Near-infrared spectroscopy of primitive asteroid families
► We compared 13 NIR spectra of two asteroid families and found significant differences. ► Themis family spectra have positive slopes from 1.6 to 2.4 μm. ► Veritas family spectra in contrast have flat slopes from 1.6 to 2.4 μm. ► Themis family spectra have positive concavities from 1.0 to 1.5 μm ► V...
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creator | Ziffer, Julie Campins, Humberto Licandro, Javier Walker, Matthew E. Fernandez, Yanga Clark, Beth Ellen Mothe-Diniz, Thais Howell, Ellen Deshpande, Rohit |
description | ► We compared 13 NIR spectra of two asteroid families and found significant differences. ► Themis family spectra have positive slopes from 1.6 to 2.4
μm. ► Veritas family spectra in contrast have flat slopes from 1.6 to 2.4
μm. ► Themis family spectra have positive concavities from 1.0 to 1.5
μm ► Veritas family spectra have negative concavities from 1.0 to 1.5
μm.
We compare 13 near-infrared (0.8–2.4
μm) spectra of two low albedo C complex outer-belt asteroid families: Themis and Veritas. The disruption ages of these two families lie at opposite extremes: 2.5
±
1.0
Gyr and 8.7
±
1.7
Myr, respectively. We found striking differences between the two families, which show a range of spectral shapes and slopes. The seven Themis family members (older surfaces) have “red” (positive) slopes in the 1.6–2.4
μm region; in contrast, the six Veritas members (younger surfaces) have significantly “flatter” slopes at these same wavelengths. Moreover, the two families are characterized by different concavity at shorter (1.0–1.5
μm) wavelengths with the Themis group being consistently flat or concave up (smile) and the Veritas group being consistently concave down (frown). Each family contains a broad range of diameters, suggesting our results are not due to comparisons of asteroids of different sizes. The statistically significant clustering of the two spectral groups could be explained by one of the following three possibilities or a combination of them: (1) space weathering effects, (2) differences in original composition, or (3) differences in thermal history perhaps as a result of the difference in parent body sizes. As a result of our analyses, we propose a new method to quantify broad and shallow structures in the spectra of primitive asteroids. We found reasonable matches between the observed asteroids and individual carbonaceous chondrite meteorites. Because these meteoritic fits represent fresh surfaces, space weathering is neither necessary nor ruled out as an explanation of spectral differences between families. The six Veritas family near-infrared (NIR) spectra represent the first NIR analysis of this family, thus significantly increasing our understanding of this family over these wavelengths. |
doi_str_mv | 10.1016/j.icarus.2011.04.008 |
format | Article |
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μm. ► Veritas family spectra in contrast have flat slopes from 1.6 to 2.4
μm. ► Themis family spectra have positive concavities from 1.0 to 1.5
μm ► Veritas family spectra have negative concavities from 1.0 to 1.5
μm.
We compare 13 near-infrared (0.8–2.4
μm) spectra of two low albedo C complex outer-belt asteroid families: Themis and Veritas. The disruption ages of these two families lie at opposite extremes: 2.5
±
1.0
Gyr and 8.7
±
1.7
Myr, respectively. We found striking differences between the two families, which show a range of spectral shapes and slopes. The seven Themis family members (older surfaces) have “red” (positive) slopes in the 1.6–2.4
μm region; in contrast, the six Veritas members (younger surfaces) have significantly “flatter” slopes at these same wavelengths. Moreover, the two families are characterized by different concavity at shorter (1.0–1.5
μm) wavelengths with the Themis group being consistently flat or concave up (smile) and the Veritas group being consistently concave down (frown). Each family contains a broad range of diameters, suggesting our results are not due to comparisons of asteroids of different sizes. The statistically significant clustering of the two spectral groups could be explained by one of the following three possibilities or a combination of them: (1) space weathering effects, (2) differences in original composition, or (3) differences in thermal history perhaps as a result of the difference in parent body sizes. As a result of our analyses, we propose a new method to quantify broad and shallow structures in the spectra of primitive asteroids. We found reasonable matches between the observed asteroids and individual carbonaceous chondrite meteorites. Because these meteoritic fits represent fresh surfaces, space weathering is neither necessary nor ruled out as an explanation of spectral differences between families. The six Veritas family near-infrared (NIR) spectra represent the first NIR analysis of this family, thus significantly increasing our understanding of this family over these wavelengths.