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ORNL-1771 - Oak Ridge National Laboratory

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UNCLASSIFIED<br />

ORNIL-LR-DWG 3032<br />

r--<br />

300 500 700 900 1100 1300<br />

TEMPERATURE (OK)<br />

Fig. 6.22. Free Energy of Formation Data as a<br />

function of Temperature for the Hydroxide, the<br />

Peroxide, and the Superoxide of Sodium.<br />

sodium hydroxide' and the entropies of sodium<br />

hydroxide," hydrogen, oxygen, and sodium in their<br />

standard reference states. The computation shows<br />

that AF;,,(NaOH) = -91.0 kcal/mole. At higher<br />

temperatures, values of the standard free energy of<br />

formation hove been given in the literature for only<br />

sodium oxide,' ' Howeverp values have been esti-<br />

mated for sodium peroxide, sodium superoxide, and<br />

sodium hydroxide in the following way. The curves<br />

of the standard free energy of formation vs temper-<br />

ature for the class of compounds dealt with here<br />

are known to a fairly good degree of approximation<br />

to consist of segmented straight lines with dis-<br />

continuous changes in slope at the transition<br />

points of the compound and of its component ele-<br />

ments. One point on each of these curves can be<br />

fixed from the values for the standord free energy<br />

of formation data at 25"C, mentioned above. The<br />

'Unless otherwise specified, literature values used<br />

herein are taken from F. D. Rossini, Selected Values o/<br />

Cb emzcal The mzodynumzc Prope rt ze s, Notion al Bureau of<br />

Standards, Washington, 0. C., 1952.<br />

'OJ. C. R. Kelly and P. E. Snyder, J. Am. Chern. Soc.<br />

73, 41 14 (1951).<br />

"F. D. Richardson and J. H. E. Jeffes, J. Iron Steel<br />

Insf. (London) 160, 261 (1948).<br />

PERIOD ENDING SEPTEMBER 70, 1954<br />

slope at this point is determined from values of<br />

the standard entropy of formation by using the<br />

1 relation<br />

These entropy data are obtained from the standord-<br />

state entropy values. The change in slope at each<br />

transition point is determined from the transition<br />

entropy, which, of course, is readily computed from<br />

the heat of trans it ion.<br />

Recently obtained datal2 on the heat capacity of<br />

liquid sodium hydroxide will permit a more precise<br />

evaluation to be made of the slope of the free<br />

energy curve from the melting point up to 1000°C.<br />

The heat of fusion of sodium peroxide (TLM<br />

= 980°K)<br />

was not available, but it should introduce only a<br />

small change in slope, which may be considered to<br />

be negligible for the computations which follow.<br />

Decomposition of Hydroxides. In considering any<br />

solvent as a reaction medium it is important to de-<br />

termine whether the solvent tends to decompose to<br />

an appreciable extent, particularly if any of the<br />

products of the decomposition take part in the re-<br />

action. The classic example is, of course, water.<br />

Here the covalent water molecules decompose<br />

slightly into ions. The resulting equilibrium fre-<br />

quently exerts a controlling influence on the course<br />

of aqueous reactions. The following is an outline<br />

of the results obtained to date in a theoretical<br />

search for the significant decomposition equilibria<br />

in fused alkali-metal hydroxides. It should be<br />

emphasized that the work presented here is in no<br />

sense definitive or complete.<br />

The most important result of the treatment given<br />

here is the evidence for the possible occurrence of<br />

appreciable quantities of peroxide as the result of<br />

decomposition equilibria. The way in which this<br />

peroxide may play a decisive role in mass transfer<br />

and corrosion will be shown in a later report.<br />

In a fused alkali-metal hydroxide in an inert<br />

environment such that the volume of any gas phase<br />

is small compared with that of the liquid phase,<br />

the fused hydroxide may be regarded thermodynami-<br />

cally as being in equilibrium with every chemical<br />

species composed of nothing more than oxygen,<br />

hydrogen, and the alkali metal. In practice, many<br />

of these chemical species can be ignored for either<br />

"W. D. Powers and G. C. Blalock, Enthalpies md<br />

Speczftc Heats of Alkali and Alkaline Earth Hydroxzdes<br />

at ffzgh Temperatures, <strong>ORNL</strong>-1653 (Jan. 7, 1954).<br />

1 03

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