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PEROXY RADICAL MEASUREMENT BY CHEMICAL AMPLIFICATION.

机译:化学放大法测定过氧自由基。

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摘要

Odd hydrogen radicals play an important role in nearly every chemical cycle of the atmosphere. Of particular current interest are tropospheric ozone production (catalyzed by NO(,x), CO, and CH(,4)) and acid rain formation. Hydroxyl radicals (HO) react with NO(,2) to form nitric acid, and begin a sequence which converts SO(,2) to sulfuric acid. The hydroperoxy radical (HO(,2)) reacts with NO to form NO(,2), thus allowing ozone to build up from oxygen atoms produced by NO(,2) photolysis. Development of measurement techniques for free radicals is important to improving our understanding of the chemistry of the atmosphere.;HO(,2) + NO (--->) NO(,2) + HO (1).;HO + CO (--->) H + CO(,2) (2).;H + O(,2) + M (--->) HO(,2) + M (3).;Our new technique for PEroxy Radical measurement by Chemical Amplification (PERCA) takes advantage of the chain reaction in which peroxy (e.g. HO(,2)) and oxy- (e.g. HO) radicals catalize the air oxidation of NO and CO: (UNFORMATTED TABLE FOLLOWS).;(TABLE ENDS).;This chain reaction forms 1100 NO(,2) molecules in 4.2 seconds for each HO(,x) (HO(,2) + HO) entering the system. Typical reagent concentrations are 3 ppmv for NO and 10% by volume for CO. The NO(,2) generated from the chain reaction is differentiated from ambient NO(,2), and NO(,2) from NO + O(,3) by substituting N(,2) for CO at a fixed frequency and measuring the NO(,2) modulation. The NO(,2) is detected by observing the photons produced from a gas-liquid surface chemiluminescence reaction with a basic aqueous luminol solution.;Calibration is accomplished by monitoring the second order decay of HO(,2) radicals generated by various techniques in the laboratory. Dividing the accepted rate constant for 2HO(,2) (--->) H(,2)O(,2) + O(,2) by the slope of the inverse radical signal versus decay time, yields the instrumental HO(,2) sensitivity. Some field measurements and a smog chamber study have been performed which demonstrate the feasibility of the method. Potential interferences using this technique are also discussed.
机译:奇怪的氢自由基在大气的几乎每个化学循环中都起着重要作用。当前特别关注的是对流层臭氧的产生(由NO(,x),CO和CH(,4)催化)和酸雨形成。羟基(HO)与NO(,2)反应形成硝酸,并开始将SO(,2)转化为硫酸的序列。氢过氧自由基(HO(,2))与NO反应形成NO(,2),从而使臭氧从NO(,2)光解产生的氧原子中积累。自由基测量技术的发展对于增进我们对大气化学的理解非常重要。; HO(,2)+ NO(---)NO(,2)+ HO(1).; HO + CO( --->)H + CO(,2)(2).; H + O(,2)+ M(--->)HO(,2)+ M(3).;我们的过氧自由基新技术化学放大法(PERCA)的测量利用了链反应,其中过氧(例如HO(,2))和氧-(例如HO)自由基催化了NO和CO的空气氧化:(未格式化的表格如下)。 ENDS)。;此链反应在4.2秒内对进入系统的每个HO(,x)(HO(,2)+ HO)形成1100个NO(,2)分子。 NO的典型试剂浓度为3 ppmv,CO的典型体积浓度为10体积%。链式反应生成的NO(,2)与环境NO(,2)有所区别,NO(,2)与NO + O(,3 ),以固定频率用N(,2)代替CO并测量NO(,2)调制。通过观察由碱性鲁米诺水溶液在气液表面化学发光反应中产生的光子来检测NO(,2);通过监测由各种技术产生的HO(,2)自由基的二阶衰减来完成校准。实验室。用2HO(,2)(--->)H(,2)O(,2)+ O(,2)的可接受速率常数除以反激基信号对衰减时间的斜率,得出仪器HO( ,2)灵敏度。已经进行了一些现场测量和烟雾室研究,证明了该方法的可行性。还讨论了使用此技术的潜在干扰。

著录项

  • 作者单位

    University of Michigan.;

  • 授予单位 University of Michigan.;
  • 学科 Analytical chemistry.
  • 学位 Ph.D.
  • 年度 1983
  • 页码 211 p.
  • 总页数 211
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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