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ESO's VLT Sphere and DAMIT
ESO’s VLT Sphere and DAMIT ESO’s VLT SPHERE (using adaptive optics) and Joseph Durech (DAMIT) have a program to observe asteroids and collect light curve data to develop rotating 3D models with respect to time. Up till now, due to the limitations of modelling software, only convex profiles were produced. The aim is to reconstruct reliable nonconvex models of about 40 asteroids. Below is a list of targets that will be observed by SPHERE, for which detailed nonconvex shapes will be constructed. Special request by Joseph Durech: “If some of these asteroids have in next let's say two years some favourable occultations, it would be nice to combine the occultation chords with AO and light curves to improve the models.” 2 Pallas, 7 Iris, 8 Flora, 10 Hygiea, 11 Parthenope, 13 Egeria, 15 Eunomia, 16 Psyche, 18 Melpomene, 19 Fortuna, 20 Massalia, 22 Kalliope, 24 Themis, 29 Amphitrite, 31 Euphrosyne, 40 Harmonia, 41 Daphne, 51 Nemausa, 52 Europa, 59 Elpis, 65 Cybele, 87 Sylvia, 88 Thisbe, 89 Julia, 96 Aegle, 105 Artemis, 128 Nemesis, 145 Adeona, 187 Lamberta, 211 Isolda, 324 Bamberga, 354 Eleonora, 451 Patientia, 476 Hedwig, 511 Davida, 532 Herculina, 596 Scheila, 704 Interamnia Occultation Event: Asteroid 10 Hygiea – Sun 26th Feb 16h37m UT The magnitude 11 asteroid 10 Hygiea is expected to occult the magnitude 12.5 star 2UCAC 21608371 on Sunday 26th Feb 16h37m UT (= Mon 3:37am). Magnitude drop of 0.24 will require video. DAMIT asteroid model of 10 Hygiea - Astronomy Institute of the Charles University: Josef Ďurech, Vojtěch Sidorin Hygiea is the fourth-largest asteroid (largest is Ceres ~ 945kms) in the Solar System by volume and mass, and it is located in the asteroid belt about 400 million kms away. -
Asteroid Family Identification 613
Bendjoya and Zappalà: Asteroid Family Identification 613 Asteroid Family Identification Ph. Bendjoya University of Nice V. Zappalà Astronomical Observatory of Torino Asteroid families have long been known to exist, although only recently has the availability of new reliable statistical techniques made it possible to identify a number of very “robust” groupings. These results have laid the foundation for modern physical studies of families, thought to be the direct result of energetic collisional events. A short summary of the current state of affairs in the field of family identification is given, including a list of the most reliable families currently known. Some likely future developments are also discussed. 1. INTRODUCTION calibrate new identification methods. According to the origi- nal papers published in the literature, Brouwer (1951) used The term “asteroid families” is historically linked to the a fairly subjective criterion to subdivide the Flora family name of the Japanese researcher Kiyotsugu Hirayama, who delineated by Hirayama. Arnold (1969) assumed that the was the first to use the concept of orbital proper elements to asteroids are dispersed in the proper-element space in a identify groupings of asteroids characterized by nearly iden- Poisson distribution. Lindblad and Southworth (1971) cali- tical orbits (Hirayama, 1918, 1928, 1933). In interpreting brated their method in such a way as to find good agree- these results, Hirayama made the hypothesis that such a ment with Brouwer’s results. Carusi and Massaro (1978) proximity could not be due to chance and proposed a com- adjusted their method in order to again find the classical mon origin for the members of these groupings. -
