The Minor Planet Bulletin, 30(3), Pp

Total Page:16

File Type:pdf, Size:1020Kb

The Minor Planet Bulletin, 30(3), Pp 1 THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 31, NUMBER 1, A.D. 2004 JANUARY-MARCH 1. ASTROMETRIC PROGRAM FOR JR refers to asteroids nearby to the 3:1 mean motion resonance NEAR-EARTH OBJECT SOURCES with Jupiter, MC are the Mars Crossers, NU are objects in the ν 6 secular resonance. Sergio Foglia UAI Minor Planets Section Recorder References F. Bisleri 11, I-20148 Milano, Italy € [email protected] Morbidelli et. al. (2003). Understanding the distribution on Near Earth Objects. http://www.obs-nice.fr/morby/ESA/ esa.html (Received: 24 September Revised: 6 October) MPC Orbit Database. ftp://ftp-cfa.harvard.edu/pub/MPCORB/ 2003 Sep. 17, Minor Planet Center A new astroometric program is proposed for asteroids located in likely source regions supplying the near-Earth Proper Elements of Minor Planets. http://hamilton.dm object population. .unipi.it/astdys/ 2003 Sep. 17, Asteroid Dynamic Site According to Morbidelli et al. (2003), near-Earth objects (NEOs) come mainly from 5 sources with the following contributions to the population: the ν 6 resonance region at the inner border of the asteroid main belt (37 ± 8 %), the 3:1 resonance region in the middle of the asteroid main belt (23 ± 8 %), the Intermediate Mars-Crossing (IMC) population (25 ± 3 %), the Outer Belt (OB) population€ (8 ± 1 %), and the population of dormant Jupiter Family Comets (JFC) (6 ± 4 %). Astrometric measurements of objects in these source regions would be very useful to increase knowledge about the NEO source population and solar system dynamics. Thus a new astrometric program for NEO source bodies involving amateur astronomers is suggested. For this program, most objects are usually brigther than 18.0 V magnitude and thus are within the range of equipment for many observers to obtain good measurements. Our goal is to suggest an observing program named Near Earth Figure 1. Depiction of asteroids for the NEOSAP program. Light Objects Source Astrometric Program (NEOSAP) involving the grey bordered rectangles are the Mars Crossers, dark grey following objects: Mars Crossers having q < 1.52 and Q > 1.52, bordered rectangles are objects in the ν 6 secular resonance, and where q and Q are perihelion and aphelion distances in AU; filled rectangles are asteroids nearby to the 3:1 mean motion asteroids in the ν 6 secular resonance; asteroids nearby to the 3:1 resonance with Jupiter. mean motion resonance with Jupiter. € Interested observers will find ephemeris and other information at the following€ URL: http://www.uai.it/sez_ast/neosap.htm Table I: Numbers of NEOSAP asteroids. Astrometric measurements must be sent to the Minor Planet Center in the usual way; no other action is required by observers JR 717 and the listed URL serves only to provide information and MC 726 ephemerides for recommended targets. MC + JR 5 MC + NU 10 NU 116 Figure 1 shows the distribution of these objects in the plane of the Total 1574 orbital elements semi-major axis (a) and inclination (i). Table I gives numbers of NEOSAP asteroids in the different categories: Minor Planet Bulletin 31 (2004) 2 ROTATION PERIOD AND LIGHTCURVE OF ASTEROID We were lucky enough to observe a well defined peak every night 1635 BOHRMANN we observed. I measured the time differences between peaks on different nights to generate a list of possible alias periods and then Christine M. Simpson to narrow these periods down to a rotation period of 11.73 ±0.01 Whitin Observatory hours. From this period it can be deduced that 2.0 rotations Wellesley College elapsed between the peaks on Sept. 6 and Sept. 7; 22.5 rotations 106 Central Street elapsed between the peaks on Sept. 6 and Sept. 17; and 31.0 Wellesley, MA 02481 rotations elapsed between the peaks on Sept. 6 and Sept. 21. I then translated our differential magnitudes for each night onto the (Received: 14 October Revised: 6 November) time scale for Sept. 6 modulo the period. This result is shown in Figure 1, showing an amplitude near 0.28 magnitudes. I also have observations of 1635 Bohrmann for two more nights during this Koronis family asteroid 1635 Bohrmann was observed 15 day interval and for three nights after this interval. I am over the course of 15 days in September, 2003 at Whitin planning to use these data and other observations during the Observatory in Wellesley, Massachusetts. A period of current apparition to get a solar phase angle curve for the asteroid. 