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机构地区:[1]淮阴工学院生命科学与化学工程学院,江苏淮安223003
出 处:《冶金分析》2012年第11期36-39,共4页Metallurgical Analysis
基 金:淮安市科技支撑计划(HAG09002);2011年江苏省高等学校大学生实践创新训练计划
摘 要:在H2SO4介质中,加热80℃条件下,Fe?对溴酸钾氧化中性红褪色反应具有较强的阻抑作用,基于在波长520nm处Fe?的量与阻抑反应体系(吸光度为A)和非阻抑反应体系(吸光度为A0)吸光度差值呈线性关系,建立了阻抑褪色动力学光度法测定痕量Fe?的分析方法。在优化实验条件下,方法的线性范围为0.000 4~0.064μg/mL,检出限为1.41×10-4μg/mL。测定了动力学参数,该阻抑反应为准一级反应,表观速率常数k=4.53×10-4s-1,表观活化能为69.25kJ/mol。方法用于天然水中痕量铁的测定,标准加入回收率为99.0%~99.5%;RSD为3.8%~6.2%。Under the conditions of 80℃ and in sulfuric acid medium,Fe had strong inhibitory action on the colour decolorization of neutral red oxidized by potassium bromate.There was a linear relationship between the amount of Fe and the absorbance difference of the inhibitory reaction system(absorbance A) and un-inhibitory reaction system(absorbance A0) at the wavelength of 520 nm.Based on the fact,a inhibition kinetic spectrophotometry for the determination of trace Fe was established.Under optimal experimental conditions,the linear range of the method was between 0.000 4 μg/mL and 0.064 μg/mL,and the detection limit was 1.41 × 10-4 μg/mL.The kinetic parameters were determined.It was shown that the inhibitory reaction was first-order reaction,the apparent rate constant k was 4.53 × 10-4 s-1 and the apparent activation energy was 69.25 kJ/mol.The method was used for the determination of the trace iron in natural water,with the recoveries of 99.0%-99.5% and the relative standard deviation(RSD) of 3.8%-6.2%.
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