摘要
View large Download slide View large Download slide Close modal Pyrrhotite (Fe 1-x S) was prepared by the pyrolysis of pyrite and the sulfidation of hematite, and subsequently used to activate H 2 O 2 for the degradation of tetracycline (TC). The pyrite-derived Fe 1-x S samples (P600 and P700) and the hematite-derived Fe 1-x S samples (S600, S700), prepared at 600 and 700 °C, respectively, were characterized using X-ray diffraction (XRD), X-ray photoelectronic spectroscopy (XRS), scanning electron microscopy (SEM) and magnetism analysis. The effects of annealing temperature, preparation method, and initial solution pH on TC degradation were systematically investigated. The results showed that the degradation of TC increased with the decrease in annealing temperature and initial solution pH. Quenching experiments and electron spin resonance (ESR) demonstrated that • OH and 1 O 2 were reactive oxygen species (ROSs) in acidic and alkaline media, respectively. Moreover, the sulfidation-derived pyrrhotite, featuring a monoclinic Fe 1-x S shell, exhibited superior catalytic performance than pyrolysis-derived pyrrhotite with a hexagonal Fe 1-x S shell. Notably, 1 O 2 was easier to produce in the P600/H 2 O 2 system. Both P600 and S600 maintained a high catalytic activity after five runs. These findings offer a novel approach for pyrrhotite preparation and promote the comprehensive utilization of pyrite and hematite. Pyrolytic pyrrhotite and sulfurized pyrrhotite were prepared by a one-step method. Sulfurized pyrrhotite exhibited superior catalytic activity than pyrolytic pyrrhotite. • OH was the dominant ROS under acidic conditions, while 1 O 2 prevailed under alkaline conditions. The magnetic pyrrhotite showed excellent reusability over five cycles.
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