{"id":2093,"date":"2018-09-04T14:49:22","date_gmt":"2018-09-04T05:49:22","guid":{"rendered":"http:\/\/www.eri.u-tokyo.ac.jp\/en\/?p=2093"},"modified":"2018-10-03T08:34:59","modified_gmt":"2018-10-02T23:34:59","slug":"the-condition-of-eruption-column-collapse-part-1-a-reference-model-based-on-analytical-solutions-part-2-three%e2%80%90dimensional-3d-numerical-simulations-of-eruption-column-dynamics","status":"publish","type":"post","link":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/research\/2093\/","title":{"rendered":"The condition of eruption column collapse: Part 1. A reference model based on analytical solutions\/Part 2. Three\u2010dimensional (3D) numerical simulations of eruption column dynamics"},"content":{"rendered":"<p>The condition of eruption column collapse:<\/p>\n<p style=\"text-align: center\"><strong>Part 1. A reference model based on analytical solutions<\/strong><\/p>\n<p style=\"text-align: center\">Takehiro Koyaguchi\u00a0\u00a0\u00a0Yujiro J. Suzuki<br \/>\n<a href=\"https:\/\/doi.org\/10.1029\/2017JB015308\">https:\/\/doi.org\/10.1029\/2017JB015308<\/a><\/p>\n<p style=\"text-align: center\">Journal of Geophysical Research: Solid Earth, 123<\/p>\n<p>Abstract<br \/>\nThe critical condition at which an eruption column collapses to generate a pyroclastic flow (the column collapse condition) generally depends on magmatic properties, crater shape (radius, depth, and opening angle), and the magma supply rate through the volcanic conduit. Here, we propose a reference model for the column collapse condition based on analytical solutions of a one\u2010dimensional (1D) eruption column model and a quasi\u20101D conduit flow model, which considers the effects of the crater. In the reference model, the column collapse condition is expressed by a single surface in a dimensionless parameter space related to magma discharge rate, magma supply rate (per unit area) at the crater base, and the ratio of the cross\u2010sectional areas at the top and base of the crater. The dependence of the column collapse condition on magmatic properties is included in the normalization factors of these dimensionless parameters. Previous criteria for the column collapse condition, which were based on the relationship between water content and magma discharge rate and that between magma discharge rate and crater radius, are regarded as part of, or a projection of, the present reference model. The reference model provides a framework for a comprehensive analysis of the diverse scenarios resulting in column collapse during explosive eruptions.<\/p>\n<p style=\"text-align: center\"><strong>Part 2. Three\u2010dimensional (3D) numerical simulations of eruption column dynamics<\/strong><br \/>\nTakehiro Koyaguchi\u00a0\u00a0\u00a0Yujiro J. Suzuki\u00a0\u00a0\u00a0Kai Takeda\u00a0\u00a0\u00a0Satoshi Inagawa <a href=\"https:\/\/doi.org\/10.1029\/2017JB015308\">https:\/\/doi.org\/10.1029\/2017JB015308<\/a><\/p>\n<p style=\"text-align: center\">Journal of Geophysical Research: Solid Earth, 123<\/p>\n<p style=\"text-align: left\">Abstract<br \/>\nThe critical condition at which an eruption column collapses to generate a pyroclastic flow (the column collapse condition) generally depends on magmatic properties, crater shape (radius, depth, and opening angle), and the magma supply rate through the volcanic conduit. Here, we propose a reference model for the column collapse condition based on analytical solutions of a one\u2010dimensional (1D) eruption column model and a quasi\u20101D conduit flow model, which considers the effects of the crater. In the reference model, the column collapse condition is expressed by a single surface in a dimensionless parameter space related to magma discharge rate, magma supply rate (per unit area) at the crater base, and the ratio of the cross\u2010sectional areas at the top and base of the crater. The dependence of the column collapse condition on magmatic properties is included in the normalization factors of these dimensionless parameters. Previous criteria for the column collapse condition, which were based on the relationship between water content and magma discharge rate and that between magma discharge rate and crater radius, are regarded as part of, or a projection of, the present reference model. The reference model provides a framework for a comprehensive analysis of the diverse scenarios resulting in column collapse during explosive eruptions.<\/p>\n<p>Video: Partial collapse (click to see video)<\/p>\n<div style=\"width: 840px;\" class=\"wp-video\"><!--[if lt IE 9]><script>document.createElement('video');<\/script><![endif]-->\n<video class=\"wp-video-shortcode\" id=\"video-2093-1\" width=\"840\" height=\"473\" preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/partial_collapse.mp4?_=1\" \/><a href=\"http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/partial_collapse.mp4\">http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/partial_collapse.mp4<\/a><\/video><\/div>\n<p>Video: Oscilation (click to see video)<\/p>\n<div style=\"width: 840px;\" class=\"wp-video\"><video class=\"wp-video-shortcode\" id=\"video-2093-2\" width=\"840\" height=\"473\" preload=\"metadata\" controls=\"controls\"><source type=\"video\/mp4\" src=\"http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/oscilation.mp4?_=2\" \/><a href=\"http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/oscilation.mp4\">http:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-content\/uploads\/sites\/2\/2018\/09\/oscilation.mp4<\/a><\/video><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The condition of eruption column collapse: Part 1. A reference model based on analytical solutions Takehiro Ko &hellip; <a href=\"https:\/\/www.eri.u-tokyo.ac.jp\/en\/research\/2093\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;The condition of eruption column collapse: Part 1. A reference model based on analytical solutions\/Part 2. Three\u2010dimensional (3D) numerical simulations of eruption column dynamics&#8221;<\/span><\/a><\/p>\n","protected":false},"author":9,"featured_media":2094,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[11],"tags":[],"class_list":["post-2093","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-research"],"_links":{"self":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/2093"}],"collection":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/users\/9"}],"replies":[{"embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/comments?post=2093"}],"version-history":[{"count":9,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/2093\/revisions"}],"predecessor-version":[{"id":2143,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/posts\/2093\/revisions\/2143"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/media\/2094"}],"wp:attachment":[{"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/media?parent=2093"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/categories?post=2093"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.eri.u-tokyo.ac.jp\/en\/wp-json\/wp\/v2\/tags?post=2093"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}