热力学
等结构
相变
凝聚态物理
材料科学
等温过程
熵(时间箭头)
朗道理论
热的
热涨落
热容
磁化
组态熵
绝热过程
工作(物理)
过渡态理论
相(物质)
量热法
相界
模数
热膨胀
长度刻度
电荷(物理)
传热
转变温度
作者
Jefferson Delgado-Quesada,G. G. Guzmán-Verri
标识
DOI:10.1002/advs.202516375
摘要
ABSTRACT We develop a minimal Landau theory of the concomitant intersite charge‐transfer, antiferromagnetic, and isostructural phase transitions in the barocaloric quadruple perovskites (A = La, Pr, Nd, Sm, Eu, Gd, Tb). A non‐symmetry‐breaking order parameter for the Cu–Fe intersite transfer is taken as primary, with the staggered magnetization and the volume strain enslaved to the charge transfer through magnetoelastic and charge‐strain couplings. The volume and entropy discontinuities, the thermal expansivities and bulk moduli of the two phases, and the slope of the pressure–temperature phase boundary are thereby tied to one another through the model couplings. The model yields a pressure‐independent transition entropy, so the latent heat is proportional to the transition temperature, accounting for its near‐constancy under A‐site substitution. Applied to , the theory reproduces the charge, magnetic, and structural responses across the transition from parameters fixed by experimental data, and resolves the transition entropy into comparable charge and magnetic contributions by anchoring the magnetic sector on the intrinsic ordering scale of the charge‐transferred state. The barocaloric effect is inverse, with a peak isothermal entropy change at 0.5 GPa of , comparable to the quasi‐direct value of . The theory makes explicit the intrinsic thermal expansion of each phase, a contribution omitted in the entropy construction underlying the quasi‐direct determination.
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