Constraints on the Original Ejection Velocity Fields of Asteroid Families
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Asteroid Family Physical Properties, Numerical Sim- Constraints on the Ages of Families
Asteroid Family Physical Properties Joseph R. Masiero NASA Jet Propulsion Laboratory/Caltech Francesca DeMeo Harvard/Smithsonian Center for Astrophysics Toshihiro Kasuga Planetary Exploration Research Center, Chiba Institute of Technology Alex H. Parker Southwest Research Institute An asteroid family is typically formed when a larger parent body undergoes a catastrophic collisional disruption, and as such family members are expected to show physical properties that closely trace the composition and mineralogical evolution of the parent. Recently a number of new datasets have been released that probe the physical properties of a large number of asteroids, many of which are members of identified families. We review these data sets and the composite properties of asteroid families derived from this plethora of new data. We also discuss the limitations of the current data, and the open questions in the field. 1. INTRODUCTION techniques that rely on simulating the non-gravitational forces that depend on an asteroid’s albedo, diameter, and Asteroid families provide waypoints along the path of density. dynamical evolution of the solar system, as well as labo- In Asteroids III, Zappala` et al. (2002) and Cellino et ratories for studying the massive impacts that were com- al. (2002) reviewed the physical and spectral properties mon during terrestrial planet formation. Catastrophic dis- (respectively) of asteroid families known at that time. Zap- ruptions shattered these asteroids, leaving swarms of bod- pala` et al. (2002) primarily dealt with asteroid size distri- ies behind that evolved dynamically under gravitational per- butions inferred from a combination of observed absolute turbations and the Yarkovsky effect to their present-day lo- H magnitudes and albedo assumptions based on the subset cations, both in the Main Belt and beyond. -
The Minor Planet Bulletin 36, 188-190
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 37, NUMBER 3, A.D. 2010 JULY-SEPTEMBER 81. ROTATION PERIOD AND H-G PARAMETERS telescope (SCT) working at f/4 and an SBIG ST-8E CCD. Baker DETERMINATION FOR 1700 ZVEZDARA: A independently initiated observations on 2009 September 18 at COLLABORATIVE PHOTOMETRY PROJECT Indian Hill Observatory using a 0.3-m SCT reduced to f/6.2 coupled with an SBIG ST-402ME CCD and Johnson V filter. Ronald E. Baker Benishek from the Belgrade Astronomical Observatory joined the Indian Hill Observatory (H75) collaboration on 2009 September 24 employing a 0.4-m SCT PO Box 11, Chagrin Falls, OH 44022 USA operating at f/10 with an unguided SBIG ST-10 XME CCD. [email protected] Pilcher at Organ Mesa Observatory carried out observations on 2009 September 30 over more than seven hours using a 0.35-m Vladimir Benishek f/10 SCT and an unguided SBIG STL-1001E CCD. As a result of Belgrade Astronomical Observatory the collaborative effort, a total of 17 time series sessions was Volgina 7, 11060 Belgrade 38 SERBIA obtained from 2009 August 20 until October 19. All observations were unfiltered with the exception of those recorded on September Frederick Pilcher 18. MPO Canopus software (BDW Publishing, 2009a) employing 4438 Organ Mesa Loop differential aperture photometry, was used by all authors for Las Cruces, NM 88011 USA photometric data reduction. The period analysis was performed using the same program. David Higgins Hunter Hill Observatory The data were merged by adjusting instrumental magnitudes and 7 Mawalan Street, Ngunnawal ACT 2913 overlapping characteristic features of the individual lightcurves. -
Evidence for Asteroid Space Weathering from the Sloan Digital Sky Survey