11.73 ± 0.01 hours was determined with an amplitude of about 0.28 mag. Acknowledgements I would like to thank Steve Slivan for advising me on this project Introduction and observing with me on Sept. 21. Also, many thanks go to Jeff Regester for fixing the CCD coolant chiller when it shorted. Asteroid 1635 Bohrmann is a member of the Koronis family of asteroids, located in the main asteroid belt. Asteroid families like References Koronis are thought to be the fragments of larger bodies broken apart in collisions. This formation method would suggest random Binzel, R. P. (2003). “Spin control for asteroids.” Nature 425, rotation periods and spin vector orientations, but recent 131-132. observations and analysis of some of the larger members of the Koronis family have shown that there are statistically significant Slivan, S. M. (2003). “A Web-Based Tool to Calculate clusters of rotation periods and spin vector orientations (Slivan et Observability of Koronis Program Asteroids.” The Minor Planet al. 2002). Just this year Vokrouhlicky´ et al. (2003) have proposed Bulletin 30, 71-72. thermal re-radiation or the “YORP effect” as an explanation for these phenomena (see also Binzel 2003). Bohrmann is a smaller Slivan, S. M., R. P. Binzel, L. D. Crespo da Silva, M. Kaasalainen, member of the Koronis family, and our observations, combined M. M. Lyndaker, and M. Krco. (2002). “Spin Vectors in the with future observations, will be used to determine Bohrmann’s Koronis Family: Comprehensive Results from Two Independent spin vector orientation. Information for observing 1635 Analyses of 213 Rotation Lightcurves.” Icarus 162, 285-307. Bohrmann and other Koronis family asteroids can be found at http://www.koronisfamily.com (Slivan 2003). Vokrouhlicky´, D., D. Nesvorny´, and W. F. Bottke. (2003). “The vector alignments of asteroid spins by thermal torques.” Nature Observations and Analysis 425, 147-151. I observed 1635 Bohrmann for four nights in September of 2003 from Whitin Observatory at Wellesley College in Wellesley, Massachusetts. A 1024 square pixel CCD camera was used to image the asteroid through a V filter at the Cassegrain focus of the 0.61m Sawyer telescope. The field of view was approximately 16 arcminutes square. Observations were made during clear (1635) Bohrmann 2.65 UT Sept 6 conditions, except for those made during the first hour of UT Sept 7 2.7 UT Sept 17 observations on September 21 when there were some clouds UT Sept 21 2.75 moving in and out. The exposure time for each observation was Magnitude 240s. IRAF software packages were used to analyze the data. All V 2.8 images were corrected for bias, dark and flat field effects. 2.85 Instrumental For each night of data, I selected a non-variable comparison star in 2.9 the field that was brighter than the asteroid. The instrumental magnitude of the comparison star was subtracted from the 2.95 Differential instrumental magnitude of the asteroid to get a differential 3 instrumental magnitude for each image. I then selected a non- -5 -4 -3 -2 -1 0 1 2 3 4 5 6 7 UT hours on 2003 Sept 6 variable check star in our field similar in brightness to the asteroid. For each image I found a differential instrumental magnitude for Figure 1: Composite lightcurve for (1635) Bohrmann for a this check star with respect to the same comparison star used for rotation period of 11.73 ± 0.01hours. These data are light time the asteroid differential magnitude. The standard deviation of this corrected. The error bars are a one-sigma estimation of the differential instrumental magnitude was then used to estimate the uncertainty with respect to the local comparison star used for each uncertainty in the differential instrumental magnitude of our night. asteroid. Minor Planet Bulletin 31 (2004) 3 LIGHTCURVE ANALYSIS OF KORONIS FAMILY Table 1: Observing session details. ASTEROID 1635 BOHRMANN Observer Date Obs Phase Robert D. Stephens Stephens Sept 17 85 3.3 Santana Observatory Stephens Sept 18 86 2.9 11355 Mount Johnson Court Stephens Sept 19 21 2.4 Rancho Cucamonga, CA 91737 USA Stephens Sept 20 94 2.0 [email protected] Stephens Sept 21 33 1.5 Stephens Sept 22 62 1.1 Brian D. Warner Warner Sept 29 79 1.9 Palmer Divide Observatory Warner Oct 02 59 3.2 17995 Bakers Farm Road Total 519 Colorado Springs, CO 80908 [email protected] analysis routine developed by Alan Harris (Harris et al., 1989). (Received: 15 October) This program allows combining data from different observers and adjusting the zero points to compensate for different equipment and comparison stars. All observations were corrected for light The lightcurve for 1635 Bohrmann was obtained by the time. All observations were unfiltered. Dark frames and flat authors in September and October 2003. The rotational fields were used to calibrate the images. period was determined to be 11.730 ± 0.005 hours with an amplitude of 0.28 ± 0.03 mag. Bohrmann was discovered on March 7, 1924 by Karl Reinmuth at Heidelberg. It is named in honor of Alfred Bohrmann who was at the Königstuhl Observatory from 1924 to 1969.
