{"id":100573,"date":"2026-07-12T13:42:12","date_gmt":"2026-07-12T11:42:12","guid":{"rendered":""},"modified":"2026-07-13T06:55:32","modified_gmt":"2026-07-13T04:55:32","slug":"019938c3cb10-3774f106-fb5a-4f74-b11c-27812d56e862","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/019938c3cb10-3774f106-fb5a-4f74-b11c-27812d56e862\/","title":{"rendered":"SPREDNING AV TUNGE GASSER. \u00c5RSRAPPORT 1984."},"content":{"rendered":"<p class=\"wp-block-paragraph\">Data fra fors\u00f8kene p\u00e5 Thorney Island er bearbeidet og sammenholdt med modellberegning. Et fors\u00f8k er simulert b\u00e5de i vind- og vanntunnel.<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-12 13:42:12","footnotes":""},"nva_tax_category":[1055],"class_list":["post-100573","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-report"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/100573","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication"}],"about":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/types\/nva_publication"}],"version-history":[{"count":1,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/100573\/revisions"}],"predecessor-version":[{"id":100574,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/100573\/revisions\/100574"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=100573"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=100573"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}