“…The use of both quadrupoles and oxygen in the CRC allows for the removal of spectral interferences for all isotopes of sulfur and accurate quantification of trace-level 32 S despite spectral overlap with the abundant 16 O 2 + (Baken et al, 2011;Balcaen et al, 2015;Bolea-Fernandez et al, 2017;Giner Martínez-Sierra et al, 2015). This instrumentation has been used to quantify sulfur in many complex organic matrices, including natural organic matter from marine environments (Ksionzek, 2019;Ksionzek et al, 2018;Lechtenfeld et al, 2011), biomolecules (Amaral et al, 2015;Fernández et al, 2012;Gong et al, 2015;Kroepfl et al, 2017;Zhu et al, 2015), wine (Lajin & Goessler, 2019), and crude oil (Fletcher et al, 2020(Fletcher et al, , 2021Walkner et al, 2017). Indirect quantification of sulfur associated with DOM has been done by quantifying total sulfur in freshwater samples by ICP-MS/MS and then subtracting the concentration of sulfate determined by ion chromatography (Ossola et al, 2019); however, at present, there is no published method for direct quantification of sulfur in freshwater DOM by ICP-MS/MS.…”