{"id":600,"date":"2013-11-16T19:03:52","date_gmt":"2013-11-16T19:03:52","guid":{"rendered":"http:\/\/www.atmos.washington.edu\/~thornton"},"modified":"2014-03-23T00:21:32","modified_gmt":"2014-03-23T00:21:32","slug":"jpac-chamber-2012","status":"publish","type":"page","link":"https:\/\/www.atmos.washington.edu\/~thornton\/field-campaigns\/jpac-chamber-2012","title":{"rendered":"JPAC Chamber 2012"},"content":{"rendered":"

The HR-ToF-CIMS was deployed as part of an effort to investigate the oxidation of alpha-pinene and subsequent SOA formation at the Forschungszentrum\u00a0J\u00fclich Plant Atmosphere Chamber<\/a> (J\u00fclich, Germany) in Oct.-Nov. of 2012. The chemistry was probed over a wide range of conditions (light, NOx<\/sub>, O3<\/sub>, particles…) while monitoring with numerous instruments including two HR-ToF-CIMS (Iodide-adduct, Nitrate-adduct), HR-ToF-AMS and PTR-ToF-MS. The FIGAERO inlet [Lopez-Hilfiker et al.<\/em>, 2013, submitted to AMT] to measure the chemical composition of both the particle and gas-phases was first employed during these experiments.<\/p>\n

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Chamber at JPAC<\/figcaption><\/figure>\n
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Felipe and Mikael hard at work<\/figcaption><\/figure>\n
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Beautiful bike ride to work!<\/figcaption><\/figure>\n

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\nPapers published<\/span>:<\/p>\n

Ehn M. et al., (2013<\/strong>), A large source of low-volatility secondary organic aerosol, Nature<\/em>, 506, doi.10.1038\/nature13032.<\/p>\n","protected":false},"excerpt":{"rendered":"

The HR-ToF-CIMS was deployed as part of an effort to investigate the oxidation of alpha-pinene and subsequent SOA formation at the Forschungszentrum\u00a0J\u00fclich Plant Atmosphere Chamber (J\u00fclich, Germany) in Oct.-Nov. of 2012. The chemistry was probed over a wide range of conditions (light, NOx, O3, particles…) while monitoring with numerous instruments including two HR-ToF-CIMS (Iodide-adduct, Nitrate-adduct), HR-ToF-AMS and PTR-ToF-MS. The FIGAERO inlet [Lopez-Hilfiker et al., 2013, submitted to AMT] to measure the chemical composition of both the particle and gas-phases was first employed during these experiments. Papers published: Ehn M. et <\/p>\n","protected":false},"author":1,"featured_media":0,"parent":37,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-600","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/600","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/comments?post=600"}],"version-history":[{"count":28,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/600\/revisions"}],"predecessor-version":[{"id":812,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/600\/revisions\/812"}],"up":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/37"}],"wp:attachment":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/media?parent=600"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}