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1,. ,-- ,-- ~XECKDING PAGE BLANK WT FIL,,q DYNAMICAL EVIDENCE REGARDING THE RELATIONSHIP BETWEEN ASTEROIDS AND METEORITES GEORGE W. WETHERILL Department of Temcltricrl kgnetism ~amregie~mtittition of Washington Washington, D. C. 20025 Meteorites are fragments of small solar system bodies (comets, asteroids and Apollo objects). Therefore they may be expected to provide valuable information regarding these bodies. How- ever, the identification of particular classes of meteorites with particular small bodies or classes of small bodies is at present uncertain. It is very unlikely that any significant quantity of meteoritic material is obtained from typical ac- tive comets. Relatively we1 1-studied dynamical mechanisms exist for transferring material into the vicinity of the Earth from the inner edge of the asteroid belt on an 210~-~year time scale. It seems likely that most iron meteorites are obtained in this way, and a significant yield of complementary differec- tiated meteoritic silicate material may be expected to accom- pany these differentiated iron meteorites. Insofar as data exist, photometric measurements support an association between Apollo objects and chondri tic meteorites. Because Apol lo ob- jects are in orbits which come close to the Earth, and also must be fragmented as they traverse the asteroid belt near aphel ion, there also must be a component of the meteorite flux derived from Apollo objects. Dynamical arguments favor the hypothesis that most Apollo objects are devolatilized comet resiaues. However, plausible dynamical , petrographic, and cosmogonical reasons are known which argue against the simple conclusion of this syllogism, uiz., that chondri tes are of cometary origin. Suggestions are given for future theoretical , observational, experimental investigations directed toward improving our understanding of this puzzling situation. -
Asteroid Rotation - Hunting for Arecord: 1689 Floris-Jan
per cent reported by the ESO staff at 8500 Ausing the 3.6 Table 1 (after Natta et al. 1980) shows our present m telescope. Fig. 1 shows the near-infrared spectra of two knowledge of the total sulfur abundances in nebulae. gaseous nebulae: IC 418, a galactic PN, and N 81, a H 11 These figures indicate that the average sulfur abundance region in the Small Magellanic Cloud. Exposure times are for galactic PN is lower than the one in the Sun and the 10 and 30 min. respectively. Orion Nebula. Consequently, one of the first concerns has The Y-axis represents analog to digital converter units been to compare the Reticon sulfur abundance with the (ADG). The system is set such that 1 ADC corresponds to on es reported by Natta et al. (1980). So far, and for the rms noise, which is about 1,000 counts. Saturation of galactic PN only, my values for log (S/H)+ 12 range from an individual diode occurs at about 4 x 106 counts or 6.35 ± 0.20 to 6.75 ± 0.33, depending on the object and about 4,000 ADC units. Therefore, a signal of 600 ADC ICF method used. In any case, my results seem to confirm (Ha line of N 81) corresponds to about 15 per cent of the a total sulfur abundance in PN lower than the one in the saturation level of the detector. Sun and in the Orion Nebula. A large number of questions The [S 111) f..'A 9060, 9532 Alines were detected in N 8, remain to be answered. -
Occultation Newsletter Volume 8, Number 4
Volume 12, Number 1 January 2005 $5.00 North Am./$6.25 Other International Occultation Timing Association, Inc. (IOTA) In this Issue Article Page The Largest Members Of Our Solar System – 2005 . 4 Resources Page What to Send to Whom . 3 Membership and Subscription Information . 3 IOTA Publications. 3 The Offices and Officers of IOTA . .11 IOTA European Section (IOTA/ES) . .11 IOTA on the World Wide Web. Back Cover ON THE COVER: Steve Preston posted a prediction for the occultation of a 10.8-magnitude star in Orion, about 3° from Betelgeuse, by the asteroid (238) Hypatia, which had an expected diameter of 148 km. The predicted path passed over the San Francisco Bay area, and that turned out to be quite accurate, with only a small shift towards the north, enough to leave Richard Nolthenius, observing visually from the coast northwest of Santa Cruz, to have a miss. But farther north, three other observers video recorded the occultation from their homes, and they were fortuitously located to define three well- spaced chords across the asteroid to accurately measure its shape and location relative to the star, as shown in the figure. The dashed lines show the axes of the fitted ellipse, produced by Dave Herald’s WinOccult program. This demonstrates the good results that can be obtained by a few dedicated observers with a relatively faint star; a bright star and/or many observers are not always necessary to obtain solid useful observations. – David Dunham Publication Date for this issue: July 2005 Please note: The date shown on the cover is for subscription purposes only and does not reflect the actual publication date. -
