Stellar Occultation Observations with MAGIC

Total Page:16

File Type:pdf, Size:1020Kb

Stellar Occultation Observations with MAGIC Croatian group MAGIC & CTA meeting Status report: Stellar occultation observations September 25, 2019 University of Zagreb - FER with MAGIC Stefan Cikota, mag. phys. University of Zagreb, Faculty of Electrical Engineering and Computing - FER • A stellar occultation occurs when the light from a star is blocked by an intervening body (such as an asteroid) Stellar from reaching an observer. Occultations • Short duration event - takes normally between a few seconds, up to ~100 seconds for distant and large objects • Used to determine physical characteristics of Small Solar System objects • Beloved for amateur astronomers S. Cikota: Stellar occultation observations by MAGIC 2 / 18 DETERMINING PHYSICAL CHARACTERISTICS Small OF SMALL SOLAR SYSTEM OBJECTS Solar • Direct observations System - large telescopes & spacecraft missions Objects • Indirect observations - Astrometry & Photometry - Occultations • Occultations allow us to estimate the objects’ size, shape, atmosphere, other features • Resolutions of a few kilometers: several orders of magnitude better than the resolution of any other Earth-based method. S. Cikota: Stellar occultation observations by MAGIC 3 / 18 Determination of precise diameter of dwarf planet Eris Ortiz Scientific et ERIS ± . • R = 1163 6 km al Importance: IAA,2010 ., TNOs • RPLUTO = 1153 ± 10 km • Almost same diameter • Mass of Eris is 27% larger than Mass of Pluton. • AlbedoPLUTON = ~0.58 AlbedoERIS = ~0.96 S. Cikota: Stellar occultation observations by MAGIC 4 / 18 Recently used to probe ring systems and atmospheres outer solar system 4 very high impact publications published in the Journal Nature: • Sicardy et al. (2011): A Pluto-like radius and a high albedo for the dwarf planet Eris Scientific from an occultation • Ortiz, J.L. et al. (2012): Albedo and atmospheric constraints of dwarf planet Importance: Makemake from a stellar occultation • Braga-Ribas, F. et al. (2014): A ring system detected around the Centaur (10199) TNOs Chariklo • Ortiz, J.L. et al. (2017): The size, shape, density and ring of the dwarf planet Haumea from a stellar occultation Braga - Ribas , F. et (201 et al. F. , 4) S. Cikota: Stellar occultation observations by MAGIC 5 / 18 Eris • Stellar occultations by TNOs are extremely rare events from which plenty of scientific information can be gathered Occultation • They are very difficult to predict predictions and observe because the ephemeris of all the TNOs are far more uncertain than their angular diameters. • Angular size of Eris: like a tennis ball on a distance of 411 km • Seen from the Earth, the stars are always point-like sources S. Cikota: Stellar occultation observations by MAGIC 6 / 18 Optical telescopes vs. MAGIC Why Optical telescopes with CCD cameras MAGIC? Sampling rate: 1-10 Hz sampling frequency Best case resolution on TNO occultations: ~ 5 - 10 km Telescope mirror diameters: 0.4 – 10.4 m MAGIC II Central Pixel MAGIC is sensitive to millisecond-duration optical pulses (periodic signals from the Crab pulsar are regularly monitored) Sampling rate: 10000 Hz Best case resolution on TNO resolution: 0.5 - 1 m MAGIC mirror diameter: 17 m S. Cikota: Stellar occultation observations by MAGIC 7 / 18 MAGIC is capable of detecting the Crab pulsation in very short observation time (Hassan, T. et al., 2017, Proceedings of the 35th Central pixel International Cosmic Ray Conference: MAGIC sensitivity to millisecond-duration optical pulses) performance SAMPLING PERIOD: 0.000100 SEC VOLTAGE RANGE: 2000 MILLIVOLTS Hassan , T. et al. et , 2017 Left: Crab light-curve after 5 minutes Upper: Raw Central Pixel data of Crab of observation with the MAGIC II CPix pulsar – individual pulses detectable S. Cikota: Stellar occultation observations by MAGIC 8 / 18 Hassan, T. et al., 2017: Sensitivity test to isolated optical pulses Central pixel • experimental determination of the sensitivity of the central pixel to isolated 1-10 ms long optical pulses performance • Central pixel’s data was collected during