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Evidence for Water Ice Near Mercury's North Pole from MESSENGER Neutron Spectrometer Measurements
Measurements by the Neutron Spectrometer on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft show decreases in the flux of epithermal and fast neutrons from Mercury's north polar region that are consistent with the presence of water ice in permanently sha...
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Published in: | Science (American Association for the Advancement of Science) 2013-01, Vol.339 (6117), p.292-296 |
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creator | Lawrence, David J. Feldman, William C. Goldsten, John O. Maurice, Sylvestre Peplowski, Patrick N. Anderson, Brian J. Bazell, David McNutt, Ralph L. Nittler, Larry R. Prettyman, Thomas H. Rodgers, Douglas J. Solomon, Sean C. Weider, Shoshana Z. |
description | Measurements by the Neutron Spectrometer on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft show decreases in the flux of epithermal and fast neutrons from Mercury's north polar region that are consistent with the presence of water ice in permanently shadowed regions. The neutron data indicate that Mercury's radar-bright polar deposits contain, on average, a hydrogen-rich layer more than tens of centimeters thick beneath a surficial layer 10 to 30 cm thick that is less rich in hydrogen. Combined neutron and radar data are best matched if the buried layer consists of nearly pure water ice. The upper layer contains less than 25 weight % water-equivalent hydrogen. The total mass of water at Mercury's poles is inferred to be 2 × 10 16 to 10 18 grams and is consistent with delivery by comets or volatile-rich asteroids. |
doi_str_mv | 10.1126/science.1229953 |
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The neutron data indicate that Mercury's radar-bright polar deposits contain, on average, a hydrogen-rich layer more than tens of centimeters thick beneath a surficial layer 10 to 30 cm thick that is less rich in hydrogen. Combined neutron and radar data are best matched if the buried layer consists of nearly pure water ice. The upper layer contains less than 25 weight % water-equivalent hydrogen. The total mass of water at Mercury's poles is inferred to be 2 × 10 16 to 10 18 grams and is consistent with delivery by comets or volatile-rich asteroids.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.1229953</identifier><identifier>PMID: 23196909</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>United States: American Association for the Advancement of Science</publisher><subject>Backscattering ; Deposition ; Environmental conditions ; Fast neutrons ; Hydrogen ; Italian ices ; Latitude ; Mercury (planet) ; Mercury surface ; MESSENGER Mission ; Neutrons ; North Pole ; Onboard ; Online ; Planets ; Polar regions ; Radar ; Radio astronomy ; Scientific Concepts ; Signals ; Simulations ; Spacecraft ; Spectrum analysis ; Water</subject><ispartof>Science (American Association for the Advancement of Science), 2013-01, Vol.339 (6117), p.292-296</ispartof><rights>Copyright © 2013 American Association for the Advancement of Science</rights><rights>Copyright © 2013, American Association for the Advancement of Science</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a510t-1fac1e4b69f351bb4fb7afcd30405ccdba58808dda277c10ff8cd3c0d0d7f1433</citedby><cites>FETCH-LOGICAL-a510t-1fac1e4b69f351bb4fb7afcd30405ccdba58808dda277c10ff8cd3c0d0d7f1433</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/23337861$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/23337861$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,2884,2885,27924,27925,58238,58471</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/23196909$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Lawrence, David J.</creatorcontrib><creatorcontrib>Feldman, William C.</creatorcontrib><creatorcontrib>Goldsten, John O.</creatorcontrib><creatorcontrib>Maurice, Sylvestre</creatorcontrib><creatorcontrib>Peplowski, Patrick N.</creatorcontrib><creatorcontrib>Anderson, Brian J.</creatorcontrib><creatorcontrib>Bazell, David</creatorcontrib><creatorcontrib>McNutt, Ralph L.</creatorcontrib><creatorcontrib>Nittler, Larry R.</creatorcontrib><creatorcontrib>Prettyman, Thomas H.</creatorcontrib><creatorcontrib>Rodgers, Douglas J.</creatorcontrib><creatorcontrib>Solomon, Sean C.</creatorcontrib><creatorcontrib>Weider, Shoshana Z.</creatorcontrib><title>Evidence for Water Ice Near Mercury's North Pole from MESSENGER Neutron Spectrometer Measurements</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Measurements by the Neutron Spectrometer on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft show decreases in the flux of epithermal and fast neutrons from Mercury's north polar region that are consistent with the presence of water ice in permanently shadowed regions. 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subjects | Backscattering Deposition Environmental conditions Fast neutrons Hydrogen Italian ices Latitude Mercury (planet) Mercury surface MESSENGER Mission Neutrons North Pole Onboard Online Planets Polar regions Radar Radio astronomy Scientific Concepts Signals Simulations Spacecraft Spectrum analysis Water |
title | Evidence for Water Ice Near Mercury's North Pole from MESSENGER Neutron Spectrometer Measurements |
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