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首页> 外文期刊>Advances in Chemical Engineering and Science >Fenton-Like Oxidation of Acid Yellow 23 in the Presence of Iron Rich Soil
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Fenton-Like Oxidation of Acid Yellow 23 in the Presence of Iron Rich Soil

机译:富铁土壤中酸性黄23的Fenton氧化

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Treatment of yellow dye 23 by heterogeneous Fenton-like process was studied using iron rich soil as an iron source. The iron rich soil sample was characterized by XRD, SEM and BET analysis. XRD pattern indicates that the iron rich soil is made of goethite and hematite. The reaction was systematically investigated under various experimental conditions such as pH, iron rich soil dosage, oxidant and dye concentrations. The result revealed that using iron rich soil as catalyst led to high discoloration efficiency (97.71% for 140 min of treatment) at pH = 2.5, 2 g/L iron rich soil and 16 m·mol/L H2O2. The degradation kinetics of acid yellow 23 can be described by a pseudo-first-order reaction following the Langmuir-Hinshelwood mechanism. The main roles of hydroxyl radicals in degradation process were investigated by adding of various radical scavengers.
机译:研究了使用富铁土壤作为铁源,通过非均相的Fenton样工艺处理黄色染料23。通过XRD,SEM和BET分析对富铁土壤样品进行表征。 XRD图谱表明富铁土壤由针铁矿和赤铁矿组成。在各种实验条件下,例如pH,富铁土壤剂量,氧化剂和染料浓度,系统地研究了该反应。结果表明,在pH = 2.5、2 g / L富铁土壤和16 m·mol / L H2O2的条件下,使用富铁土壤作为催化剂可导致较高的变色效率(处理140分钟,达到97.71%)。酸性黄23的降解动力学可以通过遵循Langmuir-Hinshelwood机理的拟一级反应来描述。通过添加各种自由基清除剂,研究了羟基自由基在降解过程中的主要作用。

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