Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Comet
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
=== Nucleus === [[File:Comet Hartley 2.jpg|thumb|Nucleus of [[103P/Hartley]] as imaged during a [[Deep Impact (spacecraft)|spacecraft flyby]]. The nucleus is about 2 km in length.]] {{Main|Comet nucleus}} The solid, core structure of a comet is known as the nucleus. Cometary nuclei are composed of an amalgamation of [[rock (geology)|rock]], [[Comet dust|dust]], [[ice|water ice]], and frozen [[carbon dioxide]], [[carbon monoxide]], [[methane]], and [[ammonia]].<ref>{{cite journal |bibcode=1998A&A...330..375G |title=Making a comet nucleus |last1=Greenberg |first1=J. Mayo |volume=330 |date=1998 |pages=375 |journal=[[Astronomy & Astrophysics]]}}</ref> As such, they are popularly described as "dirty snowballs" after [[Fred Whipple]]'s model.<ref>{{cite web |url=http://starryskies.com/solar_system/Comet/dirty_snowballs.html |title=Dirty Snowballs in Space |publisher=Starryskies |access-date=15 August 2013 |url-status=dead |archive-url=https://web.archive.org/web/20130129035627/http://starryskies.com/solar_system/Comet/dirty_snowballs.html |archive-date=29 January 2013}}</ref> Comets with a higher dust content have been called "icy dirtballs".<ref>{{cite news |url=http://www.timeshighereducation.co.uk/news/evidence-from-esas-rosetta-spacecraft-suggests-that-comets-are-more-icy-dirtball-than-dirty-snowball/199168.article |title=Evidence from ESA's Rosetta Spacecraft Suggests that Comets are more "Icy Dirtball" than "Dirty Snowball" |date=21 October 2005 |work=Times Higher Education}}</ref> The term "icy dirtballs" arose after observation of [[Tempel 1|Comet 9P/Tempel 1]] collision with an "impactor" probe sent by NASA Deep Impact mission in July 2005. Research conducted in 2014 suggests that comets are like "[[Fried ice cream|deep fried ice cream]]", in that their surfaces are formed of dense crystalline ice mixed with [[organic compound]]s, while the interior ice is colder and less dense.<ref name="NASA-20150210" /> The surface of the nucleus is generally dry, dusty or rocky, suggesting that the ices are hidden beneath a surface crust several metres thick. Nuclei contain a variety of organic compounds, which may include [[methanol]], [[hydrogen cyanide]], [[formaldehyde]], [[ethanol]], [[ethane]], and perhaps more complex molecules such as long-chain [[hydrocarbon]]s and [[amino acid]]s.<ref>{{cite web |last=Meech |first=M. |title=1997 Apparition of Comet Hale–Bopp: What We Can Learn from Bright Comets |url=http://www.psrd.hawaii.edu/Feb97/Bright.html |publisher=Planetary Science Research Discoveries |date=24 March 1997 |access-date=30 April 2013}}</ref><ref>{{cite web |title=Stardust Findings Suggest Comets More Complex Than Thought |url=http://stardust.jpl.nasa.gov/news/news110.html |publisher=NASA |date=14 December 2006 |access-date=31 July 2013}}</ref> In 2009, it was confirmed that the amino acid [[glycine]] had been found in the comet dust recovered by NASA's [[Stardust (spacecraft)|Stardust mission]].