{"id":8254,"date":"2026-03-02T11:50:42","date_gmt":"2026-03-02T10:50:42","guid":{"rendered":"https:\/\/academiespatiale.fr\/?post_type=tribe_events&#038;p=8254"},"modified":"2026-03-02T11:51:40","modified_gmt":"2026-03-02T10:51:40","slug":"seminaire-latmos-observations-of-lunar-surface-origin-and-exospheric-ions-by-the-kaguya-ion-mass-analyzer","status":"publish","type":"tribe_events","link":"https:\/\/academiespatiale.fr\/index.php\/event\/seminaire-latmos-observations-of-lunar-surface-origin-and-exospheric-ions-by-the-kaguya-ion-mass-analyzer\/","title":{"rendered":"[S\u00e9minaire LATMOS] Observations of lunar surface-origin and exospheric ions by the Kaguya Ion Mass Analyzer"},"content":{"rendered":"<div  class=\"tribe-events-schedule tribe-clearfix\" >\n\t<p class=\"tribe-events-schedule__datetime\">\n\t\t<span class=\"tribe-events-schedule__date tribe-events-schedule__date--start\">\n\t\t\t3 mars\t\t<\/span>\n\n\t\t\t\t\t<span class=\"tribe-events-schedule__separator tribe-events-schedule__separator--date\">\n\t\t\t\t : \t\t\t<\/span>\n\t\t\t<span class=\"tribe-events-schedule__time tribe-events-schedule__time--start\">\n\t\t\t\t11h30\t\t\t<\/span>\n\t\t\n\t\t\t\t\t\t\t\t\t<span class=\"tribe-events-schedule__separator tribe-events-schedule__separator--time\">\n\t\t\t\t\t&#8211;\t\t\t\t<\/span>\n\t\t\t\n\t\t\t\t\t\t\t<span class=\"tribe-events-schedule__time tribe-events-schedule__time--end\">\n\t\t\t\t\t13h00\t\t\t\t<\/span>\n\t\t\t\n\t\t\t\t\t\t<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-cover is-light\" style=\"padding-top:var(--wp--preset--spacing--80);padding-right:var(--wp--preset--spacing--80);padding-bottom:var(--wp--preset--spacing--80);padding-left:var(--wp--preset--spacing--80)\"><span aria-hidden=\"true\" class=\"wp-block-cover__background has-white-background-color has-background-dim-100 has-background-dim\"><\/span><div class=\"wp-block-cover__inner-container is-layout-constrained wp-container-core-cover-is-layout-10bc4538 wp-block-cover-is-layout-constrained\">\n<div class=\"wp-block-columns has-text-color has-link-color wp-elements-e673af4000d0b3c096a66b181f7b0bbd is-layout-flex wp-container-core-columns-is-layout-deb2fee4 wp-block-columns-is-layout-flex\" style=\"color:#b1b1b1;margin-top:-25px;margin-bottom:20px;padding-top:0;padding-right:0;padding-bottom:0;padding-left:0;font-size:15px\">\n<div class=\"wp-block-column has-text-color has-link-color wp-elements-5a4d4e7b16cdb21f05469acdf2368671 is-layout-flow wp-block-column-is-layout-flow\" style=\"color:#a1a1a1;padding-top:0;padding-bottom:0;font-size:15px;font-style:normal;font-weight:100;flex-basis:100%\"><div class=\"aioseo-breadcrumbs\"><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"https:\/\/academiespatiale.fr\" title=\"Home\">Home<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"https:\/\/academiespatiale.fr\/index.php\/events\/\" title=\"\u00c9v\u00e8nements\">\u00c9v\u00e8nements<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"https:\/\/academiespatiale.fr\/index.php\/events\/categorie\/seminaire\/\" title=\"S\u00e9minaire \/ webinaire\">S\u00e9minaire \/ webinaire<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\t[S\u00e9minaire LATMOS] Observations of lunar surface-origin and exospheric ions by the Kaguya Ion Mass Analyzer\n\t\t<\/span><\/div><\/div>\n<\/div>\n\n\n\n<p class=\"has-text-align-left\">Mardi 3 mars, Kei Masunaga (Yamataga Univ.) donnera un s\u00e9minaire intitul\u00e9 \u00ab\u00a0Observations of lunar surface-origin and exospheric ions by the Kaguya Ion Mass Analyzer\u00a0\u00bb. Le s\u00e9minaire aura lieu \u00e0 11h30 au LATMOS \u00e0 Guyancourt en salle 2202. Il sera retransmis sur Zoom.<\/p>\n\n\n\n<p class=\"has-text-align-left\"><em>On Tuesday March 3th, Kei Masunaga (Yamataga Univ.) will give a seminar on the \u00ab\u00a0Observations of lunar surface-origin and exospheric ions by the Kaguya Ion Mass Analyzer\u00a0\u00bb. The seminar will take place at 11:30am in LATMOS Guyancourt in room 2202. It will be retransmitted on Zoom.<\/em><\/p>\n\n\n\n<div class=\"wp-block-columns are-vertically-aligned-center is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\">\n<hr class=\"wp-block-separator has-alpha-channel-opacity\" style=\"margin-top:var(--wp--preset--spacing--60);margin-bottom:var(--wp--preset--spacing--60)\"\/>\n\n\n\n<p class=\"has-text-align-center\"><strong>Observations of lunar surface-origin and exospheric ions by the Kaguya Ion Mass Analyzer<\/strong><\/p>\n\n\n\n<p class=\"has-text-align-center\"><strong>Mardi 3 mars 2026<\/strong><br><strong>11h30<br><\/strong><br>LATMOS<br>Salle 2202<br>11, boulevard d&rsquo;Alembert<br>Guyancourt<\/p>\n\n\n\n<p class=\"has-text-align-center has-small-font-size\">&gt;&gt;&gt;&nbsp;<strong>VISIOCONFERENCE&nbsp;<\/strong>&lt;&lt;&lt;<br>Le s\u00e9minaire sera retransmis sur Zoom CNRS.