{"id":183,"date":"2020-11-26T20:05:32","date_gmt":"2020-11-26T20:05:32","guid":{"rendered":"https:\/\/geocore.atomki.hu\/laboratory\/infrastruktura\/"},"modified":"2024-04-01T14:44:25","modified_gmt":"2024-04-01T14:44:25","slug":"infrastructure","status":"publish","type":"page","link":"https:\/\/geocore.atomki.hu\/en\/laboratory\/infrastructure\/","title":{"rendered":"Infrastructure"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><p>[vc_row][vc_column][vc_custom_heading source=&#8221;post_title&#8221; font_container=&#8221;tag:h3|text_align:left&#8221; use_theme_fonts=&#8221;yes&#8221;][vc_text_separator title=&#8221;LABORATORY&#8221; title_align=&#8221;separator_align_left&#8221; color=&#8221;custom&#8221; style=&#8221;dotted&#8221; border_width=&#8221;2&#8243; css_animation=&#8221;right-to-left&#8221; accent_color=&#8221;#b37a2b&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<strong>Within the frame of the project an Argus VI multicollector nobe gas mass spectrometer, designed for the simultaneous analysis of the isotopes of argon has been purchased.<\/strong>[\/vc_column_text][vc_column_text]The instrument is equipped with 5 Faraday cells and an electron multiplier, which enables the analysis of the isotopes of argon (36, 37, 38, 39, 40) simultaneously, with special attention to the <sup>36<\/sup>Ar that is measured normally on the electron multiplier. The instrument along with the attached, locally developed gas cleaning line, with the high frequency furnace and a CO<sub>2<\/sub> laser is appropriate for <sup>39<\/sup>Ar\/<sup>40<\/sup>Ar and for K\/Ar radiometric age dating, as well.[\/vc_column_text][vc_row_inner][vc_column_inner width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;347&#8243; img_size=&#8221;full&#8221;][\/vc_column_inner][vc_column_inner width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;350&#8243; img_size=&#8221;full&#8221;][\/vc_column_inner][\/vc_row_inner][vc_column_text]K\/Ar dating is performed in our lab using the Cassignol-Gillot method, without the addition of <sup>38<\/sup>Ar spike.[\/vc_column_text][vc_row_inner][vc_column_inner width=&#8221;1\/6&#8243;][\/vc_column_inner][vc_column_inner width=&#8221;2\/3&#8243;][vc_single_image image=&#8221;353&#8243; img_size=&#8221;full&#8221;][\/vc_column_inner][vc_column_inner width=&#8221;1\/6&#8243;][\/vc_column_inner][\/vc_row_inner][vc_column_text]Supported by the Institute, a ZnSe window has been purchased as well, that allows the analysis of very small amount of samples and the in-situ <sup>39<\/sup>Ar\/<sup>40<\/sup>Ar dating as well.[\/vc_column_text][\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>[vc_row][vc_column][vc_custom_heading source=&#8221;post_title&#8221; font_container=&#8221;tag:h3|text_align:left&#8221; use_theme_fonts=&#8221;yes&#8221;][vc_text_separator title=&#8221;LABORATORY&#8221; title_align=&#8221;separator_align_left&#8221; color=&#8221;custom&#8221; style=&#8221;dotted&#8221; border_width=&#8221;2&#8243; css_animation=&#8221;right-to-left&#8221; accent_color=&#8221;#b37a2b&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]Within the frame of the project an Argus VI multicollector nobe gas mass spectrometer, designed for<span class=\"excerpt-hellip\"> [\u2026]<\/span><\/p>\n","protected":false},"author":1,"featured_media":353,"parent":170,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inline_featured_image":false,"footnotes":""},"class_list":["post-183","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/pages\/183","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/comments?post=183"}],"version-history":[{"count":6,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/pages\/183\/revisions"}],"predecessor-version":[{"id":358,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/pages\/183\/revisions\/358"}],"up":[{"embeddable":true,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/pages\/170"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/media\/353"}],"wp:attachment":[{"href":"https:\/\/geocore.atomki.hu\/en\/wp-json\/wp\/v2\/media?parent=183"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}