MAGIC’s slewing • optical pulses of ∼20 ms were produced by the stars of known brightness and length passing through the central pixels’ FOV (∼0.1 deg) were used to determine the correlation between the maximum voltage of a pulse with the known magnitude of the stars S. Cikota: Stellar occultation observations by MAGIC 9 / 18 Direct measurement of voltage vs. magnitude dependence • The central pixel’s sensitivity to isolated optical pulses is Central pixel determined by extrapolating the fitted curve to the voltage performance corresponding to a 5-σ excess over the background noise level Hassan , T. • The limiting al. et , magnitude 2017 to detect a 1 ms optical flash is m = 13.5 ± 0.6 S. Cikota: Stellar occultation observations by MAGIC 10 / 18 • Hardware limitations: CPix is designed to detect very fast brightness changes (RC-circuit, normalizing the signal within ~3 ms) Expectation • We know we can detect such fast pulses down to magnitude B~14, on observation so an equivalent drop of ~14 m would be detectable. Occultation LC A drop in flux lasting for ~1 ms will turn into a Cpix signal spike of ~3 ms width and the same amplitude S. Cikota: Stellar occultation observations by MAGIC 11 / 18 Central pixel sensitivity test for Stellar Occultation observations • General goal: use the central pixel detector for specific occultations, Our goals like those of TNOs with rings • Because such occultation events are very rare (in average less than once per year for a specific location): find an appropriate Main Belt Asteroid occultation candidate to test the method • For the sensitivity test, we propose to follow up some well known, high-probability occultation events • The required observation time is generally very short • Predictions usually come with a relatively short notice, therefore observations should be scheduled as targets of opportunity (or similar) • Interesting side-results: stelar radii S. Cikota: Stellar occultation observations by MAGIC 12 / 18 (50) Virginia (746) Marlu (13) Egeria 21 Dec 2017 , 04:22 UT 10 Apr 2018 , 03:40 UT 12 May 2018, 22:21 UT Combined brightness: Target star: 11.2 mag. Combined brightness: 11.2 mag. Brightness drop: 3.3 mag. 9.6 mag. Missed Brightness drop: 0.6 mag. Brightness drop: 0.7 m Additional astrometry from opportunities Scheduled, but no San Pedro de Atacama DDT, scheduled, later observations due to strong confirmed shadow removed from schedule due wind to misunderstanding No observations due to humidity, wind and later ice S. Cikota: Stellar occultation observations by MAGIC 13 / 18 • Less discussions, more action: VERITAS is more effective than MAGIC in immplementing new ideas Nature Astronomy S. Cikota: Stellar occultation observations by MAGIC 14 / 18 Nature Astronomy „The authors want to acknowledge discussions with S. Cikota and J. Cortina.” S. Cikota: Stellar occultation observations by MAGIC 15 / 18 • Proposal approved (PI) for Cycle 14: Central pixel observations of stellar occultations by asteroids Cycle 14 • 10 x 10 minutes of telescope time approved • Focusing tests performed during observation shift P199 S. Cikota: Stellar occultation observations by MAGIC 16 / 18 One promising candidate until now: Asteroid: (751) Faina (mag 12.9) Target star: UCAC4-465-51138 Cycle 14 (mag 10.1) Date: 27 April 2019 , 00:57 UT -> fluid leakage in the MAGIC II server racks S. Cikota: Stellar occultation observations by MAGIC 16 / 18 • MAGIC is a world-class optical telescope to detect brief optical signals in millisecond scale • Star occultations are a field in which MAGIC, because of his Conclusions large aperture and high sensitivity, might have a significant scientific impact • There is no Project Working Groups for non-high energy physics projects like this, although it deserves special attention Future plan: • Keep searching for appropriate MBA candidates to test the method, and looking for good TNO candidates S. Cikota: Stellar occultation observations by MAGIC 17 / 18 Croatian group MAGIC & CTA meeting Thank you for your attention! September 25, 2019 University of Zagreb - FER Questions? Contact: Stefan Cikota, [email protected].
