Asteroid Science
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Deutsches Zentrum für Luft- und Raumfahrt e.V. German Aerospace Center Institut für Planetenforschung Institute of Planetary Research DEPARTMENT: “ASTEROIDS AND COMETS” IX. Annual Report 2005 Comets ASTEROIDS MODELS SPACE MISSIONS http://solarsystem.dlr.de/KK From left to right Dr. Jörg Knollenberg [email protected] Scientific staff member Dr. Gerhard Hahn [email protected] Scientific staff member Dr. Ekkehard Kührt [email protected] Section leader Prof. Uwe Motschmann [email protected] Guest scientist Laura Brumm [email protected] Secretary Detlef de Niem [email protected] Scientific staff member Dr. Carmen Tornow [email protected] Scientific staff member Michael Müller [email protected] PhD student Dr. Alan W. Harris [email protected] Deputy section leader Not appearing in the photo: Dr. Stefano Mottola [email protected] Scientific staff member Thermal-infrared image (8 – 14 μm), changed order 2 Contents 1. Introduction (EK) 2. Asteroid science 2.1 Investigations of the physical properties of asteroids with the NASA Infrared Telescope Facility (Harris, Müller) 2.2 Observations of asteroids with the Spitzer Space Telescope (Harris, Mueller) 2.3 Asteroid thermal modelling (Müller, Harris) 2.4 Photometric observations of main-belt and near-Earth asteroids (Mottola, Hahn, Harris, Müller) 2.5 Asteroid search and follow-up programmes (Hahn) 2.6 Orbital evolution studies of Saturn family comets (Hahn) 3. Comet science 3.1 Hydrodynamical influence on formation of HCN molecules in hot cores (Tornow, Kührt, Motschmann) 3.2 Modelling the solar wind interaction with weakly outgassing comets by a hybrid model (Motschmann, Kührt) 4. Impact phenomena 4.1 Meteorite ejecta range after terrestrial impacts (de Niem, Kührt, Motschmann) 4.2. Physical limits of solar collectors in deflecting Earth-threatening asteroids (Kahle, Kührt, Hahn, Knollenberg) 5. Contributions to space missions 5.1 Rosetta-Mupus (Knollenberg, Kührt, Spohn, Schrödter) 5.2 Rosetta-Rolis (S. Mottola, H. Michaelis) 5.3 DAWN (S. Mottola, R. Jaumann) 5.4 Don Quijote: Study of a hazardous asteroid mitigation pre-cursor mission (Harris) 5.5 Deep Impact measurements and simulations (Knollenberg, de Niem, Kührt) 6. Technology projects 6.1 HP3 (Knollenberg, Nadalini) 6.2 FIREWATCH (Kührt, Knollenberg, Behnke, Mertens) 7. Appendix 7.1 Scientific publications in refereed journals and books (submitted or published in 2004) 7.2 Scientific publications in other journals and proceedings (published in 2004) 7.3. Minor Planet Circulars/Electronic Circulars 7.4 Publications in the popular literature and public outreach 7.5 Observing campaigns 2004 7.6 Space mission responsibilities 7.7 Other events and activities 7.8 Funding 3 1. Introduction (E. Kührt) This report describes the work of the “Asteroids and Comets” Department of the Institute of Planetary Research of the DLR (German Aerospace Center) during the year 2005. The Department consisted of 7 scientists and 1 PhD student; two guest scientists, one from the Assam University, India, and one from the Technical University Braunschweig, worked in the Department during the year. Our scientific goal is to investigate small bodies by observing them in the visible, infrared, and other wavelength ranges, contributing to relevant space missions and modelling physical processes associated with this class of object. Other fields of interest are risk evaluation of impacts of Near Earth Objects (NEOs) on our home planet, the origin of life and the transfer of space technology to solve environmental problems on Earth. Scientific interest in the minor bodies of the Solar System stems mainly from the crucial role they appear to have played in the formation of the planets and the development of life. Asteroids and comets are thought to be remnant material from the process of formation and the initial development of planets. Due to their peculiar dynamical and physical properties, such as small size, lack of a permanent atmosphere, and relatively little thermal processing, these objects have remained largely unaltered since the time of Solar System formation. Consequently, comets and asteroids should contain a wealth of information on conditions in the protoplanetary nebula. Many scientists believe that comets and asteroids have significantly influenced the evolution of the terrestrial planets and life on Earth. In particular, scientific and public interest in near-Earth asteroids has risen in recent years. Activities in these fields are a part of our DLR-project “Comets and asteroids”. They are summarized in Sections 2, 3, and 4. Contributions to several space missions are described in Section 5. We are involved in Rosetta to comet Churyumov-Gerasimenko with 1 Principal Investigator, 1 Project Manager and 8 Coinvestgator-ships and in the Science Team of the DAWN mission to asteroids Ceres and Vesta. The progress in our technology transfer projects is discussed in Section 6. The Appendix summarises publications, project contributions, observation campaigns, public outreach activities, and our funding. 