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1994 | Buch

The Structure and Reaction Processes of Coal

verfasst von: K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire

Verlag: Springer US

Buchreihe : The Springer Chemical Engineering Series

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Founded on the work of the renowned Advanced Combustion Engineering Research Center, the authors document and integrate current knowledge of the organic and inorganic structure of coal and its reaction processes. With the urgent need for cleaner, more efficient use of this worldwide fuel, their work will set a clear course for future research.

Inhaltsverzeichnis

Frontmatter
Chapter 1. Introduction
Abstract
Coal has been used as an important source of fuel by humankind for thousands of years. Known international reserves of coal are greater than any other fossil fuel, including oil and gas (Smoot, 1993). Further, fossil fuels are currently and will remain for some time, the major resource to meet increasing worldwide energy demands. For example, in some countries, like China, coal is the major fossil fuel consumed. South Africa makes liquid transportation fuels from coal. Many other industrialized nations, such as the United States, select coal as the fuel of choice for power generation. Metallurgical coke, vital in the production of steel, is also made from coal. It is commercially consumed or converted in fixed beds, fluidized beds, rotary kilns, entrained beds, suspended beds, and rotating beds (Smoot, 1993). It is clear that coal is a vital, worldwide resource that must be used judiciously to meet our future energy needs.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Chapter 2. Selection of a Suite of Commonly Used Research Coals
Abstract
The selection and initial characterization of the suite of 11 commonly used research coals is summarized in this chapter (Smith and Smoot, 1988, 1990). A group of standard coals has helped to coordinate experimental research efforts and has helped to relate data obtained among programs of coal combustion research. These standard coals have been selected from available U.S. coal data bases. Organizations that provide coal samples and/or coal characterization data include (1) Pennsylvania State University, which has characterized many of the nation’s coal resources, as documented in the Penn State Coal Data Base operated by the Energy and Fuels Research Center, (2) Argonne National Laboratory’s Premium Coal Sample Program, and (3) the coal sample suite used in Pittsburgh Energy Technology Center’s Direct Utilization-Advanced Research and Technology Development program. The suite of 11 selected coals is emphasized throughout this book.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Chapter 3. Geochemistry and Macromolecular Structure of Coal
Abstract
Coal is a complex sedimentary rock derived from plant remains that underwent peatification and subsequent coalification. Coals originated as peat deposits formed in prehistoric swamps through the accumulation of plant substances whose components underwent differing degrees of chemical decomposition and polymerization. The most uniform microscopic constituents of coal, whose morphologically preserved or repolymerized materials retain distinct characteristics, are known as macerais. A brief study of the organic geochemistry of coal and its macerai characteristics will be helpful in clarifying the nature of coal structure and will give a basis for the understanding of coal structural characteristics. Given (1984b) states that even though the organic chemistry of coal has been studied for more than 100 years, the geological factors in coal chemistry have been almost totally ignored. According to Given (1984b), it is the geoscience of coals, or their geochemistry of origin and postburial geological history, that is responsible for the fact that coals are a very diverse set of materials. Consequently, it is only a study based on geological origins of coal chemistry that will enable coal researchers to rationalize the diversity in coal and to express this in a systematic manner.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Chapter 4. Coal Structural Characterization by Advanced Techniques
Abstract