Recommended publications
  • 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.
    [Show full text]
  • The Minor Planet Bulletin
    THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 36, NUMBER 3, A.D. 2009 JULY-SEPTEMBER 77. PHOTOMETRIC MEASUREMENTS OF 343 OSTARA Our data can be obtained from http://www.uwec.edu/physics/ AND OTHER ASTEROIDS AT HOBBS OBSERVATORY asteroid/. Lyle Ford, George Stecher, Kayla Lorenzen, and Cole Cook Acknowledgements Department of Physics and Astronomy University of Wisconsin-Eau Claire We thank the Theodore Dunham Fund for Astrophysics, the Eau Claire, WI 54702-4004 National Science Foundation (award number 0519006), the [email protected] University of Wisconsin-Eau Claire Office of Research and Sponsored Programs, and the University of Wisconsin-Eau Claire (Received: 2009 Feb 11) Blugold Fellow and McNair programs for financial support. References We observed 343 Ostara on 2008 October 4 and obtained R and V standard magnitudes. The period was Binzel, R.P. (1987). “A Photoelectric Survey of 130 Asteroids”, found to be significantly greater than the previously Icarus 72, 135-208. reported value of 6.42 hours. Measurements of 2660 Wasserman and (17010) 1999 CQ72 made on 2008 Stecher, G.J., Ford, L.A., and Elbert, J.D. (1999). “Equipping a March 25 are also reported. 0.6 Meter Alt-Azimuth Telescope for Photometry”, IAPPP Comm, 76, 68-74. We made R band and V band photometric measurements of 343 Warner, B.D. (2006). A Practical Guide to Lightcurve Photometry Ostara on 2008 October 4 using the 0.6 m “Air Force” Telescope and Analysis. Springer, New York, NY. located at Hobbs Observatory (MPC code 750) near Fall Creek, Wisconsin.
    [Show full text]
  • Measuring the Astronomical Unit from Your Backyard Two Astronomers, Using Amateur Equipment, Determined the Scale of the Solar System to Better Than 1%
    Measuring the Astronomical Unit from Your Backyard Two astronomers, using amateur equipment, determined the scale of the solar system to better than 1%. So can you. By Robert J. Vanderbei and Ruslan Belikov HERE ON EARTH we measure distances in millimeters and throughout the cosmos are based in some way on distances inches, kilometers and miles. In the wider solar system, to nearby stars. Determining the astronomical unit was as a more natural standard unit is the tUlronomical unit: the central an issue for astronomy in the 18th and 19th centu· mean distance from Earth to the Sun. The astronomical ries as determining the Hubble constant - a measure of unit (a.u.) equals 149,597,870.691 kilometers plus or minus the universe's expansion rate - was in the 20th. just 30 meters, or 92,955.807.267 international miles plus or Astronomers of a century and more ago devised various minus 100 feet, measuring from the Sun's center to Earth's ingenious methods for determining the a. u. In this article center. We have learned the a. u. so extraordinarily well by we'll describe a way to do it from your backyard - or more tracking spacecraft via radio as they traverse the solar sys­ precisely, from any place with a fairly unobstructed view tem, and by bouncing radar Signals off solar.system bodies toward the east and west horizons - using only amateur from Earth. But we used to know it much more poorly. equipment. The method repeats a historic experiment per­ This was a serious problem for many brancht:s of as­ formed by Scottish astronomer David Gill in the late 19th tronomy; the uncertain length of the astronomical unit led century.
