{"id":300,"date":"2010-05-18T15:29:12","date_gmt":"2010-05-18T15:29:12","guid":{"rendered":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/?p=300"},"modified":"2015-07-18T15:33:01","modified_gmt":"2015-07-18T15:33:01","slug":"300","status":"publish","type":"post","link":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/2010\/05\/18\/300\/","title":{"rendered":"Identifying Complex AOM using Ultrahigh Resolution FT-ICR MS\/MS"},"content":{"rendered":"<h3><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\"><b>Identification of Atmospheric Organic Matter by Multi-Step Mass Spectrometric Analysis<\/b><\/span><\/h3>\n<div><em>Michigan Tech Research for Excellence Research Seed 2009-2010<\/em><\/div>\n<div><span class=\"ws11\" style=\"color: #800080; font-family: Tahoma;\"><b>\u00a0<\/b><\/span><\/div>\n<div>\n<div id=\"attachment_303\" style=\"width: 235px\" class=\"wp-caption alignright\"><a href=\"http:\/\/chem.sites.mtu.edu\/mazzoleni\/wp-content\/uploads\/2015\/07\/Tule_Fog_California_-_2005.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-303\" class=\"wp-image-303 size-medium\" src=\"http:\/\/chem.sites.mtu.edu\/mazzoleni\/wp-content\/uploads\/2015\/07\/Tule_Fog_California_-_2005-225x300.jpg\" alt=\"Image source: Wikipedia Commons Tule_Fog_California_-_2005.jpg\" width=\"225\" height=\"300\" srcset=\"http:\/\/chem.sites.mtu.edu\/mazzoleni\/wp-content\/uploads\/2015\/07\/Tule_Fog_California_-_2005-225x300.jpg 225w, http:\/\/chem.sites.mtu.edu\/mazzoleni\/wp-content\/uploads\/2015\/07\/Tule_Fog_California_-_2005-768x1024.jpg 768w\" sizes=\"auto, (max-width: 225px) 100vw, 225px\" \/><\/a><p id=\"caption-attachment-303\" class=\"wp-caption-text\">Image source: Wikipedia Commons Tule_Fog_California_-_2005.jpg<\/p><\/div>\n<p><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">Atmospheric organic matter (OM) associated with aerosol particles significantly influences the chemical and physical properties of aerosol particles.\u00a0 This suggests that atmospheric OM directly modulates the role that aerosol particles play in the atmosphere affecting the Earth&#8217;s climate.\u00a0 Although uncertain, it appears the combined effects of aerosol particles may lead to a large net reduction in the solar radiation absorbed by the Earth&#8217;s surface thus masking the true warming of the greenhouse gases.\u00a0 However, quantifying the magnitude of aerosol impact on climate is much more challenging than quantifying the effects of greenhouse gases.\u00a0 This is largely due to the fact that many aerosols are not directly emitted; rather they are formed in the atmosphere from various precursor gases.\u00a0 Identification of atmospheric OM is urgently needed to assess the chemical effect upon the physical properties of aerosol particles.\u00a0 Atmospheric OM is transformed in the atmosphere by a number of chemical oxidation processes.\u00a0 The transformations that increase the ability of aerosol to interact with water are the most crucial; therefore identification is focused on the polar organic compounds.\u00a0\u00a0 Since oxidation reactions are non-specific, this class of compounds is quite complex and spans the mass range of 100-1000 atomic mass units.\u00a0\u00a0\u00a0<\/span><\/p>\n<\/div>\n<div><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">\u00a0<\/span><\/div>\n<div><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">In this project, we focus on uniting the benefits of tandem mass spectrometry (MS) with the power of ultra-high resolution MS for comprehensive identification of atmospheric OM.\u00a0 This will be done using a multi-step approach.\u00a0 The first step includes a pre-screening of collected samples by ultra-high resolution and empirical formula generation.\u00a0 The second step involves development of tandem MS methods using conventional instrumentation (recently acquired).\u00a0 The third step moves the tandem MS analysis to a more powerful platform which includes an ultra-high resolution MS analysis of precursor and fragmented analytes from each MSn generation.\u00a0\u00a0<\/span><\/div>\n<div><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">\u00a0<\/span><\/div>\n<div><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">MS Student Jeffrey LeClair contributed to this project.\u00a0<\/span><\/div>\n<div>\n<hr \/>\n<p><strong><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">Representative Publication:<\/span><\/strong><\/p>\n<\/div>\n<div>\n<p>LeClair, J.P., J.L. Collett and L.R. Mazzoleni, <strong>Fragmentation Analysis of Water-Soluble Atmospheric Organic Matter using Ultrahigh-Resolution Mass Spectrometry<\/strong>, <em>Environmental Science and Technology<\/em>, 46(8), 4312\u20134322, 2012. <a href=\"http:\/\/pubs.acs.org\/doi\/full\/10.1021\/es203509b\" target=\"_blank\">View text here<\/a>.<\/p>\n<p><span class=\"ws11\" style=\"color: #000000; font-family: Tahoma;\">\u00a0<\/span><\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Identification of Atmospheric Organic Matter by Multi-Step Mass Spectrometric Analysis Michigan Tech Research for Excellence Research Seed 2009-2010 \u00a0 Atmospheric organic matter (OM) associated with aerosol particles significantly influences the chemical and physical properties of aerosol particles.\u00a0 This suggests that atmospheric OM directly modulates the role that aerosol particles play in the atmosphere affecting the Earth&#8217;s climate.\u00a0 Although uncertain, it<\/p>\n","protected":false},"author":2,"featured_media":302,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[6,21,10],"tags":[19,27,26,22],"class_list":["post-300","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aqueous-phase-chemistry","category-projects","category-research","tag-biomass-burning","tag-fog","tag-leclair","tag-projects"],"aioseo_notices":[],"views":2165,"_links":{"self":[{"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/posts\/300","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/comments?post=300"}],"version-history":[{"count":3,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/posts\/300\/revisions"}],"predecessor-version":[{"id":307,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/posts\/300\/revisions\/307"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/media\/302"}],"wp:attachment":[{"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/media?parent=300"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/categories?post=300"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/chem.sites.mtu.edu\/mazzoleni\/index.php\/wp-json\/wp\/v2\/tags?post=300"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}