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Tuning of magnetic and electronic states by control of oxygen content in lanthanum strontium cobaltites

机译:通过控制镧锶锶钴中的氧含量来调节磁态和电子态

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We report on the magnetic, resistive, and structural studies of perovskite La_(1/3)Sr_(2/3)CoO_(3-δ). By using the relation of synthesis temperature and oxygen partial pressure to oxygen stoichiometry obtained from thermo-gravimetric analysis, we have synthesized a series of samples with precisely controlled δ=0.00-0.49. These samples show three structural phases at δ=0.00-0.15, ≈0.25, ≈0.5, and two-phase behavior for other oxygen contents. The stoichiometric material with δ=0.00 is a cubic ferromagnetic metal with the Curie temperature T_C=274 K. The increase of δ to 0.15 is followed by a linear decrease of T_C to ≈ 160 K and a metal-insulator transition near the boundary of the cubic structure range. A further increase of δ results in the formation of a tetragonal 2a_p X 2a_p X 4a_p phase for δ≈0.25 and a brownmillerite phase for δ ≈ 0.5. At low temperatures, these are weak ferromagnetic insulators (canted antiferromagnets) with magnetic transitions at T_m ≈ 230 and 120 K, respectively. At higher temperatures, the 2a_p x 2a_p X 4a_p phase is G-type antiferromagnetic between 230 K and ≈360 K. Low temperature magnetic properties of this system for δ < 1/3 can be described in terms of a mixture of Co~(3+) ions in the low-spin state and Co~(4+) ions in the intermediate-spin state and a possible spin transition of Co~(3+) to the intermediate-spin state above T_C. For δ > 1/3, there appears to be a combination of Co~(2+) and Co~(3+) ions, both in the high-spin state with dominating antiferromagnetic interactions.
机译:我们报告钙钛矿La_(1/3)Sr_(2/3)CoO_(3-δ)的磁性,电阻和结构研究。通过使用合成温度和氧气分压与通过热重分析获得的氧气化学计量关系,我们合成了一系列具有精确控制的δ= 0.00-0.49的样品。这些样品显示出在δ= 0.00-0.15,≈0.25,≈0.5的三个结构相,以及其他氧含量的两相行为。 δ= 0.00的化学计量材料是立方铁磁金属,居里温度T_C = 274K.δ增大到0.15之后,T_C线性减小到≈160 K,并且金属绝缘子过渡到T的边界附近。立方结构范围。 δ的进一步增加导致形成δ≈0.25的四方2a_p X 2a_p X 4a_p相和δ≈0.5的棕褐色相。在低温下,它们是弱的铁磁绝缘体(倾斜的反铁磁体),分别具有T_m≈230和120 K的磁跃迁。在较高温度下,2a_p x 2a_p X 4a_p相在230 K和≈360K之间为G型反铁磁性。对于δ<1/3,该系统的低温磁性能可以用Co〜(3低自旋态的+)离子和中旋态的Co〜(4+)离子以及Co_(3+)可能在T_C以上自旋跃迁到中旋态。对于δ> 1/3,似乎存在Co〜(2+)和Co〜(3+)离子的组合,两者均处于高自旋状态,并具有主要的反铁磁相互作用。

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