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Heat capacities, order-disorder transitions, and thermodynamic properties of rare-earth orthoferrites and rare-earth iron garnets

机译:稀土矫正物和稀土铁石榴石的热能,秩序转变和热力学性质

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摘要

Rare-earth orthoferrites, RFeO3, and rare-earth iron garnets (RIGs) R3Fe5O12 (R = rare-earth elements) were prepared by citrate-nitrate gel combustion method and characterized by X-ray diffraction method. Isobaric molar heat capacities of these oxides were determined by using differential scanning calorimetry from 130 to 860 K. Order-disorder transition temperatures were determined from the heat capacity measurements. The Neel temperatures (T-N) due to antiferromagentic to paramagnetic transitions in orthoferrites and the Curie temperatures (T-C) due to ferrimagnetic to paramagnetic transitions in garnets were determined from the heat capacity data. Both T-N and T-C systematically decrease with increasing atomic number of R across the series. Lattice, electronic and magnetic contributions to the total heat capacity were calculated. Debye temperatures as a function of absolute temperature were calculated for these compounds. Thermodynamic functions like C-p,C-m degrees, S-m degrees, H degrees, G degrees, (H-T degrees - H-0 degrees), (H-T degrees - H-298.15K degrees), - (G(T)degrees - H-298.15K degrees) / T, Delta H-f(m)degrees, and Delta fG(m)degrees have been generated for the compounds RFeO3(S) and R3Fe5O12(s) based on the experimental data obtained in this study and the available data in the literature.
机译:通过柠檬酸盐 - 硝酸凝胶燃烧方法制备稀土镍酯,RFEO3和稀土铁石榴石(R =稀土元素),其特征在于X射线衍射法。通过使用从130至860k的差示扫描量热法测定这些氧化物的同位摩尔热容量。从热容量测量中确定订单障碍转变温度。从热容量数据确定由于邻铁矿的邻铁虫和居曲调(T-C)中的邻晶符到顺磁性温度(T-C)而导致的Neel温度(T-N)被加热容量数据确定。 T-N和T-C都随着跨越系列的r增加而系统地减小。计算晶格,电子和磁力贡献总热容量。对这些化合物计算了作为绝对温度的函数的德比温度。热力学功能,如CP,CM度,SM度,H度,G度,(HT度 - H-0度),(HT度 - H-298.15K度), - (G(T)度 - H-298.15K基于本研究中获得的实验数据和文献中的可用数据,已经为化合物RFEO3(S)和R3FE5012(S)生成了学位)/ T,Delta HF(M)度和Delta FG(M)度。和文献中的可用数据。

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