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Peter Jenniskens ( SETI Institute). The story of asteroid 2008 TC3. 07/14/09. Meteorites are great, but from which asteroid do they come?. Earth is in a shooting gallery, lots of asteroids passing close. http://www.cfa.harvard.edu/iau/Animations/EarthRide2008.gif.
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Peter Jenniskens (SETI Institute) The story of asteroid 2008 TC3 07/14/09
Earth is in a shooting gallery,lots of asteroids passing close... http://www.cfa.harvard.edu/iau/Animations/EarthRide2008.gif
2008 October 6, 6:39 UTDiscovery of a small asteroid, soon called 2008 TC3 Discovery Image Catalina Sky Survey (Richard Kowalski)
2008 October 6, 14:59 UTMinor Planet Center: It’s coming right at us! MPEC 2008-T50: “The nominal orbit given above has 2008 TC3 coming to within one earth radius around Oct. 7.1. The absolute magnitude indicates that the object will not survive passage through the atmosphere.” “ Steve Chesley (JPL) reports that atmospheric entry will occur on 2008 Oct 07 0246 UTC over northern Sudan.”
2008 October 6, about 18h UTUnusual: Meteor community (a.o. Dr. Jenniskens) is alerted.Small asteroid = Big meteoroid!
Over the course of 20 hours, the asteroid’s position relative to the stars is measured some 570 times... La Sagra Sky Survey - S. Sanchez et al., Mallorca
Orbit in space determined 10,000 times better than typical orbit derived from few seconds long bolide Orbital elements (Steven R. Chesley): • a = 1.308201 ±0.000009 AU • q = 0.899957 ±0.000002 AU • i = 2.54220 ±0.00004º • W = 194.101139 ±0.000002º • w = 234.44897 ±0.00008º J2000
Astronomical reflectance spectrum: color of the asteroid is grayA. Fitzsimmons and collaborators (La Palma / U.K.)
Asteroid flickering: tumbling and shapeR. Dantowitz and M. Kozubal, Clay Center Observatory, USA
Impact point in Nubian Desert of northern Sudan Meteosat 8 In Kenya: Distant rumble (Infrasound) P. Brown, UWO
End of the story…? 37-km explosion: Apparently, object will not survive passage through the atmosphere, no fragments survived. Never before have meteorites been recovered from such a high explosion. But was this really the end of the meteor?
October - early November 2008:Jenniskens established contact with Dr. Muawia Shaddad (University of Khartoum) to gather eye witness accounts. Shaddad forwards images of train taken by cell phone. M. Elhassan
2008 Dec. 4: Visit location of APOD train image Mohamed Elhassan, Wadi Halfa
Train drift due to winds Calculations by Jim Albers Wadi Halfa
Sinking feeling... • Fireball had abrupt ending: No big fragments emerged from the explosion below about 32 km • Search for small pieces…? • These should have fallen close to explosion (deep into desert) • If anything small survived, it would be spread over huge area because, at this high altitude, the asteroid had not significantly slowed down.
Back at “Station 6”: Busload of students from U. of Khartoum!
Next day: take bus along freshly created~30-km long ‘Asteroid Track’
Foot search required: gravel plain,hard to see small things far away...
Very end of day #1: They can be found!“Incredible” - M. H. Shaddad Mohammed Alameen
3rd day they finally got bigger as they should, but 29 km down track... #15
Peter Jenniskens, SETI Institute Muawia Shaddad, U. of Khartoum Mike Zolensky, JSC Doug Rumble, Carnegie Institute Jon Friedman, Univ. Fordham, NY Andrew Steele, Carnegie Institute Scott Sandford, NASA Ames Kees Welten, Berkeley Rainer Weiler, Switzerland Carla Taricco, Turin, Italy Noriko Kita, Univ. Wisconsin-Madison S.V.S. Murty, Navrangpura, India U. Ott, MPI fuer Chemie, Mainz Takahiro Hiroi, Brown Univ. …. Reflection spectroscopy Mass, type, density, XRF SEM, EPMA, petrography Oxygen isotopes Bulk chemistry Raman spectroscopy Mid-IR transmission spectroscopy Cosmic radio nucleides Nobel gasses Gamma-ray spectroscopy SEM, EPMA, SIMS Nobel gasses Nobel gasses Reflection spectroscopy …. Almahata Sitta Consortiumhttp://asima.seti.org/2008TC3/
#7 broken along white layer: tensile strength 56 ± 26 MPastrength of asteroid (explosion) ~ 0.2-0.3 MPa!
Meteorite spectrum = asteroid spectrum(no dust/sand on the surface)
Astronomical spectrum: F Average asteroid spectra by Takahiro Hiroi
Size: 3-4 meter object • From brightness asteroid + albedo > size: • Kinetic energy = 6.4 x 10^12 J (Albedo = 0.046: 4.1m, assume density 2.3 g/cm3) • From acoustic signal: • Kinetic energy = 6.7 ± 2.1 x 10^12 J • Bolide light curve (Meteosat 8): • Kinetic energy ~ 4 x 10^12 J
Find out what type of meteorite this is from oxygen isotopes 17 16 O/ O 18 16 O/ O
anomalous polymict Ureilite (an achondrite)!(Data: Doug Rumble, Carnegie Institution of Washington) 17 16 O/ O 18 16 O/ O
Rare Earth Element abundances: residue of partial melt (Data: Jon Friedman, Fordham University, NY) < chondrite < everything molten and sunk
Ureilites: a brief history in the origin of differentiated planets like Earth -on the cusp of complete melting Chondrite Ureilites Basaltic achondrite Iron meteorite
Trail of crumbs: trace F-class asteroids back to their region of origin in the asteroid belt Elongation of orbit (eccentricity) Orbital period (semi-major axis)
The moral of the story... • As far as asteroids are concerned: smaller can be better (but not easier). • As far as meteorite falls are concerned: whole new game in town by following up on high explosions. • As far as meteorites are concerned: Ureilites may finally be understood. • As far as impact location (Sudan) is concerned: We couldn’t have been more lucky with this one! University of Khartoum staff and students: Well done!
P. Jenniskens et al., 2009. May 26 issue of Nature The impact and recovery of asteroid 2008 TC3