<ref>{{cite journal |doi=10.1111/j.1945-5100.2009.tb01224.x |title=Cometary glycine detected in samples returned by Stardust |date=2009 |last1=Elsila |first1=Jamie E. |last2=Glavin |first2=Daniel P. |last3=Dworkin |first3=Jason P. |display-authors=1 |journal=Meteoritics & Planetary Science |volume=44 |issue=9 |pages=1323 |bibcode=2009M&PS...44.1323E|doi-access=free }}</ref> In August 2011, a report, based on [[NASA]] studies of [[meteorite]]s found on Earth, was published suggesting [[DNA]] and [[RNA]] components ([[adenine]], [[guanine]], and related organic molecules) may have been formed on [[asteroid]]s and comets.<ref name="Callahan">{{cite journal |doi=10.1073/pnas.1106493108 |title=Carbonaceous meteorites contain a wide range of extraterrestrial nucleobases |date=2011 |last1=Callahan |first1=M. P. |last2=Smith |first2=K. E. |last3=Cleaves |first3=H. J. |last4=Ruzicka |first4=J. |last5=Stern |first5=J. C. |last6=Glavin |first6=D. P. |last7=House |first7=C. H. |last8=Dworkin |first8=J. P. |display-authors=1 |journal=Proceedings of the National Academy of Sciences |volume=108 |issue=34 |pages=13995–8 |bibcode=2011PNAS..10813995C |pmid=21836052 |pmc=3161613|doi-access=free }}</ref><ref name="Steigerwald">{{cite web |last=Steigerwald |first=John |title=NASA Researchers: DNA Building Blocks Can Be Made in Space |url=http://www.nasa.gov/topics/solarsystem/features/dna-meteorites.html |publisher=NASA |date=8 August 2011 |access-date=31 July 2013 |archive-date=26 April 2020 |archive-url=https://web.archive.org/web/20200426055700/https://www.nasa.gov/topics/solarsystem/features/dna-meteorites.html |url-status=dead }}</ref> The outer surfaces of cometary nuclei have a very low [[albedo]], making them among the least reflective objects found in the Solar System. The [[Giotto (spacecraft)|Giotto]] [[space probe]] found that the nucleus of [[Halley's Comet]] (1P/Halley) reflects about four percent of the light that falls on it,<ref name="dark">{{cite journal |title=The Activity and Size of the Nucleus of Comet Hale-Bopp (C/1995 O1) |journal=Science |last1=Weaver |first1=H. A. |last2=Feldman |first2=P. D. |last3=a'Hearn |first3=M. F. |last4=Arpigny |first4=C. |last5=Brandt |first5=J. C. |last6=Festou |first6=M. C. |last7=Haken |first7=M. |last8=McPhate |first8=J. B. |last9=Stern |first9=S. A. |last10=Tozzi |first10=G. P. |display-authors=1 |volume=275 |issue=5308 |pages=1900–1904 |date=1997 |pmid=9072959 |doi=10.1126/science.275.5308.1900 |bibcode=1997Sci...275.1900W|s2cid=25489175 }}</ref> and [[Deep Space 1]] discovered that [[19P/Borrelly|Comet Borrelly]]'s surface reflects less than 3.0%;<ref name="dark" /> by comparison, [[Bitumen|asphalt]] reflects seven percent. The dark surface material of the nucleus may consist of complex organic compounds. Solar heating drives off lighter [[Volatility (chemistry)|volatile]] [[Chemical compound|compounds]], leaving behind larger organic compounds that tend to be very dark, like [[tar]] or [[petroleum|crude oil]]. The low reflectivity of cometary surfaces causes them to absorb the heat that drives their [[outgassing]] processes.<ref>{{cite book |url=https://books.google.com/books?id=PRqVqQKao9QC&pg=PA91 |page=91 |title=Habitability and Cosmic Catastrophes |isbn=978-3-540-76945-3 |last1=Hanslmeier |first1=Arnold |date=2008|publisher=Springer }}</ref> Comet nuclei with radii of up to {{convert|30|km|mi|sp=us}} have been observed,<ref>{{cite journal |doi=10.1023/A:1021545031431 |title=The Nucleus of Comet Hale-Bopp (C/1995 O1): Size and Activity |date=2000 |last1=Fernández |first1=Yanga R. |journal=Earth, Moon, and Planets |volume=89 |issue=1 |pages=3–25 |bibcode=2002EM&P...89....3F|s2cid=189899565 }}</ref> but ascertaining their exact size is difficult.