335 Roberta: Difference between revisions
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{{Short description|Large main belt asteroid}} |
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{{Use dmy dates|date=October 2019}} |
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{{Infobox planet |
{{Infobox planet |
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| minorplanet=yes |
| minorplanet=yes |
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| background=# |
| background=#D6D6D6 |
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| name=335 Roberta |
| name=335 Roberta |
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|image= Орбита астероида 335.png |
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|caption=Orbital diagram |
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| discoverer=[[Anton Staus]] |
| discoverer=[[Anton Staus]] |
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| discovered=1 September 1892 |
| discovered=1 September 1892 |
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| mpc_name=(335) Roberta |
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| alt_names=1892 C |
| alt_names=1892 C |
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| named_after=[[ |
| named_after=[[Carl Robert Osten-Sacken]] |
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| mp_category=[[Asteroid belt|Main belt]] |
| mp_category=[[Asteroid belt|Main belt]] |
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| orbit_ref=<ref name=jpldata/> |
| orbit_ref=<ref name=jpldata/> |
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Under the [[SMASS classification]] taxonomy, this asteroid is listed as a [[B-type asteroid|B-type]]; a group that combines both the Tholen B and F types. The spectrum of this object suggests the presence of [[magnetite]] (Fe<sub>3</sub>O<sub>4</sub>), which gives it the spectrally-blue coloration that is a characteristic of this SMASS class. The spectrum of this asteroid also displays a band feature near 2.9 μm that indicate the presence of a hydrated mineral. This suggests that the asteroid has undergone significant water-based alteration.<ref name=aj140_3_692/> |
Under the [[SMASS classification]] taxonomy, this asteroid is listed as a [[B-type asteroid|B-type]]; a group that combines both the Tholen B and F types. The spectrum of this object suggests the presence of [[magnetite]] (Fe<sub>3</sub>O<sub>4</sub>), which gives it the spectrally-blue coloration that is a characteristic of this SMASS class. The spectrum of this asteroid also displays a band feature near 2.9 μm that indicate the presence of a hydrated mineral. This suggests that the asteroid has undergone significant water-based alteration.<ref name=aj140_3_692/> |
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335 Roberta was identified as one of three asteroids that were likely to be a parent body for [[chondrite]]s along with [[449 Hamburga]] and [[304 Olga]].<ref name="books.google.com">[https://books.google.com/books?id=kJDvAAAAMAAJ&q=%22449+Hamburga%22 |
335 Roberta was identified as one of three asteroids that were likely to be a parent body for [[chondrite]]s along with [[449 Hamburga]] and [[304 Olga]].<ref name="books.google.com">[https://books.google.com/books?id=kJDvAAAAMAAJ&q=%22449+Hamburga%22 Lunar and planetary science: abstracts of papers submitted to the ... Lunar and Planetary Science Conference, Volume 27, Part 1 - Lunar and Planetary Institute, Jan 1, 1996]</ref> All three asteroids were known to have low-albedo (not reflect as much light) and be close to "meteorite producing resonances".<ref name="books.google.com"/> Chrondrites are the most common type of meteor found on Earth, accounting for over 80% of all meteors.<ref name="ASU - Chondrites">{{Cite web |url=https://meteorites.asu.edu/meteorites/meteorite-types/stony-meteorites/chondrites |title=ASU - Chondrites |access-date=31 August 2015 |archive-date=22 June 2019 |archive-url=https://web.archive.org/web/20190622023849/https://meteorites.asu.edu/meteorites/meteorite-types/stony-meteorites/chondrites |url-status=dead }}</ref> They are named for the tiny spherical silicate particles that are found inside them (those particles are called chondrules).<ref name="ASU - Chondrites"/> |
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==References== |
==References== |
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<ref name="Obituary">{{Cite journal |
