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On the Formation of Nitrogen Oxides During the Combustion of ...

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2 <strong>Combustion</strong> Theory<br />

before it follows <strong>the</strong> prompt NO mechanism [443]. The formation <strong>of</strong> fuel NO is<br />

relevant for temperatures above 1100 K. For coal and medium fuel oil (MFO),<br />

for instance, 60 to 80 % <strong>of</strong> <strong>the</strong> fuel-bound N 2 are converted into NO [19, 451].<br />

<strong>Formation</strong> <strong>of</strong> NO 2<br />

Equation (2.18) illustrates <strong>the</strong> exo<strong>the</strong>rmic reaction that is responsible to some<br />

extent for NO 2 present in <strong>the</strong> combustion emissions but only <strong>of</strong> minor importance<br />

in most ambient situations due to its slow progress under <strong>the</strong> associated<br />

ambient conditions [214]:<br />

2NO+O 2 → 2NO 2 . (2.18)<br />

According to Sano [373, 374] and Miller and Bowman [289], <strong>the</strong> essential step<br />

<strong>of</strong> NO 2 formation in flames is represented by Equation (2.19). Significant<br />

amounts <strong>of</strong> <strong>the</strong> hydroperoxy radical (HO 2 ) are produced in flame regions <strong>of</strong><br />

lower temperatures and transported by diffusion into <strong>the</strong> high-temperature<br />

regime, where NO is formed and available for oxidation. The subsequent HO 2<br />

attack on NO (Eq. (2.19)) is two orders <strong>of</strong> magnitude faster than <strong>the</strong> reaction<br />

<strong>of</strong> Equation (2.18) [149]:<br />

NO+HO 2 → NO 2 + OH. (2.19)<br />

As NO 2 is an efficient absorber <strong>of</strong> light over a broad range <strong>of</strong> ultraviolet and<br />

visible wavelengths, it participates in photochemical smog reactions by photolysis<br />

(i.e. photodissociation). <strong>Nitrogen</strong> dioxide absorbs sunlight and subsequently<br />

decomposes to NO and O, thus triggering a complex series <strong>of</strong> reactions<br />

involving organic compounds that lead to photochemical smog:<br />

NO 2 + hν→NO+O, (2.20)<br />

O+O 2 + M → O 3 + M. (2.21)<br />

Here, M represents a third body molecule that absorbs <strong>the</strong> excess vibrational<br />

energy and <strong>the</strong>reby stabilizes <strong>the</strong> O 3 molecule formed [149, 391, 451].<br />

36

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