<ref>{{cite web |url=http://www2.ess.ucla.edu/~jewitt/nucleus.html | first=David | last=Jewitt |title=The Cometary Nucleus |publisher=Department of Earth and Space Sciences, UCLA |date=April 2003 |access-date=31 July 2013}}</ref> The nucleus of [[322P/SOHO]] is probably only {{convert|100|-|200|m|ft|sp=us}} in diameter.<ref name="soho1">{{cite web |title=SOHO's new catch: its first officially periodic comet |publisher=European Space Agency |url=http://www.esa.int/Our_Activities/Space_Science/SOHO_s_new_catch_its_first_officially_periodic_comet |access-date=16 August 2013}}</ref> A lack of smaller comets being detected despite the increased sensitivity of instruments has led some to suggest that there is a real lack of comets smaller than {{convert|100|m|ft|sp=us}} across.<ref>{{harvnb|Sagan|Druyan|1997|p=137}}</ref> Known comets have been estimated to have an average density of {{convert|0.6|g/cm3|oz/cuin|abbr=on}}.<ref name="Britt2006">{{cite journal |bibcode=2006LPI....37.2214B |title=Small Body Density and Porosity: New Data, New Insights |last1=Britt |first1=D. T. |last2=Consolmagno |first2=G. J. |last3=Merline |first3=W. J. |display-authors=1 |volume=37 |date=2006 |pages=2214 |journal=37th Annual Lunar and Planetary Science Conference |url=http://www.lpi.usra.edu/meetings/lpsc2006/pdf/2214.pdf |access-date=25 August 2013 |archive-url=https://web.archive.org/web/20081217064607/http://www.lpi.usra.edu/meetings/lpsc2006/pdf/2214.pdf |archive-date=17 December 2008 |url-status=dead}}</ref> Because of their low mass, comet nuclei do not [[gravitational collapse|become spherical]] under their own [[gravity]] and therefore have irregular shapes.<ref>{{cite web |url=https://history.nasa.gov/SP-467/ch7.htm |title=The Geology of Small Bodies |date=January 1984 |publisher=NASA |access-date=15 August 2013 |last1=Veverka |first1=J. }}</ref> [[File:Comet wild 2.jpg|thumb|220px|Comet [[81P/Wild]] exhibits jets on light side and dark side, stark relief, and is dry.]] Roughly six percent of the [[near-Earth asteroid]]s are thought to be the [[Extinct comet|extinct nuclei of comets]] that no longer experience outgassing,<ref name="dormant">{{cite journal |doi=10.1016/j.icarus.2006.02.016 |arxiv=astro-ph/0603106v2 |date=2006 |title=The size–frequency distribution of dormant Jupiter family comets |last1=Whitman |first1=K. |last2=Morbidelli |first2=A. |last3=Jedicke |first3=R. |display-authors=1 |journal=Icarus |volume=183 |issue=1 |pages=101–114 |bibcode=2006Icar..183..101W|s2cid=14026673 }}</ref> including [[14827 Hypnos]] and [[3552 Don Quixote]]. Results from the [[Rosetta (spacecraft)|''Rosetta'']] and [[Philae (spacecraft)|''Philae'']] spacecraft show that the nucleus of [[67P/Churyumov–Gerasimenko]] has no magnetic field, which suggests that magnetism may not have played a role in the early formation of [[planetesimal]]s.