The essence of the comment by Cisternas(1) is that (1) the model of Cisternas and Lam,(2,3) developed for the temperatures between 273 and 413 K, can be extended to correlate and predict the vapor pressure data we reported for the ternary system NaCl–KCl–H2O at temperatures from 493.15 to 693.25 K4. Also (2) their model can be enhanced by (a) adjusting the water parameters Cs and Ds to the water vapor

Re: Ying Chen and I-Ming Chou, Measurements of Vapor Pressures of Aqueous Solutions in the NaCl–KCl–H2O System from 493.15 to 693.25 K in a Fused Silica Capillary High-Pressure Optical Cell.(1) In the article cited above, vapor pressures of aqueous solutions containing NaCl and KCl were measured at temperatures from 493.15 to 693.25 K. These measurements are valuable in geological processes because

As the Vϕ values listed in Table 4 of the original published article are miscalculated, the corrected table is provided below. The caption and uncertainties are correct in the published article and are listed here for clarity. Standard uncertainties u are u(p) = 0.50 kPa, u(T) = 0.01 K, uc(x) = 0.0002, and uc(Vϕ) = 0.01 cm3·mol–1. As a consequence of the revision of the Vϕ values, the sentence “According

This article is part of the Alternative Refrigerants special issue. In this issue of the Journal of Chemical& Engineering Data (JCED) we are pleased to present a collection of manuscripts showcasing new trends in refrigerants for application in improved cooling systems. The Montreal protocol has had an indisputable positive impact on the protection of the ozone layer by phasing out the manufacture