<ref name="Obituary">{{Cite journal |
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|language = |
|language = de |
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|author = Kutter, A. |
|author = Kutter, A. |
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|date = December 1957 |
|date = December 1957 |
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| work = Discovery Circumstances |
| work = Discovery Circumstances |
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| publisher = IAU Minor Planet center |
| publisher = IAU Minor Planet center |
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| url = |
| url = https://www.minorplanetcenter.net/iau/lists/NumberedMPs000001.html |
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| |
| access-date= 7 April 2013 |
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| postscript= . |
| postscript= . |
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}}</ref> |
}}</ref> |
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| title = 335 Roberta |
| title = 335 Roberta |
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| work = JPL Small-Body Database Browser |
| work = JPL Small-Body Database Browser |
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| publisher = NASA Jet Propulsion Laboratory |
| publisher = [[NASA Jet Propulsion Laboratory]] |
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| url = |
| url = https://ssd.jpl.nasa.gov/sbdb.cgi?sstr=335 |
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| |
| access-date= 11 May 2016 |
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}}</ref> |
}}</ref> |
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| postscript= . |
| postscript= . |
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}}</ref> |
}}</ref> |
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}} |
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}} <!-- end of reflist --> |
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⚫ | |||
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* [http://www.minorplanetobserver.com/pdolc/A335_2007.HTM Lightcurve plot of 335 Roberta], Palmer Divide Observatory, [[Brian D. Warner|B. D. Warner]] (2007) |
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* [http://www.minorplanet.info/PHP/lcdbsummaryquery.php Asteroid Lightcurve Database (LCDB)], query form ([http://www.minorplanet.info/lightcurvedatabase.html info] {{Webarchive|url=https://web.archive.org/web/20171216050541/http://www.minorplanet.info/lightcurvedatabase.html |date=16 December 2017 }}) |
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* [https://books.google.com/books?id=aeAg1X7afOoC Dictionary of Minor Planet Names], Google books |
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* [http://obswww.unige.ch/~behrend/page_cou.html Asteroids and comets rotation curves, CdR] – Observatoire de Genève, Raoul Behrend |
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* [https://www.minorplanetcenter.net/iau/lists/NumberedMPs000001.html Discovery Circumstances: Numbered Minor Planets (1)-(5000)] – Minor Planet Center |
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* {{AstDys|335}} |
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* {{JPL small body}} |
* {{JPL small body}} |
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{{Minor planets navigator|334 Chicago|number=335|336 Lacadiera}} |
{{Minor planets navigator |334 Chicago |number=335 |336 Lacadiera}} |
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{{Small Solar System bodies}} |
{{Small Solar System bodies}} |
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{{Authority control}} |
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{{DEFAULTSORT: |
{{DEFAULTSORT:Roberta}} |
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[[Category: |
[[Category:Background asteroids|000335]] |
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[[Category: |
[[Category:Discoveries by Anton Staus]] |
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[[Category: |
[[Category:Named minor planets]] |
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[[Category: |
[[Category:FP-type asteroids (Tholen)|000335]] |
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[[Category: |
[[Category:B-type asteroids (SMASS)|000335]] |
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[[Category:FP-type asteroids (Tholen)]] |
