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Photodegradation of bitumen-derived organics in oil sands process-affected water
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Rekke forfattare: 72020 (engelsk)Inngår i: Environmental Science: Processes & Impacts, ISSN 2050-7887, E-ISSN 2050-7895, Vol. 22, nr 5, s. 1243-1255Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The chemical composition of water-soluble organics in oil sands process-affected water (OSPW) is primarily composed of natural constituents of bitumen that are solubilized and concentrated during aqueous extraction of oil sands. OSPW organics are persistent and acutely toxic, and a leading remediation strategy is long-term ageing in end-pit lakes, despite limited data available on its photochemical fate. Here, direct photolysis of whole OSPW, or of its constituent fractions, was examined at environmentally relevant wavelengths (>290 nm) in bench-top studies. Changes in the chemical profiles of whole OSPW, acid- (AEO), and base-extractable organics (BEO) were characterized by liquid chromatography with ultra-high resolution mass spectrometry in negative (-) and positive (+) ionization modes. Following 18 d of irradiation, photolysis reduced the total ion intensity in all samples in both modes. The most photo-labile species included the O-2(-), O-3(-), O-4(-), O2S-, and O4S- chemical classes, which were depleted in whole OSPW by 93-100% after only 5 d. In positive mode, detected species were more recalcitrant than those detected in negative mode, with an average reduction across all heteroatomic classes of 75 +/- 11.0% after 18 d. Estimated environmental half-lives for heteroatomic classes ranged from 57 d (O4S-) to 545 d (O3N+), with a greater recalcitrance for classes detected in positive mode compared to negative mode. Under field conditions in end-pit lakes, natural photolysis may be an important mechanism for effective OSPW remediation, and we suggest that future end-pit lakes be shallow to maximize light penetration and natural photolysis in ageing OSPW.

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2020. Vol. 22, nr 5, s. 1243-1255
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URN: urn:nbn:se:su:diva-183106DOI: 10.1039/d0em00005aISI: 000537868200008PubMedID: 32227038OAI: oai:DiVA.org:su-183106DiVA, id: diva2:1452728
Tilgjengelig fra: 2020-07-07 Laget: 2020-07-07 Sist oppdatert: 2025-01-31bibliografisk kontrollert

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Challis, Jonathan K.Martin, Jonathan W.Wong, Charles S.Ross, Matthew S.

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