{"id":788994,"date":"2024-09-13T16:28:50","date_gmt":"2024-09-13T21:28:50","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=788994"},"modified":"2024-09-13T16:28:50","modified_gmt":"2024-09-13T21:28:50","slug":"scientists-recreate-mars-spiders-in-the-lab","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=788994","title":{"rendered":"Scientists Recreate Mars Spiders in the Lab"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div>\n<p>In 2003, strange features on Mars\u2019s surface got scientists\u2019 \u201cspidey senses\u201d tingling when they saw them. That\u2019s when unusual \u201canareiform terrain\u201d landforms appeared in images from the Mars Reconnaissance Orbiter. They\u2019ve returned each year, spreading across the southern hemisphere surface. <\/p>\n<p><span id=\"more-168525\"\/><\/p>\n<p>At first, nobody knew what caused these weird wrinkly spider-like formations. Now, NASA researchers have duplicated them in the lab to explain their existence. No doubt about it, though, these Mars spiders look weird. Some of them stretch across a kilometer and generally appear in clusters. <\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large\"><figcaption class=\"wp-element-caption\">Since discovering them in 2003 via images from orbiters, scientists have marveled at these Mars spiders sprawled across the southern hemisphere of Mars. No one is entirely sure how these geologic features are created but lab simulations may provide clues. Credit: NASA\/JPL-Caltech\/University of Arizona<\/figcaption><\/figure>\n<\/div>\n<p>Since carbon dioxide is common on Mars, scientists figured it had something to do with creating these weird formations. They used the \u201cKieffer model\u201d to delve into the history of Mars spiders. That model explains how carbon dioxide ice slabs under the surface trap gas as it sublimates (turns to gas), usually during southern hemisphere spring.<\/p>\n<p>Sunlight heats the surface and shines through transparent slabs of carbon dioxide. Those ice layers build up each winter. The soil beneath the ice absorbs heat from the Sun and causes the ice closest to it to sublimate. Gas pressure builds up, which cracks the ice and allows gas to escape. As it seeps upward, the gas takes with it a stream of dark dust and sand from the soil that lands on the surface of the ice. Those deposits take the form of spidery landforms.<\/p>\n<h3 class=\"wp-block-heading\" id=\"h-confirming-mars-spiders\">Confirming Mars Spiders<\/h3>\n<p>To see if that process is what\u2019s creating Mars spiders, NASA JPL scientists, led by Lauren McKeown, decided to simulate Mars conditions in their lab. \u201cThe spiders are strange, beautiful geologic features in their own right,\u201d said McKeown. \u201cThese experiments will help tune our models for how they form.\u201d<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-medium\"><img loading=\"lazy\" decoding=\"async\" width=\"435\" height=\"580\" src=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1-435x580.jpg\" alt=\"The DUSTIE chamber at JPL. This is where scientists simulated the surface conditions under which Mars spiders form. Credit: NASA\/JPL-Caltech.\" class=\"wp-image-168532\" srcset=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1-435x580.jpg 435w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1-768x1024.jpg 768w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1-188x250.jpg 188w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1-1152x1536.jpg 1152w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e1-pia26405-a-look-inside-of-jpls-dustie-rotated-1.jpg 1500w\" sizes=\"auto, (max-width: 435px) 100vw, 435px\"\/><figcaption class=\"wp-element-caption\">The DUSTIE chamber at JPL. This is where scientists simulated the surface conditions under which Mars spiders form. Credit: NASA\/JPL-Caltech.<\/figcaption><\/figure>\n<\/div>\n<p>Not that it\u2019s easy to replicate Mars on Earth, even in strict laboratory conditions. For Mc Keown and her team, the hardest part was re-creating conditions found on the Martian polar surface. That region experiences extremely low air pressure. Seasonal changes bring the air and surface temperatures down to a chilly -301 degrees Fahrenheit (minus 185 degrees Celsius). To make it work, the team used a liquid-nitrogen-cooled test chamber at JPL\u2014the Dirty Under-vacuum Simulation Testbed for Icy Environments, or DUSTIE.<\/p>\n<p>\u201cI love DUSTIE. It\u2019s historic,\u201d Mc Keown said, noting that the wine barrel-size chamber was used to test a prototype of a rasping tool designed for NASA\u2019s Mars Phoenix lander. For their experiment, the team chilled Martian soil simulant in a container dipped into a nitrogen bath. Then they put the whole thing into DUSTIE and replaced Earth-normal pressure with Mars air pressure. Carbon dioxide gas flowed in and condensed to ice. The next step was to put a heater inside to simulate Martian conditions in early spring. The team did this several times before the experiment created simulated \u201cspiders\u201d similar to those on Mars.