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<strong>The</strong> first chemiluminscence analyser to measure NO was built in 1970 utilizing these<br />

principles <strong>of</strong> chemical reaction. A vacuum <strong>of</strong> reduced pressure (approximately negative l-15<br />

mmHg) is used to draw the gaseous sample into a reaction chamber through a valve where<br />

ozone is generated by electrical discharge. <strong>The</strong> vacuum is also necessary to evacuate gases<br />

that could potentially absorb energy from NO2., and to stabilise NO by removing 02, to<br />

prevent any 02 reacting with the NO to produce NOz which does not emit light (Hampl,<br />

Walters et al. 1996). <strong>The</strong> NO and 03 are then mixed in front <strong>of</strong> a photomultiplier tube<br />

sensitive to low levels <strong>of</strong> light at the red sensitive end <strong>of</strong> the spectrum (660 - 900nm). <strong>The</strong><br />

photons from the reaction strike a photosensitive surface and the impact releases electrons<br />

which are accelerated toward an electron sensitive surface (the first dynode) by an electric<br />

field. Each electron impact on this first dynode then causes emission <strong>of</strong> several electrons and<br />

these are accelerated to a second dynode. This step is repeated but the electrons are attracted<br />

to the terminal electrically charged element - the anode - and the resulting current is<br />

measured. This amplification achieved by the photomultiplier is necessary to measure the<br />

signal as the NO2'rosction emits a relatively weak red light (Hampl, Walters et al. 1996) and<br />

means that each electron emitted from the original photosensitive surface becomes a signal<br />

from millions <strong>of</strong> electrons at the anode (Turner 1985).<br />

Figure 4.2: Diagram <strong>of</strong> the chemiluminscence analyser<br />

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