{"id":147,"date":"2021-07-09T13:04:56","date_gmt":"2021-07-09T17:04:56","guid":{"rendered":"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/?page_id=147"},"modified":"2021-07-09T14:42:13","modified_gmt":"2021-07-09T18:42:13","slug":"thermodynamics","status":"publish","type":"page","link":"https:\/\/www.geol.umd.edu\/facilities\/lmdr\/thermodynamics\/","title":{"rendered":"Thermodynamics"},"content":{"rendered":"<div id=\"pl-147\"  class=\"panel-layout\" ><div id=\"pg-147-0\"  class=\"panel-grid panel-no-style\" ><div id=\"pgc-147-0-0\"  class=\"panel-grid-cell\" ><div id=\"panel-147-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child panel-last-child\" data-index=\"0\" ><div\n\t\t\t\n\t\t\tclass=\"so-widget-sow-editor so-widget-sow-editor-base\"\n\t\t\t\n\t\t>\n<div class=\"siteorigin-widget-tinymce textwidget\">\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/first-and-second-laws-of-thermodynamics\/\">Combined First and Second Laws<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/thermodynamic-components-of-phases-and-systems\/\">Thermodynamic Components<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/chemical-potential\/\">Chemical Potential<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/fugacity-definitions-concepts-and-geology\/\">Fugacity<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/the-phase-rule\/\">The Phase Rule<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/matter\/\">Matter<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/the-stress-and-pressure-page\/\">Stress and Pressure<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/fractures-and-fracturing\/\">Fractures and Fracturing<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/vapor-melt-and-mineral-melt-partitioning\/\">Vapor\/Melt and Mineral\/Vapor Partitioning<\/a><\/p>\n<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/lmdr-temp\/thermodynamics\/activity-coefficient-tutorial\/\">Activity coefficients in low-T aqueous solutions<\/a><\/p>\n<\/div>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"<p>Combined First and Second Laws Thermodynamic Components Chemical Potential Fugacity The Phase Rule Matter Stress and Pressure Fractures and Fracturing Vapor\/Melt and Mineral\/Vapor Partitioning Activity coefficients in low-T aqueous solutions<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"default","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center 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