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Revision of the Osmotic Coefficients, Water Activities and Mean Activity Coefficients of the Aqueous Trivalent Rare Earth Chlorides at T=298.15 K

机译:修改三价稀土氯化物在T = 298.15 K时的渗透系数,水活度和平均活度系数

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The analysis by Wang et al. (J. Solution Chem. 35:1137-1156, 2006) of the osmotic and activity coefficients of fourteen of the aqueous rare earth trichlorides at the temperature 298.15 K is based mainly on the isopiestic results reported by Spedding et al. (J. Chem. Eng. Data 21:341-360, 1976) and Rard and Spedding (J. Chem. Eng. Data 27:454-461, 1982), but corrected for more recent critical reviews of the osmotic coefficients of the KCl(aq) and CaCl2(aq) reference solutions used in these measurements. Also included were the potential difference (emf) measurements by Malatesta et al. (Phys. Chem. Chem. Phys. 4:121-126, 2002) for LaCl3(aq) using cells with a liquid ion-exchange membrane electrode and earlier results for concentration cells with transport for the rare earth trichlorides. Our reexamination of osmotic coefficients calculated from these potential differences of cells with a liquid ion-exchange electrode indicates their values are skewed relative to osmotic coefficients obtained more directly from the isopiestic measurements, being significant higher for molalities between (0.025 and 0.3) mol center dot kg(-1) and significantly lower at higher molalities. As a consequence, the combined results yielded mean, molality-based, activity coefficients that are systematically too large for the light and intermediate rare earths. Although restricted to a narrower molality region of about (0.02-0.04) mol center dot kg(-1), potential difference measurements for aqueous rare earth trichlorides from concentration cells with AgCl(s) electrodes appear to yield more reliable results. The extended ion-interaction model parameters of Wang et al. have been reevaluated using the cited isopiestic results together with osmotic coefficients derived from the concentration cells with transport as reported by Spedding et al. (J. Chem. Eng. Data 21:341-360, 1976). Mean activity coefficients calculated using these new model parameters should be more accurate than those previously reported.
机译:王等人的分析。 (J.Solution Chem.35:1137-1156,2006),14种三氯化稀土水溶液在298.15 K温度下的渗透系数和活度系数主要基于Spedding等人的报道。 (J. Chem。Eng。Data 21:341-360,1976)和Rard and Spedding(J. Chem。Eng。Data 27:454-461,1982),但已针对该产品的渗透系数进行了更近期的评论。这些测量中使用的KCl(aq)和CaCl2(aq)参考溶液。 Malatesta等人的电势差(emf)测量也包括在内。 (Phys。Chem。Chem。Phys。4:121-126,2002)的LaCl3(aq)使用带有液体离子交换膜电极的电解池,早期的结果是浓缩了带有转运三氯化稀土的电解池。我们用液体离子交换电极对由这些电势差计算得出的渗透系数进行了重新检验,结果表明它们的值相对于更直接从同构测量获得的渗透系数而言是偏斜的,对于摩尔浓度在(0.025和0.3)mol中心点之间的摩尔浓度而言,显着更高kg(-1),在更高的摩尔浓度下显着降低。结果,组合结果产生了基于摩尔浓度的平均活度系数,该系数对于轻稀土和中间稀土系统地太大。尽管限制在大约(0.02-0.04)mol中心点kg(-1)的较窄摩尔浓度区域,但使用AgCl电极从浓化池中对三氯化稀土水溶液进行电势差测量似乎会产生更可靠的结果。 Wang等人的扩展的离子相互作用模型参数。使用Spedding等人的报道,使用引用的同功结果以及来自带有运输的浓集细胞的渗透系数,重新评估了这些物质。 (J.Chem.Eng.Data 21:341-360,1976)。使用这些新的模型参数计算出的平均活度系数应比以前报告的更为准确。

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