Continuous Emission Monitoring. James A. Jahnke
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Название: Continuous Emission Monitoring

Автор: James A. Jahnke

Издательство: John Wiley & Sons Limited

Жанр: Биология

Серия:

isbn: 9781119434023

isbn:

СКАЧАТЬ

      The majority of instruments used in CEM systems are based on principles associated with the interaction of light with matter. Opacity monitors measure the effects of light scattering and absorption; a nondispersive infrared analyzer measures the amount of light absorbed by a pollutant molecule; and a chemiluminescence analyzer senses the light emitted in a chemical reaction. One could treat the operation of CEM system analyzers as “black boxes” that give out answers, but an understanding of their operation is necessary to properly apply an analyzer for monitoring at a source. Although some techniques will work well in a given application, other techniques will have problems in the same application. Also, for proper evaluation of system performance, a knowledge of how an analyzer works is essential to understand the effects of interferences, temperature, pressure, and so on. This understanding will be developed by first reviewing some of the basic properties of light and how these properties can be applied to measure pollutant gas concentrations.

      The Wave Nature of Light

Schematic illustration of an oscillating electric field and its wavelength. upper F r e q u e n c y o f l i g h t equals StartFraction v e l o c i t y o f l i g h t Over w a v e l e n g t h o f l i g h t EndFraction

      (4‐1)v equals StartFraction c Over lamda EndFraction

      where c is the velocity of light, 3.0 × 108 m/s.

      Literature describing continuous monitoring instruments often specifies the wavelength to characterize the spectral region used in the analytical method. Different units are often used for wavelength in different regions of the electromagnetic spectrum although the nanometer (nm) = 10−9 m has become the standard unit. Another unit, the Angstrom, Å = 10−10 m, has been used historically in the ultraviolet region. In the infrared region, both the μm = 10−6 m (also called 1 “micron”) and the wavenumber are commonly used by spectroscopists. The wavenumber is expressed as

      (4‐2)v overbar equals StartFraction 1 Over lamda EndFraction left-parenthesis c m Superscript negative 1 Baseline right-parenthesis

      Note that the units of v overbarare given in terms of the number of wavelengths per centimeter, called reciprocal centimeters or wavenumbers. The wavenumber v overbaris essentially a measure of frequency, differing from v by the constant factor of the velocity of light. The wavenumber is calculated by calculating the reciprocal of the wavelength expressed in μm and multiply by 104 to obtain wavenumbers in units of cm−1.

      The infrared spectral region is particularly important for the measurement of gaseous pollutants, and many instruments have been designed to operate in the infrared region. The infrared region is separated into the near infrared (NIR), mid infrared (MIR), and far infrared. Although an ISO standard does exist (ISO 2015), the boundaries of these regions are not universally agreed upon; there exists some ambiguity as to where the mid infrared ends and the far infrared begins, depending upon the usage by instrument manufacturers, spectroscopists, astronomers, or others.

      Absorption of Light by Molecules

      where h is Planck's constant and has a numerical value of 6.62 × 10−27 erg‐s. Clearly, the energy of a photon is dependent upon the frequency or wavelength of the light. Light (photons) of short wavelengths (such as in the ultraviolet) will carry more energy than light (photons) of longer wavelengths (such as in the infrared). Photons of different energies will have different effects. From a practical sense, sitting on the beach too long in bright sunlight can cause a severe sunburn. On the other hand, sitting under an infrared heat lamp will soothe sore muscles without causing sunburn. The effects of UV radiation are extremely severe under the Antarctic ozone hole, but less severe where the stratospheric ozone layer reduces the number of photons per unit time reaching Earth's surface. Light of different wavelengths (photons of different energies) will have a variety of effects on molecules. In a monitoring instrument, the manufacturer determines the best way to use these effects to make gas concentration measurements.

Schematic illustration of the electromagnetic spectrum for continuous emission monitoring analyzers.