A Radar Survey of Main-Belt Asteroids: Arecibo Observations of 55 Objects During 1999–2003
Icarus 186 (2007) 126–151 www.elsevier.com/locate/icarus A radar survey of main-belt asteroids: Arecibo observations of 55 objects during 1999–2003 Christopher Magri a,∗, Michael C. Nolan b,StevenJ.Ostroc, Jon D. Giorgini d a University of Maine at Farmington, 173 High Street—Preble Hall, Farmington, ME 04938, USA b Arecibo Observatory, HC3 Box 53995, Arecibo, PR 00612, USA c 300-233, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA d 301-150, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099, USA Received 3 June 2006; revised 10 August 2006 Available online 24 October 2006 Abstract We report Arecibo observations of 55 main-belt asteroids (MBAs) during 1999–2003. Most of our targets had not been detected previously with radar, so these observations more than double the number of radar-detected MBAs. Our bandwidth estimates constrain our targets’ pole directions in a manner that is geometrically distinct from optically derived constraints. We present detailed statistical analyses of the disk-integrated properties (radar albedo and circular polarization ratio) of the 84 MBAs observed with radar through March 2003; all of these observations are summarized in the online supplementary information. Certain conclusions reached in previous studies are strengthened: M asteroids have higher mean radar albedos and a wider range of albedos than do other MBAs, suggesting that both metal-rich and metal-poor M-class objects exist; and C- and S-class MBAs have indistinguishable radar albedo distributions, suggesting that most S-class objects are chondritic. Also in accord with earlier results, there is evidence that primitive asteroids from outside the C taxon (F, G, P, and D) are not as radar-bright as C and S objects, but a convincing statistical test must await larger sample sizes. -
INPOP08, a 4-D Planetary Ephemeris: from Asteroid and Time-Scale Computations to ESA Mars Express and Venus Express Contributions
A&A 507, 1675–1686 (2009) Astronomy DOI: 10.1051/0004-6361/200911755 & c ESO 2009 Astrophysics INPOP08, a 4-D planetary ephemeris: from asteroid and time-scale computations to ESA Mars Express and Venus Express contributions A. Fienga1,2, J. Laskar1,T.Morley3,H.Manche1, P. Kuchynka1, C. Le Poncin-Lafitte4, F. Budnik3, M. Gastineau1, and L. Somenzi1,2 1 Astronomie et Systèmes Dynamiques, IMCCE-CNRS UMR8028, 77 Av. Denfert-Rochereau, 75014 Paris, France 2 Observatoire de Besançon, CNRS UMR6213, 41bis Av. de l’Observatoire, 25000 Besançon, France e-mail: [email protected] 3 ESOC, Robert-Bosch-Str. 5, Darmstadt 64293, Germany 4 SYRTE, CNRS UMR8630, Observatoire de Paris, 77 Av. Denfert-Rochereau, 75014 Paris, France Received 31 January 2009 / Accepted 24 August 2009 ABSTRACT The latest version of the planetary ephemerides developed at the Paris Observatory and at the Besançon Observatory is presented. INPOP08 is a 4-dimension ephemeris since it provides positions and velocities of planets and the relation between Terrestrial Time and Barycentric Dynamical Time. Investigations to improve the modeling of asteroids are described as well as the new sets of observations used for the fit of INPOP08. New observations provided by the European Space Agency deduced from the tracking of the Mars Express and Venus Express missions are presented as well as the normal point deduced from the Cassini mission. We show importance of these observations in the fit of INPOP08, especially in terms of Venus, Saturn and Earth-Moon barycenter orbits. Key words. ephemerides – astrometry – time – minor planets, asteroids – solar system: general – space vehicules 1. -
Cumulative Index to Volumes 1-45