</description><identifier>ISSN: 0019-1035</identifier><identifier>EISSN: 1090-2643</identifier><identifier>DOI: 10.1016/j.icarus.2011.04.008</identifier><identifier>CODEN: ICRSA5</identifier><language>eng</language><publisher>Amsterdam: Elsevier Inc</publisher><subject>Albedo ; Asteroids ; Asteroids, Composition ; Asteroids, Surfaces ; Astronomy ; Concavity ; Earth, ocean, space ; Exact sciences and technology ; Infrared observations ; Meteorites ; Slopes ; Solar system ; Spectra ; Spectroscopy ; Wavelengths ; Weathering</subject><ispartof>Icarus (New York, N.Y. 1962), 2011-06, Vol.213 (2), p.538-546</ispartof><rights>2011 Elsevier Inc.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c401t-d49d434b226b41f6ba1719f0cabe3c9618c7516238a1a851de72938f0eb35cd93</citedby><cites>FETCH-LOGICAL-c401t-d49d434b226b41f6ba1719f0cabe3c9618c7516238a1a851de72938f0eb35cd93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.icarus.2011.04.008$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24218655$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Ziffer, Julie</creatorcontrib><creatorcontrib>Campins, Humberto</creatorcontrib><creatorcontrib>Licandro, Javier</creatorcontrib><creatorcontrib>Walker, Matthew E.</creatorcontrib><creatorcontrib>Fernandez, Yanga</creatorcontrib><creatorcontrib>Clark, Beth Ellen</creatorcontrib><creatorcontrib>Mothe-Diniz, Thais</creatorcontrib><creatorcontrib>Howell, Ellen</creatorcontrib><creatorcontrib>Deshpande, Rohit</creatorcontrib><title>Near-infrared spectroscopy of primitive asteroid families</title><title>Icarus (New York, N.Y. 1962)</title><description>► We compared 13 NIR spectra of two asteroid families and found significant differences. ► Themis family spectra have positive slopes from 1.6 to 2.4
μm. ► Veritas family spectra in contrast have flat slopes from 1.6 to 2.4
μm. ► Themis family spectra have positive concavities from 1.0 to 1.5
μm ► Veritas family spectra have negative concavities from 1.0 to 1.5
μm.
We compare 13 near-infrared (0.8–2.4
μm) spectra of two low albedo C complex outer-belt asteroid families: Themis and Veritas. The disruption ages of these two families lie at opposite extremes: 2.5
±
1.0
Gyr and 8.7
±
1.7
Myr, respectively. We found striking differences between the two families, which show a range of spectral shapes and slopes. The seven Themis family members (older surfaces) have “red” (positive) slopes in the 1.6–2.4
μm region; in contrast, the six Veritas members (younger surfaces) have significantly “flatter” slopes at these same wavelengths. Moreover, the two families are characterized by different concavity at shorter (1.0–1.5
μm) wavelengths with the Themis group being consistently flat or concave up (smile) and the Veritas group being consistently concave down (frown). Each family contains a broad range of diameters, suggesting our results are not due to comparisons of asteroids of different sizes. The statistically significant clustering of the two spectral groups could be explained by one of the following three possibilities or a combination of them: (1) space weathering effects, (2) differences in original composition, or (3) differences in thermal history perhaps as a result of the difference in parent body sizes. As a result of our analyses, we propose a new method to quantify broad and shallow structures in the spectra of primitive asteroids. We found reasonable matches between the observed asteroids and individual carbonaceous chondrite meteorites. Because these meteoritic fits represent fresh surfaces, space weathering is neither necessary nor ruled out as an explanation of spectral differences between families. The six Veritas family near-infrared (NIR) spectra represent the first NIR analysis of this family, thus significantly increasing our understanding of this family over these wavelengths.</description><subject>Albedo</subject><subject>Asteroids</subject><subject>Asteroids, Composition</subject><subject>Asteroids, Surfaces</subject><subject>Astronomy</subject><subject>Concavity</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Infrared observations</subject><subject>Meteorites</subject><subject>Slopes</subject><subject>Solar system</subject><subject>Spectra</subject><subject>Spectroscopy</subject><subject>Wavelengths</subject><subject>Weathering</subject><issn>0019-1035</issn><issn>1090-2643</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNp9kD1PwzAURS0EEqXwDxiyIFgS3rOdxF6QUMWXVMECs-U4L5KrtCl2Wqn_HletGDu95dx3dQ9jtwgFAlaPi8I7Gzax4IBYgCwA1BmbIGjIeSXFOZsAoM4RRHnJrmJcAECptJgw_Uk25H7VBRuozeKa3BiG6Ib1Lhu6bB380o9-S5mNI4XBt1lnl773FK_ZRWf7SDfHO2U_ry_fs_d8_vX2MXue504CjnkrdSuFbDivGold1VisUXfgbEPC6QqVq0usuFAWrSqxpZproTqgRpSu1WLK7g9_12H43VAczdJHR31vVzRsolFKIQCXIpEPJ0msahSpKWmYMnlAXRobA3Vmv9SGnUEwe6dmYQ5Ozd6pAWmS0xS7OzbY6GyfpK2cj_9ZLjmqqiwT93TgKInZegomOk8rR60PSbBpB3-66A_j342w</recordid><startdate>20110601</startdate><enddate>20110601</enddate><creator>Ziffer, Julie</creator><creator>Campins, Humberto</creator><creator>Licandro, Javier</creator><creator>Walker, Matthew E.