Icarus 173 (2005) 132–152 www.elsevier.com/locate/icarus Evidence for asteroid space weathering from the Sloan Digital Sky Survey David Nesvorný a,∗, Robert Jedicke b, Robert J. Whiteley c, Željko Ivezic´ d a Southwest Research Institute, 1050 Walnut St, Suite 400, Boulder, CO 80302, USA b Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA c Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA d Princeton University Observatory, Princeton, NJ 08544, USA Received 11 April 2004; revised 29 July 2004 Available online 12 October 2004 Abstract By studying color variations between young and old asteroid families we find evidence for processes that modify colors of asteroids over time. We show that colors of aging surfaces of S-type asteroids become increasingly ‘redder’ and measure the rate of these spectral changes. ≈ −1 × We estimate that the mean spectral slope between 0.35 and 0.9 µm increases with time t (given in My) as 0.01 µm log10 t.This empirical fit is valid only for 2.5 t 3000 My (the time interval where we have data) and for the mean spectral slope determined from wide-wavelength filter photometry obtained by the Sloan Digital Sky Survey. We also find that Gy-old terrains of S-type asteroids reflect about 15% more light at ∼ 1-µm wavelengths than an ∼ 5-My-old S-type asteroid surface when the flux is normalized by the reflected light at 0.55 µm. We attribute these effects to space weathering. This result has important implications for asteroid geology and the origin of meteorites that reach the Earth. -
In-Space Production of Storable Propellants
Deep Space Industries Inc. In-Space Production NNX15AL85G of Storable Propellants NIAC Phase I Final Report for NNX15AL85G: In-Space Production of Storable Propellants Deep Space Industries Inc. John S. Lewis, P. I. 1 March 2016 Deep Space Industries Inc. In-Space Production NNX15AL85G of Storable Propellants Table of Contents Overview and Conclusions ............................................................................................................................ 1 Introduction .................................................................................................................................................. 5 1. Available Feedstock on C-cadre Asteroids ................................................................................................ 5 2. Energy Requirements for Heating Feedstock ........................................................................................... 6 3. Recovered Water and its Uses ................................................................................................................ 16 4. Electrolysis of Water for STP or Direct Combustion .............................................................................. 17 5. Electrolysis of Water for Manufacture of Storables .............................................................................. 19 6. Where Should we Make Propellants? ..................................................................................................... 20 7. Storage and Transportation of Water and Carbon Dioxide .................................................................. -
The Minor Planet Bulletin Semi-Major Axis of 2.317 AU, Eccentricity 0.197, Inclination 7.09 (Warner Et Al., 2018)
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 45, NUMBER 3, A.D. 2018 JULY-SEPTEMBER 215. LIGHTCURVE ANALYSIS FOR TWO NEAR-EARTH 320ʺ/min during the close approach. The eclipse was observed, ASTEROIDS ECLIPSED BY EARTH’S SHADOW within minutes of the original prediction. Preliminary rotational and eclipse lightcurves were made available soon after the close Peter Birtwhistle approach (Birtwhistle, 2012; Birtwhistle, 2013; Miles, 2013) but it Great Shefford Observatory should be noted that a possible low amplitude 8.7 h period (Miles, Phlox Cottage, Wantage Road 2013) has been discounted in this analysis. Great Shefford, Berkshire, RG17 7DA United Kingdom Several other near-Earth asteroids are known to have been [email protected] eclipsed by the Earth’s shadow, e.g. 2008 TC3 and 2014 AA (both before impacting Earth), 2012 KT42, and 2016 VA (this paper) (Received 2018 