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Ambient Air quality Monitoring Guidlines. - Maharashtra Pollution ...

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5.1.1 Up to 100 fold ratio of sulfur dioxide to oxidant may be eliminated with out loss of<br />

oxidant by incorporating a chromic acid paper absorber in the sampling train<br />

upstream from the impinger (2).<br />

5.1.2 The absorber removes sulfur dioxide without loss of oxidant but will also oxidize<br />

nitric oxide to nitrogen dioxide.<br />

5.1.3 When sulfur dioxide is less than 10% of the nitric oxide concentration, the use of chromic acid<br />

paper is not recommended. In this case, the effect of sulfur dioxide on the oxidant reading can<br />

be corrected for by concurrently analyzing for sulfur dioxide and adding this concentration to the<br />

total oxidant value.<br />

5.2 Nitrogen dioxide is known to give a response in 1% KI (1), equivalent to 10% of<br />

that of an equimolar concentration of ozone. The contribution of nitrogen dioxide<br />

to the oxidant reading can be eliminated by concurrently analyzing for nitrogen<br />

dioxide by an appropriate method from this volume and subtracting one-tenth of<br />

the nitrogen dioxide concentration from the total oxidant value.<br />

5.3 Peroxyacetyl nitrite gives approximately a response equivalent to 50% of that of<br />

an equimolar concentration of ozone (3). Concentrations in the atmosphere may<br />

range up to 0.1 ppm.<br />

5.4 Other oxidizing substances besides ozone will liberate iodine with this method :<br />

e.g., halogens, proxy compounds, hydro-peroxides, organic nitrites and<br />

hydrogen peroxide (4, 5).<br />

5.5 Hydrogen sulfide, reducing dusts or droplets can act as negative interferences.<br />

5.6 It has been shown that the amount of iodine formed increases with relative<br />

humidity during sampling (6, 7). This effect is nearly linear. Increase of iodine<br />

formation is 0-10% with RH values ranging from 0-60%. Insignificant effects<br />

were observed by increases of RH from 60 to 75%.<br />

6.0 SAMPLE PRESERVATION<br />

6.1 Ozone liberates iodine through both a fast and a slow set of reactions. Some of<br />

the organic oxidants also have been shown to cause slow formation of iodine (4,<br />

5). Some indication of the presence of such oxidants and of gradual fading due<br />

to reductant can be obtained by making several readings during an extended<br />

period of time, e.g., every 20 min.<br />

6.2 Occasionally mold may grow in the absorbing reagent. When this occurs discard<br />

the reagent because reducing substances and a change in pH make it useless.<br />

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