Critical Evaluation of the Standard Molar Entropies, Enthalpies of Formation, Gibbs Energies of Formation and Heat Capacities of the Aqueous Trivalent Rare Earth Ions, and the Corresponding Standard Molar Entropies, Enthalpies of Formation and Gibbs Energies of Formation of the Thermodynamically Stable RECl3·7H2O(cr) and RECl3·6H2O(cr)

In an earlier evaluation (F.H. Spedding, J.A. Rard, A. Habenschuss, J. Phys. Chem. 81: 1069–1074, 1977) the standard molar entropies of the aqueous trivalent rare earth ions RE 3+ (aq) were calculated based on the standard molar entropies of the hydrated rare earth chlorides RECl 3 ·7H 2 O(cr) (RE =...

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Veröffentlicht in:Journal of solution chemistry 2016-09, Vol.45 (9), p.1332-1376
1. Verfasser: Rard, Joseph A.
Format: Artikel
Sprache:eng
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Zusammenfassung:In an earlier evaluation (F.H. Spedding, J.A. Rard, A. Habenschuss, J. Phys. Chem. 81: 1069–1074, 1977) the standard molar entropies of the aqueous trivalent rare earth ions RE 3+ (aq) were calculated based on the standard molar entropies of the hydrated rare earth chlorides RECl 3 ·7H 2 O(cr) (RE = La, Pr) and RECl 3 ·6H 2 O(cr) (RE = Nd, Gd, Tb, Dy, Ho, Er, Lu) at T  = 298.15 K and p  = 0.1 MPa, along with their corresponding standard molar enthalpies and Gibbs energies of solution, which are known for nearly all of the RECl 3 ·7H 2 O(cr) and RECl 3 ·6H 2 O(cr) including YCl 3 ·6H 2 O(cr). However, the entropies of these RECl 3 ·7H 2 O(cr) and of several of the RECl 3 ·6H 2 O(cr) have large uncertainties because the source heat capacities only extend up to T  = 223–262 K and not to T  = 298.15 K and the crystals used for these measurements contained some occluded solution (water excess). Simple methods are described to correct these entropies of the RECl 3 ·7H 2 O(cr) and RECl 3 ·6H 2 O(cr) and to estimate the standard molar entropies of the RECl 3 ·6H 2 O(cr) from those of the corresponding anhydrous RECl 3 (cr). By using these entropies, standard molar enthalpies of solution and revised results for the standard molar Gibbs energy changes to form the saturated solutions, revised and CODATA-compatible values of the standard molar entropies of the RE 3+ (aq), S m o ( RE 3 + , aq , 298.15 K ) where RE = (La, Nd, Pm, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Y), were evaluated or estimated (RE = Pm). By combining these results with critically-assessed standard molar enthalpies of formation of the RE 3+ (aq), the standard molar Gibbs energies of formation of these trivalent rare earth aquo ions were calculated, as were the corresponding standard molar Gibbs energies and enthalpies of formation of the thermodynamically stable RECl 3 ·7H 2 O(cr) and RECl 3 ·6H 2 O(cr) phases at T  = 298.15 K and p  = 0.1 MPa. In addition, standard molar heat capacities of most of the RE 3+ (aq) were evaluated from published results for dilute solutions from flow microcalorimetry.
ISSN:0095-9782
1572-8927
DOI:10.1007/s10953-016-0520-8