March18) but internet searches have not found any eclipse lightcurves. The asteroid lightcurve database (LCDB; Warner et al., 2009) lists a Photometry was obtained from Great Shefford reference to an unpublished result for 2012 XE54 by Pollock Observatory of near-Earth asteroids 2012 XE54 in 2012 (2013) without lightcurve details, but these have been provided on and 2016 VA in 2016 during close approaches. A request and give the rotation period as 0.02780 ± 0.00002 h, superfast rotation period has been determined for 2012 amplitude 0.33 mag derived from 101 points over a period of 30 XE54 and H-G magnitude system coefficients have been minutes for epoch 2012 Dec 10.2 UT at phase angle 19.5°, estimated for 2016 VA. -
Asteroid Taxonomic Signatures from Photometric Phase Curves
Asteroid taxonomic signatures from photometric phase curves D. A. Oszkiewicz1;2;3, E. Bowell2, L. H. Wasserman2, K. Muinonen1;4, A. Penttil¨a1, T. Pieniluoma1, D. E. Trilling3, C. A. Thomas3 1 Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland. 2 Lowell Observatory, 1400 West Mars Hill Road, Flagstaff, AZ 86001, U.S.A. 3 Department of Physics and Astronomy, Northern Arizona University, P.O. Box 6010, Flagstaff, AZ 86011, U.S.A. 4 Finnish Geodetic Institute, P.O. Box 15, FI-02431 Masala, Finland. Abstract We explore the correlation between an asteroid's taxonomy and photometric phase curve using the H;G12 photometric phase function, with the shape of the phase function described by the single parameter G12. We explore the usability of G12 in taxonomic classification for individual objects, asteroid families, and dynamical groups. We conclude that the mean values of G12 for the considered taxonomic complexes are statistically different, and also discuss the overall shape of the G12 distribution for each taxonomic complex. Based on the values of G12 for about half a million asteroids, we compute the probabilities of C, S, and X com- plex membership for each asteroid. For an individual asteroid, these probabilities are rather evenly distributed over all of the complexes, thus preventing meaning- ful classification. We then present and discuss the G12 distributions for asteroid families, and predict the taxonomic complex preponderance for asteroid families arXiv:1202.2270v1 [astro-ph.EP] 10 Feb 2012 given the distribution of G12 in each family. For certain asteroid families, the probabilistic prediction of taxonomic complex preponderance can clearly be made. -
Irregular Satellites of the Giant Planets 411
Nicholson et al.: Irregular Satellites of the Giant Planets 411 Irregular Satellites of the Giant Planets Philip D. Nicholson Cornell University Matija Cuk University of British Columbia Scott S. Sheppard Carnegie Institution of Washington David Nesvorný Southwest Research Institute Torrence V. Johnson Jet Propulsion Laboratory The irregular satellites of the outer planets, whose population now numbers over 100, are likely to have been captured from heliocentric orbit during the early period of solar system history. They may thus constitute an intact sample of the planetesimals that accreted to form the cores of the jovian planets. Ranging in diameter from ~2 km to over 300 km, these bodies overlap the lower end of the presently known population of transneptunian objects (TNOs). Their size distributions, however, appear to be significantly shallower than that of TNOs of comparable size, suggesting either collisional evolution or a size-dependent capture probability. Several tight orbital groupings at Jupiter, supported by similarities in color, attest to a common origin followed by collisional disruption, akin to that of asteroid families. But with the limited data available to date, this does not appear to be the case at Uranus or Neptune, while the situa- tion at Saturn is unclear. Very limited spectral evidence suggests an origin of the jovian irregu- lars in the outer asteroid belt, but Saturn’s Phoebe and Neptune’s Nereid have surfaces domi- nated by water ice, suggesting an outer solar system origin. The short-term dynamics of many of the irregular satellites are dominated by large-amplitude coupled oscillations in eccentricity and inclination and offer several novel features, including secular resonances. -
