Measurements are reported on the difference in vapor pressures of H2O and T2O ( − 9°‐114°C) and of H2O and D2O (4°‐114°C). The relative vapor pressures of the pure liquids are represented by ln (pH2O / pT2O) = ( − 103.87 ± 0.57) / T + (46 480 ± 210) / T2 and ln (pH2O / pD2O) = ( − 70.87 ± 0.43) / T + (33 630 ± 160) / T2. The normal boiling points of T2O and D2O are 101.51° and 101.42°C. Isotopic differences in heats of vaporization are given from 10° to 110°C. Triple‐point temperatures and pressures are summarized. Vapor‐pressure crossover temperatures are: D2O–T2O, 116.2° ± 0.5°C; H2O–T2O, 190 ± 10°C (estimated); H2O–D2O, 220.7° ± 0.1°C (literature).

The data were also fitted to extensions of the above equations which included correction terms based on Bigeleisen's formulation of the vapor‐pressure isotope effect and a uniformist harmonic‐oscillator model of water. Estimates of the coefficients of 1 / T and 1 / T2 for H2O–D2O from Raman spectra are in reasonable agreement with coefficients from this data fit. Ratios of corresponding coefficients for H2O–D2O and H2O–T2O agree with theory.

1.
After completion of the present experimental work T2O vapor pressures were reported by
M. M.
Popov
and
F. P.
Tazetdinov
,
At. Energ. USSR
8
,
420
(
1960
);
M. M.
Popov
and
F. P.
Tazetdinov
,
Nucl. Sci. Abstr.
14
,
2113
(
1960
).
2.
For a summary and references to previous D2O work see: I. Kirshenbaum, Physical Properties of Heavy Water (McGraw‐Hill Book Co., New York, 1951).
3.
J.
Bigeleisen
,
J. Chem. Phys.
34
,
1485
(
1961
).
4.
M.
Goldblatt
and
W. M.
Jones
,
Anal. Chem.
36
,
431
(
1964
).
5.
Distillation of waters onto the Hg surface was not allowed to be excessive. H2OH2O blank measurements showed that the effects were not serious. The condensation of waters throughout the tensimeter was considered desirable in the T2O measurements because (a) this helped ensure a uniform concentration of radiolytic gas, as assumed in the correction for it, and (b) a large surface was created for dissipation of radioactive heat; a large blob of Hg was also placed in the 1‐cc bulbs for this purpose; however, distillation from an overheated area should fix the vapor pressure at bath temperature. Experiments at several temperatures with H2O on both sides of a tensimeter showed that, even at the highest temperatures, a systematic error in Δp would not be more than 0.01 cm Hg. Experiments with H2O on both sides, but with heat introduced electrically on one side at the same rate as was generated in T2O, suggest that the effect of radioactive heating in T2O could amount to 0.01 cm Hg at the highest temperature. No correction was made, since nonuniform introduction of heat in this test may make the case less favorable than with T2O.
6.
A.
Gould
and
T.
Vickers
,
J. Sci. Instr.
29
,
85
(
1952
).
7.
International Critical Tables (McGraw‐Hill Book Co., New York, 1927), Val. 2, p. 458.
8.
The error made by this procedure is less than 0.001 cm Hg. For a more general method of correction see
G. N.
Lewis
and
R. E.
Cornish
,
J. Am. Chem. Soc.
55
,
2616
(
1933
).
9.
(a)
N. S.
Osborne
and
C. H.
Meyers
,
J. Res. Natl. Bur. Std.
13
,
1
(
1934
).
(b) In order to get PT2O(s) for the lowest temperatures on T2O (s), pressures of H2O (s) were taken from Handbook of Chemistry and Physics (Chemical Rubber Publ. Co., Cleveland, Ohio, 1961), 43rd ed.
10.
R. H. Moore and R. K. Zeigler, Los Alamos Rept. LA‐2367; available from the Office of Technical Services, U.S. Dept. Commerce, Washington 25, D.C.
11.
The root‐mean‐square deviations of Δpobs from Δpcalc in Tables I and II are 0.015 cm Hg both for 43 H2OT2O points and 64 H2OD2O points. Equations of the forms A+B/T+CT,A/T+B/T2+C/T3, and A/T+B/T2+C/T4 were also tried, using the same least‐squares criterion as for (1) and (2). These three forms all reduced the rms deviations to 0.011 cm Hg for H2OT2O and 0.013 for H2OD2O, and gave better distributions of the signs of the deviations. It is doubtful that the improvements in fit are statistically significant. The uncertainties in the parameters become quite large due to their greater number. Equations of the form A+B/T were unsatisfactory.
12.
G. N.
Lewis
and
R. T.
MacDonald
,
J. Am. Chem. Soc.
55
,
3057
(
1933
).
13.
R. L.
Combs
,
J. M.
Googin
, and
H. A.
Smith
,
J. Phys. Chem.
58
,
1000
(
1954
).
14.
H. A.
Smith
and
K. R.
Fitch
,
J. Phys. Chem.
67
,
920
(
1963
).
15.
H. S.
Frank
,
Federation Proc.
Suppl. 15,
24
, Pt. 3, 1 (
1965
).
16.
B. E.
Conway
,
Ann. Rev. Phys. Chem.
17
,
481
(
1966
).
17.
J.
Bigeleisen
,
J. Chim. Phys.
60
,
35
(
1963
).
18.
J. Bigeleisen, Proc. Intern. Symp. Isotope Separation, Amsterdam, 1957, 127 (1958).
19.
M. J.
Stern
,
W. A.
Van Hook
, and
M.
Wolfsberg
,
J. Chem. Phys.
39
,
3179
(
1963
); eq. 13.
20.
G. E.
Walrafen
(private communication);
J. Chem. Phys.
47
,
114
(
1967
).
Walrafen also provided estimates of full widths at half‐maximum. These are 300, 300, and 150 cm−1 for the frequencies 717, 538, and 439 cm−1, respectively. From these data we estimate r = 0.2 as an average which is applied to all librational bands.
21.
The equations obtained are
and
22.
(a)
J. W.
Schultz
and
D. F.
Hornig
,
J. Phys. Chem.
65
,
2131
(
1961
);
(b)
W. R.
Busing
and
D. F.
Hornig
,
J. Phys. Chem.
65
,
284
(
1961
).
23.
R. E.
Weston
, Jr.
,
Spectrochim. Acta
18
,
1257
(
1962
).
24.
G. Herzberg, Infrared and Raman Spectra (D. Van Nostrand Co., Inc., New York, 1945), p. 282.
25.
For T2O gas frequencies see
W. F.
Libby
,
J. Chem. Phys.
11
,
101
(
1943
);
W. F.
Libby
,
15
,
339
(
1947
).,
J. Chem. Phys.
26.
W. F.
Giauque
and
J. W.
Stout
,
J. Am. Chem. Soc.
58
,
1144
(
1936
).
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