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 Impact Crater at the Origin of the Julia Family Detected with VLT/SPHERE??,?? P
    A&A 618, A154 (2018) Astronomy https://doi.org/10.1051/0004-6361/201833477 & © ESO 2018 Astrophysics The impact crater at the origin of the Julia family detected with VLT/SPHERE??,?? P. Vernazza1, M. Brož2, A. Drouard1, J. Hanuš2, M. Viikinkoski3, M. Marsset4, L. Jorda1, R. Fetick1, B. Carry5, F. Marchis6, M. Birlan7, T. Fusco1, T. Santana-Ros8, E. Podlewska-Gaca8,9, E. Jehin10, M. Ferrais10, P. Bartczak8, G. Dudzinski´ 8, J. Berthier7, J. Castillo-Rogez11, F. Cipriani12, F. Colas7, C. Dumas13, J. Durechˇ 2, M. Kaasalainen3, A. Kryszczynska8, P. Lamy1, H. Le Coroller1, A. Marciniak8, T. Michalowski8, P. Michel5, M. Pajuelo7,14, P. Tanga5, F. Vachier7, A. Vigan1, B. Warner15, O. Witasse12, B. Yang16, E. Asphaug17, D. C. Richardson18, P. Ševecekˇ 2, M. Gillon10, and Z. Benkhaldoun19 1 Aix-Marseille Université, CNRS, LAM (Laboratoire d’Astrophysique de Marseille), Marseille, France e-mail: [email protected] 2 Institute of Astronomy, Charles University, Prague, V Holešovickᡠch 2, 18000, Prague 8, Czech Republic 3 Department of Mathematics, Tampere University of Technology, PO Box 553, 33101 Tampere, Finland 4 Astrophysics Research Centre, Queen’s University Belfast, BT7 1NN, UK 5 Université Côte d’Azur, Observatoire de la Côte d’Azur, CNRS, Laboratoire Lagrange, 06304 Nice Cedex 4, France 6 SETI Institute, Carl Sagan Center, 189 Bernado Avenue, Mountain View CA 94043, USA 7 IMCCE, Observatoire de Paris, 77 avenue Denfert-Rochereau, 75014 Paris Cedex, France 8 Astronomical Observatory Institute, Faculty of Physics, Adam Mickiewicz University,
    [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]
  • 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]
  • 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]
  • Hydrated Minerals on Asteroids: the Astronomical Record
    Hydrated Minerals on Asteroids: The Astronomical Record A. S. Rivkin, E. S. Howell, F. Vilas, and L. A. Lebofsky March 28, 2002 Corresponding Author: Andrew Rivkin MIT 54-418 77 Massachusetts Ave. Cambridge MA, 02139 [email protected] 1 1 Abstract Knowledge of the hydrated mineral inventory on the asteroids is important for deducing the origin of Earth’s water, interpreting the meteorite record, and unraveling the processes occurring during the earliest times in solar system history. Reflectance spectroscopy shows absorption features in both the 0.6-0.8 and 2.5-3.5 pm regions, which are diagnostic of or associated with hydrated minerals. Observations in those regions show that hydrated minerals are common in the mid-asteroid belt, and can be found in unex- pected spectral groupings, as well. Asteroid groups formerly associated with mineralogies assumed to have high temperature formation, such as MAand E-class asteroids, have been observed to have hydration features in their reflectance spectra. Some asteroids have apparently been heated to several hundred degrees Celsius, enough to destroy some fraction of their phyllosili- cates. Others have rotational variation suggesting that heating was uneven. We summarize this work, and present the astronomical evidence for water- and hydroxyl-bearing minerals on asteroids. 2 Introduction Extraterrestrial water and water-bearing minerals are of great importance both for understanding the formation and evolution of the solar system and for supporting future human activities in space. The presence of water is thought to be one of the necessary conditions for the formation of life as 2 we know it.
