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Mathilde (minor planet designation: 253 Mathilde) is an asteroid in the intermediate asteroid belt, approximately 50 kilometers in diameter, that was discovered by Austrian astronomer Johann Palisa at Vienna Observatory on 12 November 1885. It has a relatively elliptical orbit that requires more than four years to circle the Sun. This tumbling asteroid has an unusually slow rate of rotation, requiring 17.4 days to complete a 360° revolution about its axis. It is a primitive C-type asteroid, which means the surface has a high proportion of carbon; giving it a dark surface that reflects only 4% of the light that falls on it.[8]

253 Mathilde
253 Mathilde as seen by NEAR in 1997
Discovery[1]
Discovered byJ. Palisa
Discovery siteVienna Obs.
Discovery date12 November 1885
Designations
MPC designation
(253) Mathilde
Pronunciation/məˈtɪldə/
Named after
Mathilde Loewy
Alternative designations
A885 VA, 1915 TN
1949 OL1
Minor planet category
Main belt
Orbital characteristics[2]
Epoch 31 July 2016 (JD 2457600.5)
Uncertainty parameter 0
Observation arc130.38 yr (47622 d)
Aphelion3.35003411 AU (501.157970 Gm)
Perihelion1.9467702 AU (291.23268 Gm)
Semi-major axis
2.648402147 AU (396.1953219 Gm)
Eccentricity0.26492652
Orbital period (sidereal)
4.31 yr (1574.3 d)
Average orbital speed
17.98 km/s[3]
Mean anomaly
170.584348°
Mean motion
0° 13m 43.248s / day
Inclination6.7427122°
Longitude of ascending node
179.58936°
Argument of perihelion
157.39642°
Earth MOID0.939032 AU (140.4772 Gm)
Jupiter MOID2.06073 AU (308.281 Gm)
TJupiter3.331
Physical characteristics
Dimensions52.8 km[2]
(66×48×46 km[4])
Mass(1.033±0.044)×1017 kg[5]
Mean density
1.3 g/cm3[5]
Equatorial surface gravity
0.00989 m/s2
Equatorial escape velocity
22.9 m/s
Synodic rotation period
417.7 h (17.40 d)[2]
17.406 ± 0.010 d[6]
(17 d 9 h 45 min)
Geometric albedo
0.0436±0.004[2]
Temperature≈ 174[7] K
Spectral type
Cb[2]
Absolute magnitude (H)
10.3[2]

    Mathilde was visited by the NEAR Shoemaker spacecraft during June 1997, on its way to asteroid 433 Eros. During the flyby, the spacecraft imaged a hemisphere of the asteroid, revealing many large craters that had gouged out depressions in the surface. It was the first carbonaceous asteroid to be explored and, until 21 Lutetia was visited in 2010, was the largest asteroid to be visited by a spacecraft.


    Observation history


    Animation of NEAR Shoemaker trajectory from February 19, 1996 to February 12, 2001..mw-parser-output .legend{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .legend-color{display:inline-block;min-width:1.25em;height:1.25em;line-height:1.25;margin:1px 0;text-align:center;border:1px solid black;background-color:transparent;color:black}.mw-parser-output .legend-text{}  NEAR Shoemaker;    433 Eros;   Earth;   253 Mathilde ;   Sun;
    Animation of NEAR Shoemaker trajectory from February 19, 1996 to February 12, 2001.
      NEAR Shoemaker;    433 Eros;   Earth;   253 Mathilde ;   Sun;

    In 1880, Johann Palisa, the director of the Austrian Naval Observatory (538), was offered a position as an assistant at the newly completed Vienna Observatory. Although the job represented a demotion for Johann, it gave him access to the new 27-inch (690 mm) refractor, the largest telescope in the world at that time. By this point Johann had already discovered 27 asteroids, and he would employ the Vienna 27-inch (690 mm) and 12-inch (300 mm) instruments to find an additional 94 asteroids before he retired.[9]

    Among his discoveries was the asteroid 253 Mathilde, found on November 12, 1885. The initial orbital elements of the asteroid were then computed by V. A. Lebeuf, another Austrian astronomer working at the Paris Observatory.[10] The name of the asteroid was suggested by Lebeuf, after Mathilde, the wife of Moritz Loewywho was the vice director of the observatory in Paris.[1][10]

    In 1995, ground-based observations determined that Mathilde is a C-type asteroid. It was also found to have an unusually long period of rotation of 418 hours.[10]

    On June 27, 1997, the NEAR Shoemaker spacecraft passed within 1,212 km of Mathilde while moving at a velocity of 9.93 km/s. This close approach allowed the spacecraft to capture over 500 images of the surface,[8] and provided data for more accurate determinations of the asteroid's dimensions and mass (based on gravitational perturbation of the spacecraft).[5] However, only one hemisphere of Mathilde was imaged during the fly-by.[11] This was only the third asteroid to be imaged from a nearby distance, following 951 Gaspra and 243 Ida.


