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What Coexists with the Ferromagnetic Metallic Phase in Manganites?
Colossal magnetoresistance, whereby the application of a magnetic field reduces the resistivity of a manganite by orders of magnitude, is generally believed to occur because of coexisting phases. Development of a complete theory to explain the phenomenon requires that the exact nature of these phases be known. We used resonant elastic soft x-ray scattering to examine the superlattice order that exists in La{sub 0.35}Pr{sub 0.275}Ca{sub 0.375}MnO{sub 3} above and below the Curie temperature. By measuring the resonance profile of the scattered x-rays at different values of q, we disentangle the contributions of orbital order and antiferromagnetism to the scattering signal above the Curie temperature. Below the Curie temperature, we see no signal from orbital order, and only antiferromagnetism coexists with the dominant ferromagnetic metallic phase
Terahertz-driven magnetism dynamics in the orthoferrite DyFeO3
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149641.pdf (publisher's version ) (Open Access
Лексические средства выражения состояния страха в английском языке (на материале рассказов Говарда Филлипса Лавкрафта): дипломная работа (проект) специалиста по направлению подготовки: 45.05.01 - Перевод и переводоведение
We determined the magnetic ground-state moments of ultrathin epitaxial Fe films on Ni(110) and found that the overlayer spins orient at an angle of 55 degrees relative to the substrate magnetization direction. This surprising behaviour is a direct consequence of the contribution of orbital magnetic moment to the magnetocrystalline anisotropy
Effects of spin-dependent quasiparticle renormalization in fe, co, and ni photoemission spectra: An experimental and theoretical study
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103323.pdf (publisher's version ) (Open Access
Nanoscale Confinement of All-Optical Magnetic Switching in TbFeCo - Competition with Nanoscale Heterogeneity
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149621.pdf (Publisher’s version ) (Closed access