八面体
结晶学
中子衍射
钙钛矿(结构)
晶体结构
焓
化学
材料科学
热力学
物理
作者
E.H.P. Cordfunke,D.J.W. IJdo
标识
DOI:10.1006/jssc.1995.1137
摘要
The crystal structures of α- and β-Na2UO4 have been determined by neutron powder diffraction. In α-Na2UO4 edge-shared UO6 octahedra extend in chains along the c axis. In β-Na2UO4 the UO6 octahedra share corners with each other to form two-dimensional perovskite layers. The octahedra are tilted around both the b and c axes of the unit cell, α- and β-Na2NpO4 probably have the same structures. The enthalpy of transition of α-Na2UO4 to β-Na2UO4 has been determined both by DTA measurements and by calorimetric measurements. The unusually high value obtained can be explained from a structural point of view.
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