首页> 外文OA文献 >Thermodynamics of the solid solution - Aqueous solution system (Ba,Sr,Ra)SO$_{4}$ + H$_{2}$O: I. The effect of strontium content on radium uptake by barite
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Thermodynamics of the solid solution - Aqueous solution system (Ba,Sr,Ra)SO$_{4}$ + H$_{2}$O: I. The effect of strontium content on radium uptake by barite

机译:固溶体的热力学-水溶液系统(Ba,Sr,Ra)SO $ _ {4} $ + H $ _ {2} $ O:I.锶含量对重晶石吸收镭的影响

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摘要

Thermodynamic properties of mixing in the ternary (Ba,Sr,Ra)SO4 solid solution are determined using first principles based total energy calculations and Monte Carlo simulations. Two levels of theory, which correspond to the regular mixing and the generalized Ising model, are considered. The results show that the regular mixing parameters increase along the row of Ba-Ra, Ba-Sr and Sr-Ra binary systems proportionally to the squared difference of molar volumes of the end-members. The magnitudes of pairwise interactions similarly increase along the same row, manifesting a tendency to short-range ordering (SRO). In the (Ba,Sr)SO4 system the SRO effect is approximately equivalent to a 40% decrease in the value of the regular mixing parameter. The ternary solid solution is well described as a regular mixture with the binary parameters WBaRa = 2.47 ± 0.22, WBaSr = 4.95 ± 0.75 and WSrRa = 17.50 ± 1.40 kJ/mol. These values imply that admixing RaSO4 to the (Ba,Sr)SO4 solid solution stabilizes Ba-rich and destabilizes Sr-rich compositions. Consequently, an addition of a small amount of RaSO4 to a Sr-rich solid solution leads to a nucleation of a Ba- and Ra rich phase. This phenomenon, predicted in our thermodynamic modelling study, is directly confirmed by our experiments on recrystallizing a powder of celestite with traces of Ba in the presence of an aqueous Ra-bearing solution. At a measurably high content of Ra in the system Ra-uptake by celestite occurs via a formation of a Ra-rich phase. The aqueous concentration of Ra in such systems would be governed mainly by the common anion effect caused by the relatively high solubility of Sr-rich sulphates. At lower Ra contents the retention of Ra would be enhanced both by the common anion and the dilution effects. Our simulations with the GEM-Selektor code predict that the optimum condition for Ra uptake is achieved when the barite solid solution contains 10 ± 5 mol % of SrSO4.
机译:使用基于总能量计算的第一原理和蒙特卡洛模拟确定三元(Ba,Sr,Ra)SO4固溶体中混合的热力学性质。考虑了两个级别的理论,分别对应于常规混合和广义Ising模型。结果表明,规则的混合参数沿着Ba-Ra,Ba-Sr和Sr-Ra二元体系的行增加,并与端基摩尔体积的平方差成正比。成对相互作用的幅度类似地沿着同一行增加,表现出短程排序(SRO)的趋势。在(Ba,Sr)SO4系统中,SRO效应大约等于常规混合参数值降低40%。三元固溶体很好地描述为具有二元参数WBaRa = 2.47±0.22,WBaSr = 4.95±0.75和WSrRa = 17.50±1.40 kJ / mol的规则混合物。这些值意味着将RaSO4混合到(Ba,Sr)SO4固溶体中会使富Ba稳定并使富Sr组成不稳定。因此,向富含Sr的固溶体中添加少量RaSO4会导致富含Ba和Ra的相成核。在我们的热力学模型研究中预测到的这种现象,可以通过在含Ra的水溶液存在下用痕量Ba重结晶天青石粉末的实验得到证实。当体系中的Ra含量高得可观时,天青石通过富Ra相的形成而吸收Ra。在这样的系统中,Ra的水浓度主要由富Sr硫酸盐的较高溶解度引起的常见阴离子效应所控制。在较低的Ra含量下,普通阴离子和稀释作用都会提高Ra的保留率。我们使用GEM-Selektor代码进行的模拟预测,当重晶石固溶体包含10±5 mol%的SrSO4时,可以获得最佳的Ra吸收条件。

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