Source Identification of Organophosphate Esters through the Profiles in Proglacial and Ocean Sediments from Ny-Ålesund, the Arctic

• Published in: Environmental science & technology Vol. 57; no. 5; pp. 1919 - 1929
• Main Authors: Fu, Jie, Fu, Kehan, Hu, Boyuan, Zhou, Wei, Fu, Yilin, Gu, Luyao, Zhang, Qinghua, Zhang, Aiqian, Fu, Jianjie, Jiang, Guibin
• Format: Journal Article
• Language: English
• Published: United States American Chemical Society 07.02.2023
• Subjects: Aromatic compounds; China; Contaminants in Aquatic and Terrestrial Environments; Contamination; Environmental behavior; Environmental Monitoring; Esters; Flame Retardants - analysis; Human settlements; Humans; Hydrophobicity; Oceans and Seas; Organophosphates; Organophosphates - analysis; Photodegradation; Polar environments; Sediments; China; Arctic region; the Arctic; organophosphate tri-esters; ocean sediment; source identification; proglacial sediment; organophosphate di-esters
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/acs.est.2c06747

Little is known about the sources and environmental behavior of organophosphate esters (OPEs) in the Arctic, especially their transformation products. The present study unprecedentedly investigated both 16 tri-OPEs and 8 di-OPEs in proglacial and ocean sediments from Ny-Ålesund, the Arctic. Mean concentrations of tri-OPEs and di-OPEs in proglacial sediments were 487 and 341 pg/g dry weight (dw), respectively, which were significantly lower than those in ocean sediments (1692 and 525 pg/g dw). Ocean sediments might be simultaneously influenced by long-range atmospheric transport (LRAT), oceanic transport, and human activities, whereas proglacial sediments, since they are isolated from human settlements, may be dominantly affected by LRAT. Such source difference was evidenced by the contamination profile of OPEs: chlorinated tri-OPEs with high environmental persistence and high LRAT were dominant in proglacial sediments (66%); however, weakly environmentally persistent and highly hydrophobic aryl tri-OPEs were dominant in ocean sediments (47%), which were plausibly from local emission sources due to their low LRAT potential. Di-OPEs in proglacial and ocean sediments were dominated by groups of parent tri-OPEs with strong photodegradability, such as alkyl (75%) and aryl (58%). A higher mean molar ratio of di-OPE/tri-OPE in the proglacial sediment (14) than that in the ocean sediment (2.2) may be related to its higher photodegradation than that of the ocean sediment.