Interferences chemiluminescence

Ozone can be analyzed by titrimetry, direct and colorimetric spectrometry, amperometry, oxidation—reduction potential (ORP), chemiluminescence, calorimetry, thermal conductivity, and isothermal pressure change on decomposition. The last three methods ate not frequently employed. Proper measurement of ozone in water requites an awareness of its reactivity, instabiUty, volatility, and the potential effect of interfering substances. To eliminate interferences, ozone sometimes is sparged out of solution by using an inert gas for analysis in the gas phase or on reabsorption in a clean solution. Historically, the most common analytical procedure has been the iodometric method in which gaseous ozone is absorbed by aqueous KI. 

Using the luminol photochemiluminescence it is possible to determine not only the nitrates (as reported by us earlier), but also the nitrites. The urotropin is added to the water sample, and the solution obtained is illuminated by the Hg lamp. The chemiluminescence is measured after the addition of basic luminol solution to the illuminated solution. The detection limit is 2-10 M. The nitrates contained in the drinking water do not interfere at tenfold excess. 

Describe the potential interferences (a) in the nondispersive infrared (NDIR) method for measuring CO and (b) in the chemiluminescent method for measuring NO2. 

The current trends toward miniaturization and the need of massively parallel measurements led to the development of biochips. In this area, biocatalyzed and electrogenerated chemiluminescence reactions appear attractive and represent an alternative to fluorescence detection which is still widespread used despite the numerous problems of quantitative measurements and interference fluorescence emission. 

The chemiluminescence technique has been used to determine trivalent chromium in seawater. Chang et al. [187] showed Luminol techniques for determination of chromium (III) were hampered by a salt interference, mainly due to magnesium ions. Elimination of this interference is achieved by seawater dilution and utilising bromide ion chemiluminescence signal enhancement (Fig. 5.7). The chemiluminescence results were comparable with those obtained by a graphite furnace flameless atomic absorption analysis for the total chromium present in samples. The detection limit is 3.3 x 10 9 mol/1 (0.2 ppb) for seawater with a salinity of 35%, with 0.5 M bromide enhancement. 

The effect of calcium interference is somewhat different. At its concentration in seawater, 0.010 M, calcium ion had no effect upon chemiluminescence analysis of a 6 x 10 8 M Crm solution in the absence of bromide ion. The... 

Gundermann et al. [21, 22] have extended Drew s work and showed that alkylation of the amino group enhances the efficiency, provided that the steric bulk of the alkyl groups does not interfere with the planarity of the nitrogen and the ring. Later work [23] showed that the chemiluminescent efficiency increased with the size of the aromatic ring. 

Selectivity derives from the fact that the analyte of interest generates its signal in the presence of compounds that normally interfere in fluorescence measurement and that do not themselves produce light when the chemiluminescent reagents are mixed together. 

The analytic principles that have been applied to accumulate air quality data are colorimetry, amperometry, chemiluminescence, and ultraviolet absorption. Calorimetric and amperometric continuous analyzers that use wet chemical techniques (reagent solutions) have been in use as ambient-air monitors for many years. Chemiluminescent analyzers, which measure the amount of chemiluminescence produced when ozone reacts with a gas or solid, were developed to provide a specific and sensitive analysis for ozone and have also been field-tested. Ultraviolet-absorption analyzers are based on a physical detection principle, the absorption of ultraviolet radiation by a substance. They do not use chemical reagents, gases, or solids in their operation and have only recently been field-tested. Ultraviolet-absorption analyzers are ideal as transfer standards, but, as discussed earlier, they have limitations as air monitors, because aerosols, mercury vapor, and some hydrocarbons could, interfere with the accuracy of ozone measurements made in polluted air. 

A diagram of a typical gas-phase (ozone-ethylene) chemiluminescent ozone analyzer is shown in Figure 6-10. The detector responds linearly to ozone concentrations between 0.003 and 30 ppm no interferences were initially observed. More recently, however, it has been established that, as the relative humidity goes from 0 to 60% and the temperature from 20° to 25° C, water vapor produces a small positive signal that results in an increase of about 8% in the ozone concentration measurement. This potential source of error can be minimized by using humidified, rather than dry, ozone in air streams when calibrating. 

Gas-diffusion flow injection analysis is capable of detecting very low concentrations of chlorine dioxide in water (i.e., detection limit is 5 ppb). A chemiluminescence flow-through detector cell is used to measure the concentration chlorine dioxide as a function of chemiluminescence intensity. A gas diffusion membrane separates the donor stream from the detecting stream and removes ionic interferences from iron and manganese compounds, as well as from other oxychlorinated compounds, such as chlorate and chlorite (Hollowell et al. 1986 Saksa and Smart 1985). 

Colorimetric assays are commonly used in molecular biology and biotechnology laboratories for determining protein concentrations because the procedures and their instrumentation requirements are simple. Two forms of assays are used. The first involves reactions between the protein and a suitable chemical to yield a colored, fluorescent, or chemiluminescence product. Second, a colored dye is bound to the protein and the absorbance shift is observed. Disadvantages of both these methods include limited sensitivity at below 1 pg/mL, interferences from buffers, and unstable chromophores (Jain et al. 1992). 

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