    Characteristics


    Damodar, a 20 km-wide crater on Mathilde
    Damodar, a 20 km-wide crater on Mathilde
    Image sequence of Mathilde during NEAR Shoemaker's flyby
    Image sequence of Mathilde during NEAR Shoemaker's flyby

    Mathilde is very dark, with an albedo comparable to fresh asphalt,[12] and is thought to share the same composition as CI1 or CM2 carbonaceous chondrite meteorites, with a surface dominated by phyllosilicate minerals.[13] The asteroid has a number of extremely large craters, with the individual craters being named for coal fields and basins around the world.[14] The two largest craters, Ishikari (29.3 km) and Karoo (33.4 km), are as wide as the asteroid's average radius.[4] The impacts appear to have spalled large volumes off the asteroid, as suggested by the angular edges of the craters.[8] No differences in brightness or colour were visible in the craters and there was no appearance of layering, so the asteroid's interior must be very homogeneous. There are indications of material movement along the downslope direction.[4]

    The density measured by NEAR Shoemaker, 1,300 kg/m3, is less than half that of a typical carbonaceous chondrite; this may indicate that the asteroid is very loosely packed rubble pile.[5] The same is true of several C-type asteroids studied by ground-based telescopes equipped with adaptive optics systems (45 Eugenia, 90 Antiope, 87 Sylvia and 121 Hermione). Up to 50% of the interior volume of Mathilde consists of open space. However, the existence of a 20-km-long scarp may indicate that the asteroid does have some structural strength, so it could contain some large internal components.[11] The low interior density is an inefficient transmitter of impact shock through the asteroid, which also helps to preserve the surface features to a high degree.[4]

    Mathilde's orbit is eccentric, taking it to the outer reaches of the main belt. Nonetheless, the orbit lies entirely between the orbits of Mars and Jupiter; it does not cross the planetary orbits. It also has one of the slowest rotation periods of the known asteroidsmost asteroids have a rotation period in the range of 224 hours.[15] Because of the slow rotation rate, NEAR Shoemaker was only able to photograph 60% of the asteroid's surface. The slow rate of rotation may be accounted for by a satellite orbiting the asteroid, but a search of the NEAR images revealed none larger than 10 km in diameter out to 20 times the radius of Mathilde.[16]


