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ORNL-1771 - Oak Ridge National Laboratory

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K, I r3<br />

(G2<br />

PERIOD ENDING SEPTEMBER 70, 7954<br />

YM 0 yhf<br />

three values of the decomposition pressure with<br />

respect to hydrogen. Except over unique temper-<br />

2 ature ranges, one of these three decomposition<br />

uizl Q H<br />

pressures will be much larger than the other two<br />

- I I', = - I<br />

4:<br />

d2<br />

YMO, YMMH<br />

K =r--l<br />

4 4<br />

I'4 - 4----"<br />

4 O H di<br />

The above equations are exact. However, a rrtore<br />

useful form can be obtained by assuming that the<br />

extent of decomposition is very small. As will be<br />

shown later, this assumption involves a negligible<br />

error for all four reactions. From this assumption<br />

two conclusions can be drawn: (1) the activity of<br />

the hydroxide as used in the above equations may<br />

be taken to be unity because of the choice of<br />

standard states; (2) the partial pressures of water<br />

and hydrogen in the gas phase may be taken to be<br />

equal to the fugacities in the gas phase and hence<br />

equal to the fugacities in the liquid phase. Finally,<br />

by definition, the fugacity of the gases in the<br />

standard reference state is unity. Substituting<br />

these conclusions into the above equations, solving<br />

for the partial pressures, and applying the reaction<br />

isotherm give<br />

2/5<br />

where (pH- ) is to be read as the partial presswe<br />

[ ..2Ii<br />

of hydrogen provided that no other hydrogenproducing<br />

reaction is operative save the Ith.<br />

From the original choice of mole fr~cti~ns it<br />

may be noted that the ubove partial pressures are<br />

1<br />

'<br />

and hence, by the law of mass action, will stabilize<br />

the others. Thus, Qnly one of the three pressures<br />

will be the decomposition pressure of ,llOH with<br />

regard to hydrogen.<br />

Because of the lack of thermodynamic data on<br />

all the alkali-metal hydroxides except sodium, it<br />

is necessary, in most applications, to use ratios<br />

of decomposition pressures. Thus, it IS assumed<br />

that reactior~s 1 and 2 are simultaneously at equi-<br />

librium and that they determine the gaseous water<br />

and hydrogen pressures, respectively. By dividing<br />

Eq. 56 into 5a, the decomposition pressure ratio<br />

becomes<br />

where<br />

The concentrations of the oxide in reaction 1 and<br />

of the peroxide in reaction 2 are not independent<br />

but are related through the equilibrium<br />

4"s" .<br />

Furtkrrrrore, the concentrations of oxygen in this<br />

equilibrium atid of hydrugen in reuction 2 are<br />

related through the equilibrium<br />

the decomposition pressures and that there ure (8) AF,. a

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