首页> 外文期刊>Journal of Solution Chemistry >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 center dot 7H(2)O(cr) and RECl3 center dot 6H(2)O(cr)
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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 center dot 7H(2)O(cr) and RECl3 center dot 6H(2)O(cr)

机译:对三价稀土水溶液的标准摩尔熵,形成焓,形成吉布斯能量和热容量的严格评估,以及热力学稳定的RECl3中心点7H的相应标准摩尔熵,形成焓和吉布斯能量形成(2)O(cr)和RECl3中心点6H(2)O(cr)

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摘要

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 RE3+(aq) were calculated based on the standard molar entropies of the hydrated rare earth chlorides RECl3 center dot 7H(2)O(cr) (RE = La, Pr) and RECl3 center dot 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 RECl3 center dot 7H(2)O(cr) and RECl3 center dot 6H(2)O(cr) including YCl3 center dot 6H(2)O(cr). However, the entropies of these RECl3 center dot 7H(2)O(cr) and of several of the RECl3 center dot 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 RECl3 center dot 7H(2)O(cr) and RECl3 center dot 6H(2)O(cr) and to estimate the standard molar entropies of the RECl3 center dot 6H(2)O(cr) from those of the corresponding anhydrous RECl3(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 RE3+(aq), 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 RE3+(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 RECl3 center dot 7H(2)O(cr) and RECl3 center dot 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 RE3+(aq) were evaluated from published results for dilute solutions from flow microcalorimetry.
机译:在较早的评估中(FH Spedding,JA Rard,A。Habenschuss,J。Phys。Chem。81:1069-1074,1977),根据标准计算了三价稀土离子水溶液RE3 +(aq)的标准摩尔熵。水合稀土氯化物RECl3中心点7H(2)O(cr)(RE = La,Pr)和RECl3中心点6H(2)O(cr)的摩尔熵(RE = Nd,Gd,Tb,Dy,Ho ,Er,Lu)在T = 298.15 K和p = 0.1 MPa时,以及它们相应的标准摩尔焓和溶液的吉布斯能,几乎对于所有RECl3中心点7H(2)O(cr)和RECl3都是已知的中心点6H(2)O(cr)包括YCl3中心点6H(2)O(cr)。但是,这些RECl3中心点7H(2)O(cr)和几个RECl3中心点6H(2)O(cr)的熵具有很大的不确定性,因为源热容仅扩展到T = 223-262 K,而不是T = 298.15 K,并且用于这些测量的晶体包含一些被封闭的溶液(水分过多)。描述了简单的方法来校正RECl3中心点7H(2)O(cr)和RECl3中心点6H(2)O(cr)的这些熵,并估计RECl3中心点6H(2)O的标准摩尔熵。 (cr)来自相应的无水RECl3(cr)。通过使用这些熵,溶液的标准摩尔焓和标准摩尔Gibbs能量的修正结果发生变化,从而形成饱和溶液,RE3 +(aq)的标准摩尔熵的修正值和CODATA兼容值,其中RE =(La,对Nd,Pm,Sm,Eu,Gd,Tb,Dy,Ho,Er,Tm,Yb,Lu,Y进行评估或估算(RE = Pm)。通过将这些结果与严格评估的RE3 +(aq)的标准摩尔焓相结合,可以计算出这些三价稀土水族离子的标准摩尔Gibbs能,以及相应的标准摩尔Gibbs能量和氢的生成焓。热力学稳定的RECl3中心点7H(2)O(cr)和RECl3中心点6H(2)O(cr)在T = 298.15 K和p = 0.1 MPa时相。此外,从流式微量热法的稀溶液的公开结果中评估了大多数RE3 +(aq)的标准摩尔热容。

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