always for the re-moisturized <strong>coals</strong>. The total evolution <strong>of</strong> CO, and CO from pyrolysis is changed significantly by cation- exchange. However, only in the case <strong>of</strong> CO does the evolution pr<strong>of</strong>ile change significantly. After careful demineralization, a calcium form Zap or Wyodak coal can be prepared at pH= 8, which is similar to the raw coal with regard to pyrolysis and <strong>liquefaction</strong> behavior. At pH =8, cations are most likely to be coordinating multiple oxygen functionalities around themselves through electrostatic type interactions, which diminishes the importance <strong>of</strong> valency. Some <strong>of</strong> the moisture in a coal is associated with the cations. The moisture content has a larger role in <strong>liquefaction</strong> than in pyrolysis because it is present for a longer period <strong>of</strong> time. ACKNOWLEDGEMENTS This work was supported by the U.S. D.O.E. Pittsburgh Energy Technology Center under Contract No. DE-AC22-91 PC91026. REFERENCES 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. Whitehurst, D.b., Mitchell, T.O., and Farcasiu, M., Coal Liauefaction. The Chemistrv and Technoloav <strong>of</strong> Thermal Processes, Academic Press, NY (1 980). Mochida, I., Shimohara, T., Korai, Y., Fujitsu, H.. and Takeshita, IC, Fuel 62,659, (1983). Tyler, R.J. and Schafer, H.N.S., Fuel, 59, 487, (1980). Morgan, M.E. and Jenkins, Fuel, 65, 757, (1986). Morgan, M.E. and Jenkins, Fuel, 65, 764, (1986). Morgan, M.E. and Jenkins, Fuel, 65, 769, (1986). Wornat, M.J., and Nelson P.F., Energy and Fuel, 6 (2) (1992). Bishop, M., and Ward, D.L., Fuel, 37, 191, (1958). Vorres, KS., Energy and Fuel, 4 (5). 420 (1990). Schafer, H., Fuel, 49, 197, (1970). Serio, M.A., Kroo, E., Teng, H., Charpenay, S., and Solomon, P.R., 'The Dual Role <strong>of</strong> Oxygen Functions in Coal Pretreatment and Liquefaction: Crosslinking and Cleavage Reactions," Fifth Quarterly Report, U.S. DOE Contract No. DE-AC22-91-PC91026 (1992). van Bodegom, E., van Veen, J.A., van Kessel. G.M.M., Sinnige-Nijssen, M.W.A., and Stuiver, H.C.M, Fuel, 63, 346 (1984). Suuberg, EM., Lee, D., and Larsen, J.W., Fuel, 64, 1668, (1985). Suuberg, E.M., Unger, P.E., and Larsen, J.W., Energy & Fuels, 1, 305, (1987). Solomon, P.R., Serio, M.A., Deshpande, G.V., and Kroo, E., Energy & Fuels, 4 (I), 42, (1 990). Schafer, H., Fuel, 51, 4, (1972). 582
Table 1. F'yrolysis Results <strong>of</strong> Vacuum Dried Modified Zap Samples. Coal Pyndysb Products (d.% ,d& Tars Cop CO Ha0 CH4 Char Fresh 7 8.9 14.7 14.3 2.2 57 Demin. 20 4.8 10.4 8.4 2.7 fA Demin. +IC+ (pH6) 11 8.6 9.9 16.0 1.9 57 Demin. + Ce* (pH8) 10 8.6 13.5 10.3 2.4 58 Demin. + Be* (pH8) 6 11.7 15.8 18.6 2.6 55 Demin. + K+ (pHl2.5) 5 9.9 12.4 13.5 1.6 57 Demin. + Ce* (pHl2.5) 4 8.2 22.6 12.6 2.0 51 Demin. + Ba* (pHl2.5) 3 10.5 24.1 15.5 2.6 52 Table 2. Liquefaction Results <strong>of</strong>vacuum Dried Modified Zap Samples. Toluene Solubles GlM Total Oils Auphaltenes Cop CO CH4 Fresh 26 12 14 4.3 0.24 0.25 Demin. 52 26 26 1.1 0.43 0.27 Demin. +I(+ (pH8) 30 11 19 7.7 0.27 0.17 Demin. + Ca++ (pH81 25 13 12 2.7 0.30 0.22 Demin. + Ba++ (pH81 37 25 12 7.3 0.40 0.20 Demin. + IC+ (pH1z.5) Demin. + Ca++ (pHl2.5) 17 * 5 * 12 3 5.0 0.7 0.24 0.04 0.27 0.08 Demin. + Ba++ (pHl2.5) 15 15 0.5 0.3 0.27 0.02 Yields Calculated by Difierenca were Negative. Solvent heorparation is Sunperred. Notes V3.R = Vohmetrlc Swelling Ratio in Pyridine, Pa = pyridine Sohbles (daO Moisture was Dstermined by TG-FlYR and ls Reponed on an Abreesived Baals. NM =Not Measured. Table 4. The Carbonyl and Phenolic Contents <strong>of</strong> Zap and Wyodak Coals Determined by Barium Titration. (meq g' daf basis) Carboxyl Groups Phenolic Groups Total Acidity Zap Lignite 2.52 6.74 9.26 Wyodak Sub. 2.40 5.76 8.16 583
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LIQUEFACTION PATHWAYS OF BITUMINOUS
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the conversion of A+P and O+G with
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Asphaltcncs PrCasphaltenCS Cwr%, da
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NEW DIRECTIONS TO PRECONVERSION PRO
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ecause of incorporation of the coal
