{"id":375881,"date":"2026-09-05T10:06:03","date_gmt":"2026-09-05T10:06:03","guid":{"rendered":"https:\/\/wolfscientific.com\/?p=375881"},"modified":"2026-09-05T10:06:03","modified_gmt":"2026-09-05T10:06:03","slug":"plutos-core-nitrogen-ice-layer-free-of-craters-and-liquid-nitrogen-recoagulating-at-the-boundaries-of-convection-cells","status":"publish","type":"post","link":"https:\/\/wolfscientific.com\/?p=375881","title":{"rendered":"Pluto&#8217;s Core: Nitrogen Ice Layer Free of Craters and Liquid Nitrogen Recoagulating at the Boundaries of Convection Cells"},"content":{"rendered":"<p>**Investigating Pluto&#8217;s Surface: Discoveries from New Horizons on Sputnik Planitia**<\/p>\n<p>In July 2015, NASA&#8217;s New Horizons spacecraft achieved a groundbreaking flyby of Pluto, transmitting intricate images and information of the faraway dwarf planet. Among its most fascinating findings was a panchromatic image of Sputnik Planitia, the luminous plain that constitutes the left segment of Pluto&#8217;s &#8220;heart.&#8221; The image, processed at a resolution of approximately 300 meters per pixel, provided revelations about a complex network of dark lines and designs on Pluto&#8217;s frigid surface.<\/p>\n<p>**Dark Features on Sputnik Planitia**<\/p>\n<p>The images showcased polygonal cells on the ice sheet, divided by dark lines stretching for tens of kilometers. These lines follow the seams of the cells and are surrounded by softer dark halos that extend significantly beyond the slender lines they encase. In 2023, a team headed by Alan Stern, the principal investigator of New Horizons, offered an explanation for these characteristics in The Planetary Science Journal. They suggest that the dark lines denote regions where liquid nitrogen surfaced and accumulated on the outer layer.<\/p>\n<p>**Comprehending the Icy Landscape**<\/p>\n<p>Sputnik Planitia, an extensive nitrogen-rich ice expanse, covers about 850 kilometers in the east-west direction and 1,500 kilometers in the north-south direction, situated within an ancient impact basin. It exhibits cellular plains with polygons ranging from 20 to 35 kilometers in diameter, interpreted as the upper portions of slow-moving convection cells. This area is particularly notable for its lack of impact craters, indicating continuous convective resurfacing.<\/p>\n<p>The dark lines are categorized as Discrete Dark, Narrow Features, while the adjacent halos are referred to as Diffuse Dark Aprons. These aprons appear roughly 0.10 darker against the mean broadband albedo of the ice sheet, which stands at 0.8, similar to Earth&#8217;s polar ice. Unlike the reddish deposits resulting from atmospheric haze, the aprons maintain a more neutral hue. The publication proposes that rising liquid may either pull dark material from below or modify the porosity of the surface ice, influencing its light-scattering characteristics.<\/p>\n<p>**Possibility of Liquid Nitrogen**<\/p>\n<p>Even with Pluto&#8217;s icy surface temperature hovering around 37 kelvin, the existence of liquid nitrogen is not out of the question. Nitrogen requires pressures at or above its triple point of 12,523 pascals to become liquid. Considering Pluto&#8217;s gravitational force and ice density, this pressure can be reached at depths of about 20 meters. Although heat conduction could potentially melt the ice at depths ranging from 300 meters to 1.4 kilometers, an external mechanism is necessary to provide the warmth due to the convective cooling of the ice sheet&#8217;s foundation.<\/p>\n<p>**Deciphering the Puzzle**<\/p>\n<p>The study delves into potential explanations for the emergence of liquid nitrogen. Topographic changes during a Milankovitch cycle might generate frictional heat as ice shifts, but this is considered inadequate. Another theory is that nitrogen within water ice bedrock could reach melting points through geological phenomena. The predominant hypothesis, however, revolves around the stresses and grain development resulting from ice thinning, which leads to decreased convection and subsequent heating.<\/p>\n<p>**Difficulties and Modeling**<\/p>\n<p>The team simulates the possible ascent of liquid nitrogen through subsurface dikes, likening the process to volcanic activity. Nonetheless, these modeled fractures are narrower than what New Horizons&#8217; cameras could discern. The proposed eruptions, characterized as sporadic events lasting from hours to days, suggest that the dark lines indicate surface pools instead of the eruption sites themselves.<\/p>\n<p>**Further Exploration and Laboratory Experiments**<\/p>\n<p>The findings, while enlightening, rely on models that await validation. Essential parameters derived from other materials require confirmation in cryogenic laboratories on Earth. In the meantime, to achieve a thorough understanding, additional exploration of Pluto, especially areas not yet observed in high resolution, is essential.<\/p>\n<p>New Horizons continues to enhance our comprehension of Pluto&#8217;s geological processes, challenging our preconceptions about remote icy planets and emphasizing the necessity for future missions and Earth-based studies to uncover these cosmic enigmas.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>**Investigating Pluto&#8217;s Surface: Discoveries from New Horizons on Sputnik Planitia** In July 2015, NASA&#8217;s New Horizons spacecraft achieved a groundbreaking flyby of Pluto, transmitting intricate images and information of the faraway dwarf planet. Among its most fascinating findings was a panchromatic image of Sputnik Planitia, the luminous plain that constitutes the left segment of Pluto&#8217;s [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":375882,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"Default","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[179],"class_list":["post-375881","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-source-scienceblog-com"],"_links":{"self":[{"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/posts\/375881","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=375881"}],"version-history":[{"count":0,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/posts\/375881\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=\/wp\/v2\/media\/375882"}],"wp:attachment":[{"href":"https:\/\/wolfscientific.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=375881"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=375881"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/wolfscientific.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=375881"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}