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

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

nor generally considered to be an air pollutant. Still, it is a greenhouse gas<br />

and participates in atmospheric chemistry involving <strong>the</strong> ozone layer by forming<br />

NO and destroying <strong>the</strong> ozone [428, 451]. Currently, N 2 O emission is <strong>the</strong><br />

single most important ozone-depleting emission and expected to remain so<br />

throughout <strong>the</strong> 21 st century. In <strong>the</strong> troposphere, N 2 O has a lifetime <strong>of</strong> 100 to<br />

200 years, compared to NO x in <strong>the</strong> range <strong>of</strong> minutes to days. Thus, <strong>the</strong> contribution<br />

<strong>of</strong> combustion processes to <strong>the</strong> overall N 2 O formation is meaningful,<br />

despite <strong>the</strong> fact that combustion is only a minor direct source <strong>of</strong> N 2 O formation<br />

and NO x formation is predominant with regard to <strong>the</strong> sum <strong>of</strong> all oxides <strong>of</strong><br />

nitrogen [19, 51, 135, 347].<br />

The remaining representatives <strong>of</strong> oxides <strong>of</strong> nitrogen, as introduced above,<br />

(NO 3 , N 2 O 3 , N 2 O 4 , and N 2 O 5 ) are present in <strong>the</strong> lower atmosphere only in very<br />

low concentrations, even in polluted environments. None<strong>the</strong>less, <strong>the</strong>y play a<br />

role in atmospheric chemistry leading to <strong>the</strong> transformation, transport, and<br />

ultimate removal <strong>of</strong> nitrogen compounds from ambient air [451]. Discussing<br />

<strong>the</strong> mechanisms on photochemical smog formation, Demerjian et al. [98] for<br />

instance provide estimates <strong>of</strong> concentrations <strong>of</strong> <strong>the</strong> various oxides and acids<br />

<strong>of</strong> nitrogen that would be present in <strong>the</strong> equilibrium state, initially assuming<br />

only molecules <strong>of</strong> nitrogen and oxygen at atmospheric pressure, 25 ◦ C, and a<br />

relative humidity <strong>of</strong> 50 %.<br />

Extended Zeldovich Mechanism<br />

The two most important parts <strong>of</strong> NO x chemistry are <strong>the</strong> <strong>the</strong>rmal NO and<br />

prompt NO reactions. These two pathways comprise <strong>the</strong> major initial steps<br />

<strong>of</strong> breaking up air nitrogen molecules. Thermal NO can be described by<br />

<strong>the</strong> chain reactions <strong>of</strong> Equations (2.7) and (2.8) that were first postulated by<br />

Zel’dovich in 1946 [471, 472]. The strong temperature dependence from which<br />

this particular type <strong>of</strong> NO derives its name is due to <strong>the</strong> fact that <strong>the</strong> N 2<br />

molecule has an extremely strong triple bond. This bond needs to be broken<br />

in order to form NO [19]:<br />

O+N 2 ⇋ NO+N, (2.7)<br />

N+O 2 ⇋ NO+O. (2.8)<br />

32

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