Understanding of coal structure has improved markedly over the last decade. The review of the geochemical and macromolecular structure of coal showed that coal is expected to be a heterogeneous mixture composed of a macromolecular network of varying degrees of cross-linking with a molecular phase imbibed or associated with this network. The macromolecular network is thought to consist mostly of modified lignin remnants with a still unknown contribution of cellulose and melanoidin-type materials. In coals of mvb rank and lower, the network is considered to be cross-linked by alkyl and aryl ether groups with decreasing oxygen functional groups and increasing aromaticity at higher ranks. The dominant coalification process is likely to be similar to mild pyrolysis with weakly linked moieties in the coal network cleaved and eliminated during the low-temperature conversion processes of coal and an eventual increase in polycyclic aromatic structures. Because of coal’s inherent heterogeneity, a broad range of proven and developing coal characterization techniques is needed to describe and quantify coal structure. The recent progress in coal structure research has been reviewed by Haenel (1992), who points out that the significant progress made during the past decade is due, in large part, to the increasing number of research tools used to study coal structure. With a correlated and integrated program of coal characterization, important structural features of a coal can be better identified.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Chapter 5. Devolatilization Rate Processes and Products
Abstract
Pyrolysis (devolatilization in an inert atmosphere) and hydropyrolysis (devolatilization in a hydrogen atmosphere) of coal are particularly dependent on the organic properties and structural characteristics of the coal. Many approaches are taken to characterize coal conversion and reaction processes. The most advanced of these approaches relate the observed coal conversion processes to coal structure and composition. Much evidence supports the hypothesis that the devolatilization of coal is a chemical reaction (e. g., Gavalas, 1982). With an increased availability of coal structure and characteristics by advanced methods as documented in Chapter 4, a monumental task lies in understanding the devolatilization mechanisms, relating coal structure to its devolatilization behavior, and developing accurate predictive capabilities. New devolatilization models are being developed which are based, at least in part, on the chemical structure of coals. Devolatilization, as the first step in thermally driven coal conversion and utilization processes, has a profound effect on course of combustion processes (Howard, 1981; Brewster et al., 1988; Nelson et al., 1988). Previous studies have demonstrated the key role of devolatilization processes in coal conversion and utilization through the use of comprehensive combustion codes (J. D. Smith et al., 1987, 1991; Brewster et al., 1988; Smith and Smith, 1990). In parametric sensitivity studies of a two-dimensional combustion model, J. D. Smith et al. (1987, 1991; Smith and Smith, 1990) showed that one of the most critical issues or critical subprocesses in the combustion code for both coal combustion and gasification is the devolatilization process.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Chapter 6. Char Oxidation, Conversion, and Reaction Rate Processes
Abstract
The heterogeneous carbon oxidation and char gasification step is the second process to occur in the utilization of coal, and proceeds simultaneously or after devolatilization, depending on reaction conditions (Saito et al., 1991). The time required for the combustion of a char particle can be several orders of magnitude larger than that for devolatilization, ranging from 30 ms to over an hour, and is often the rate-determining step in the overall combustion of pulverized fuels (Essenhigh, 1981; I. Smith, 1982; Smoot and Smith, 1985). The processes of char oxidation are no less complex than those of devolatilization. The chemical structure of the coal does not control the reaction processes to the same extent as devolatilization, but, due to the high temperatures generally associated with char oxidation, pore diffusion and external diffusion often play a pronounced role. Thus, the physical structure of coal, including pore structure, surface area, particle size, and inorganic content, is important in understanding and modeling char oxidation processes. Intrinsic reactivity of char refers to the chemical reaction on the pore walls, after diffusion of gas through the pores inside the char. When intrinsic reactivity is the ratecontrolling process, oxygen migrates toward the center of the char particle, the particle size remains nearly constant during combustion, and the particle density decreases with conversion. However, if the reaction is fast, typically at high temperature, oxygen diffusion is the dominant process; the oxygen is consumed as it reaches the particle surface, and the density of the particle is near constant while the particle size decreases in a shrinking core mode.
K. Lee Smith, L. Douglas Smoot, Thomas H. Fletcher, Ronald J. Pugmire
Backmatter
Metadaten
Titel
The Structure and Reaction Processes of Coal
verfasst von
K. Lee Smith
L. Douglas Smoot
Thomas H. Fletcher
Ronald J. Pugmire
Copyright-Jahr
1994
Verlag
Springer US
Electronic ISBN
978-1-4899-1322-7
Print ISBN
978-1-4899-1324-1
DOI
https://doi.org/10.1007/978-1-4899-1322-7