<br>Contacter audrey.chatain [at] latmos.ipsl.fr pour obtenir le lien.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure data-wp-context=\"{&quot;imageId&quot;:&quot;69e757fca5f5b&quot;}\" data-wp-interactive=\"core\/image\" data-wp-key=\"69e757fca5f5b\" class=\"aligncenter size-full wp-lightbox-container\"><img loading=\"lazy\" decoding=\"async\" width=\"2560\" height=\"1664\" data-wp-class--hide=\"state.isContentHidden\" data-wp-class--show=\"state.isContentVisible\" data-wp-init=\"callbacks.setButtonStyles\" data-wp-on--click=\"actions.showLightbox\" data-wp-on--load=\"callbacks.setButtonStyles\" data-wp-on-window--resize=\"callbacks.setButtonStyles\" src=\"https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-scaled.jpg\" alt=\"\" class=\"wp-image-8256\" srcset=\"https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-scaled.jpg 2560w, https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-300x195.jpg 300w, https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-1024x666.jpg 1024w, https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-768x499.jpg 768w, https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-1536x998.jpg 1536w, https:\/\/academiespatiale.fr\/wp-content\/uploads\/2026\/03\/2026_03_LATMOS-seminars_Masunaga-2048x1331.jpg 2048w\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" \/><button\n\t\t\tclass=\"lightbox-trigger\"\n\t\t\ttype=\"button\"\n\t\t\taria-haspopup=\"dialog\"\n\t\t\taria-label=\"Agrandir\"\n\t\t\tdata-wp-init=\"callbacks.initTriggerButton\"\n\t\t\tdata-wp-on--click=\"actions.showLightbox\"\n\t\t\tdata-wp-style--right=\"state.imageButtonRight\"\n\t\t\tdata-wp-style--top=\"state.imageButtonTop\"\n\t\t>\n\t\t\t<svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" width=\"12\" height=\"12\" fill=\"none\" viewBox=\"0 0 12 12\">\n\t\t\t\t<path fill=\"#fff\" d=\"M2 0a2 2 0 0 0-2 2v2h1.5V2a.5.5 0 0 1 .5-.5h2V0H2Zm2 10.5H2a.5.5 0 0 1-.5-.5V8H0v2a2 2 0 0 0 2 2h2v-1.5ZM8 12v-1.5h2a.5.5 0 0 0 .5-.5V8H12v2a2 2 0 0 1-2 2H8Zm2-12a2 2 0 0 1 2 2v2h-1.5V2a.5.5 0 0 0-.5-.5H8V0h2Z\" \/>\n\t\t\t<\/svg>\n\t\t<\/button><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<p>Abstract:<\/p>\n\n\n\n<p>Low-energy ions associated with the lunar surface and exosphere provide valuable information on surface composition and volatile-related processes on airless bodies. In this seminar, I will present an overview of ion observations obtained by the Ion Mass Analyzer (IMA) onboard the Kaguya spacecraft, focusing on the spatial and temporal characteristics of lunar-origin ions.<br>Using approximately one year of time-of-flight (TOF) data, we examined the distributions of multiple ion species commonly observed in the lunar environment, including He\u207a, C\u207a, O\u207a, Na\u207a, Al\u207a, K\u207a, and Ar\u207a, primarily in the low-energy range below 300 eV. Assuming that these ions are accelerated by the motional electric field of the solar wind prior to detection, the observed fluxes were mapped to corresponding regions on the lunar surface. The results reveal systematic asymmetries in ion occurrence, with enhanced fluxes on the dawnside compared to the duskside.<br>In addition to major atomic ions, the TOF spectra occasionally exhibit residual signals at mass-to-charge ratios consistent with water-related ion species. These signals show a tendency to be more frequently observed at high latitudes than at low latitudes, qualitatively consistent with previously reported distributions of lunar water inferred from remote sensing observations. These observations suggest that ion measurements can offer complementary information on the presence and activity of lunar water.<br>Overall, this seminar shows how ion observations by Kaguya\/IMA provide information on various lunar-origin ion species, including water-related ions, and how these results are relevant to future ion measurements, including the Martian Moons Exprolation mission.<\/p>\n\n\n\n<p class=\"has-background-color-background-color has-background\">Previous LATMOS seminars are now available on Youtube:<br><a href=\"https:\/\/youtube.com\/playlist?list=PLVDexVGJCe0duF4LANooppLeGAdmlDRnN&amp;si=mi5wjsxRsKgQQ6iC\" target=\"_blank\" rel=\"noopener\" title=\"\">https:\/\/youtube.com\/playlist?list=PLVDexVGJCe0duF4LANooppLeGAdmlDRnN&amp;si=mi5wjsxRsKgQQ6iC<\/a><br><\/p>\n<\/div><\/div>\n\n\n\t<div  class=\"tribe-block tribe-block__events-link\" >\n\t\t<div class=\"tribe-events tribe-common\">\n\t\t\t<div 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