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liquefaction pathways of bituminous subbituminous coals andtheir

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I<br />

I<br />

s<br />

F<br />

B<br />

1:<br />

8<br />

a<br />

cc<br />

30 40 50 60 70 80<br />

CO evolved before 750°C<br />

(%<strong>of</strong> total CO)<br />

""L3<br />

10<br />

n -<br />

10 20 30<br />

Total CO evolution (wt% dat7<br />

Correlation <strong>of</strong> P olysis Tar<br />

%%%rand oluene Soluges from<br />

Li uefaction 2) for Zap Lpte with,<br />

a)(hyrolysis COEvoluhon efore 750 C;<br />

b) Total Pyrolysis CO Evolution.<br />

Time (minutas) h Time (minutes)<br />

Time (minutea) (minutas)<br />

Figme 4. CO Evolution Dunn Coal P olysis. a) Raw Zap; b) Remoisturized Zap;<br />

c) aw Wyodal?; d) Remoistunzef Wyodag<br />

586

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