Role of Snow Deposition of Perfluoroalkylated Substances at Coastal Livingston Island (Maritime Antarctica)

• Published in: Environmental Science & Technology
• Main Authors: Casal, P., Zhang, Y., Martin, J. W., Pizarro, M., Jiménez, Begoña, Dachs, Jordi
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Chemical Society 2017
• Subjects: Antarctic; Livingston Island; The Antarctic; Antarc*; Antarctica
• Online Access: http://hdl.handle.net/10261/235228; https://doi.org/10.1021/acs.est.7b02521

Perfluoroalkyl substances (PFAS) are ubiquitous in the environment, including remote polar regions. To evaluate the role of snow deposition as an input of PFAS to Maritime Antarctica, fresh snow deposition, surface snow, streams from melted snow, coastal seawater, and plankton samples were collected over a three-month period (December 2014-February 2015) at Livingston Island. Local sources of PFASs were significant for perfluoroalkyl sulfonates (PFSAs) and C7-14 perfluoroalkyl carboxylates (PFCAs) in snow but limited to the transited areas of the research station. The concentrations of 14 ionizable PFAS (-PFAS) in freshly deposited snow (760-3600 pg L) were 1 order of magnitude higher than those in background surface snow (82-430 pg L). -PFAS ranged from 94 to 420 pg L in seawater and from 3.1 to 16 ng g in plankton. Ratios of individual PFAS concentrations in freshly deposited snow relative to surface snow (C/C), snowmelt (C/C), and seawater (C/C) were close to 1 (from 0.44 to 1.4) for all perfluorooctanesulfonate (PFOS) isomers, suggesting that snowfall does not contribute significantly to PFOS in seawater. Conversely, these ratios for PFCAs ranged from 1 to 33 and were positively correlated with the number of carbons in the PFCA alkylated chain. These trends suggest that snow deposition, scavenging sea-salt aerosol bound PFAS, plays a role as a significant input of PFCAs to the Maritime Antarctica. The UTM and JC1 staffare acknowledged for theirindispensable support during the Antarctic campaign 2014/2015. The AEMET is acknowledged for providing themeteorological data. This work has beenfinanced by the Spanish Ministry of Economy and Competitiveness (REMAR-CA-CTM2012-34673, SENTINEL-CTM2015-70535-P). P.C.acknowledges a FPI fellow ship from the Economy and Competiveness Ministry. Belén González-Gaya is thanked forher logistical support and helpful comments during thesampling campaign planning phase. J.M. acknowledges financial support from an NSERC Discovery grant and Alberta Healthfor support of daily ...