2018
DOI: 10.1007/s11467-018-0862-3
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Tuning spin reorientation in Er1-xYxFeO3 single crystal family

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Cited by 15 publications
(11 citation statements)
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“…Subsequently, the Er 3+ magnetic moment increases further, leading to an increase in total magnetization until the highest positive value is reached at T ssw2 = 30.5 K. When the temperature is cooled to T ssw2 = 30.5 K, a small sudden drop in the magnetization along a -axis occurs, which is due to the magnetic moment flip of partial Er 3+ ions. Compared with ErFeO 3 , the SR transition temperature zone of the Pr 0.3 Er 0.7 FeO 3 shifts toward higher temperatures, and both of the characteristic temperatures in the M – T curve of this system, i.e., the magnetization compensation temperature ( T comp ) and spin switching triggering temperature ( T ssw ), shift toward higher temperatures. ,, In the FCW mode along the a -axis (orange color curve), as shown in Figure . As the temperature increases to T ssw3 = 93.9 K, the type-I spin switching effect occurs, caused by the change in three ionic magnetic moments in Pr 3+ ↓Er 3+ ↑Fe 3+ ↓ coupling configuration to Pr 3+ ↑Er 3+ ↓Fe 3+ ↑ coupling configuration, which leads to the change in the magnetization from negative to positive.…”
Section: Resultsmentioning
confidence: 89%
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“…Subsequently, the Er 3+ magnetic moment increases further, leading to an increase in total magnetization until the highest positive value is reached at T ssw2 = 30.5 K. When the temperature is cooled to T ssw2 = 30.5 K, a small sudden drop in the magnetization along a -axis occurs, which is due to the magnetic moment flip of partial Er 3+ ions. Compared with ErFeO 3 , the SR transition temperature zone of the Pr 0.3 Er 0.7 FeO 3 shifts toward higher temperatures, and both of the characteristic temperatures in the M – T curve of this system, i.e., the magnetization compensation temperature ( T comp ) and spin switching triggering temperature ( T ssw ), shift toward higher temperatures. ,, In the FCW mode along the a -axis (orange color curve), as shown in Figure . As the temperature increases to T ssw3 = 93.9 K, the type-I spin switching effect occurs, caused by the change in three ionic magnetic moments in Pr 3+ ↓Er 3+ ↑Fe 3+ ↓ coupling configuration to Pr 3+ ↑Er 3+ ↓Fe 3+ ↑ coupling configuration, which leads to the change in the magnetization from negative to positive.…”
Section: Resultsmentioning
confidence: 89%
“…After reviewing the relevant literature and comparing the spectra obtained in the experiments, we obtained five Raman peaks presented in this condition, corresponding to the wavenumbers: 269, 342, 430, 502, and 643 cm –1 . , The Raman peaks all reflect rotational and stretching operations associated with Fe–O bonds or FeO 6 octahedra because the Raman modes at wavenumbers greater than 300 cm –1 are associated with the vibration of O 2– or FeO 6 octahedra. Compared with the Raman test results of ErFeO 3 , the positions of each Raman peak are offset, and the Raman peak of Pr 0.3 Er 0.7 FeO 3 moves to the low-wavenumber direction . This is because the radius of Pr 3+ is larger than Er 3+ , and the partial substitution of Pr 3+ increases the volume of Pr 0.3 Er 0.7 FeO 3 , which affects the Raman peak moving in the low-wavenumber direction.…”
Section: Resultsmentioning
confidence: 99%
“…Chapter 5 -Structural distortions of orthorhombic RFeO3 and RMnO3 substitution is less studied, which may be due to the fact that the rare-earth sublattice can also couple with the iron sublattice, yielding a more intricated behavior of these compounds [60,61] . Thus, this substitution cannot be reduced to a simple tune of the structure, as the interplay between the R 3+ and the Fe 3+ spins is also being changed.…”
Section: Continuously Tuning the Jahn-teller Distortionmentioning
confidence: 99%
“…Considering the strong coupling between the R 3+ and Fe 3+ in determining the SR transition temperature [10], one strategy to modulate the SR transition temperature is by rare-earth doping and this has been investigated intensively in various orthoferrites [16][17][18][19][20][21][22]. In contrast, there has been considerably less investigations of rare-earth or-thoferrites by introducing transition-metal elements at the Fe site.…”
Section: Introductionmentioning
confidence: 99%