECTROMETER; GRAIN IMPACT ANALYZER; PHILAE LANDING SITE; LIGHT-SCATTERING; COSMIC DUST; IN-SITU; LABORATORY EXPERIMENTS; AGGREGATE COLLISIONS; PHYSICAL-PROPERTIES; STARDUST AEROGEL;
D O I
10.1051/0004-6361/201834751
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Before Rosetta, the space missions Giotto and Stardust shaped our view on cometary dust, supported by plentiful data from Earth based observations and interplanetary dust particles collected in the Earth's atmosphere. The Rosetta mission at comet 67P/Churyumov-Gerasimenko was equipped with a multitude of instruments designed to study cometary dust. While an abundant amount of data was presented in several individual papers, many focused on a dedicated measurement or topic. Different instruments, methods, and data sources provide different measurement parameters and potentially introduce different biases. This can be an advantage if the complementary aspect of such a complex data set can be exploited. However, it also poses a challenge in the comparison of results in the first place. The aim of this work therefore is to summarize dust results from Rosetta and before. We establish a simple classification as a common framework for intercomparison. This classification is based on the dust particle structure, porosity, and strength and also on its size. Depending on the instrumentation, these are not direct measurement parameters, but we chose them because they were the most reliable for deriving our model. The proposed classification has proved helpful in the Rosetta dust community, and we offer it here also for a broader context. In this manner, we hope to better identify synergies between different instruments and methods in the future.
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页数:15
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