</creator><creator>Fernandez, Yanga</creator><creator>Clark, Beth Ellen</creator><creator>Mothe-Diniz, Thais</creator><creator>Howell, Ellen</creator><creator>Deshpande, Rohit</creator><general>Elsevier Inc</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>20110601</creationdate><title>Near-infrared spectroscopy of primitive asteroid families</title><author>Ziffer, Julie ; Campins, Humberto ; Licandro, Javier ; Walker, Matthew E. ; Fernandez, Yanga ; Clark, Beth Ellen ; Mothe-Diniz, Thais ; Howell, Ellen ; Deshpande, Rohit</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c401t-d49d434b226b41f6ba1719f0cabe3c9618c7516238a1a851de72938f0eb35cd93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Albedo</topic><topic>Asteroids</topic><topic>Asteroids, Composition</topic><topic>Asteroids, Surfaces</topic><topic>Astronomy</topic><topic>Concavity</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Infrared observations</topic><topic>Meteorites</topic><topic>Slopes</topic><topic>Solar system</topic><topic>Spectra</topic><topic>Spectroscopy</topic><topic>Wavelengths</topic><topic>Weathering</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ziffer, Julie</creatorcontrib><creatorcontrib>Campins, Humberto</creatorcontrib><creatorcontrib>Licandro, Javier</creatorcontrib><creatorcontrib>Walker, Matthew E.</creatorcontrib><creatorcontrib>Fernandez, Yanga</creatorcontrib><creatorcontrib>Clark, Beth Ellen</creatorcontrib><creatorcontrib>Mothe-Diniz, Thais</creatorcontrib><creatorcontrib>Howell, Ellen</creatorcontrib><creatorcontrib>Deshpande, Rohit</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Icarus (New York, N.Y. 1962)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ziffer, Julie</au><au>Campins, Humberto</au><au>Licandro, Javier</au><au>Walker, Matthew E.</au><au>Fernandez, Yanga</au><au>Clark, Beth Ellen</au><au>Mothe-Diniz, Thais</au><au>Howell, Ellen</au><au>Deshpande, Rohit</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Near-infrared spectroscopy of primitive asteroid families</atitle><jtitle>Icarus (New York, N.Y. 1962)</jtitle><date>2011-06-01</date><risdate>2011</risdate><volume>213</volume><issue>2</issue><spage>538</spage><epage>546</epage><pages>538-546</pages><issn>0019-1035</issn><eissn>1090-2643</eissn><coden>ICRSA5</coden><abstract>► We compared 13 NIR spectra of two asteroid families and found significant differences. ► Themis family spectra have positive slopes from 1.6 to 2.4
μm. ► Veritas family spectra in contrast have flat slopes from 1.6 to 2.4
μm. ► Themis family spectra have positive concavities from 1.0 to 1.5
μm ► Veritas family spectra have negative concavities from 1.0 to 1.5
μm.
We compare 13 near-infrared (0.8–2.4
μm) spectra of two low albedo C complex outer-belt asteroid families: Themis and Veritas. The disruption ages of these two families lie at opposite extremes: 2.5
±
1.0
Gyr and 8.7
±
1.7
Myr, respectively. We found striking differences between the two families, which show a range of spectral shapes and slopes. The seven Themis family members (older surfaces) have “red” (positive) slopes in the 1.6–2.4
μm region; in contrast, the six Veritas members (younger surfaces) have significantly “flatter” slopes at these same wavelengths. Moreover, the two families are characterized by different concavity at shorter (1.0–1.5
μm) wavelengths with the Themis group being consistently flat or concave up (smile) and the Veritas group being consistently concave down (frown). Each family contains a broad range of diameters, suggesting our results are not due to comparisons of asteroids of different sizes. The statistically significant clustering of the two spectral groups could be explained by one of the following three possibilities or a combination of them: (1) space weathering effects, (2) differences in original composition, or (3) differences in thermal history perhaps as a result of the difference in parent body sizes. As a result of our analyses, we propose a new method to quantify broad and shallow structures in the spectra of primitive asteroids. We found reasonable matches between the observed asteroids and individual carbonaceous chondrite meteorites. Because these meteoritic fits represent fresh surfaces, space weathering is neither necessary nor ruled out as an explanation of spectral differences between families. The six Veritas family near-infrared (NIR) spectra represent the first NIR analysis of this family, thus significantly increasing our understanding of this family over these wavelengths.</abstract><cop>Amsterdam</cop><pub>Elsevier Inc</pub><doi>10.1016/j.icarus.2011.04.008</doi><tpages>9</tpages></addata></record> |
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subjects | Albedo Asteroids Asteroids, Composition Asteroids, Surfaces Astronomy Concavity Earth, ocean, space Exact sciences and technology Infrared observations Meteorites Slopes Solar system Spectra Spectroscopy Wavelengths Weathering |
title | Near-infrared spectroscopy of primitive asteroid families |
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