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Structure-thermodynamics relationship of schoepite from first-principles

机译:第一个原则的斯基封的结构 - 热力学关系

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The relationship between the structure and thermodynamic properties of schoepite, an important uranyl phase with formula [(UO2)(8)O-2(OH)(12)]center dot 12H(2)O formed upon corrosion of UO2, has been investigated within the framework of density functional perturbation theory (DFPT). Experimental crystallographic lattice parameters are well reproduced in this study using standard DFT. Phonon calculations within the quasi-harmonic approximation predict standard molar entropy and isobaric heat capacity of S-0 = 179.60 J mol(-1) K-1 and C-P(0) = 157.4 J mol(-1) K-1 at 298.15 K, i.e., similar to 6% and similar to 4% larger than existing DFPT-D2 calculations. The computed variation of the standard molar isobaric heat capacity with water content from schoepite (UO3 center dot xH(2)O, x = 2.25) to dehydrated schoepite (x = 1) is predicted to be essentially linear along isotherms ranging from 100 to 500 K. These findings have important implications for the dehydration of layered uranyl corrosion phases and hygroscopic materials.
机译:研究了在UO 2腐蚀时形成的脱噻e的结构和热力学性质,其中包含式[(UO 2)(8)o-2(OH)(2)o的重要铀酰相。在密度函数扰动理论(DFPT)框架内。实验结晶晶格参数使用标准DFT在本研究中再现。声子近似值内的卡隆计算预测S-0 = 179.60J mol(-1)k-1和Cp(0)= 157.4J mol(-1)K-1的标准摩尔熵和摄热能力。298.15 k ,即类似于6%并且类似于比现有DFPT-D2计算大的4%。预计脱水斯基硫岩(X = 1)的脱水(UO3中心点XH(2)O,X = 2.25)的标准摩尔摄取热容的计算变化预测,沿着从100至500的等温线基本上是线性的K.这些发现对层状铀酰腐蚀阶段和吸湿材料的脱水具有重要意义。

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