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[[Category:B-type asteroids (SMASS)]] |
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[[Category:Astronomical objects discovered in 1892|18920901]] |
[[Category:Astronomical objects discovered in 1892|18920901]] |
Latest revision as of 09:21, 2 August 2024
Discovery | |
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Discovered by | Anton Staus |
Discovery date | 1 September 1892 |
Designations | |
(335) Roberta | |
Named after | Carl Robert Osten-Sacken |
1892 C | |
Main belt | |
Orbital characteristics[1] | |
Epoch 31 July 2016 (JD 2457600.5) | |
Uncertainty parameter 0 | |
Observation arc | 123.58 yr (45137 d) |
Aphelion | 2.9014 AU (434.04 Gm) |
Perihelion | 2.04926 AU (306.565 Gm) |
2.47530 AU (370.300 Gm) | |
Eccentricity | 0.17212 |
3.89 yr (1422.5 d) | |
Average orbital speed | 18.93 km/s |
355.460° | |
0° 15m 11.095s / day | |
Inclination | 5.1005° |
148.454° | |
140.006° | |
Earth MOID | 1.03587 AU (154.964 Gm) |
Jupiter MOID | 2.2733 AU (340.08 Gm) |
TJupiter | 3.456 |
Physical characteristics | |
Dimensions | 89.07±2.0 km[1] |
12.054 h (0.5023 d) | |
0.0580±0.003[1] 0.058[2] | |
B–V = 0.624 U–B = 0.235 FP (Tholen) B (SMASS)[1] | |
8.96[1] | |
335 Roberta is a large main belt asteroid. It was discovered on 1 September 1892, by German astronomer Anton Staus at Heidelberg Observatory.[3] Roberta was the 12th asteroid that was discovered using photography, and the only asteroid discovery made by Staus.[4]
Photometric observations of this asteroid from multiple sites during 2007 gave a light curve with a period of 12.054 ± 0.003 hours and a brightness variation of 0.13 ± 0.02 in magnitude. This agrees with a result reported in 1992, but differs from period estimates of 8.03 hours and 4.349 reported in 1987 and 2001, respectively.[5]
Under the SMASS classification taxonomy, this asteroid is listed as a B-type; a group that combines both the Tholen B and F types. The spectrum of this object suggests the presence of magnetite (Fe3O4), which gives it the spectrally-blue coloration that is a characteristic of this SMASS class. The spectrum of this asteroid also displays a band feature near 2.9 μm that indicate the presence of a hydrated mineral. This suggests that the asteroid has undergone significant water-based alteration.[2]
335 Roberta was identified as one of three asteroids that were likely to be a parent body for chondrites along with 449 Hamburga and 304 Olga.[6] All three asteroids were known to have low-albedo (not reflect as much light) and be close to "meteorite producing resonances".[6] Chrondrites are the most common type of meteor found on Earth, accounting for over 80% of all meteors.[7] They are named for the tiny spherical silicate particles that are found inside them (those particles are called chondrules).[7]
References
[edit]- ^ a b c d e "335 Roberta", JPL Small-Body Database Browser, NASA Jet Propulsion Laboratory, retrieved 11 May 2016
- ^ a b Yang, Bin; Jewitt, David (September 2010), "Identification of Magnetite in B-type Asteroids", The Astronomical Journal, 140 (3): 692–698, arXiv:1006.5110, Bibcode:2010AJ....140..692Y, doi:10.1088/0004-6256/140/3/692
- ^ "Numbered Minor Planets 1–5000", Discovery Circumstances, IAU Minor Planet center, retrieved 7 April 2013.
- ^ Kutter, A. (December 1957). "Nachruf auf Anton Staus (Obituary)". Mitteilungen der Astronomischen Gesellschaft (in German). 9: 5. Bibcode:1958MitAG...9....5K. Retrieved 6 July 2016.
- ^ Warner, Brian D.; et al. (December 2007), "Lightcurve Analysis of 335 Roberta", The Minor Planet Bulletin, vol. 34, no. 4, p. 99, Bibcode:2007MPBu...34...99W.
- ^ a b Lunar and planetary science: abstracts of papers submitted to the ... Lunar and Planetary Science Conference, Volume 27, Part 1 - Lunar and Planetary Institute, Jan 1, 1996
- ^ a b "ASU - Chondrites". Archived from the original on 22 June 2019. Retrieved 31 August 2015.
External links
[edit]- Lightcurve plot of 335 Roberta, Palmer Divide Observatory, B. D. Warner (2007)
- Asteroid Lightcurve Database (LCDB), query form (info Archived 16 December 2017 at the Wayback Machine)
- Dictionary of Minor Planet Names, Google books
- Asteroids and comets rotation curves, CdR – Observatoire de Genève, Raoul Behrend
- Discovery Circumstances: Numbered Minor Planets (1)-(5000) – Minor Planet Center
- 335 Roberta at AstDyS-2, Asteroids—Dynamic Site
- 335 Roberta at the JPL Small-Body Database