Near-Ir Reflectance Spectra of M-Asteroids 250 Bettina, 369 Aeria, 413 Edburga, and 931 Whittemora
Lunar and Planetary Science XXXVIII (2007) 1956.pdf NEAR-IR REFLECTANCE SPECTRA OF M-ASTEROIDS 250 BETTINA, 369 AERIA, 413 EDBURGA, AND 931 WHITTEMORA. P. S. Hardersen1,2, M. J. Gaffey1,2, S. Kumar1,2, S. K. Fieber-Beyer1,2, J. J. Crowell1,2, and A. M. Crowell1. 1University of North Dakota, Department of Space Studies, 4149 University Avenue Stop 9008, Grand Forks, ND 58201, 2Visiting Astronomer at the Infrared Telescope Facility under contract from the Na- tional Aeronautics and Space Administration, which is operated by the University of Hawai’i, Mauna Kea, HI 96720. [email protected]. Introduction: The study of asteroids via ground- of a 3-µm absorption feature. The nature of 3-µm ab- based near-infrared (NIR: ~0.8 to 2.5-µm) spectral sorptions is problematic as they are not diagnostic reflectance measurements is currently the most effi- identifiers of phyllosilicate minerals [1]. The abun- cient and diagnostic technique to constrain asteroid dance of surface phyllosilicates necessary to produce surface major mineral abundances of a large number of a ~3-µm absorption is also not constrained. If the phyl- objects [1,2,3,4,5,6]. When combined with comple- losilicate interpretation is correct, however, then it mentary data at other wavelength intervals (i.e., visi- becomes potentially necessary to reconcile differing ble-λ, ~3-µm, radar), the ability to constrain an aster- interpretations. oid’s dominant surface mineral(s) and metallic abun- Observations/Data reduction: Observations of dance becomes stronger when the various datasets 250 Bettina, 369 Aeria, 413 Edburga, and 931 Whit- produce consistent interpretations [7,8,9]. -
Asteroid-Comet Continuum Objects in the Solar System
Asteroid-Comet Continuum Objects in the Solar System rsta.royalsocietypublishing.org Henry H. Hsieh1;2 1Planetary Science Institute, 1700 East Fort Lowell Research Rd., Suite 106, Tucson, Arizona 85719, USA 2Institute of Astronomy and Astrophysics, Academia Sinica, P.O. Box 23-141, Taipei 10617, Taiwan Article submitted to journal In this review presented at the Royal Society meeting, “Cometary Science After Rosetta”, I present Subject Areas: an overview of studies of small solar system Solar system objects that exhibit properties of both asteroids and comets (with a focus on so-called active Keywords: asteroids). Sometimes referred to as “transition asteroids, comets, meteors, objects”, these bodies are perhaps more appropriately dynamics, solar system evolution described as “continuum objects”, to reflect the notion that rather than necessarily representing actual transitional evolutionary states between asteroids Author for correspondence: and comets, they simply belong to the general H. H. Hsieh population of small solar system bodies that happen e-mail: [email protected] to exhibit a continuous range of observational, physical, and dynamical properties. Continuum objects are intriguing because they possess many of the properties that make classical comets interesting to study (e.g., relatively primitive compositions, ejection of surface and subsurface material into space where it can be more easily studied, and orbital properties that allow us to sample material from distant parts of the solar system that would otherwise be inaccessible), while allowing us to study regions of the solar system that are not sampled by classical comets. 1. Background Asteroids are classically understood to be essentially inert objects composed primarily of non-volatile material. -
Spectroscopic Survey of M-Type Asteroids S