    See also



    References


    1. Moore, Sir Patrick (1999). The Wandering Astronomer. CRC Press. ISBN 0-7503-0693-9.
    2. Unless otherwise noted, parameters are per: Yeomans, Donald K. (29 August 2003). "253 Mathilde". JPL Small-Body Database Browser. NASA. Retrieved 12 May 2016.
    3. For semi-major axis a, orbital period T and eccentricity e, the average orbital speed is given by:
      For the circumference of an ellipse, see: H. St̀eocker; J. Harris (1998). Handbook of Mathematics and Computational Science. Springer. pp. 386. ISBN 0-387-94746-9.
    4. J. Veverka; et al. (1999). "NEAR Encounter with Asteroid 253 Mathilde: Overview". Icarus. 140 (1): 3–16. Bibcode:1999Icar..140....3V. doi:10.1006/icar.1999.6120.
    5. D. K. Yeomans; et al. (1997). "Estimating the mass of asteroid 253 Mathilde from tracking data during the NEAR flyby". Science. 278 (5346): 2106–9. Bibcode:1997Sci...278.2106Y. doi:10.1126/science.278.5346.2106. PMID 9405343.
    6. Stefano Mottola; et al. (1995). "The slow rotation of 253 Mathilde". Planetary and Space Science. 43 (12): 1609–1613. Bibcode:1995P&SS...43.1609M. doi:10.1016/0032-0633(95)00127-1.
    7. For asteroid albedo α, semimajor axis a, solar luminosity , Stefan–Boltzmann constant σ and the asteroid's infrared emissivity ε (≈ 0.9), the approximate mean temperature T is given by:
      See: Torrence V. Johnson; Paul R. Weissman; Lucy-Ann A. McFadden (2007). Encyclopedia of the Solar System. Elsevier. pp. 294. ISBN 978-0-12-088589-3.
    8. Williams, David R. (18 December 2001). "NEAR Flyby of Asteroid 253 Mathilde". NASA. Archived from the original on 18 August 2006. Retrieved 10 August 2006.
    9. Raab, Herbert (2002). "Johann Palisa, the most successful visual discoverer of" (PDF). Astronomical Society of Linz. Archived from the original (PDF) on 28 September 2007. Retrieved 27 August 2007.
    10. Savage, D.; Young, L.; Diller, G.; Toulouse, A. (February 1996). "Near Earth Asteroid Rendezvous (NEAR) Press Kit". NASA. Retrieved 29 August 2007.
    11. Cheng, Andrew F. (2004). "Implications of the NEAR mission for internal structure of Mathilde and Eros". Advances in Space Research. 33 (9): 1558–1563. Bibcode:2004AdSpR..33.1558C. doi:10.1016/S0273-1177(03)00452-6.
    12. Pon, Brian (30 June 1999). "Pavement Albedo". Heat Island Group. Archived from the original on 29 August 2007. Retrieved 27 August 2007.
    13. Kelley, M. S.; Gaffey, M. J.; Reddy, V. (12–16 March 2007). "Near-IR Spectroscopy and Possible Meteorite Analogs for Asteroid (253)". 38th Lunar and Planetary Science Conference. League City, Texas: Lunar & Planetary Institute. p. 2366. Bibcode:2007LPI....38.2366K.
    14. Blue, Jennifer (29 August 2007). "Categories for Naming Features on Planets and Satellites". USGS. Archived from the original on 24 August 2007. Retrieved 29 August 2007.
    15. Lang, Kenneth R. (2003). "2. Asteroids and meteorites, Size, color and spin". NASA's Cosmos. NASA. Archived from the original on 6 August 2012. Retrieved 29 August 2007.
    16. W. J. Merline; et al. (1998). "Search for Satellites of 253 Mathilde from Near-Earth Asteroid Rendezvous Flyby Data". Meteoritics & Planetary Science. 33 (S4): A105. Bibcode:1998M&PSA..33..105M. doi:10.1111/j.1945-5100.1998.tb01327.x.



    На других языках


    [de] (253) Mathilde

    (253) Mathilde ist ein Asteroid des Asteroidenhauptgürtels mit einem mittleren Durchmesser von etwa 53 km. Im Juni 1997 flog die Raumsonde NEAR-Shoemaker in 2.400 km Entfernung an Mathilde vorbei und sandte fotografische Aufnahmen zur Erde.
    - [en] 253 Mathilde

    [es] (253) Mathilde

    (253) Mathilde es un asteroide, situado en el cinturón de asteroides, que fue descubierto por Johann Palisa en 1885. Mathilde tiene una órbita relativamente elíptica, que requiere más de cuatro años para rodear el Sol. Este asteroide realiza una rotación relativamente muy lenta, ya que precisa de 17,4 días para girar sobre su eje. Es un asteroide de tipo C, lo que quiere decir que su superficie contiene una alta proporción de carbono, lo que le convierte en una superficie oscura que refleja solo el 4 % de la luz que incide sobre ella.[5]

    [ru] (253) Матильда

    (253) Мати́льда (нем. Mathilde) — астероид главного пояса, который принадлежит к тёмному спектральному классу C. Астероиды этого класса богаты различными углеродными соединениями, которые сильно поглощают свет, давая очень низкое альбедо. Матильда — один из немногих астероидов с крайне медленным вращением вокруг своей оси: она делает один оборот за 17,4 суток. Она была открыта 27 июня 1884 года австрийским астрономом Иоганном Пализой в Венской обсерватории[9] и назван в честь жены французского астронома Мориса Леви, ставшего впоследствии вице-директором Парижской обсерватории. Название было предложено сотрудником Парижской обсерватории В. А. Лебёфом (фр. V. A. Lebeuf), который просчитал орбитальные параметры Матильды[10].



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