    [Show full text]
  • Observations from Orbiting Platforms 219
    Dotto et al.: Observations from Orbiting Platforms 219 Observations from Orbiting Platforms E. Dotto Istituto Nazionale di Astrofisica Osservatorio Astronomico di Torino M. A. Barucci Observatoire de Paris T. G. Müller Max-Planck-Institut für Extraterrestrische Physik and ISO Data Centre A. D. Storrs Towson University P. Tanga Istituto Nazionale di Astrofisica Osservatorio Astronomico di Torino and Observatoire de Nice Orbiting platforms provide the opportunity to observe asteroids without limitation by Earth’s atmosphere. Several Earth-orbiting observatories have been successfully operated in the last decade, obtaining unique results on asteroid physical properties. These include the high-resolu- tion mapping of the surface of 4 Vesta and the first spectra of asteroids in the far-infrared wave- length range. In the near future other space platforms and orbiting observatories are planned. Some of them are particularly promising for asteroid science and should considerably improve our knowledge of the dynamical and physical properties of asteroids. 1. INTRODUCTION 1800 asteroids. The results have been widely presented and discussed in the IRAS Minor Planet Survey (Tedesco et al., In the last few decades the use of space platforms has 1992) and the Supplemental IRAS Minor Planet Survey opened up new frontiers in the study of physical properties (Tedesco et al., 2002). This survey has been very important of asteroids by overcoming the limits imposed by Earth’s in the new assessment of the asteroid population: The aster- atmosphere and taking advantage of the use of new tech- oid taxonomy by Barucci et al. (1987), its recent extension nologies. (Fulchignoni et al., 2000), and an extended study of the size Earth-orbiting satellites have the advantage of observing distribution of main-belt asteroids (Cellino et al., 1991) are out of the terrestrial atmosphere; this allows them to be in just a few examples of the impact factor of this survey.
    [Show full text]
  • Modelling and Scaling Neglected Asteroids
    Asteroid studies via lightcurves Selection effects TPM Shape models vs. occultations Summary Modelling and scaling neglected asteroids A. Marciniak1 with V. Alí-Lagoa, T. Müller, P. Bartczak, R. Behrend, M. Butkiewicz-B ˛ak, G. Dudzinski,´ R. Duffard, K. Dziadura, S. Fauvaud, M. Ferrais, S. Geier, J. Grice, R. Hirsch, J. Horbowicz, K. Kaminski,´ P. Kankiewicz, D.-H. Kim, M.-J. Kim, I. Konstanciak, V. Kudak, L. Molnár, F. Monteiro, W. Ogłoza, D. Oszkiewicz, A. Pál, N. Parley, F. Pilcher, E. Podlewska - Gaca, T. Polakis, J. J. Sanabria, T. Santana-Ros, B. Skiff, K. Sobkowiak, R. Szakáts, S. Urakawa, M. Zejmo,˙ K. Zukowski˙ 1. Astronomical Observatory Institute, Faculty of Physics, A. Mickiewicz University, Poznan,´ Poland ESOP XXXIX, 29 August 2020 Asteroid studies via lightcurves Selection effects TPM Shape models vs. occultations Summary Asteroid lightcurves (219) Thusnelda P = 59.74 h 487 Venetia P = 13.355h 2014 -2,1 Oct 11.1 Suhora 2012/2013 -2,2 Oct 12.1 Suhora Oct 29.0 Bor Oct 24.1 Bor. -2,05 Nov 10.2 Suh Oct 28.1 Bor. Nov 11.1 Suh CCCCCC Nov 4.0 Bor. CCCCCCCCC CC C C Nov 7.4 Organ M. Dec 28.8 Bor C Mar 2.8 Bor C Nov 8.4 Organ M. AAAA -2 Mar 3.8 Bor AAAAAA C Nov 13.4 Organ M. AAAA C CCC Nov 14.4 Organ M. A -2,1 AAA CCC A Nov 15.4 Organ M. A AA Nov 21.4 Winer -1,95 Dec 2.1 OAdM Dec 3.0 OAdM Dec 5.0 Bor.
