Stony background asteroid
1147 Stavropolis (prov. designation :1929 LF ) is a stonybackground asteroid from the inner regions of theasteroid belt . It was discovered on 11 June 1929, by Georgian–Russian astronomerGrigory Neujmin at theSimeiz Observatory on the Crimean peninsula.[ 1] TheS-type asteroid has arotation period of 5.7 hours and measures approximately 14 kilometers (9 miles) in diameter. It was named after the Russian city ofStavropol .[ 2]
Orbit and classification [ edit ] Stavropolis is a non-family asteroid of the main belt'sbackground population when applying thehierarchical clustering method to itsproper orbital elements .[ 4] [ 5] It orbits the Sun in theinner asteroid belt at a distance of 1.7–2.8 AU once every 3 years and 5 months (1,250 days). Its orbit has aneccentricity of 0.23 and aninclination of 4° with respect to theecliptic .[ 3] The body'sobservation arc begins at with its official discovery observation at Simeiz.[ 1]
Thisminor planet was named by the discover after the Russian city ofStavropol , located innorthern Caucasus region. From 1936 to 1946, the city was named "Woroschilowsk". Thenaming was mentioned inThe Names of the Minor Planets byPaul Herget in 1955 (H 107 ).[ 2]
Physical characteristics [ edit ] In the Bus–BinzelSMASS classification ,Stavropolis is a common stonyS-type asteroid ,[ 3] while in theBus–DeMeo classification , it is an Sw-subtype.[ 5]
Rotation period and poles [ edit ] In September 2001, a rotationallightcurve ofStavropolis was obtained fromphotometric observations by AmericansLarry Robinson andBrian Warner at the Sunflower (739 ) and Palmer Divide Observatory (716 ) in Kansas and Colorado, respectively. Lightcurve analysis gave arotation period of 5.66± 0.01 hours with a brightness variation of 0.42magnitude (U=3 ).[ 12]
In October 2015, another lightcurve was obtained by French amateur astronomerPierre Antonini . It gave a well-defined period of 5.66070 ± 0.00003 hours with an amplitude of 0.32 magnitude (U=3 ).[ 11] A 2016-published lightcurve, using modeled photometric data from the Lowell Photometric Database (LPD), gave a concurring period of 5.66079 ± 0.00001 hours, as well as twospin axes of (78.0°, −50.0°) and (267.0°, −51.0°) inecliptic coordinates (λ, β).[ 13]
Diameter and albedo [ edit ] According to the survey carried out by theNEOWISE mission of NASA'sWide-field Infrared Survey Explorer ,Stavropolis measures between 10.94 and 13.898 kilometers in diameter and its surface has analbedo between 0.146 and 0.406,[ 6] [ 7] [ 8] while the JapaneseAkari satellite found a diameter of 13.92 kilometers with an albedo of 0.145.[ 9] TheCollaborative Asteroid Lightcurve Link assumes a standard albedo for stony asteroids of 0.20 and calculates a diameter of 14.89 kilometers based on anabsolute magnitude of 11.5.[ 10]
^a b c d e "1147 Stavropolis (1929 LF)" .Minor Planet Center . Retrieved8 September 2017 .^a b c Schmadel, Lutz D. (2007). "(1147) Stavropolis".Dictionary of Minor Planet Names .Springer Berlin Heidelberg . p. 97 .doi :10.1007/978-3-540-29925-7_1148 .ISBN 978-3-540-00238-3 . ^a b c d e f "JPL Small-Body Database Browser: 1147 Stavropolis (1929 LF)" (2017-03-29 last obs.).Jet Propulsion Laboratory . Retrieved8 September 2017 .^a b "Asteroid 1147 Stavropolis – Proper Elements" . AstDyS-2, Asteroids – Dynamic Site. Retrieved14 March 2020 .^a b c d e f "Asteroid 1147 Stavropolis" .Small Bodies Data Ferret . Retrieved14 March 2020 .^a b c d Masiero, Joseph R.; Mainzer, A. K.; Grav, T.; Bauer, J. M.; Cutri, R. M.; Nugent, C.; et al. (November 2012)."Preliminary Analysis of WISE/NEOWISE 3-Band Cryogenic and Post-cryogenic Observations of Main Belt Asteroids" .The Astrophysical Journal Letters .759 (1): 5.arXiv :1209.5794 .Bibcode :2012ApJ...759L...8M .doi :10.1088/2041-8205/759/1/L8 . Retrieved8 September 2017 . ^a b c Masiero, Joseph R.; Grav, T.; Mainzer, A. K.; Nugent, C. R.; Bauer, J. M.; Stevenson, R.; et al. (August 2014)."Main-belt Asteroids with WISE/NEOWISE: Near-infrared Albedos" .The Astrophysical Journal .791 (2): 11.arXiv :1406.6645 .Bibcode :2014ApJ...791..121M .doi :10.1088/0004-637X/791/2/121 . Retrieved8 September 2017 . ^a b c d Mainzer, A.; Grav, T.; Masiero, J.; Hand, E.; Bauer, J.; Tholen, D.; et al. (November 2011). "NEOWISE Studies of Spectrophotometrically Classified Asteroids: Preliminary Results".The Astrophysical Journal .741 (2): 25.arXiv :1109.6407 .Bibcode :2011ApJ...741...90M .doi :10.1088/0004-637X/741/2/90 . ^a b c d Usui, Fumihiko; Kuroda, Daisuke; Müller, Thomas G.; Hasegawa, Sunao; Ishiguro, Masateru; Ootsubo, Takafumi; et al. (October 2011)."Asteroid Catalog Using Akari: AKARI/IRC Mid-Infrared Asteroid Survey" .Publications of the Astronomical Society of Japan .63 (5):1117– 1138.Bibcode :2011PASJ...63.1117U .doi :10.1093/pasj/63.5.1117 . (online ,AcuA catalog p. 153 )^a b c d "LCDB Data for (1147) Stavropolis" . Asteroid Lightcurve Database (LCDB). Retrieved8 September 2017 .^a b Behrend, Raoul."Asteroids and comets rotation curves – (1147) Stavropolis" .Geneva Observatory . Retrieved8 September 2017 . ^ Robinson, L. E.; Warner, B. D. (March 2002)."A Collaborative Work on Three Asteroid Lightcurves: 506 Marion, 585 Bilkis, 1506 Xosa" (PDF) .Minor Planet Bulletin .29 (1):6– 7.Bibcode :2002MPBu...29....6R . Archived fromthe original (PDF) on 4 October 2021. Retrieved14 March 2020 . ^ Durech, J.; Hanus, J.; Oszkiewicz, D.; Vanco, R. (March 2016)."Asteroid models from the Lowell photometric database" .Astronomy and Astrophysics .587 : 6.arXiv :1601.02909 .Bibcode :2016A&A...587A..48D .doi :10.1051/0004-6361/201527573 . Retrieved8 September 2017 .