<ref name="esa20150414">{{cite news |url=http://www.esa.int/Our_Activities/Space_Science/Rosetta/Rosetta_and_Philae_find_comet_not_magnetised |title=Rosetta and Philae Find Comet Not Magnetised |publisher=European Space Agency |first=Markus |last=Bauer |date=14 April 2015 |access-date=14 April 2015}}</ref><ref name="nature20150414">{{cite journal |title=Rosetta's comet has no magnetic field |journal=[[Nature (journal)|Nature]] |first=Quirin |last=Schiermeier |date=14 April 2015 |doi=10.1038/nature.2015.17327|s2cid=123964604 }}</ref> Further, the [[Rosetta (spacecraft)#Instruments|ALICE spectrograph]] on ''Rosetta'' determined that [[electron]]s (within {{convert|1|km|mi|abbr=on}} above the [[comet nucleus]]) produced from [[photoionization]] of water molecules by [[Sunlight|solar radiation]], and not [[photon]]s from the Sun as thought earlier, are responsible for the degradation of water and [[carbon dioxide]] [[molecule]]s released from the comet nucleus into its coma.<ref name="NASA-20150602">{{cite web |last1=Agle |first1=D. C. |last2=Brown |first2=Dwayne |last3=Fohn |first3=Joe |last4=Bauer |first4=Markus |display-authors=1 |title=NASA Instrument on Rosetta Makes Comet Atmosphere Discovery |url=http://www.jpl.nasa.gov/news/news.php?feature=4609 |date=2 June 2015 |publisher=[[NASA]] |access-date=2 June 2015}}</ref><ref name="AA-20150602">{{cite journal |last1=Feldman |first1=Paul D. |last2=A'Hearn |first2=Michael F. |last3=Bertaux |first3=Jean-Loup |last4=Feaga |first4=Lori M. |last5=Parker |first5=Joel Wm. |last6=Schindhelm |first6=Eric |last7=Steiffl |first7=Andrew J. |last8=Stern |first8=S. Alan |last9=Weaver |first9=Harold A. |last10=Sierks |first10=Holger |last11=Vincent |first11=Jean-Baptiste |display-authors=1 |title=Measurements of the near-nucleus coma of comet 67P/Churyumov-Gerasimenko with the Alice far-ultraviolet spectrograph on Rosetta |url=http://www.aanda.org/articles/aa/pdf/forth/aa25925-15.pdf |archive-url=https://web.archive.org/web/20150608071334/http://www.aanda.org/articles/aa/pdf/forth/aa25925-15.pdf |archive-date=2015-06-08 |url-status=live |date=2 June 2015 |journal=[[Astronomy & Astrophysics]] |doi=10.1051/0004-6361/201525925 |access-date=3 June 2015 |arxiv=1506.01203 |bibcode=2015A&A...583A...8F |volume=583 |pages=A8|s2cid=119104807 }}</ref> Instruments on the ''Philae'' lander found at least sixteen organic compounds at the comet's surface, four of which ([[acetamide]], [[acetone]], [[methyl isocyanate]] and [[propionaldehyde]]) have been detected for the first time on a comet.<ref name="wapo20150730">{{cite news |url=https://www.washingtonpost.com/world/philae-probe-finds-evidence-that-comets-can-be-cosmic-labs/2015/07/30/63a2fc0e-36e5-11e5-ab7b-6416d97c73c2_story.html |archive-url=https://web.archive.org/web/20181223235109/https://www.washingtonpost.com/world/philae-probe-finds-evidence-that-comets-can-be-cosmic-labs/2015/07/30/63a2fc0e-36e5-11e5-ab7b-6416d97c73c2_story.html |url-status=dead |archive-date=23 December 2018 |title=Philae probe finds evidence that comets can be cosmic labs |newspaper=The Washington Post |agency=Associated Press |first=Frank |last=Jordans |date=30 July 2015 |access-date=30 July 2015}}</ref><ref name="esa20150730">{{cite web |url=http://www.esa.int/Our_Activities/Space_Science/Rosetta/Science_on_the_surface_of_a_comet |title=Science on the Surface of a Comet |publisher=European Space Agency |date=30 July 2015 |access-date=30 July 2015}}</ref><ref name="SCI-20150731">{{cite journal |last1=Bibring |first1=J.