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Systematic control of strain-induced perpendicular magnetic anisotropy in epitaxial europium and terbium iron garnet thin films

机译:外延euro和iron铁石榴石薄膜中应变诱导的垂直磁各向异性的系统控制

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We show tunable strain-induced perpendicular magnetic anisotropy (PMA) over a wide range of thicknesses in epitaxial ferrimagnetic insulator Eu3Fe5O12 (EuIG) and Tb3Fe5O12 (TbIG) thin films grown by pulsed-laser deposition on Gd3Ga5O12 with (001) and (111) orientations, respectively. The PMA field is determined by measuring the induced anomalous Hall loops in Pt deposited on the garnet films. Due to positive magnetostriction constants, compressive in-plane strain induces a PMA field as large as 32.9 kOe for 4 nm thick EuIG and 66.7 kOe for 5 nm thick TbIG at 300 K and relaxes extremely slowly as the garnet film thickness increases. In bilayers consisting of Pt and EuIG or Pt and TbIG, robust PMA is revealed by squared anomalous Hall hysteresis loops in Pt, the magnitude of which appears to be only related to the net magnetic moment of iron sublattices. Furthermore, the magnetostriction constant is found to be 2.7 × 10?5 for EuIG and 1.35 × 10?5 for TbIG, comparable with the values for bulk crystals. Our results demonstrate a general approach of tailoring magnetic anisotropy of rare earth iron garnets by utilizing modulated strain via epitaxial growth.
机译:我们显示了在外延铁磁绝缘体Eu3Fe5O12(EuIG)和Tb3Fe5O12(TbIG)薄膜中通过在(001)和(111)取向的Gd3Ga5O12上进行脉冲激光沉积而生长的厚度范围很宽的可调应变感应垂直磁各向异性(PMA) , 分别。 PMA场是通过测量石榴石薄膜上沉积的Pt中引起的霍尔霍尔异常回路来确定的。由于正磁致伸缩常数,在300 K时,压缩面内应变会引起4MA厚EuIG的PMA场为32.9 kOe,5nm TbIG的PMA场为66.7 kOe,并且随着石榴石膜厚度的增加而非常缓慢地松弛。在由Pt和EuIG或Pt和TbIG组成的双层中,Pt中的平方霍尔异常磁滞回线显示出坚固的PMA,其幅度似乎仅与铁亚晶格的净磁矩有关。此外,发现与EuIG的磁致伸缩常数为2.7×10 -5,对TbIG的磁致伸缩常数为1.35×10 -5,与块状晶体的值相当。我们的结果证明了通过利用外延生长的调制应变来调整稀土铁石榴石磁各向异性的一般方法。

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