The Minor Planet Bulletin Cumulative Index 1 Table of Contents Tedesco, E. F. “Determination of the Index to Volume 1 (1974) Absolute Magnitude and Phase Index to Volume 1 (1974) ..................... 1 Coefficient of Minor Planet 887 Alinda” Index to Volume 2 (1975) ..................... 1 Chapman, C. R. “The Impossibility of 25-27. Index to Volume 3 (1976) ..................... 1 Observing Asteroid Surfaces” 17. Index to Volume 4 (1977) ..................... 2 Tedesco, E. F. “On the Brightnesses of Index to Volume 5 (1978) ..................... 2 Dunham, D. W. (Letter regarding 1 Ceres Asteroids” 3-9. Index to Volume 6 (1979) ..................... 3 occultation) 35. Index to Volume 7 (1980) ..................... 3 Wallentine, D. and Porter, A. Index to Volume 8 (1981) ..................... 3 Hodgson, R. G. “Useful Work on Minor “Opportunities for Visual Photometry of Index to Volume 9 (1982) ..................... 4 Planets” 1-4. Selected Minor Planets, April - June Index to Volume 10 (1983) ................... 4 1975” 31-33. Index to Volume 11 (1984) ................... 4 Hodgson, R. G. “Implications of Recent Index to Volume 12 (1985) ................... 4 Diameter and Mass Determinations of Welch, D., Binzel, R., and Patterson, J. Comprehensive Index to Volumes 1-12 5 Ceres” 24-28. “The Rotation Period of 18 Melpomene” Index to Volume 13 (1986) ................... 5 20-21. Hodgson, R. G. “Minor Planet Work for Index to Volume 14 (1987) ................... 5 Smaller Observatories” 30-35. Index to Volume 15 (1988) ................... 6 Index to Volume 3 (1976) Index to Volume 16 (1989) ................... 6 Hodgson, R. G. “Observations of 887 Index to Volume 17 (1990) ................... 6 Alinda” 36-37. Chapman, C. R. “Close Approach Index to Volume 18 (1991) .................. -
Style and Intensity of Hydration Among C-Complex Asteroids: a Comparison to Desiccated Carbonaceous Chondrites S
Style and intensity of hydration among C-complex asteroids: a comparison to desiccated carbonaceous chondrites S. Potin1, P. Beck1, F. Usui2, L. Bonal1, P. Vernazza3, B. Schmitt1 1Université Grenoble Alpes, CNRS, Institut de Planétologie et d’Astrophysique de Grenoble (IPAG), 414 rue de la Piscine 38400 Saint-Martin d’Hères, France. 2Center for Planetary Science, Graduate School of Science, Kobe University, 7-1-48 Minatojima- Minamimachi, Chuo-Ku, Kobe 650-0047, Japan. 3Laboratoire d’Astrophysique de Marseille (LAM), 38 rue Frédéric Joliot-Curie 13388 Marseille, France. ABSTRACT Here we report a comparison between reflectance spectroscopy of meteorites under asteroidal environment (high vacuum and temperature) and Main Belt and Near Earth Asteroids spectra. Focusing on the –OH absorption feature around 3µm, we show that the asteroidal environment induces a reduction of depth and width of the band, as well as a shift of the reflectance minimum. We then decompose the –OH feature into several components with a new model using Exponentially Modified Gaussians. Unlike previous studies, we confirme the link between these components, the aqueous alteration history and the amount of water molecules inside of the sample, using the shape of this spectral feature only. We then apply this deconvolution model to asteroids spectra which were obtained with a space-borne telescope and two space probes, and find a strong similarity with the components detected on meteorites, and among asteroids from a same type. Based on the conclusions drawn from our meteorites experiment, we suggest to use the 3-µm band as a tracer of the alteration history of the small bodies. -
ARMIN OTTO LEUSCHNER January 16,1868-April 22,1953