2. Asteroid Science 2.1. Investigations of the physical properties of asteroids with the NASA Infrared Telescope Facility (Harris, Müller) The NASA Infrared Telescope Facility (IRTF) is a 3-m telescope situated on Mauna Kea, Hawaii. Our project has been awarded observing time on the IRTF regularly over the past 5 years. It has recently become possible to carry out observations remotely from Berlin, which means that, without heavy travel costs, observing time can be scheduled at intervals of a few days over a total period of weeks to study the variation of infrared emission from asteroids as their observing geometry changes. The resulting data can reveal important information on the surface characteristics of asteroids, especially thermal inertia. A major focus of our work with the IRTF is near-Earth asteroids (NEAs). This year saw the publication in Icarus of our work on (1580) Betulia, in which revised values of size and albedo and a thermal inertia of 180 J m-2s-0.5 K-1 were obtained for this unusual C- type NEA. This is amongst the first determinations of thermal inertia for NEAs; it is some three times higher than the lunar value but an order of magnitude less than that expected for a bare rock surface. Our result for Betulia is consistent with recently obtained values for other NEAs discussed in Section 2.3. Our programme was awarded a total of 8 x 0.5 nights of observing time with the NASA IRTF in the 2005 observing schedule. However, the quality of thermal-infrared data, especially in the case of weak targets, is very dependent on atmospheric conditions and on several occasions in 2005 we were forced to turn to a back-up programme of observations of relatively bright main-belt M-type asteroids because of unfavourable conditions. 4 Fig. 2.1 Thermal-infrared flux measurements of the M-type asteroid (16) Psyche, Higher thermal inertia with model thermal continua for different values of thermal inertia overlaid. The flux measurements in the case of Psyche are Very low thermal inertia indicative of relatively high thermal inertia. The data set shown was taken in 2004. Similar data sets were obtained in 2005 for all the M-type asteroids mentioned in the text. One of the major current questions concerning asteroid mineralogy is the nature of M-type asteroids. Are M-type asteroids really metallic or not? We were able to obtain useful multi-filter thermal-infrared flux measurements of the main-belt M-type asteroids (16) Psyche, (21) Lutetia, (129) Antigone, (135) Hertha, (201) Penelope, (216) Kleopatra, and (785) Zwetana. Preliminary results indicate that (16) Psyche and (216) Kleopatra have relatively high values of thermal inertia. Furthermore, Psyche and Kleopatra also have very high radar albedos and therefore presumably have metallic surfaces. On the other hand, Lutetia appears to have normal values of thermal inertia and radar reflectivity. In the cases of Lutetia, Antigone, Hertha, and Penelope, for which our observations indicate normal thermal inertia, near-infrared reflectance spectroscopy provides evidence for hydrated surfaces, indicating that these objects are not metallic. To summarize: there may be a correlation between thermal inertia and radar reflectivity, which would indicate that thermal inertia is a useful indicator of metallic surfaces, and our results are consistent with recent findings that many M-type asteroids appear to be of non-metallic composition. Our study of the physical characteristics of (21) Lutetia was completed with the acceptance of the work for publication in Astronomy and Astrophysics. Our derived albedo of 0.21, typical for an M- type object, agrees well with the IRAS albedo and rules out the possibility, suggested on the basis of spectroscopic observations, that Lutetia may actually have a carbonaceous composition. 2.2. Observations of asteroids with the Spitzer Space Telescope (Harris, Mueller) Two proposals submitted for observing time with Spitzer (Figure 2.2) in 2005 were awarded a total of 24 hr. observing time. The programmes are led by Harris and Mueller, respectively, and include a total of 7 co-investigators from Europe and the USA: 1. The Karin cluster asteroids in the main belt display very similar proper orbital elements and are therefore assumed to be dynamically related. The cluster, named after its largest member, (832) Karin, is believed to have been formed 5.8 ± 0.2 Myr ago in a catastrophic collision and thus to be significantly younger than most known asteroid families. The cluster is of great interest due to the fact that the physical properties of its members may preserve unique information about asteroid fragmentation and surface processes on small asteroids, which include regolith formation and modification of albedo and spectral properties via space weathering. Our Spitzer observations of 17 Karin cluster members should allow us to determine their sizes, albedos and information on thermal inertia. The questions that can be addressed with these observations include: Are the distributions of sizes and albedos compatible with the Karin cluster being the result of a single catastrophic collision Fig.