{"id":790264,"date":"2024-10-14T10:41:57","date_gmt":"2024-10-14T15:41:57","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=790264"},"modified":"2024-10-14T10:41:57","modified_gmt":"2024-10-14T15:41:57","slug":"ice-on-the-moon-is-widespread-new-study-shows","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=790264","title":{"rendered":"Ice on the moon is widespread, new study shows"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<figure id=\"attachment_489756\" aria-describedby=\"caption-attachment-489756\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><figcaption id=\"caption-attachment-489756\" class=\"wp-caption-text\">View larger. | Moon-orbiting spacecraft from various nations confirmed the presence of water ice at the moon\u2019s poles in the early 2000s. The deposits of water ice lie in deep, permanently shadowed moon craters. Now new data from NASA\u2019s Lunar Reconnaissance Orbiter (LRO) suggests that ice on the moon is even more widespread than we thought. Image via NASA\/ GSFC\/ Arizona State University.<\/figcaption><\/figure>\n<ul>\n<li><strong>We know there\u2019s water ice in deep, shadowed craters<\/strong>, near the moon\u2019s poles. The ice remains frozen due to the lack of sunlight and extreme cold.<\/li>\n<li><strong>There\u2019s even more ice on the moon<\/strong> than we knew previously, according to a new NASA study. The evidence comes from data obtained by NASA\u2019s Lunar Reconnaissance Orbiter.<\/li>\n<li><strong>There are various theories to explain the origin of the ice<\/strong>, including impacts from comets or meteors, interior gas or chemical reactions.<\/li>\n<\/ul>\n<p>Exciting news! Six months ago, just as we were ending our spring fundraiser, EarthSky received a $50,000 gift, with a request that it be used to collect matching funds. Whoa! We were so thrilled and grateful. And now it\u2019s time to make good on our obligation. Please help us meet this match by donating to EarthSky today!<\/p>\n<p>The moon is an extremely dry place compared to Earth. There are no rivers or lakes, not even puddles. There are, however, water molecules bound in the regolith, and ice deposits, primarily near the South Pole. But now, a new study by NASA scientists shows that ice deposits are widespread and more extensive than first thought. The researchers said on October 3, 2024, that new analysis of data from NASA\u2019s Lunar Reconnaissance Orbiter (LRO) revealed the additional deposits.<\/p>\n<p>The researchers published their peer-reviewed findings in <em>The Planetary Science Journal<\/em> on October 2, 2024.<\/p>\n<h3>Ice on the moon more widespread than thought<\/h3>\n<p>Scientists already knew there were ice deposits in permanently shadowed regions (PSRs) in craters near the South Pole. But the new study reveals ice deposits well outside of that region.<\/p>\n<p>Timothy McClanahan at NASA\u2019s Goddard Space Flight Center in Greenbelt, Maryland, is the lead author of the study. He said:<\/p>\n<blockquote>\n<p>We find that there is widespread evidence of water ice within PSRs outside the South Pole, towards at least 77 degrees south latitude. Our model and analysis show that greatest ice concentrations are expected to occur near the PSRs\u2019 coldest locations below 75 Kelvin (-198\u00b0C or -325\u00b0F) and near the base of the PSRs\u2019 poleward-facing slopes.<\/p>\n<\/blockquote>\n<p>The researchers don\u2019t know yet exactly how much ice there is or how deep it may be buried. McClanahan continued:<\/p>\n<blockquote>\n<p>We can\u2019t accurately determine the volume of the PSRs\u2019 ice deposits or identify if they might be buried under a dry layer of regolith. However, we expect that for each surface 1.2 square yards (1 square meter) residing over these deposits there should be at least about five more quarts (five more liters) of ice within the surface top 3.3 feet (1 meter), as compared to their surrounding areas.<\/p>\n<\/blockquote>\n<figure id=\"attachment_489843\" aria-describedby=\"caption-attachment-489843\" style=\"width: 800px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/earthsky.org\/upl\/2024\/10\/moon-permanently-shadowed-regions-LOLA-LRO-October-3-2024.jpeg\" alt=\"Circle with mottled gray interior and many small irregular blue spots. 2 white dashed lines and 1 white dashed ring form a bullseye pattern. Black text labels are outside the circle.\" width=\"800\" height=\"784\" class=\"size-full wp-image-489843\" srcset=\"https:\/\/earthsky.org\/upl\/2024\/10\/moon-permanently-shadowed-regions-LOLA-LRO-October-3-2024.jpeg 800w, https:\/\/earthsky.org\/upl\/2024\/10\/moon-permanently-shadowed-regions-LOLA-LRO-October-3-2024-300x294.jpeg 300w, https:\/\/earthsky.org\/upl\/2024\/10\/moon-permanently-shadowed-regions-LOLA-LRO-October-3-2024-768x753.jpeg 768w\" sizes=\"auto, (max-width: 800px) 100vw, 800px\"\/><figcaption id=\"caption-attachment-489843\" class=\"wp-caption-text\">View larger. | This map shows the distribution of permanently shadowed regions (PSRs), in blue, around the lunar South Pole. The PSRs reach up to about 80 degrees south latitude. The elevation map is from Lunar Orbiter Laser Altimeter instrument on NASA\u2019s Lunar Reconnaissance Orbiter (LRO) spacecraft. Image via NASA\/ GSFC\/ Timothy P. McClanahan.