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Thermodynamics and Stability of Rhabdophanes, Hydrated Rare Earth Phosphates REPO4 · n H2O

机译:大黄烷,水合稀土磷酸盐REPO4·n H2O的热力学和稳定性

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Rare earth phosphates comprise a large family of compounds proposed as possible nuclear waste disposal forms. We report structural and thermodynamic properties of a series of rare earth rhabdophanes and monazites. The water content of the rhabdophanes, including both adsorbed and structural water, decreases linearly with increase in ionic radius of the rare earth. The energetics of the transformation of rhabdophane to monazite plus water and the enthalpy of formation of rhabdophane from the constituent oxides was determined by high temperature drop solution calorimetry. The former varies linearly with the ionic radius of the lanthanide, except for cerium. By combining the enthalpy of formation determined by high temperature drop solution calorimetry and the free energy of formation determined previously by solubility experiments, a complete set of thermodynamic data was derived for the rhabdophanes. They are thermodynamically metastable with respect to the corresponding monazites plus water at all temperatures under ambient pressure conditions. This conclusion strengthens the case for monazites being an excellent nuclear waste form.
机译:稀土磷酸盐包含大量建议作为可能的核废料处置形式的化合物。我们报告了一系列稀土大黄石和独居石的结构和热力学性质。大黄烷的水含量,包括吸附水和结构水,都随着稀土离子半径的增加而线性降低。通过高温降溶液量热法确定了横纹烷烃向独居石加水的转化的能量以及由组成氧化物形成的横​​纹烷烃的焓。除铈外,前者随镧系元素的离子半径线性变化。通过将高温滴溶液量热法确定的形成焓与先前通过溶解度实验确定的形成自由能结合在一起,就得出了大黄烷的完整热力学数据。它们在环境压力条件下在所有温度下相对于相应的独居石加水在热力学上都是亚稳态的。这一结论进一步证明了独居石是一种极好的核废料形式。

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