LARGE MAGNETIC ENTROPY CHANGE NEAR CHARGE-ORDERED TRANSITION TEMPERATURE IN PEROVSKITE-TYPE MANGANITE
Chen Peng (陈鹏)ab, Du You-wei (都有为)b
a Department of Physics, South-West Normal University, Chongqing 400715, China; b State Key Laboratory of Solid State Microstructures, Nanjing University, Nanjing 210093, China
Abstract The magnetocaloric effect in polycrystalline of Pr1-xSrxMnO3 (x=0.33, 0.43, 0.50) has been investigated. A large magnetic entropy change (7.1J/kgK) was discovered in Pr0.5Sr0.5MnO3 under a low magnetic field of 1T at charge-ordered state transition temperature (161K). The physical mechanism is related to a drastic magnetization change at a temperature where the field-induced magnetic, electron and structural phase transitions occur (from the antiferromagnetic charge-ordered state to the ferromagnetic charge-disordered state).
(Crystallographic aspects of phase transformations; pressure effects)
Fund: Project supported by the State Key Development Program for Basic Research of China (Grant No. 1999064508) and by the Major Program of the National Natural Science Foundation of China (Grant No. 19890310).
Cite this article:
Chen Peng (陈鹏), Du You-wei (都有为) LARGE MAGNETIC ENTROPY CHANGE NEAR CHARGE-ORDERED TRANSITION TEMPERATURE IN PEROVSKITE-TYPE MANGANITE 2001 Chinese Physics 10 970
Altmetric calculates a score based on the online attention an article receives. Each coloured thread in the circle represents a different type of online attention. The number in the centre is the Altmetric score. Social media and mainstream news media are the main sources that calculate the score. Reference managers such as Mendeley are also tracked but do not contribute to the score. Older articles often score higher because they have had more time to get noticed. To account for this, Altmetric has included the context data for other articles of a similar age.