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Facile synthesis of alkaline-earth metal manganites for the efficient degradation of phenolic compounds via catalytic ozonation and evaluation of the reaction mechanism

Journal 2019 · IF 6.361 · 发表于 2019 年 5 月 3 日
作者: Cunxia Fang,Xingmin Gao,Xiangcheng Zhang,Jiahui Zhu,Sheng-Peng Sun,Xiaoning Wang,Winston Duo Wu,Zhangxiong Wu
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摘要

In this paper, we demonstrate the facile and general synthesis of alkaline-earth metal manganites , denoted as A(Mg, Ca, Ba)Mn x O y , for efficient degradation of high-concentration phenolic compounds via catalytic ozonation . The representative CaMn x O y oxides show a hierarchical spherical structure constructed by crystalline nanorods and numerous macropores. They possess mixed Mn 4+ /Mn 3+ chemical valences and abundant surface hydroxyl (OH) groups. The ozone (O 3 ) decomposition rate on the CaMn x O y catalysts is greatly accelerated and follows the first-order law. These catalysts are promising for the degradation of phenolic compounds via catalytic ozonation, exhibiting rapid pseudofirst-order degradation kinetics, a high total organic carbon (TOC) removal efficiency and an excellent stability. Under optimized conditions (a low O 3 dosage of 1.5 mg/min and a catalyst dosage of 7.5 g/L), for the treatment of concentrated phenol (50–240 mg/L), the CaMn x O y catalysts show 100% degradation and 50–70% mineralization within 1.0 h. The Ca 2+ ions are essential to create redox Mn 4+ /Mn 3+ couples and to significantly reduce manganese leaching. High surface ratios of Mn 4+ /Mn 3+ and OH/lattice oxygen (O lat ) are beneficial for enhancing the catalytic performance. Superoxide anion free radicals ( O 2 – ) and singlet oxygen ( 1 O 2 ) are the predominant reactive species for the oxidation degradation. The O 2 – reaction pathway is proposed. Specifically, the surface OH sites activate O 3 , displaying highly enhanced decomposition rates. The generated O 2 – and 1 O 2 play a role in oxidation. The redox Mn 4+ /Mn 3+ and the O lat /oxygen vacancy (O lat /O vac ) couples play important roles in electron transfer . The proposed mechanism is supported by active site probing, radical scavenging, spectroscopic studies, and the results in the degradation of substituted phenols.

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