In the past century, the homogeneous nucleation of light water (H2O) has repeatedly been studied using
various experimental techniques. Generally, the onset of nucleation was recorded, while less frequently, the
actual nucleation rates were determined. In contrast, the nucleation of heavy water (D2O) has been examined
only in a single instance with no nucleation rates measured. Here, we report the first nucleation rate study of
D2O along with nucleation rate measurements for H2O, which we repeated for comparison under identical
conditions. We find that the nucleation rates for H2O and D2O differ by a factor of 2500, if compared at the
same respective vapor pressure p
v and temperature T, whereas the comparison at the same supersaturation S
shows an agreement within experimental scatter. Also, the numbers of molecules in the critical clusters,
which are determined from the slopes of the ln J versus ln S curves, are nearly the same for both isotopic
waters. A satisfactory agreement with previous nucleation rate measurements of H2O made by Viisanen et al.
(Viisanen, Y.; Strey, R.; Reiss, H. J.
Chem. Phys. 1993, 99, 4680; 2000, 112, 8205) is observed, if the onset
supersaturations S
0 at nucleation rates of J
0 = 107 cm-3 s-1 are compared. Using the most recent expressions
for temperature-dependent vapor pressures, we calculated surface tensions and densities predictions by the
classical Becker−Döring nucleation theory. Around T = 240 K, the predictions quantitatively agree with the
experimental data. However, as in the case of other systems (e.g., alcohols and alkanes), classical theory
shows a stronger temperature dependence than experimentally observed. A temperature-dependent correction
of the classical theory is developed which permits analytical calculation of nucleation rates as function of
supersaturation and temperature over extended ranges.