Sulfide precipitation is an efficient method for separation. However, its application is limited due to the significant H2S pollution caused by conventional reagents. The utilization of amorphous FeS lead to a substantial reduction in H2S escape, while concurrently enhancing the crystallization and settling characteristics of As-precipitates. Under the conditions of an initial arsenic and H2SO4 concentration in the solution of 2 g/L and 50 g/L, respectively, and a FeS dosage of 1.5 times the molar amount of S/As, the arsenic removal exhibited a significant decrease from 89.8 % to 40.8 % over a FeS aging period of 0 to 84 days. Notably, no H2S emissions were detected during the entire reaction process. XRD analysis revealed a transformation of FeS from its amorphous form to a crystalline state as it undergoes aging. This transition is primarily characterized by a reduction in interlayer spacing and FeS bond length within the FeS lattice. The lattice energy experienced a decrease from −3071 to −3688 kJ/mol, indicating the progressive stabilization of the FeS structure. FTIR and TG-DSC analyses have demonstrated the infiltration of water molecules into both the interlamellar spaces and the lattice of FeS during the process of crystallization. Additionally, As3+ ions were observed to initially adsorb onto the surface of aged FeS through the hydroxyl group, followed by their diffusion into the lattice. The products of arsenic removal undergone a transformation from As2S3 to predominantly FeAsS-like complexes, as the mechanism of arsenic removal shifted from precipitate transformation to adsorption and co-precipitation.
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