Water activities of aqueous electrolyte solutions of HCl(aq), LiCl(aq), NaCl(aq), KCl(aq), CsCl(aq), NH 4 Cl(aq), MgCl 2 (aq), CaCl 2 (aq), and BaCl 2 (aq) have been determined at T = 298.15 K by the hygrometric method, and at molalities ranging from 0.2 mol โข kg -1 to saturation. From measurements
Determination of water activities, osmotic and activity coefficients in aqueous solutions using the hygrometric method
โ Scribed by Mohamed El Guendouzi; Abderrahim Dinane
- Publisher
- Elsevier Science
- Year
- 2000
- Tongue
- English
- Weight
- 250 KB
- Volume
- 32
- Category
- Article
- ISSN
- 0021-9614
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โฆ Synopsis
In the present study we use the hygrometric method for the determination of relative humidities of aqueous electrolyte solutions. The relative humidities of KCl(aq), Na 2 SO 4 (aq), and NaNO 3 (aq) have been measured for different molalities and at temperatures from (278.15 to 323.15) K. The data on the relative humidities allow the deduction of the water activities and the osmotic coefficients at the temperature of 298.15 K. The solute activity coefficients are also determined for the three salts using Pitzer's model. The results obtained by this method are compared with those found in the literature.
๐ SIMILAR VOLUMES
The mixed aqueous electrolyte system of ammonium and sodium chlorides has been studied by the hygrometric method at the temperature 298.15 K. The relative humidities of this system were measured at total molalities from 0.3 mol โข kg -1 to 6 mol โข kg -1 for different ionic-strength fractions of NH 4
## Ah&act An apparatus for contmuous measurement of water actlvlty IS described where a water permeable membrane 1s used to separate the sample from the vacuum of a contmuously pumped chamber When the sample contams no other component than water which permeates through the membrane at a sign&ant r
The osmotic and activity coefficients of aqueous magnesium chloride solutions were experimentally determined at T = 313.15 K by the isopiestic method. Lithium chloride served as the isopiestic standard for the calculation of osmotic coefficients. The molality ranges covered in this study correspond
## It f d that the relatiomhip between the mdar DBllotic coewcients(@) andthemdarconeenh.ation(c) dthesdutiam are in a quite good agreement with the fitted polynomial equation at variw temperatures over the Merent concentratim range. 'Ibe experimental results also show that over the stdied concent