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Magnetization reversal in YIG/GGG(111) nanoheterostructures grown by laser molecular beam epitaxy

机译:激光分子束外延生长的YIG / GGG(111)纳米异质结构中的磁化反转

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摘要

Thin (4–20 nm) yttrium iron garnet (Y3Fe5O12, YIG) layers have been grown on gadolinium gallium garnet (Gd3Ga5O12, GGG) 111-oriented substrates by laser molecular beam epitaxy in 700–1000 °C growth temperature range. The layers were found to have atomically flat step-and-terrace surface morphology with step height of 1.8 Å characteristic for YIG(111) surface. As the growth temperature is increased from 700 to 1000 °C the terraces become wider and the growth gradually changes from layer by layer to step-flow regime. Crystal structure studied by electron and X-ray diffraction showed that YIG lattice is co-oriented and laterally pseudomorphic to GGG with small rhombohedral distortion present perpendicular to the surface. Measurements of magnetic moment, magneto-optical polar and longitudinal Kerr effect (MOKE), and X-ray magnetic circular dichroism (XMCD) were used for study of magnetization reversal for different orientations of magnetic field. These methods and ferromagnetic resonance studies have shown that in zero magnetic field magnetization lies in the film plane due to both shape and induced anisotropies. Vectorial MOKE studies have revealed the presence of an in-plane easy magnetization axis. In-plane magnetization reversal was shown to occur through combination of reversible rotation and abrupt irreversible magnetization jump, the latter caused by domain wall nucleation and propagation. The field at which the flip takes place depends on the angle between the applied magnetic field and the easy magnetization axis and can be described by the modified Stoner–Wohlfarth model taking into account magnetic field dependence of the domain wall energy. Magnetization curves of individual tetrahedral and octahedral magnetic Fe3+ sublattices were studied by XMCD.
机译:在700-1000°C的生长温度范围内,通过激光分子束外延在g镓镓石榴石(Gd3Ga5O12,GGG)111取向的衬底上生长了(4-20 nm)钇铁石榴石(Y3Fe5O12,YIG)薄层。发现这些层具有原子平坦的阶跃和阶跃表面形态,其YIG(111)表面的阶跃高度为1.8Å。随着生长温度从700°C升高到1000°C,梯田变得更宽,生长逐渐从逐层变化到逐步流动状态。通过电子和X射线衍射研究的晶体结构表明,YIG晶格是共取向的,并且与GGG呈横向假晶形,并且垂直于表面存在小的菱面体形变。磁矩,磁光极性和纵向克尔效应(MOKE)以及X射线磁性圆二色性(XMCD)的测量被用于研究磁场不同方向的磁化反转。这些方法和铁磁共振研究表明,由于形状和感应各向异性,在零磁场中,磁化强度位于薄膜平面内。矢量MOKE研究表明存在平面内易磁化轴。平面内磁化反转显示为通过可逆旋转和突然的不可逆磁化跳跃相结合而发生,后者是由畴壁成核和传播引起的。翻转发生的场取决于所施加的磁场和易磁化轴之间的角度,并且可以通过修正的Stoner-Wohlfarth模型(考虑了畴壁能量的磁场依赖性)来描述。利用XMCD研究了单个四面体和八面体Fe 3 + 亚晶格的磁化曲线。

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