The water activities and osmotic coefficients of aqueous solutions of {(NH 4 ) 2 SO 4 + Li 2 SO 4 } and {(NH 4 ) 2 SO 4 + Na 2 SO 4 } have been determined at a temperature of 298.15 K with a hygrometric method, at molalities in the region 0.2 mol β’ kg -1 to saturation of the solutes for different fr
Apparent molar heat capacities and apparent molar volumes ofY2(SO4)3(aq),La2(SO4)3(aq),Pr2(SO4)3(aq),Nd2(SO4)3(aq),Eu2(SO4)3(aq),Dy2(SO4)3(aq),Ho2(SO4)3(aq), andLu2(SO4)3(aq)atT =  298.15 K andp =  0.1 MPa
β Scribed by Robert A. Marriott; ; Andrew W. Hakin; ; Joseph A. Rard
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 526 KB
- Volume
- 33
- Category
- Article
- ISSN
- 0021-9614
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β¦ Synopsis
The apparent molar heat capacities C β’ p,Ο and apparent molar volumes V β’ Ο of Y 2 (SO 4 ) 3 (aq), La 2 (SO 4 ) 3 (aq), Pr 2 (SO 4 ) 3 (aq), Nd 2 (SO 4 ) 3 (aq), Eu 2 (SO 4 ) 3 (aq), Dy 2 (SO 4 ) 3 (aq), Ho 2 (SO 4 ) 3 (aq), and Lu 2 (SO 4 ) 3 (aq) were measured at T = 298.15 K and p = 0.1 MPa with a Sodev (Picker) flow microcalorimeter and a Sodev vibratingtube densimeter, respectively. These measurements extend from lower molalities of m = (0.005 to 0.018) molβ’ kg -1 to m = (0.025 to 0.434) molβ’kg -1 , where the upper molality limits are slightly below those of the saturated solutions. There are no previously published apparent molar heat capacities for these systems, and only limited apparent molar volume information. Considerable amounts of the RSO + 4 (aq) and R(SO 4 ) - 2 (aq) complexes are present, where R denotes a rare-earth, which complicates the interpretation of these thermodynamic quantities. Values of the ionic molar heat capacities and ionic molar volumes of these complexes at infinite dilution are derived from the experimental information, but the calculations are necessarily quite approximate because of the need to estimate ionic activity coefficients and other thermodynamic quantities. Nevertheless, the derived standard ionic molar properties for the various RSO + 4 (aq) and R(SO 4 ) - 2 (aq) complexes are probably realistic approximations to the actual values. Comparisons indicate that V β’ Ο {RSO + 4 , aq, 298.15 K} = -(6 Β± 4) cm 3
β’ mol -1 and V β’ Ο {R(SO 4 ) - 2 , aq, 298.15 K} = (35 Β± 3) cm 3
β’ mol -1 , with no significant variation
π SIMILAR VOLUMES
Densities of Gd(CF 3 SO 3 ) 3 (aq) solutions with molalities between (0.058 and 0.72) mol β’ kg -1 were measured with a vibrating-tube densimeter at the temperatures (373, 423, and 473) K and pressures (7 and 26) MPa. Apparent molar volumes calculated from measured densities in this work and those at
Isopiestic vapor-pressure measurements were made for Lu2(SO4)3(aq) at molalities from (0.35379 to 0.66478) molβ’kg -1 and for H2SO4(aq) at molalities from (0.27470 to 0.70512) molβ’kg -1 at the temperature T=298.15 K using KCl(aq) as the isopiestic reference standard; results for Lu2(SO4)3(aq) extend
Isopiestic vapor-pressure measurements were made for Rb 2 SO 4 (aq) from molality m = (0.16886 to 1.5679) mol β’ kg -1 at T = 298.15 K and from m = (0.32902 to 1.2282) mol β’ kg -1 at T = 323.15 K, and for Cs 2 SO 4 (aq) from m = (0.11213 to 3.10815) mol β’ kg -1 at T = 298.15 K and from m = (0.11872 t