    [Show full text]
  • The Minor Planet Bulletin 44 (2017) 142
    THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 44, NUMBER 2, A.D. 2017 APRIL-JUNE 87. 319 LEONA AND 341 CALIFORNIA – Lightcurves from all sessions are then composited with no TWO VERY SLOWLY ROTATING ASTEROIDS adjustment of instrumental magnitudes. A search should be made for possible tumbling behavior. This is revealed whenever Frederick Pilcher successive rotational cycles show significant variation, and Organ Mesa Observatory (G50) quantified with simultaneous 2 period software. In addition, it is 4438 Organ Mesa Loop useful to obtain a small number of all-night sessions for each Las Cruces, NM 88011 USA object near opposition to look for possible small amplitude short [email protected] period variations. Lorenzo Franco Observations to obtain the data used in this paper were made at the Balzaretto Observatory (A81) Organ Mesa Observatory with a 0.35-meter Meade LX200 GPS Rome, ITALY Schmidt-Cassegrain (SCT) and SBIG STL-1001E CCD. Exposures were 60 seconds, unguided, with a clear filter. All Petr Pravec measurements were calibrated from CMC15 r’ values to Cousins Astronomical Institute R magnitudes for solar colored field stars. Photometric Academy of Sciences of the Czech Republic measurement is with MPO Canopus software. To reduce the Fricova 1, CZ-25165 number of points on the lightcurves and make them easier to read, Ondrejov, CZECH REPUBLIC data points on all lightcurves constructed with MPO Canopus software have been binned in sets of 3 with a maximum time (Received: 2016 Dec 20) difference of 5 minutes between points in each bin.
    [Show full text]
  • Downloaded Freely from the Google Play Portal (
    1 2 Spiral Galaxy M51. Herrero, E. Image from Montsec Astronomical Observatory (OAdM) 3 4 5 CONTENTS The Institute 6 Board of trustees 8 Scientific advisory board 9 Board of Directors 9 Staff 10 Scientific Research 16 Scientific results 25 Publications SCI 31 Papers in which only one institute is participating 31 Papers published by two institutes in collaboration 39 Papers published by three institutes in collaboration 40 Publications non SCI 40 Papers in which only one institute is participating 40 Papers published by two institutes in collaboration 46 Books edited 47 Courses 47 Contribution to conferences and seminars 48 Contribution to conferences 48 Seminars 59 Internal seminars 59 External seminars 59 Theses 61 Finished Theses 61 PhD Theses 61 Master theses 62 On going theses 62 PhD Theses 62 Master theses 62 Visiting scientists 64 Technological development activities 65 Technical reports and documents 65 Technical reports and documents developed by only one institute 65 Technical reports and documents developed by three institutes in collaboration 69 Technological development activities 69 Finished activities 69 Ongoing activities 69 Projects managed by the IEEC 69 Finished projects 69 Ongoing projects 70 Other scientific activities 72 Space missions 73 Mission proposals 82 Ground instrument projects 89 Montsec Astronomical Observatoyy (OAdM) 95 European Projects 99 Workshops organized by the IEEC 103 Outreach activities 107 Objectives, indicators and achievement 114 6 IEEC ▪ THE INSTITUTE The Institute of Space Studies of Catalonia (IEEC) was founded in February of 1996 as an initiative of the Fundació Catalana per a la Recerca (FCR), in collaboration with the University of Barcelona (UB), the Autonomous University of Barcelona (UAB), the Polytechnic University of Catalonia (UPC) and the Spanish Research Council (CSIC) with the objective of creating a multi-disciplinary and multi-institutional institute devoted to space research and their applications.
