{"id":118516,"date":"2026-09-11T21:19:11","date_gmt":"2026-09-11T19:19:11","guid":{"rendered":"https:\/\/nilu.gnist.dev\/publikasjoner\/sources-and-seasonal-variations-of-per-and-polyfluoroalkylsubstances-pfas-in-surface-snow-in-the-arctic\/"},"modified":"2026-09-11T21:19:11","modified_gmt":"2026-09-11T19:19:11","slug":"sources-and-seasonal-variations-of-per-and-polyfluoroalkylsubstances-pfas-in-surface-snow-in-the-arctic","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/sources-and-seasonal-variations-of-per-and-polyfluoroalkylsubstances-pfas-in-surface-snow-in-the-arctic\/","title":{"rendered":"Sources and Seasonal Variations of Per- and Polyfluoroalkyl\r\nSubstances (PFAS) in Surface Snow in the Arctic"},"content":{"rendered":"<p class=\"wp-block-paragraph\">Per- and polyfluoroalkyl substances (PFAS) are persistent anthropogenic contaminants, some of which are toxic and bioaccumulative. Perfluoroalkyl carboxylic acids (PFCAs) and perfluoroalkyl sulfonic acids (PFSAs) can form during the atmospheric degradation of precursors such as fluorotelomer alcohols (FTOHs), N-alkylated perfluoroalkane sulfonamides (FASAs), and hydrofluorocarbons (HFCs). Since PFCAs and PFSAs will readily undergo wet deposition, snow and ice cores are useful for studying PFAS in the Arctic atmosphere. In this study, 36 PFAS were detected in surface snow around the Arctic island of Spitsbergen during January\u2013August 2019 (i.e., 24 h darkness to 24 h daylight), indicating widespread and chemically diverse contamination, including at remote high elevation sites. Local sources meant some PFAS had concentrations in snow up to 54 times higher in Longyearbyen, compared to remote locations. At a remote high elevation ice cap, where PFAS input was from long-range atmospheric processes, the median deposition fluxes of C2\u2013C11 PFCAs, PFOS and HFPO\u2013DA (GenX) were 7.6\u201371 times higher during 24 h daylight. These PFAS all positively correlated with solar flux. Together this suggests seasonal light is important to enable photochemistry for their atmospheric formation and subsequent deposition in the Arctic. This study provides the first evidence for the possible atmospheric formation of PFOS and GenX from precursors.<\/p>\n","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-09-11 21:16:49","footnotes":""},"nva_tax_category":[1099],"class_list":["post-118516","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-scientific-journal-publication"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/118516","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":0,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/118516\/revisions"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=118516"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=118516"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}