Chapter 8

Environmental combustion considerations

Abstract

Several forms of combustion-generated air pollutants and their mechanisms of formation and reduction are presented. These include photochemical smog, oxides of nitrogen, sulfur oxides, and carbon particulates (soot). Finally, the stratospheric ozone balance problem is examined along with the catalytic cycles of HOx, NOx, and ClOx.

Keywords

Oxides of nitrogen; Photochemical smog; Soot; Stratospheric ozone; Sulfur oxides

8.1. Introduction

In the mid 1940s, symptoms now attributable to photochemical air pollution were first encountered in the Los Angeles area. Several researchers recognized that the conditions there were producing a new kind of smog caused by the action of sunlight on the oxides of nitrogen and subsequent reactions with hydrocarbons. This smog was different from the “pea soup” conditions prevailing in London in the early twentieth century and the polluted-air disaster that struck Donora, Pennsylvania, in the 1930s. It was also different from the conditions revealed by the opening of Eastern Europe in the last part of the twentieth century. In Los Angeles, the primary atmosphere source of nitrogen oxides, CO, and hydrocarbons was readily shown to be the result of automobile exhausts. The burgeoning population and industrial growth in United States urban and exurban areas were responsible for the problem of smog, which led to controls not only on automobiles but also on other mobile and stationary sources.
Atmospheric pollution has become a worldwide concern. With the prospect of supersonic transports flying in the stratosphere came initial questions as to how the water vapor ejected by the power plants of these planes would affect the stratosphere. This concern led to the consideration of the effects of injecting large amounts of any species on the ozone balance in the atmosphere. It then became evident that the major species that would affect the ozone balance were the oxides of nitrogen. The principal nitrogen oxides found to be present in the atmosphere are nitric oxide (NO) and nitrogen dioxide (NO2)—the combination of which is referred to as NOx—and nitrous oxide (N2O). As Bowman [1] reported, the global emissions of NOx and N2O into the atmosphere have been increasing steadily since the middle of the nineteenth century. Although important natural sources of the oxides of nitrogen exist, a significant amount of this increase is attributed to human activities, particularly those involving combustion of fossil and biomass fuels. For details as to the sources of combustion-generated nitrogen oxide emissions, one should refer to Bowman’s review [1].
Improvement of the atmosphere continues to be of great concern. The continual search for fossil fuel resources can lead to the exploitation of coal, shale, and secondary and tertiary oil recovery schemes. For instance, the industrialization of China, with its substantial resource of sulfur coals, requires consideration of the effect of sulfur oxide emissions. Indeed, the sulfur problem may be the key in the more rapid development of coal usage worldwide. Furthermore, the fraction of aromatic compounds in liquid fuels derived from such natural sources or synthetically developed is found to be large, so that in general, such fuels have serious sooting characteristics.
This chapter seeks not only to provide better understanding of the oxidation processes of nitrogen and sulfur and the processes leading to particulate (soot) formation, but also to consider appropriate combustion chemistry techniques for regulating the emissions related to these compounds. The combustion—or, more precisely, the oxidation—of CO and aromatic compounds has been discussed in earlier chapters. This information and that to be developed will be used to examine the emission of other combustion-generated compounds thought to have detrimental effects on the environment and on human health. How emissions affect the atmosphere is treated first.
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