<\/p>\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-medium\"><img loading=\"lazy\" decoding=\"async\" width=\"580\" height=\"435\" src=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-580x435.jpg\" alt=\"Mars spider-like formations in soil simulant created during experiments at NASA\/JPL in the  DUSTIE chamber. Credit: NASA\/JPL-Caltech.\" class=\"wp-image-168529\" srcset=\"https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-580x435.jpg 580w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-1024x768.jpg 1024w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-250x188.jpg 250w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-768x576.jpg 768w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-1536x1152.jpg 1536w, https:\/\/www.universetoday.com\/wp-content\/uploads\/2024\/09\/e2-PIA26406-Cracks_Forming_in_Carbon_Dioxide_Ice-2048x1536.jpg 2048w\" sizes=\"auto, (max-width: 580px) 100vw, 580px\"\/><figcaption class=\"wp-element-caption\">Mars spider-like formations in soil simulant created during experiments at NASA\/JPL in the DUSTIE chamber. Credit: NASA\/JPL-Caltech.<\/figcaption><\/figure>\n<\/div>\n<h3 class=\"wp-block-heading\" id=\"h-the-next-steps\">The Next Steps<\/h3>\n<p>That simulation created plumes of carbon dioxide gas escaping from the soil simulant. It\u2019s close to what happens on Mars, but not quite. So, the next step is to do the same experiment and use a simulated Sun to heat the surface materials. If that produces the same results, then the team has a good chance of proving this is what happens on Mars.<\/p>\n<p>However, Mars being what it is\u2014there are still a lot of questions about why the spiders only form in the southern hemisphere at spring. Since subsurface carbon dioxide ice isn\u2019t limited to that region of the planet, why don\u2019t spiders form in other places? One possibility is that these aren\u2019t recent features. They could be left over from a more active time in the planet\u2019s past. Maybe the climate was very different when they formed. Or something catastrophic happened to enable the formation and growth of spiders in the southern hemisphere.<\/p>\n<p>The study at JPL is a good step forward in understanding the Martian terrain. It confirms several formation processes described by the Kieffer model. Of course, it would be really cool to visit those spiders someday. For now, however, lab work is as close as it gets to explaining them. Future rovers and landers could be used to study those landforms up close and personal. However, there aren\u2019t any planned in the near future, and no other spacecraft has landed in the spider-rich southern hemisphere region. For now, scientists will continue testing the lab to understand the conditions that make these strange-looking features.<\/p>\n<h4 class=\"wp-block-heading\" id=\"h-for-more-information\">For More Information<\/h4>\n<p>NASA Scientists Re-Create Mars \u2018Spiders\u2019 in a Lab for the First Time<br \/>A Lab-scale Investigation of the Mars Kieffer Model<\/p>\n<div class=\"sharedaddy sd-block sd-like jetpack-likes-widget-wrapper jetpack-likes-widget-unloaded\" id=\"like-post-wrapper-24000880-168525-66e4ac3d8abe8\" data-src=\"https:\/\/widgets.wp.com\/likes\/?ver=13.2#blog_id=24000880&amp;post_id=168525&amp;origin=www.universetoday.com&amp;obj_id=24000880-168525-66e4ac3d8abe8&amp;n=1\" data-name=\"like-post-frame-24000880-168525-66e4ac3d8abe8\" data-title=\"Like or Reblog\">\n<h3 class=\"sd-title\">Like this:<\/h3>\n<p><span class=\"button\"><span>Like<\/span><\/span> <span class=\"loading\">Loading&#8230;<\/span><\/p>\n<p><span class=\"sd-text-color\"\/><\/div>\n<\/p><\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/www.universetoday.com\/168525\/scientists-recreate-mars-spiders-in-the-lab\/?rand=772204\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>In 2003, strange features on Mars\u2019s surface got scientists\u2019 \u201cspidey senses\u201d tingling when they saw them. That\u2019s when unusual \u201canareiform terrain\u201d landforms appeared in images from the Mars Reconnaissance Orbiter.&hellip; <\/p>\n","protected":false},"author":1,"featured_media":788995,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[13],"tags":[],"class_list":["post-788994","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-genaero"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/788994","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=788994"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/788994\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/788995"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=788994"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=788994"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=788994"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}