NATIONAL ACADEMY OF SCIENCES A R M I N O T T O L EUSCHNER 1868—1953 A Biographical Memoir by P A U L H ERGET Any opinions expressed in this memoir are those of the author(s) and do not necessarily reflect the views of the National Academy of Sciences. Biographical Memoir COPYRIGHT 1978 NATIONAL ACADEMY OF SCIENCES WASHINGTON D.C. ARMIN OTTO LEUSCHNER January 16,1868-April 22,1953 BY PAUL HERGET RMIN OTTO LEUSCHNER was born on January 16, 1868, in A• Detroit, Michigan, and died in Berkeley, California, on April 22, 1953. His professional career, which was spent at the University of California, began in the early days of the Univer- sity's Lick Observatory. In 1939, at a banquet of the American Astronomical Society, Leuschner delivered an after-dinner speech entitled, "The Three Times I Was Fired from the Uni- versity of California." This was hyperbole, because he was never fired at all, but it is unfortunate that this speech is now lost to posterity. Two of the occasions to which he referred concerned alter- cations with the autocratic first director of the Lick Observa- tory, E. S. Holden. Leuschner had just begun his graduate studies, and, according to his story, he put up some window curtains in the rather desolate shack assigned to him as his living quarters on Mt. Hamilton. Holden berated him for such frivol- ity and waste of effort, which he declared could be put to better use. Leuschner was not a meek soul, and, in the heated words that were exchanged, he was threatened with dismissal. -
The Minor Planet Bulletin (Warner Et Al., 2009A)
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 36, NUMBER 4, A.D. 2009 OCTOBER-DECEMBER 133. NEW LIGHTCURVES OF 8 FLORA, 13 EGERIA, consistent with a period near 12.9 h. Hollis et. al. (1987) derived a 14 IRENE, 25 PHOCAEA, 40 HARMONIA, 74 GALATEA, period of 12.790 h. Di Martino (1989) and Harris and Young AND 122 GERDA (1989) also found periods of approximately 12.87 h, as did Piiornen et al. (1998). Torppa et al. (2003) found a sidereal period Frederick Pilcher of 12.79900 h using lightcurve inversion techniques. Several 4438 Organ Mesa Loop attempts have also been made to determine the spin axis Las Cruces, NM 88011 USA orientation for Flora. Hollis et al. (1987) reported a pole longitude [email protected] near 148° while Di Martino et al. (1989) found two possible solutions at longitude 140° or 320°. Torppa et al. (2003) found a (Received: 2009 Jun 30 Revised: 2009 Aug 2) pole solution of (160°, +16°) and sidereal period of 12.79900 h, similar to (155°, +5°) found by Durech (2009a), both using lightcurve inversion methods. Durech’s sidereal period, however, New lightcurves yield synodic rotation periods and was 12.86667 h. amplitudes for: 8 Flora, 12.861 ± 0.001 h, 0.08 ± 0.01 mag; 13 Egeria, 7.0473 ± 0.0001 h, 0.15 ± 0.02 mag in New observations of the asteroid obtained by the author on 8 2007, 0.37 ± 0.02 mag in 2009; 14 Irene, 15.089 ± nights from 2009 Feb. -
Case of the Missing Ceres Family
45th Lunar and Planetary Science Conference (2014) 1649.pdf THE CASE OF THE MISSING CERES FAMILY. A. S. Rivkin1 and E. Asphaug2, 1JHU/APL, Laurel, MD, USA ([email protected]). 2Arizona State University, Tempe, AZ, USA. Introduction: Most of the largest asteroids in the If a Ceres family exists, it is exceedingly unlikely to main belt are associated with an impact-generated dy- have escaped detection. namical family. The Vesta family dominates the inner Dodging bullets? Could Ceres have simply asteroid belt with its numbers [1-2], and was a critical avoided making a family? Given that it is the largest piece of evidence in tying the HED meteorites to Ves- asteroid, and thus the biggest target, it is exceedingly ta. In addition to Vesta (the third-largest asteroid), Pal- unlikely that it would have avoided impact by a sizable las (the second-largest asteroid), Hygiea (the fourth- smaller asteroid. However, it might be argued that the largest asteroid), and the largest S-class asteroid, 15 escape speed for Ceres, ∼0.5 km/s, would suppress Eunomia, all have dynamical families [3-6]. family formation, as it is higher than that of any other Twelve asteroids in the current main belt have di- body in the asteroid belt. The amount of ejecta escap- ameters over 250 km, containing two-thirds of the as- ing from Ceres might be reduced, compared to similar- teroid belt’s mass. In addition, [7] estimated that two sized impacts occurring on lower-gravity asteroids; of the largest present-day families, Themis and Eos, and the energy required to escape might lead to highly had parent bodies in the ~300-400 km size range where comminuted fragments or even vaporization.