ORNL-1771 - Oak Ridge National Laboratory
ORNL-1771 - Oak Ridge National Laboratory
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