    [Show full text]
  • The Minor Planet Bulletin, Alan W
    THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 42, NUMBER 2, A.D. 2015 APRIL-JUNE 89. ASTEROID LIGHTCURVE ANALYSIS AT THE OAKLEY SOUTHERN SKY OBSERVATORY: 2014 SEPTEMBER Lucas Bohn, Brianna Hibbler, Gregory Stein, Richard Ditteon Rose-Hulman Institute of Technology, CM 171 5500 Wabash Avenue, Terre Haute, IN 47803, USA [email protected] (Received: 24 November) Photometric data were collected over the course of seven nights in 2014 September for eight asteroids: 1334 Lundmarka, 1904 Massevitch, 2571 Geisei, 2699 Kalinin, 3197 Weissman, 7837 Mutsumi, 14927 Satoshi, and (29769) 1999 CE28. Eight asteroids were remotely observed from the Oakley Southern Sky Observatory in New South Wales, Australia. The observations were made on 2014 September 12-14, 16-19 using a 0.50-m f/8.3 Ritchey-Chretien optical tube assembly on a Paramount ME mount and SBIG STX-16803 CCD camera, binned 3x3, with a luminance filter. Exposure times ranged from 90 to 180 sec depending on the magnitude of the target. The resulting image scale was 1.34 arcseconds per pixel. Raw images were processed in MaxIm DL 6 using twilight flats, bias, and dark frames. MPO Canopus was used to measure the processed images and produce lightcurves. In order to maximize the potential for data collection, target asteroids were selected based upon their position in the sky approximately one hour after sunset. Only asteroids with no previously published results were targeted. Lightcurves were produced for 1334 Lundmarka, 1904 Massevitch, 2571 Geisei, 3197 Weissman, and (29769) 1999 CE28.
    [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 38, NUMBER 2, A.D. 2011 APRIL-JUNE 71. LIGHTCURVES OF 10452 ZUEV, (14657) 1998 YU27, AND (15700) 1987 QD Gary A. Vander Haagen Stonegate Observatory, 825 Stonegate Road Ann Arbor, MI 48103 [email protected] (Received: 28 October) Lightcurve observations and analysis revealed the following periods and amplitudes for three asteroids: 10452 Zuev, 9.724 ± 0.002 h, 0.38 ± 0.03 mag; (14657) 1998 YU27, 15.43 ± 0.03 h, 0.21 ± 0.05 mag; and (15700) 1987 QD, 9.71 ± 0.02 h, 0.16 ± 0.05 mag. Photometric data of three asteroids were collected using a 0.43- meter PlaneWave f/6.8 corrected Dall-Kirkham astrograph, a SBIG ST-10XME camera, and V-filter at Stonegate Observatory. The camera was binned 2x2 with a resulting image scale of 0.95 arc- seconds per pixel. Image exposures were 120 seconds at –15C. Candidates for analysis were selected using the MPO2011 Asteroid Viewing Guide and all photometric data were obtained and analyzed using MPO Canopus (Bdw Publishing, 2010). Published asteroid lightcurve data were reviewed in the Asteroid Lightcurve Database (LCDB; Warner et al., 2009). The magnitudes in the plots (Y-axis) are not sky (catalog) values but differentials from the average sky magnitude of the set of comparisons. The value in the Y-axis label, “alpha”, is the solar phase angle at the time of the first set of observations. All data were corrected to this phase angle using G = 0.15, unless otherwise stated.
    [Show full text]
  • The Team Adarsh Rajguru
    Asteroid Mapper / Hopper www.inl.gov Mapping and extraction of water from asteroids 1 in the main asteroid belt The team Adarsh Rajguru – University of Southern California (Systems Engineer) Juha Nieminen – University of Southern California (Astronautical Engineer) Nalini Nadupalli – University of Michigan (Electrical & Telecommunications Engineer) Justin Weatherford – George Fox University (Mechanical & Thermal Engineer) Joseph Santora – University of Utah (Chemical & Nuclear Engineer) 2 Mission Objectives Primary Objective – Map and tag the asteroids in the main asteroid belt for water. Secondary Objective – Potentially land on these water-containing asteroids, extract the water and use it as a propellant. Tertiary Objective – Map the asteroids for other important materials that can be valuable for resource utilization. 3 Introduction: Asteroid Commodities and Markets Water – Propellant and life support for future manned deep-space missions (Mapping market) Platinum group metals – Valuable on Earth and hence for future unmanned or manned deep-space mining missions (Mapping market) Regolith – Radiation shielding, 3D printing of structures (fuel tanks, trusses, etc.) for deep-space unmanned or manned spacecrafts, (Determining Regolith composition and material properties market) Aluminum, Iron, Nickel, Silicon and Titanium – Valuable structural materials for deep-space unmanned and manned colonies (Mapping market) 4 Asteroid Hopping: Main Asteroid Belt Class and Types (most interested) Resource Water Platinum Group Metals Metals Asteroid Class Type Hydrated C-Class M-Class M-Class Population (%) 10 5 5 Density (kg/m3) 1300 5300 5300 Resource Mass Fraction 8 % 35 ppm 88 % Asteroid Diameter (10 m) 44 tons 2 x 103 tons 97 kg Asteroid Diameter (100 m) 4350 tons 2 x 106 tons 97 tons Asteroid Diameter (500 m) 11000 tons 3 x 108 tons 12 x 103 tons [1] Badescu V., Asteroids: Prospective Energy and Material Resources, First edition, 2013.