-P. |last2=Taylor |first2=M.G.G.T. |last3=Alexander |first3=C. |last4=Auster |first4=U. |last5=Biele |first5=J. |last6=Finzi |first6=A. Ercoli |last7=Goesmann |first7=F. |last8=Klingehoefer |first8=G. |last9=Kofman |first9=W. |last10=Mottola |first10=S. |last11=Seidenstiker |first11=K.J. |last12=Spohn |first12=T. |last13=Wright |first13=I. |display-authors=1 |title=Philae's First Days on the Comet – Introduction to Special Issue |date=31 July 2015 |journal=[[Science (journal)|Science]] |volume=349 |number=6247 |page=493 |doi=10.1126/science.aac5116 |bibcode=2015Sci...349..493B |pmid=26228139|doi-access=free }}</ref> {| class="wikitable center" style="text-align: center; width: 530px; margin: 0.1em auto;" |+Properties of some comets |- ! width="120" | Name ! width="120" | Dimensions<br />(km) ! width="120" | Density<br />([[Gram|g]]/cm<sup>3</sup>) ! width="120" | Mass<br />([[Kilogram|kg]])<ref name="mass"> Halley: Using the [[Volume#Formulas|volume of an ellipsoid]] of 15×8×8 km * a [[rubble pile]] density of 0.6 g/cm<sup>3</sup> yields a mass (m=d*v) of 3.02E+14 kg.<br /> Tempel 1: Using a spherical diameter of 6.25 km; [[Volume#Formulas|volume of a sphere]] * a density of 0.62 g/cm<sup>3</sup> yields a mass of 7.9E+13 kg.<br /> 19P/Borrelly: Using the [[Volume#Formulas|volume of an ellipsoid]] of 8x4x4km * a density of 0.3 g/cm<sup>3</sup> yields a mass of 2.0E+13 kg.<br /> 81P/Wild: Using the [[Volume#Formulas|volume of an ellipsoid]] of 5.5x4.0x3.3 km * a density of 0.6 g/cm<sup>3</sup> yields a mass of 2.28E+13 kg.</ref> !Refs |- | align="left" | [[Halley's Comet]] | 15 × 8 × 8 | 0.6 | 3{{e|14}} |<ref>{{cite web |url=https://astrosociety.org/file_download/inline/6f0b9235-b5eb-40e6-88a3-6dd45e3b6f92 |title=What Have We Learned About Halley's Comet? |date=1986 |publisher=Astronomical Society of the Pacific |access-date=4 October 2013}}</ref><ref>{{cite journal |title=Is the nucleus of Comet Halley a low density body? |journal=Nature |last1=Sagdeev |first1=R. Z. |last2=Elyasberg |first2=P. E. |last3=Moroz |first3=V. I. |display-authors=1 |volume=331 |issue=6153 |pages=240 |date=1988 |issn=0028-0836 |doi=10.1038/331240a0 |bibcode=1988Natur.331..240S|s2cid=4335780 }}</ref> |- | align="left" | [[Tempel 1]] | 7.6 × 4.9 | 0.62 | 7.9{{e|13}} |<ref name="Britt2006" /><ref>{{cite web |url=http://ssd.jpl.nasa.gov/sbdb.cgi?sstr=9P |title=9P/Tempel 1 |publisher=JPL |access-date=16 August 2013}}</ref> |- | align="left" | [[19P/Borrelly]] | 8 × 4 × 4 | 0.3 | 2.0{{e|13}} |<ref name="Britt2006" /> |- | align="left" | [[81P/Wild]] | 5.5 × 4.0 × 3.3 | 0.6 | 2.3{{e|13}} |<ref name="Britt2006" /><ref name="wild2">{{cite web |title=Comet 81P/Wild 2 |publisher=The Planetary Society |url=http://www.planetary.org/explore/topics/asteroids_and_comets/wild2.html |access-date=20 November 2007 |url-status=dead |archive-url=https://web.archive.org/web/20090106004009/http://planetary.org./explore/topics/asteroids_and_comets/wild2.html |archive-date=6 January 2009 }}</ref> |- | align="left" | [[67P/Churyumov–Gerasimenko]] | 4.1 × 3.3 × 1.8 | 0.47 | 1.0{{e|13}} |<ref>{{cite web |url=http://www.esa.int/spaceinimages/Images/2015/01/Comet_vital_statistics |title=Comet vital statistics |publisher=European Space Agency |date=22 January 2015 |access-date=24 January 2015}}</ref><ref>{{cite web |url=http://blogs.esa.int/rosetta/2014/08/21/determining-the-mass-of-comet-67pc-g/ |title=Determining the mass of comet 67P/C-G |publisher=European Space Agency |first=Emily |last=Baldwin |date=21 August 2014 |access-date=21 August 2014}}</ref> |}
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)