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1 - Fuels and the global carbon cycle

Published online by Cambridge University Press:  05 February 2013

Harold Schobert
Affiliation:
Pennsylvania State University
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Summary

Fuels are substances that are burned to produce energy. In many practical situations, it can be advantageous first to carry out one or more processing steps on a fuel before it is burned. This might be done to improve the yield of the fuel from its source, to improve the performance of the fuel during combustion, or to mitigate potential environmental problems resulting from using the fuel. Examples include processes to enhance the yield of gasoline from petroleum, to improve gasoline performance in engines, and to convert solid coal into cleaner gaseous or liquid fuels. Some fuels, particularly natural gas and petroleum, also serve as important feedstocks for the organic chemical industry, for producing a host of useful materials. So, fuels can be used in at least three different ways: burned directly to release thermal energy; chemically transformed to cleaner or more convenient fuel forms; or converted to non-fuel chemicals or materials. These uses might appear quite different at first sight, but all have in common the making and breaking of chemical bonds and transformation of molecular structures. The ways in which we use fuels, and their behavior during conversion or utilization processes, necessarily depend on their chemical composition and molecular structure.

The world is now in a transition state between an energy economy that, in most nations, has an overwhelming dependence on petroleum, natural gas, and coal, to a new energy economy that will be based heavily on alternative, renewable sources of energy, including fuels derived from plants. This book covers both. The dominant focus is on wood, ethanol, and biodiesel among the plant-derived fuels, and on coal, petroleum, and natural gas as traditional fuels. If we were to assemble a collection of examples of each, at first sight they would appear to be wildly different. Natural gas, a transparent, colorless gas, commonly contains more than ninety percent of a single compound, methane, at least as delivered to the user. Ethanol, a transparent, volatile, low-viscosity liquid, is a single compound. Petroleum is a solution of several thousand individual compounds. Depending on its source, the color, viscosity, and odor can be very variable. Biodiesel, a lightly colored, moderate viscosity liquid, contains only perhaps a half-dozen individual compounds. Wood, a heterogeneous solid, is usually of light color, but varies in density, hardness, and color, depending on its source. Coals usually are black or brown heterogeneous solids of ill-defined and variable macromolecular structure.

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Publisher: Cambridge University Press
Print publication year: 2013

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References

Cuff, David J. and Goudie, Andrew S. The Oxford Companion to Global Change. Oxford University Press: New York, 2009. This is a very handy one-volume reference book with several hundred short articles, including useful material on the global carbon cycle, biomass and biofuels, and fossil fuels.Google Scholar
McCarthy, Terence.How on Earth?Struik Nature: Cape Town, 2009. An introductory book on geology with superb color illustrations. Chapter 3, on the Earth's atmosphere and oceans, is relevant to the material in this chapter.Google Scholar
Richardson, Steven M. and McSween, Harry Y.Geochemistry: Pathways and Processes. Prentice-Hall: Englewood Cliffs, NJ, 1989. A book on geochemical principles presented in the context of thermodynamics and kinetics. Chapter 4, on the oceans and atmosphere, and Chapter 6, on weathering of rocks, are useful for understanding the global carbon cycle.Google Scholar
Schobert, Harold H.Energy and Society. Taylor and Francis: Washington, 2002. An introductory text surveying various energy technologies and their impacts on society and on the environment. Chapter 34 discusses the global carbon cycle and introduces the concept of biomass energy being a short-circuit in the cycle.Google Scholar
Vernadsky, Vladimir I. The Biosphere. Copernicus: New York, 1998. This book was first published in 1926, and provides a remarkable discussion of how living organisms have transformed the planet, including the geochemical cycling of elements and the ways in which organisms utilize geochemical energy. The edition listed here is extensively annotated with explanations and findings through the 1990s.CrossRefGoogle Scholar
Williams, R.J.P. and Fraústo da Silva, J.J.R.The Natural Selection of the Chemical Elements. Clarendon Press: Oxford, 1996. This book presents aspects of the physical chemistry of distribution of chemical elements between living and non-living systems. Chapter 15 on element cycles includes a discussion of the global carbon cycle; other chapters also contain useful discussions of the partitioning of carbon between various natural systems.Google Scholar

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