“…The OSPW recycling process, along with the hot alkaline extraction process, results in an enrichment of natural bitumen‐derived substances in OSPW. This mixture of organics has been termed supercomplex 21 and is similar in chemical profile to natural bitumen‐affected waters, making source discrimination difficult and hampering previous attempts to detect seepage 14,17,19,21–24 . Historically, attempts to identify OSPW‐affected groundwater have considered total naphthenic acids (NAs), various geochemical indicators (major cations and anions), synchronous fluorescence spectroscopy (SFS) detection of aromatic acids, a variety of isotopic tracers, and ratios of O 2 :O 4 heteroatom ion classes and SO n ‐containing species determined by ultrahigh‐resolution mass spectrometry 15,16,18,25–37 .…”