    [Show full text]
  • Asteroid Regolith Weathering: a Large-Scale Observational Investigation
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2019 Asteroid Regolith Weathering: A Large-Scale Observational Investigation Eric Michael MacLennan University of Tennessee, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Recommended Citation MacLennan, Eric Michael, "Asteroid Regolith Weathering: A Large-Scale Observational Investigation. " PhD diss., University of Tennessee, 2019. https://trace.tennessee.edu/utk_graddiss/5467 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Eric Michael MacLennan entitled "Asteroid Regolith Weathering: A Large-Scale Observational Investigation." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Geology. Joshua P. Emery, Major Professor We have read this dissertation and recommend its acceptance: Jeffrey E. Moersch, Harry Y. McSween Jr., Liem T. Tran Accepted for the Council: Dixie L. Thompson Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) Asteroid Regolith Weathering: A Large-Scale Observational Investigation A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville Eric Michael MacLennan May 2019 © by Eric Michael MacLennan, 2019 All Rights Reserved.
    [Show full text]
  • Origin of the Near-Earth Asteroid Phaethon and the Geminids Meteor Shower
    University of Central Florida STARS Faculty Bibliography 2010s Faculty Bibliography 1-1-2010 Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower J. de León H. Campins University of Central Florida K. Tsiganis A. Morbidelli J. Licandro Find similar works at: https://stars.library.ucf.edu/facultybib2010 University of Central Florida Libraries http://library.ucf.edu This Article is brought to you for free and open access by the Faculty Bibliography at STARS. It has been accepted for inclusion in Faculty Bibliography 2010s by an authorized administrator of STARS. For more information, please contact [email protected]. Recommended Citation de León, J.; Campins, H.; Tsiganis, K.; Morbidelli, A.; and Licandro, J., "Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower" (2010). Faculty Bibliography 2010s. 92. https://stars.library.ucf.edu/facultybib2010/92 A&A 513, A26 (2010) Astronomy DOI: 10.1051/0004-6361/200913609 & c ESO 2010 Astrophysics Origin of the near-Earth asteroid Phaethon and the Geminids meteor shower J. de León1,H.Campins2,K.Tsiganis3, A. Morbidelli4, and J. Licandro5,6 1 Instituto de Astrofísica de Andalucía-CSIC, Camino Bajo de Huétor 50, 18008 Granada, Spain e-mail: [email protected] 2 University of Central Florida, PO Box 162385, Orlando, FL 32816.2385, USA e-mail: [email protected] 3 Department of Physics, Aristotle University of Thessaloniki, 54 124 Thessaloniki, Greece 4 Departement Casiopée: Universite de Nice - Sophia Antipolis, Observatoire de la Cˆote d’Azur, CNRS 4, 06304 Nice, France 5 Instituto de Astrofísica de Canarias (IAC), C/Vía Láctea s/n, 38205 La Laguna, Spain 6 Department of Astrophysics, University of La Laguna, 38205 La Laguna, Tenerife, Spain Received 5 November 2009 / Accepted 26 January 2010 ABSTRACT Aims.
    [Show full text]
  • Aqueous Alteration on Main Belt Primitive Asteroids: Results from Visible Spectroscopy1
    Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 1 LESIA, Observatoire de Paris, CNRS, UPMC Univ Paris 06, Univ. Paris Diderot, 5 Place J. Janssen, 92195 Meudon Pricipal Cedex, France 2 Univ. Paris Diderot, Sorbonne Paris Cit´e, 4 rue Elsa Morante, 75205 Paris Cedex 13 3 Department of Physics and Astronomy of the University of Padova, Via Marzolo 8 35131 Padova, Italy Submitted to Icarus: November 2013, accepted on 28 January 2014 e-mail: [email protected]; fax: +33145077144; phone: +33145077746 Manuscript pages: 38; Figures: 13 ; Tables: 5 Running head: Aqueous alteration on primitive asteroids Send correspondence to: Sonia Fornasier LESIA-Observatoire de Paris arXiv:1402.0175v1 [astro-ph.EP] 2 Feb 2014 Batiment 17 5, Place Jules Janssen 92195 Meudon Cedex France e-mail: [email protected] 1Based on observations carried out at the European Southern Observatory (ESO), La Silla, Chile, ESO proposals 062.S-0173 and 064.S-0205 (PI M. Lazzarin) Preprint submitted to Elsevier September 27, 2018 fax: +33145077144 phone: +33145077746 2 Aqueous alteration on main belt primitive asteroids: results from visible spectroscopy1 S. Fornasier1,2, C. Lantz1,2, M.A. Barucci1, M. Lazzarin3 Abstract This work focuses on the study of the aqueous alteration process which acted in the main belt and produced hydrated minerals on the altered asteroids. Hydrated minerals have been found mainly on Mars surface, on main belt primitive asteroids and possibly also on few TNOs. These materials have been produced by hydration of pristine anhydrous silicates during the aqueous alteration process, that, to be active, needed the presence of liquid water under low temperature conditions (below 320 K) to chemically alter the minerals.