<\/figcaption><\/figure>\n<h3>Lunar Reconnaissance Orbiter reveals ice deposits<\/h3>\n<p>How did the researchers find the ice deposits? They used data from instruments on NASA\u2019s Lunar Reconnaissance Orbiter (LRO). In particular, the Lunar Exploration Neutron Detector (LEND) instrument and LEND\u2019s Collimated Sensor for Epithermal Neutrons (CSETN). The instruments measured moderate-energy or \u201cepithermal\u201d neutrons on the lunar surface. Neutrons originate from intense, high-energy cosmic rays, which come from cosmic events such as exploding stars. Along with protons, they make up the nucleus of every atom except ordinary hydrogen. Eventually, some of the cosmic rays impact the moon. They break up the already existing atoms in the regolith and create subatomic neutrons.<\/p>\n<p>The neutrons can collide with other atoms in the regolith. As a result, some of them will be ejected out into space. LEND can then easily detect them, since there is virtually no atmosphere on the moon.<\/p>\n<p>How does that help find the ice? The water in the ice is made of hydrogen atoms. And hydrogen atoms have a similar mass to neutrons. So when a neutron collides with a hydrogen atom, the neutron loses more energy than it would from colliding with most other atoms. That tells scientists the atom it collided with was a hydrogen atom. Which means water, frozen as ice since it can\u2019t be liquid.<\/p>\n<h3>How did the ice get there?<\/h3>\n<p>Since the moon has no other liquid water and no atmosphere to speak of, how did the ice get there? There are three main possibilities. One is that it is delivered by comet or meteor impacts. Another is that it originates as gas from the interior of the moon itself that freezes on the surface. Chemical reactions between hydrogen in the solar wind and oxygen in the lunar regolith could also produce the ice.<\/p>\n<p>The ice can persist for billions of years because it is in the permanently shadowed regions (PSRs) of deep craters near the poles. So the ice never sees any sunlight, and therefore the PSRs are also extremely cold. In such regions, there might even be enough ice for future astronauts to mine.<\/p>\n<p>The findings are good news for the prospect of human settlement on the moon in the future. The ice, melted as water, could be used not only for drinking, but also to make rocket fuel, energy and breathable air. It could even be used to help protect from radiation.<\/p>\n<p>Bottom line: A new NASA study of permanently shadowed regions near the lunar South Pole shows that there is a lot more water ice on the moon than previously thought.<\/p>\n<p>Source: Evidence for Widespread Hydrogen Sequestration within the Moon\u2019s South Pole Cold Traps<\/p>\n<p>Via NASA<\/p>\n<p>Read more: What\u2019s the source of the ice at the moon\u2019s South Pole?<\/p>\n<p>Read more: Ice confirmed at moon\u2019s poles<\/p>\n<p><span class=\"cp-load-after-post\"\/><\/div>\n<div>\n<div class=\"post-author\">\n<h4>Paul Scott Anderson<\/h4>\n<p>                    View Articles\n                  <\/p><\/div>\n<div class=\"post-tags\">\n<h6 data-udy-fe=\"text_7c58270d\">About the Author:<\/h6>\n<p>Paul Scott Anderson has had a passion for space exploration that began when he was a child when he watched Carl Sagan\u2019s Cosmos. He studied English, writing, art and computer\/publication design in high school and college. He later started his blog The Meridiani Journal in 2005, which was later renamed Planetaria. He also later started the blog Fermi Paradoxica, about the search for life elsewhere in the universe.&#13;<br \/>\n&#13;<br \/>\nWhile interested in all aspects of space exploration, his primary passion is planetary science and SETI. In 2011, he started writing about space on a freelance basis with Universe Today. He has also written for SpaceFlight Insider and AmericaSpace and has also been published in The Mars Quarterly. He also did some supplementary writing for the iOS app Exoplanet.&#13;<br \/>\n&#13;<br \/>\nHe has been writing for EarthSky since 2018, and also assists with proofing and social media.<\/p>\n<\/p><\/div>\n<\/p><\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/earthsky.org\/space\/ice-on-the-moon-permanently-shadowed-regions-lro\/?rand=772280\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>View larger. | Moon-orbiting spacecraft from various nations confirmed the presence of water ice at the moon\u2019s poles in the early 2000s. The deposits of water ice lie in deep,&hellip; <\/p>\n","protected":false},"author":1,"featured_media":790265,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[46],"tags":[],"class_list":["post-790264","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-earth-sky"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/790264","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=790264"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/790264\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/790265"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=790264"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=790264"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=790264"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}