{"id":56473,"date":"2019-07-29T09:08:40","date_gmt":"2019-07-29T16:08:40","guid":{"rendered":"http:\/\/in.nau.edu\/news\/?p=56473"},"modified":"2019-07-29T09:08:42","modified_gmt":"2019-07-29T16:08:42","slug":"tegler-infrared-light-signature","status":"publish","type":"post","link":"https:\/\/in.nau.edu\/news\/tegler-infrared-light-signature\/","title":{"rendered":"NAU astrophysicist leads international team in \u2018unprecedented\u2019 discovery of unique infrared light signature on Neptune\u2019s moon Triton"},"content":{"rendered":"\n<p>July 29, 2019<\/p>\n\n\n\n<p>Triton orbits Neptune, the eighth planet from the Sun, some 2.7\nbillion miles from Earth\u2014at the cold outer fringe of the Solar System\u2019s major\nplanet zone. Surface temperatures hover near absolute zero, so low that common\ncompounds we know as gases on Earth freeze into ices. Triton\u2019s atmosphere,\nwhich is 70,000 times less dense than Earth\u2019s, is composed of nitrogen, methane\nand carbon monoxide. <\/p>\n\n\n\n<p>These extreme conditions have led\nto an extraordinary discovery on Triton. An international team of scientists used\nthe 8-meter Gemini South Telescope in Chile to pinpoint a very specific type of\ninfrared light signature produced when carbon monoxide and nitrogen molecules\njoin together and vibrate in unison. Individually,\ncarbon monoxide and nitrogen ices each absorb their own distinct wavelengths of\ninfrared light, but the tandem vibration of an ice mixture absorbs at an\nadditional, distinct wavelength identified in this study.<\/p>\n\n\n\n<p>The discovery, recently published\nin the <a href=\"https:\/\/iopscience.iop.org\/article\/10.3847\/1538-3881\/ab199f\"><em>Astronomical Journal<\/em><\/a><em>, <\/em>offers insights into how this volatile mixture can transport\nmaterial across the moon\u2019s surface via geysers, trigger seasonal atmospheric\nchanges and provide a context for conditions on other distant, icy worlds.<\/p>\n\n\n\n<p>\u201cWhile the icy spectral fingerprint we uncovered was entirely reasonable, especially as this combination of ices can be created in the lab, pinpointing this specific wavelength of infrared light on another world is unprecedented,\u201d said NAU professor <strong>Stephen Tegler<\/strong>, who led the study, collaborating with Will Grundy and Jennifer Hanley of <a href=\"https:\/\/lowell.edu\/\">Lowell Observatory<\/a>. Other co-authors from NAU are <strong>Terry Stufflebeam<\/strong>, <strong>Shyanne Dustrud<\/strong>, <strong>Gerrick Lindberg<\/strong>, <strong>Anna Engle, Thomas Dillingham<\/strong>, <strong>Daniel Matthew<\/strong> and <strong>David Trilling<\/strong>.<\/p>\n\n\n\n<p>In the Earth\u2019s atmosphere, carbon\nmonoxide and nitrogen molecules exist as gases,\nnot ices. In fact, molecular nitrogen is the dominant gas in the air we\nbreathe, and carbon monoxide is a rare contaminant that can be lethal. On\ndistant Triton, however, carbon monoxide and nitrogen freeze solid as ices. They\ncan form their own independent ices or can condense together in the icy mix\ndetected in the Gemini data. This icy mix could be involved in Triton\u2019s iconic\ngeysers first seen in Voyager 2\nspacecraft images as dark, windblown streaks on the surface of the distant, icy\nmoon.<\/p>\n\n\n\n<p>Looking ahead, the researchers expect these findings will shed light on the composition of ices on other distant worlds beyond Neptune. Astronomers have suspected that the mixing of carbon monoxide and nitrogen ice exists not only on Triton, but also on Pluto, where the New Horizons spacecraft found the two ices coexisting. This Gemini finding is the first direct spectroscopic evidence of these ices mixing and absorbing this type of light on either world. <\/p>\n\n\n\n<p>Tegler studies ices relevant to\nthe surfaces of Kuiper Belt Objects in the Astrophysical Ice Laboratory using\ntransmission and Raman spectroscopy. The laboratory is a collaboration between\nLowell Observatory and NAU\u2019s Department of Physics and Astronomy,\nwhich&nbsp;facilitates studies of cryogenic outer solar system materials, such\nas the methane and nitrogen ices that dominate the surfaces of Pluto, Triton,\nEris and Makemake, and the ethane-methane-nitrogen liquids that flow across the\nsurface of Titan.<\/p>\n\n\n\n<p>The laboratory consists of two\nexperimental stations, one for vapor deposition of thin ice films, and one for\nmore massive samples of cryogenic liquids and ices up to 2 cm thick.\nInstruments used to analyze cryogenic materials include Fourier-transform\ninfrared spectroscopy, mass spectroscopy and X-ray photoelectron spectroscopy.<\/p>\n\n\n\n<p><em>Photo: Voyager 2 image of Triton showing the moon\u2019s south polar region. Credit: NASA\/JPL<\/em><\/p>\n\n\n\n<div class=\"wp-block-media-text alignwide\" style=\"grid-template-columns:20% auto\"><figure class=\"wp-block-media-text__media\"><img loading=\"lazy\" decoding=\"async\" width=\"905\" height=\"643\" src=\"http:\/\/in.nau.edu\/news\/wordpresst\/uploads\/sites\/153\/wp-content\/uploads\/2018\/10\/NAU_primary-281_3514.png\" alt=\"NAU logo\" class=\"wp-image-52788\" srcset=\"https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/402\/2018\/10\/NAU_primary-281_3514.png 905w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/402\/2018\/10\/NAU_primary-281_3514-300x213.png 300w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/402\/2018\/10\/NAU_primary-281_3514-768x546.png 768w, https:\/\/in.nau.edu\/wp-content\/uploads\/sites\/402\/2018\/10\/NAU_primary-281_3514-600x426.png 600w\" sizes=\"auto, (max-width: 905px) 100vw, 905px\" \/><\/figure><div class=\"wp-block-media-text__content\">\n<p>Kerry Bennett <br>Office of the Vice President for Research<\/p>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p><a class=\"search-results-excerpt-link\" href=\"https:\/\/in.nau.edu\/news\/tegler-infrared-light-signature\/\">July 29, 2019 Triton orbits Neptune, the eighth planet from the Sun, some 2.7 billion miles from Earth\u2014at the cold outer fringe of the Solar System\u2019s major planet zone. Surface temperatures hover near absolute zero, so low that common compounds we know as gases on Earth freeze into ices. Triton\u2019s atmosphere, which is 70,000 times&hellip;<\/a><\/p>\n","protected":false},"author":59,"featured_media":56474,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[11],"tags":[],"class_list":["post-56473","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research-academics"],"acf":[],"_links":{"self":[{"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/posts\/56473","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/users\/59"}],"replies":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/comments?post=56473"}],"version-history":[{"count":0,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/posts\/56473\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/media\/56474"}],"wp:attachment":[{"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/media?parent=56473"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/categories?post=56473"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/in.nau.edu\/news\/wp-json\/wp\/v2\/tags?post=56473"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}