4.7 Article

Spatial distribution, vertical profiles and transport of legacy and emerging per- and polyfluoroalkyl substances in the Indian Ocean

Journal

JOURNAL OF HAZARDOUS MATERIALS
Volume 437, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jhazmat.2022.129264

Keywords

Open Ocean; Surface seawater; HFPO-DA; Mass transport estimates; Interbasin exchange

Funding

  1. Global Change and Air-Sea Interaction II [GASI-01-WIND-STwin]
  2. China Ocean Mineral Resources Research and Development Association [DY135-E2-1-03]
  3. National Natural Science Foundation of China [U2106205, 42176236]
  4. Shandong Provincial Natural Science Foundation of China [ZR2018MD016]

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The contamination status and transport of PFASs in the Indian Ocean and Northwest Pacific Ocean were investigated. The study found that certain PFASs were widely distributed in the surface seawater, with PFHpA and PFOA being the most predominant. The study also revealed a surface-enrichment and depth-depletion pattern for PFASs in the water column.
The contamination status and transport of per- and polyfluoroalkyl substances (PFASs) in the seawater of the Indian Ocean (IO) and an adjacent subregion of the Northwest Pacific Ocean (NWPO) were investigated. Eight legacy PFASs were widely distributed in the surface seawater, and perfluoroheptanoic acid (PFHpA) and perfluorooctanoic acid (PFOA) were the two predominant PFASs. Sigma PFAS concentration decreased in the following order: NWPO>Joining area of Asia and Indian-Pacific Oceans (JAIPO)>Northeast Indian Ocean>Southwest Indian Ocean. Hexafluoropropylene oxide-dimer acid, a replacement surfactant for PFOA was extensively detected in the IO (~34.8 pg/L) for the first time, showing an early sign of emerging PFAS spread in global open oceans. Eight depth profiles across the JAIPO (down to 5433 m depth) revealed a surface-enrichment and depth-depletion pattern for PFASs in the water column, and two noticeable fluctuations were mainly located at depths of 150-200 and 200-500 m. Physical processes, including eddy diffusion, and the origin and trajectory of water mass were crucial factors for structuring PFAS vertical profiles. Mass transport estimates revealed a remarkable PFOA contribution through the JAIPO to IO carried by the Indonesian Throughflow, and anonnegligible PFHpA contribution from Antarctic Immediate Water to deep water of the JAIPO driven by thermohaline circulation.

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