In recently, advanced oxidation processes (AOPs) based on sulfate radicals (SO4•−) have more widespread application prospect for organic wastewater treatment than hydroxyl radical (OH•)-based AOPs due to their superior oxidation potential, better selectivity, longer half-life, and a wider range of pH adaptation (Lin &Zhang 2017). The primary sources of SO4•− in AOP systems are currently peroxymonosulfate (PMS, HSO5−) and persulfate (PS, S2O82−) (Nie et al. 2019). However, PMS typically activates easier than PS, likely due to its asymmetric structure (Chen et al. 2012).
Various conventional methods for PMS activation have been established, such as homogenous and heterogeneous transition metals (Bai et al. 2020, Duan et al. 2023, Shao et al. 2022), carbon materials (Solis et al. 2020, Yang et al. 2016), heat (Fan et al. 2015), UV irradiation (Rodriguez-Chueca et al. 2018), microwave (Qi et al. 2014), and ultrasound (Hao et al. 2014). Transition metal ions has advantages in terms of high efficiency, cost-effectiveness, and ease of operation among these activation methods. However, this method also presents some disadvantages, including the high usage rate of metal ions, difficulty in recycling, and large dependence on pH, which have yet to be resolved (Li et al. 2018). Consequently, there is a growing interest in developing secure, efficient, and reusable heterogeneous transition metal catalysts (Dong et al. 2020, Li et al. 2021). Due to low cost, non-toxicity, and abundant resources of Sulfur-containing iron minerals, they have garnered attention as catalysts for PMS activation (Hou et al. 2022). Ferrous sulfide (FeS) occurs widely in nature as a former metabolite of sulfate-reducing microorganism under environmental conditions (Ikogou et al. 2017). In recent years, FeS has been widely utilized as a catalyst for activating PMS, demonstrating good activation ability (Hong et al. 2021). Because FeS has versatile chemical properties and electronic structures, allowing it to function as both a source of Fe(II) and an electron donor(Fan et al. 2018). For example, dissolved Fe2+, surface Fe2+, and lattice Fe2+ in FeS both can be used as activators in sulfate radicals based AOPs (Oh et al. 2011). Moreover, S(-II) in the FeS structure and dissolved S(-II) from FeS, as an electron donor, both can reduce Fe(III) to Fe(II), significantly contributing to the Fe2+/Fe3+ cycle (Cheng et al. 2020, Cheng et al. 2016). Hence, FeS is a promising candidate for PMS activation owing to these properties.
Mackinawite and pyrrhotite, which are two different FeS phases, are imperfect catalysts (Gao et al. 2018). Pyrrhotite, being in a stable phase of FeS, exhibits a low ability to activate peroxides. In contrast, mackinawite, a sub-stable phase of FeS, has low stability and tends to dissolve to produce ferrous ions and H2S under acidic conditions (Pankow &Morgan 1979). Gao et al. investigated the use of zinc-modified pyrrhotite and found that the addition of zinc compounds gradually transformed pyrrhotite to pyrite, resulting in a significant increase in catalytic activity (Gao et al. 2018). Because it is chalcophilic, FeS can trap various divalent metals in its natural setting by generating surface complexes, insoluble metal sulfides, or isomorphous substitution (Cheng et al. 2016). As a result, using FeS doped with transition metals may also be a viable option to increase its catalytic efficiency.
The combination of Co2+ and PMS is the most effective activation strategy compared to other metal ions (Anipsitakis &Dionysiou 2004, Xia et al. 2022, Yu et al. 2023). In addition, studies have demonstrated that incorporating Co-doping in FeWO4 (Zhang et al. 2023) and Fe3O4 (Li et al. 2018) can significantly enhance the PMS activation, and the presence of Fe can effectively reduce the heavy metal pollution caused by the leaching of Co due to Fe-Co interactions (Liu et al. 2020, Luo et al. 2021). In natural environments, Co frequently replaces Fe in pyrrhotite owing to its affinity for sulfur and similar ionic radius to iron (Dehaine et al. 2021, Savinova et al. 2023). Various genetic types of pyrrhotite contain Co as an example of this phenomenon (Dehaine et al. 2021, Khodadadmahmoudi et al. 2022). Therefore, we predict that Co isomorphism replacing FeS may serve as a highly reactive, stable, and recyclable catalyst for PMS activation.
In this study, we utilised a hydrothermal method to prepare various Co-doped FeS catalyst materials. We used several techniques, such as field emission scanning electron microscopy (FESEM), high-resolution transmission electron microscopy (HRTEM), X-ray diffraction (XRD), X-ray photoelectron spectroscopy (XPS), and Brunauer–Emmett–Teller, to examine the surface morphology and crystal properties of the Co-doped FeS composites. With bisphenol S (BPS) employed as a model contaminant, the effect of Co-doping on the catalytic activity of FeS-activated PMS was examined. We then examined the effects of different experimental factors on BPS degradation, including the initial solution pH, PMS concentration, catalyst dose, temperature, background substances, and actual water bodies. Furthermore, we evaluated the reusability and stability of the catalyst using recycling experiments. Quenching experiments and electron paramagnetic resonance (EPR) technology were used to identify the principal reactive species in the Co-doped FeS/PMS system for BPS removal and illustrate the role of non-radical pathways in the system. This study offers potential insights into improving iron sulfide catalysts in PMS activation for the degradation of refractory organic compounds.