Further understanding the involvement of Fe(IV) in peroxydisulfate and peroxymonosulfate activation by Fe(II) for oxidative water treatment
Further understanding the involvement of Fe(IV) in peroxydisulfate and peroxymonosulfate activation by Fe(II) for oxidative water treatment
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DOI:
10.1016/j.cej.2019.04.101
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发表时间:
2019-09
影响因子:
15.1
通讯作者:
Zhen Wang;W. Qiu;Su-yan Pang;Yang Zhou;Yuan Gao;Chaoting Guan;Jin Jiang
中科院分区:
文献类型:
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作者:
Zhen Wang;W. Qiu;Su-yan Pang;Yang Zhou;Yuan Gao;Chaoting Guan;Jin Jiang
Very recently, we have interestingly found that the Fe(II)-activated peroxydisulfate (PDS) process can oxidize methyl phenyl sulfoxide (PMSO) to its oxygen transfer product methyl phenyl sulfone (PMSO2), suggesting the possible occurrence of a ferryl intermediate (Fe(IV)) rather than long recognized sulfate radical (SO4radical dot−) in this process. In this work, the formation of PMSO2was also observed when PMSO was treated by the Fe(II)/peroxymonosulfate (PMS) system over the pH range of 3–7, and the yield of PMSO2(i.e., the molar ratio of PMSO2formed to PMSO lost) was quantified to be approximately 100% under acidic conditions, similar to the Fe(II)/PDS system. Moreover,18O from isotope-labeled water (H218O) was successfully incorporated into PMSO2product when PMSO was oxidized by the Fe(II)/PDS and Fe(II)/PMS systems in H218O, likely due to the competitive oxygen exchange of Fe(IV)-oxo species with H218O. Further, Fe(IV) evolution profiles in both systems were predicted by a Fe(IV)-mediated kinetic model, and these results are in good agreement with the experimental data obtained with a stopped-flow spectrophotometer.