{"id":9408,"date":"2021-11-09T07:54:42","date_gmt":"2021-11-09T06:54:42","guid":{"rendered":"https:\/\/www.icpf.cas.cz\/?p=9408"},"modified":"2021-11-09T08:02:08","modified_gmt":"2021-11-09T07:02:08","slug":"carbon-isotope-measurements-as-a-tool-to-gain-insight-into-atmospheric-processes","status":"publish","type":"post","link":"https:\/\/www.icpf.cas.cz\/en\/carbon-isotope-measurements-as-a-tool-to-gain-insight-into-atmospheric-processes\/","title":{"rendered":"Carbon isotope measurements as a tool to gain insight into atmospheric processes"},"content":{"rendered":"<p><a href=\"https:\/\/cesnet.zoom.us\/j\/94167862089\" target=\"_blank\" rel=\"noopener\">https:\/\/cesnet.zoom.us\/j\/94167862089<\/a><\/p>\n<p style=\"text-align: justify;\">Although aerosol particles are a small part of the atmosphere, they have a significant impact on, e.g., air quality, climate, or health. Isotope analysis of atmospheric aerosols is a possible way to study the processes that take place in this atmospheric component. Carbon is one of the relatively abundant elements in aerosols, so isotopic composition analysis of stable carbon <sup>13<\/sup>C can be used, for example, to roughly analyze the sources of these particles. A parameter that may provide more insight into the behavior of particles in the atmosphere is the distribution of \u03b4<sup>13<\/sup>C between the aerosol and gas phases. This inter-phase distribution of \u03b4<sup>13<\/sup>C as a function of different seasonal sources of <sup>13<\/sup>C was the focus of our research. In this lecture, the results of a seasonal study of \u03b4<sup>13<\/sup>C measurements in the fine aerosol and gaseous phase at the Prague-Suchdol station will be presented.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>https:\/\/cesnet.zoom.us\/j\/94167862089 Although aerosol particles are a small part of the atmosphere, they have a significant impact on, e.g., air quality, climate, or health. Isotope analysis of atmospheric aerosols is a possible way to study the processes that take place in this atmospheric component. Carbon is one of the relatively abundant elements in aerosols, so isotopic&hellip;<\/p>\n","protected":false},"author":19,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[85],"tags":[],"class_list":["post-9408","post","type-post","status-publish","format-standard","hentry","category-lectures-and-professional-meetings"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/posts\/9408","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/users\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/comments?post=9408"}],"version-history":[{"count":1,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/posts\/9408\/revisions"}],"predecessor-version":[{"id":9409,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/posts\/9408\/revisions\/9409"}],"wp:attachment":[{"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/media?parent=9408"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/categories?post=9408"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.icpf.cas.cz\/en\/wp-json\/wp\/v2\/tags?post=9408"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}