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should be considered more. The step
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17 18 Run no. 0 cys I ToS-CyS TS-To
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INTRODUCTION Effects of Thermal and
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apid decline in modulus. The loss m
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-0.01- . 04 5 -0.03- E 6 -0.0s- c)
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Assessment of Small Particle Iron O
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yields are calculated by subtractin
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conversion is greater than the corr
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Table 3. Effect of Superfine Iron O
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EFFECT OF A CATALYST ON THE DISSOLU
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inherent volatility of Mo(CO), perm
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Analysis of the quantity and compos
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$ EO .- 0 m L 0 c 0 0 > 40 300 350
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0 0 0 0 0.000 0.005 0.010 0.015 0.0
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of these studies indicate that cont
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Different levels of adsorption occu
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Nominal 2 Table 1. Concentration of
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- iF m 1.6 1.4 1.2 - - - 1- 0 0.8 -
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RESULTS AND DISCUSSION Swelling of
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. . % . . 9 'HF 0 0 0 *. . 0 . . 0
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1.50 KQ 1.00 0.50 I / ' 02 525 I 1
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hydrogen atoms. The hydrogen atoms
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D to generate more D atoms. It is r
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- Page 59 and 60: Figure 3. Minimum Steps to Explin D
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- Page 77 and 78: of MoCo-TC2 at the level of 0.5 wt%
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- Page 83 and 84: The effect of Corn20 preaatment on
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- Page 87 and 88: DISSOLUTION OF THE ARGONNE PREMIUM
- Page 89 and 90: A much more def~tive trend is seen
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- Page 93 and 94: same conditions and an extraction t
- Page 95 and 96: ACKNOWLEDGEMENT The authors thank t
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- Page 99 and 100: to be originally derived from demet
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- Page 115 and 116: of some of the thermobalance runs.
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- Page 131 and 132: CONCLUSIONS The characexizntion of
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Use of Biocatalysts for the Solubil
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Results Enzyme Modification with Di
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Conclusions Reducing enzymes can be
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Dynamics of the Extract Molecular-W
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where yi = (x-xi !/pi. The zero mom
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satisfactory agreement between theo
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0.8 0.6 0.4 0.2 “E \ bo Y, - 1 0
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The Use of Solid State C-13 NMR Spe
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differences lie in the fact that th
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I- z W 0 K W n PROTONATED AROMATIC
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ZAP WIO SIDE CHAINS IN PYRIDINE EXT
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ORGAFlIC VOLATILE MATER AND ITS SUL
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(Figure 1). They indicated that the
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Table 3. Elemental analysis of arom
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1- 700'C Figure 3. GClFID chromatog