    [Show full text]
  • Asteroid Observations at Low Phase Angles. IV. Average Parameters for the New H, G1, G2 Magnitude System Vasilij G
    Planetary and Space Science ∎ (∎∎∎∎) ∎∎∎–∎∎∎ Contents lists available at ScienceDirect Planetary and Space Science journal homepage: www.elsevier.com/locate/pss Asteroid observations at low phase angles. IV. Average parameters for the new H, G1, G2 magnitude system Vasilij G. Shevchenko a,b,n, Irina N. Belskaya a, Karri Muinonen c,d, Antti Penttilä c, Yurij N. Krugly a, Feodor P. Velichko a, Vasilij G. Chiorny a, Ivan G. Slyusarev a,b, Ninel M. Gaftonyuk e, Igor A. Tereschenko a a Institute of Astronomy of Kharkiv Karazin National University, Sumska str. 35, Kharkiv 61022, Ukraine b Department of Astronomy and Space Informatics of Kharkiv Karazin National University, Svobody sqr. 4, Kharkiv 61022, Ukraine c Department of Physics, University of Helsinki, P.O. Box 64, FI-00014, Finland d Finnish Geospatial Research Institute, P.O. Box 15, Masala, FI-02431, Finland e Crimean Astrophysical Observatory, Crimea, Simeiz 98680, Ukraine article info abstract Article history: We present new observational data for selected main-belt asteroids of different compositional types. The Received 21 January 2015 detailed magnitude–phase dependences including small phase angles (o1°) were obtained for these Received in revised form asteroids, namely: (10) Hygiea (down to the phase angle of 0.3°, C-type), (176) Iduna (0.2°, G-type), (214) 6 September 2015 Aschera (0.2°, E-type), (218) Bianca (0.3°, S-type), (250) Bettina (0.3°, M-type), (419) Aurelia (0.1°, F-type), Accepted 19 November 2015 (596) Scheila (0.2°, D-type), (635) Vundtia (0.2°, B-type), (671) Carnegia (0.2°, P-type), (717) Wisibada (0.1°, T-type), (1021) Flammario (0.6°, B-type), and (1279) Uganda (0.5°, E-type).
    [Show full text]
  • Occultations and 3D Shape Reconstruction
    Asteroidal Occultations High precision astronomy for all Dave Herald A little history • Efforts to observed started in the 1980’s • Predictions initially very poor • Improvements as a result of: – Hipparcos – UCAC2, then UCAC4 – Gaia, then Gaia DR2 => Steady increase in successfully observed occultations, from 39 in 2000 to 502 in 2018 The objective • To accurately measure the size and shape of asteroids • Potentially discover satellites or rings around asteroids The problem • An occultation gives an accurate profile of an asteroid for its orientation at the time of an event • Asteroids are irregular to greater or lesser extents => an accurate asteroid diameter can’t be determined from one or two occultations – only an approximate diameter Asteroid Shape Models • A group of astronomers (largely ‘unpaid’ astronomers) measure the light curves of asteroids in different parts of their orbit • These light curves can be ‘inverted’ to derive the shape of the asteroid (30) Urania Light curve measurements (Blue dots ) and light curve from a model ( Red line ) Shape model ‘issues’ • A shape model has no size – just shape • The inversion process usually results in two different orientations of the axis of rotation – with differing shapes. Inversion process cannot determine which one is correct • The inversion process is complex. Early models were limited to convex surfaces. Over the last few years models with concave surfaces have been developed • Inversion assumes uniform surface reflectivity The two shape models for (30) Urania, with different rotational axes Two shape models for (130) Electra one convex, and one concave, model Fitting occultations to shape models • The next three slides show fits of the occultation of (90) Metis on 2008 Sept 12 to three shape models available for Metis, and the conclusions to be drawn.
    [Show full text]