The osmotic and activity coefficients of aqueous sodium and potassium trichloroacetates have been determined at the temperature 298.15 K by the isopiestic method, in the molality range . y1 . y1 Ž . from about 0.2 mol kg to 9.5 and 8.0 mol kg , respectively. The results have been discussed in terms
Isopiestic determination of the osmotic and activity coefficients of Cu(NO3)2(aq) at the temperature 298.15 K
✍ Scribed by John G. Albright; Paola Rizzo; Joseph A. Rard
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 295 KB
- Volume
- 30
- Category
- Article
- ISSN
- 0021-9614
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✦ Synopsis
The four previous isopiestic investigations of Cu NO aq at the temperature 298.15 K 3 2 exhibit a remarkable lack of agreement. Consequently, isopiestic vapor-pressure Ž . Ž . measurements were performed for Cu NO aq solutions at T s 298.15 K both at the Texas 3 2 Christian University and the Lawrence Livermore National Laboratory. These measurements . y1 Ž . extend from molality m s 0.0638 to 6.9235 mol kg . Under the conditions typically used Ž . Ž . for isopiestic experiments, it is found that solutions of Cu NO aq at higher molalities lose 3 2
HNO into the vapor phase, resulting in a gradual increase in the extent of hydrolysis of their 3 solutions as the samples are re-equilibrated. This produces a progressive downward drift in the apparent osmotic coefficients. Consequently, most previous higher-molality isopiestic results for this system are believed to be unreliable. Experiments were performed to quantify and to minimize the effect of this hydrolysis on the resulting osmotic coefficients. These experiments indicate that the error in the osmotic coefficient from this HNO loss is 3 . y1 Ž . Ž . insignificant at lower molalities of Cu NO aq ; at m s 4 mol kg it is ( 0.2 per cent, 3 2 . y1 but above m f 5 mol kg it can become quite significant. Recommended values of the Ž . Ž . osmotic coefficients, water activities, and mean activity coefficients of Cu NO aq are 3 2
. y1 presented up to m s 3.00 mol kg , the maximum molality where we consider them to be . y1 completely accurate, and, with slightly lower accuracy, up to m s 6.9235 mol kg . Pitzer's equation was found to represent reliably the experimental osmotic coefficients provided the third virial coefficient was ionic-strength dependent.
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