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Carbon vitrinite concentrates

Fig. 10. Correlation between aliphatic carbon and volatile matter for oil shales ( ) and coals (o, A) and vitrinite concentrates (+). (a) Volatile Matter vs Aliphatic Carbon, (b) Volatile Matter vs Total Organic Carbon. Fig. 10. Correlation between aliphatic carbon and volatile matter for oil shales ( ) and coals (o, A) and vitrinite concentrates (+). (a) Volatile Matter vs Aliphatic Carbon, (b) Volatile Matter vs Total Organic Carbon.
Studies initiated by the author in CSIRO (13) seek to throw light on the role of the various macerals by studying the conversion, under catalytic hydrogenation conditions, in Tetralin as vehicle, of maceral concentrates from a high volatile bituminous coal. Some preliminary results, given in Fig. 3, show conversions as almost complete for the hand picked vitrain (>90% vitrinite) from a high volatile bituminous coal (Liddell seam N.S.W., 83.6% carbon and 43% volatile matter both expressed on a dry ash-free basis). However, it is evident that the conversion of the whole coal increases rapidly with increase in hydrogen pressure (under otherwise similar conditions - batch autoclave, 4h. 400°C). [Pg.64]

H/C = atomic hydrogen-to-carbon ratio V = vitrinite content of coal VM volatile matter St = total sulfur TRM = total reactive macerals The adequacies of these reactivity correlations, expressed as a percentage of the total variation in the data set explained by the model, were 80.0%, 79.2%, and 47.5% respectively. A later paper in the series (21) concentrated on the development of reactivity correlations for a set of 26 high volatile bituminous coals with high sulfur contents, and extended the models previously developed in include analyses of the liquefaction products and coal structural features. These structural features included the usual... [Pg.175]

Results on Unheated Samples. The results obtained in Southampton for the set of British samples are shown in Figures 2 and 3. In Figure 2 the spin concentration of each maceral is plotted against the carbon content (daf) of the associated vitrinite, and the points for each set of macerals from one coal are joined by a vertical line. It can be seen that the vitrinite series forms a well-defined narrow band which curves upwards sharply at about 90% carbon, and the data resemble closely those presented earlier by Austen and Ingram for whole coals. The values of exinites form a wider, approximately horizontal band lying a little below the vitrinite band, while the fusinite data appear to vary at random but lie consistently well above the vitrinite band and are appreciably higher than vitrinites of the same carbon content (90-92%) would be. [Pg.350]

Free Radicals in Macerals. Electron spin resonance (ESR) has been used to study carbon free radicals in coals, and to some extent, separated macerals. The technique provides information on radical density and the environment of the radicals. The resonance position, termed the g-value, is dependent on the structure of the molecule which contains the free electron. The line width is also sensitive to the environment of the unpaired electron. In an early study, Kroger (71) reported that the spin concentration varied between maceral groups with liptinite < vitrinite inertinite. For this limited set of samples the spin concentration increases with rank for liptinites and vitrinites and decreases for the micrinite samples. On the other hand, van Krevelen (72) found the same general results except... [Pg.18]


See other pages where Carbon vitrinite concentrates is mentioned: [Pg.196]    [Pg.103]    [Pg.309]    [Pg.345]    [Pg.352]    [Pg.357]    [Pg.125]    [Pg.149]    [Pg.41]    [Pg.42]    [Pg.114]    [Pg.3666]    [Pg.8]    [Pg.311]    [Pg.64]    [Pg.88]   
See also in sourсe #XX -- [ Pg.102 , Pg.108 ]




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