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the coking properties of coal at elevated pressures. - Argonne ...

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step, reaction (I) is suggested for both reactions, with <strong>the</strong> subsequent steps being different for<br />

C02 and H20 as <strong>the</strong> gaseous oxidant.<br />

C - C02 REACTION<br />

C - H20 REACTION<br />

M2C03 + 2C = 2M + 3CO<br />

2M + co2 = M20 + co<br />

M20 + C02 = M2C03<br />

c + co2 = 2co<br />

M2C03 + 2C = 2M + 3CO<br />

2M + 2H20 = 2MOH + H2<br />

2MOH + CO = M2C03 + H2<br />

C + H 20 = CO + H2<br />

Table n: Carbon Gasific<strong>at</strong>ion C<strong>at</strong>alyzed by Na2C03 or K2C03<br />

Although reaction (I) possesses a positive free energy change <strong>at</strong> temper<strong>at</strong>ures in <strong>the</strong> 600-<br />

1000°C range, <strong>at</strong> low partial <strong>pressures</strong> <strong>of</strong> CO <strong>the</strong> reaction can proceed rapidly, as shown by <strong>the</strong><br />

TGA d<strong>at</strong>a in Figure IS. Figure IS shows <strong>the</strong> equilibrium stability regions <strong>of</strong> K C03 and K(P, for<br />

reaction (l), calcul<strong>at</strong>ed from free energy d<strong>at</strong>a, as functions <strong>of</strong> temper<strong>at</strong>urg and <strong>the</strong> partial<br />

<strong>pressures</strong> (in <strong>at</strong>mospheres) <strong>of</strong> K(g) and CO. The sloping lines <strong>at</strong> each temper<strong>at</strong>ure separ<strong>at</strong>e <strong>the</strong><br />

region <strong>of</strong> stability <strong>of</strong> %C03 (upper left) from th<strong>at</strong> <strong>of</strong> K(g) (lower right). An overall gasific<strong>at</strong>ion<br />

r<strong>at</strong>e <strong>of</strong> 5 x IO- min- (about <strong>the</strong> maximu3<strong>at</strong>tained in this study <strong>at</strong> 9OO0C) would give an<br />

ambient partial pressure <strong>of</strong> CO <strong>of</strong> about 10 <strong>at</strong>m. above <strong>the</strong> gasifying char sample. At this<br />

value <strong>of</strong> Pco, and with a similar value <strong>of</strong> PK, Figure 15 indic<strong>at</strong>es th<strong>at</strong> reaction (1) would be<br />

<strong>the</strong>rmodynamically possible for all temper<strong>at</strong>ures above about 800°C. At a temper<strong>at</strong>ure <strong>of</strong><br />

6OO0C <strong>the</strong> measured gasific<strong>at</strong>ion r<strong>at</strong>e, and <strong>the</strong> ambient value <strong>of</strong> P are about two orders <strong>of</strong><br />

magnitude ess than <strong>at</strong> 9OO0C and Figure 15 shows th<strong>at</strong> reaction (IF?: again possible for P<br />

?l<br />

Pco = IO- <strong>at</strong>m. The steady st<strong>at</strong>e values <strong>of</strong> P reaction will in fact be much less than $ =<br />

because <strong>of</strong> <strong>the</strong> occurrence <strong>of</strong> reactions (2) and [f& DiFect evidence th<strong>at</strong> reaction (3) does oc%?<br />

has recently been obtained by Wood et al., using high temper<strong>at</strong>ure Knudsen cell mass<br />

spectrometry. On he<strong>at</strong>ing K C03 and carbon toge<strong>the</strong>r <strong>at</strong> temper<strong>at</strong>ures <strong>of</strong> 500°C and above, <strong>the</strong><br />

evolution <strong>of</strong> K vapor and 20 could be measured. Thus, reaction (I), which is inhibited by<br />

increasing amounts <strong>of</strong> CO in <strong>the</strong> gas phase, is probably <strong>the</strong> r<strong>at</strong>e determining step in <strong>the</strong> case <strong>of</strong><br />

<strong>the</strong> gasific<strong>at</strong>ion reactions c<strong>at</strong>alyzed by Na2C0 and K CO . Reactions (2) and (3) and also (4)<br />

and (5) have large neg<strong>at</strong>ive free energy values a? gasifi&ti<strong>of</strong>i temper<strong>at</strong>ures and are thus favored<br />

<strong>the</strong>rmodynamically, although little is known about <strong>the</strong>ir kinetics.<br />

A somewh<strong>at</strong> different p<strong>at</strong>hway probably oper<strong>at</strong>es in <strong>the</strong> case <strong>of</strong> <strong>the</strong> reactions c<strong>at</strong>alyzed by<br />

Li CO as Li 0 is more stable than <strong>the</strong> oxides <strong>of</strong> Na and K, also Li CO is more easily<br />

hy&olyzed<br />

3<br />

to Aydroxide than <strong>the</strong> carbon<strong>at</strong>es <strong>of</strong> Na and K. A possible sequegce Jf reactions th<strong>at</strong><br />

might be involved in <strong>the</strong> c<strong>at</strong>alysis process in <strong>the</strong> case <strong>of</strong> Li CO is shown in Table Ill below.<br />

Evidence for <strong>the</strong> occurrence <strong>of</strong> <strong>the</strong>se individual reactions is &ill,%owever, indirect and future<br />

efforts will be directed to exploring <strong>the</strong> c<strong>at</strong>alytic process by <strong>the</strong> aid <strong>of</strong> isotopic tracers and in<br />

determining <strong>the</strong> rel<strong>at</strong>ive r<strong>at</strong>es <strong>of</strong> <strong>the</strong> elementary steps involved in <strong>the</strong> c<strong>at</strong>alyzed gasific<strong>at</strong>ion<br />

process.<br />

79<br />

(2)<br />

(3)<br />

(1)<br />

(4)<br />

(5)

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