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A simple diffuse reflectance Fourier transform infrared spectroscopic determination of sulfur dioxide in ambient air using potassium tetrachloromercurate as the absorbing reagent

机译:四氯汞酸钾为吸收剂的简单漫反射傅里叶变换红外光谱法测定环境空气中的二氧化硫

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This paper presents development of a simple, rapid, and precise analytical method for determination of sulfur dioxide in ambient air by a gas to solid-phase conversion method. Sulfur dioxide is determined in the form of sulfite (SO3(2-)) because the absorbing reagent, potassium tetrachloromercurate (TCM), used in this method absorbs sulfur dioxide from the atmosphere in the form of sulfite. Determination of submicrogram levels of sulfur dioxide was based on the selection of a quantitative analytical peak at 495 cm(-1) among the 3 observed vibrational peaks for the dichlorosulfitomercurate complex formed after reaction of sulfur dioxide with TCM and measurement of absorbance using diffuse reflectance Fourier transform infrared spectroscopy. The limits of detection and quantification of the method were found to be 0.09 and 0.4 microg/g SO3(2-), respectively. The precision in terms of standard deviation and relative standard deviation (RSD) at a level of 2 microg SO3(2-)/10.1 g KBr for n = 10 was found to be 0.036 microg SO3(2-) and 1.8%, respectively. The RSD (n = 10) for determination of sulfur dioxide in ambient air was observed to be in the range of 2.7-4.2%. The method proposed is time saving and eliminates the slow and cumbersome steps of pH maintenance of the reaction mixture and color formation of the U.S. Environmental Protection Agency recommended West and Gaeke spectrophotometric method and other methods for quantitative determination of sulfur dioxide.
机译:本文提出了一种简单,快速,精确的分析方法的开发,该方法通过气相至固相转化方法测定环境空气中的二氧化硫。二氧化硫以亚硫酸盐(SO3(2-))的形式确定,因为在此方法中使用的吸收剂四氯汞钾(TCM)以亚硫酸盐的形式从大气中吸收二氧化硫。二氧化硫的亚微克水平的确定是基于在二氧化硫与TCM反应后形成的二氯次磺基乙酸酯络合物的三个观察到的振动峰中选择了一个在495 cm(-1)处的定量分析峰,并使用漫反射傅里叶测量吸光度变换红外光谱。该方法的检出限和定量限分别为0.09和0.4 microg / g SO3(2-)。在n = 10时,以2微克SO3(2-)/ 10.1 g KBr的水平表示的标准偏差和相对标准偏差(RSD)精度分别为0.036微克SO3(2-)和1.8%。测定环境空气中二氧化硫的相对标准偏差(n = 10)在2.7%至4.2%范围内。所提出的方法节省了时间,并且省去了反应混合物的pH值维持和颜色形成的缓慢而麻烦的步骤,美国环境保护署推荐了West和Gaeke分光光度法以及其他定量测定二氧化硫的方法。

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