Spectroscopic survey of M-type asteroids S. Fornasier, B.E. Clark, E. Dotto, A. Migliorini, M. Ockert-Bell, M.A. Barucci To cite this version: S. Fornasier, B.E. Clark, E. Dotto, A. Migliorini, M. Ockert-Bell, et al.. Spectroscopic survey of M- type asteroids. Icarus, Elsevier, 2010, 210 (2), pp.655. 10.1016/j.icarus.2010.07.001. hal-00693813 HAL Id: hal-00693813 https://hal.archives-ouvertes.fr/hal-00693813 Submitted on 3 May 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Spectroscopic survey of M–type asteroids S. Fornasier, B.E. Clark, E. Dotto, A. Migliorini, M. Ockert-Bell, M.A. Barucci PII: S0019-1035(10)00273-3 DOI: 10.1016/j.icarus.2010.07.001 Reference: YICAR 9497 To appear in: Icarus Received Date: 11 September 2009 Revised Date: 1 July 2010 Accepted Date: 1 July 2010 Please cite this article as: Fornasier, S., Clark, B.E., Dotto, E., Migliorini, A., Ockert-Bell, M., Barucci, M.A., Spectroscopic survey of M–type asteroids, Icarus (2010), doi: 10.1016/j.icarus.2010.07.001 This is a PDF file of an unedited manuscript that has been accepted for publication. -
The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 32, NUMBER 2, A.D. 2005 APRIL-JUNE 25. PERIOD DETERMINATION FOR 463 LOLA References Colin Bembrick Barbera, R. (2004). “AVE” Analisis de Variabilidad Estelar, Mt Tarana Observatory version 2.51, Grup Estudis Astronomics. PO Box 1537, Bathurst, NSW, Australia http://usuarios.lycos.es/rbarbera/AVE/AveInternational.htm [email protected] Binzel, Richard P., Gehrels, Tom, and Matthews, Mildred Shapley (Received: 5 January) (1989). Asteroids II. Univ. Ariz. Press, Tucson, Arizona. Minor planet 436 Lola was observed on four nights over a 13 day interval in October, 2004. The synodic period was detemined as 6.206 ± 0.002 hours. The peak to peak amplitude was 0.2 magnitudes. Table I. Aspect data for 463 Lola in 2004. Minor planet 463 Lola was discovered by Max Wolf at Heidelberg on October 31, 1900. It is most probably named from a character UT Date PAB PAB Phase % Phase in an opera. From the book Asteroids II (Binzel et al., 1989), this Long Lat Angle Coverage main-belt asteroid – originally 1900 FS – has a quoted diameter of 21.5 ± 0.8 km, an albedo of 0.077 and a B-V of 0.71. 2004 Oct 11 27.60 -4.45 7.27 72 2004 Oct 13 27.79 -4.21 6.04 100 Observations of this minor planet were made as a result of a 2004 Oct 22 28.37 -2.90 2.16 72 request for observations to back up radar work at Arecibo. -
Anniversari Asteroidali Di Michele T
Anniversari asteroidali di Michele T. Mazzucato GENNAIO 1 gen – 1801 viene scoperto l’asteroide 1 Ceres (G. Piazzi, Palermo) 2 gen – 1916 viene scoperto l’asteroide 814 Tauris (G.N. Neujmin, Simeis) 3 gen – 1918 viene scoperto l’asteroide 887 Alinda (M.F. Wolf, Heidelberg) 4 gen – 1866 viene scoperto l’asteroide 86 Semele (F. Tietjen, Berlin) - 1876 viene scoperto l’asteroide 158 Koronis (V. Knorre, Berlin) 5 gen – 1924 viene scoperto l’asteroide 1011 Laodamia (K. Reinmauth, Heindelberg) 6 gen – 1914 viene scoperto l’asteroide 775 Lumiere (J. Lagrula, Nice) 7 gen – 1985 viene lanciata la sonda Sakigake (Giappone) [1P/ Halley] 8 gen – 1894 viene scoperto l’asteroide 379 Huenna (A. Charlois, Nice) 9 gen – 1901 viene scoperto l’asteroide 464 Megaira (M.F. Wolf, Heidelberg) 10 gen – 1877 viene scoperto l’asteroide 170 Maria (J. Perrotin, Toulouse) 11 gen – 1929 viene scoperto l’asteroide 1126 Otero (K. Reinmauth, Heindelberg) 12 gen – 2005 viene lanciata la sonda Deep Impact (USA) [9P/ Tempel 1] - 1856 viene scoperto l’asteroide 38 Leda (J. Chacornac, Paris) 13 gen – 1875 viene scoperto l’asteroide 141 Lumen (P.P. Henry, Paris) - 1877 viene scoperto l’asteroide 171 Ophelia (A. Borrelly, Marseilles) 14 gen – 1905 viene scoperto l’asteroide 555 Norma (M.F. Wolf, Heindelberg) 15 gen – 1906 viene scoperto l’asteroide 584 Semiramis (A. Kopff, Heindelberg) 16 gen – 1893 viene scoperto l’asteroide 353 Ruperto-Carola (M.F. Wolf, Heindelberg) 17 gen – 1893 viene scoperto l’asteroide 354 Eleonora (A. Charlois, Nice) 18 gen – 1882 viene scoperto l’asteroide 221 Eos (J. Palisa, Vienna) 19 gen – 1903 viene scoperto l’asteroide 502 Sigune (M.F.