    [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]
  • A Study of Asteroid Pole-Latitude Distribution Based on an Extended
    Astronomy & Astrophysics manuscript no. aa˙2009 c ESO 2018 August 22, 2018 A study of asteroid pole-latitude distribution based on an extended set of shape models derived by the lightcurve inversion method 1 1 1 2 3 4 5 6 7 J. Hanuˇs ∗, J. Durechˇ , M. Broˇz , B. D. Warner , F. Pilcher , R. Stephens , J. Oey , L. Bernasconi , S. Casulli , R. Behrend8, D. Polishook9, T. Henych10, M. Lehk´y11, F. Yoshida12, and T. Ito12 1 Astronomical Institute, Faculty of Mathematics and Physics, Charles University in Prague, V Holeˇsoviˇck´ach 2, 18000 Prague, Czech Republic ∗e-mail: [email protected] 2 Palmer Divide Observatory, 17995 Bakers Farm Rd., Colorado Springs, CO 80908, USA 3 4438 Organ Mesa Loop, Las Cruces, NM 88011, USA 4 Goat Mountain Astronomical Research Station, 11355 Mount Johnson Court, Rancho Cucamonga, CA 91737, USA 5 Kingsgrove, NSW, Australia 6 Observatoire des Engarouines, 84570 Mallemort-du-Comtat, France 7 Via M. Rosa, 1, 00012 Colleverde di Guidonia, Rome, Italy 8 Geneva Observatory, CH-1290 Sauverny, Switzerland 9 Benoziyo Center for Astrophysics, The Weizmann Institute of Science, Rehovot 76100, Israel 10 Astronomical Institute, Academy of Sciences of the Czech Republic, Friova 1, CZ-25165 Ondejov, Czech Republic 11 Severni 765, CZ-50003 Hradec Kralove, Czech republic 12 National Astronomical Observatory, Osawa 2-21-1, Mitaka, Tokyo 181-8588, Japan Received 17-02-2011 / Accepted 13-04-2011 ABSTRACT Context. In the past decade, more than one hundred asteroid models were derived using the lightcurve inversion method. Measured by the number of derived models, lightcurve inversion has become the leading method for asteroid shape determination.
    [Show full text]
  • (2000) Forging Asteroid-Meteorite Relationships Through Reflectance
    Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. B.S. Physics Rensselaer Polytechnic Institute, 1988 M.S. Geology and Planetary Science University of Pittsburgh, 1991 SUBMITTED TO THE DEPARTMENT OF EARTH, ATMOSPHERIC, AND PLANETARY SCIENCES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN PLANETARY SCIENCES AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY FEBRUARY 2000 © 2000 Massachusetts Institute of Technology. All rights reserved. Signature of Author: Department of Earth, Atmospheric, and Planetary Sciences December 30, 1999 Certified by: Richard P. Binzel Professor of Earth, Atmospheric, and Planetary Sciences Thesis Supervisor Accepted by: Ronald G. Prinn MASSACHUSES INSTMUTE Professor of Earth, Atmospheric, and Planetary Sciences Department Head JA N 0 1 2000 ARCHIVES LIBRARIES I 3 Forging Asteroid-Meteorite Relationships through Reflectance Spectroscopy by Thomas H. Burbine Jr. Submitted to the Department of Earth, Atmospheric, and Planetary Sciences on December 30, 1999 in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Planetary Sciences ABSTRACT Near-infrared spectra (-0.90 to ~1.65 microns) were obtained for 196 main-belt and near-Earth asteroids to determine plausible meteorite parent bodies. These spectra, when coupled with previously obtained visible data, allow for a better determination of asteroid mineralogies. Over half of the observed objects have estimated diameters less than 20 k-m. Many important results were obtained concerning the compositional structure of the asteroid belt. A number of small objects near asteroid 4 Vesta were found to have near-infrared spectra similar to the eucrite and howardite meteorites, which are believed to be derived from Vesta.
    [Show full text]