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    • 2. 发明授权
    • Magnetic recording medium and manufacturing method thereof
    • 磁记录介质及其制造方法
    • US07183013B2
    • 2007-02-27
    • US10764813
    • 2004-01-26
    • Tadaaki OikawaTakahiro ShimizuHiroyuki UwazumiNaoki Takizawa
    • Tadaaki OikawaTakahiro ShimizuHiroyuki UwazumiNaoki Takizawa
    • G11B5/66G11B5/70
    • G11B5/7325G11B5/65G11B5/656G11B5/8404
    • A nonmagnetic foundation layer is made to have a body-centered cubic crystal structure with a preferred crystal orientation plane being the bcc (110) plane. A nonmagnetic intermediate layer, provided between the foundation layer and a granular magnetic layer, has a hexagonal close-packed structure with the hcp (100) plane or the hcp (200) plane being the preferred orientation plane. Furthermore, the crystal lattice misfit amount between the nonmagnetic intermediate layer 3 and the granular magnetic layer is made to be not more than 10% for each of an a-axis and a c-axis. As a result, epitaxial growth of ferromagnetic crystals in the granular magnetic layer, which has an hcp structure, is promoted, and hence the crystallinity of the magnetic layer is increased, and thus it becomes possible to simultaneously realize an increase in coercivity and a reduction in noise. Depositing the layers on an unheated substrate yields reduces manufacturing costs.
    • 将非磁性基础层制成具有体心立方晶体结构,其中优选的晶体取向平面是bcc(110)面。 设置在基础层和粒状磁性层之间的非磁性中间层具有hcp(100)面或hcp(200)面为优选取向面的六方密堆积结构。 此外,非磁性中间层3和粒状磁性层之间的晶格失配量对于a轴和c轴分别为10%以下。 结果,促进了具有hcp结构的粒状磁性层中的铁磁晶体的外延生长,因此磁性层的结晶度增加,因此可以同时实现矫顽力的提高和还原 在噪音 将层沉积在未加热的基底上会降低制造成本。
    • 8. 发明授权
    • Magnetic recording medium exhibiting low noise and high coercive force
    • 表现出低噪音,高矫顽力的磁记录介质
    • US07247395B2
    • 2007-07-24
    • US10319842
    • 2002-12-16
    • Miyabi NakamuraTakahiro ShimizuHiroyuki UwazumiNaoki TakizawaTadaaki Oikawa
    • Miyabi NakamuraTakahiro ShimizuHiroyuki UwazumiNaoki TakizawaTadaaki Oikawa
    • G11B5/66G11B5/70
    • G11B5/7325G11B5/65
    • A magnetic recording medium exhibiting low noise and having a sufficiently high coercive force includes a magnetic layer having a granular structure including ferromagnetic crystal grains with a hexagonal closed packed structure and a nonmagnetic grain boundary region of mainly an oxide intervening between the crystal grains. An underlayer has a body-centered cubic lattice structure. A nonmagnetic intermediate layer with the hexagonal closest packed structure includes Ru, Os, and/or Re, which are provided between the magnetic layer and the underlayer. A degree of mismatching Δ=|d1−d2|/d1 is at most 10%, for instance, in a range from 2.5% to 7.0%, where d1 is a spacing of lattice planes of the crystal grains in the magnetic layer and d2 is a spacing of the lattice planes of the crystal grains in the intermediate layer. A proportion of the crystal grains with a grain size of equal or greater than 8 nm are at most 10% of the crystal grains included in the intermediate layer and a standard deviation of the grain size is at most 1.4 nm. The layers are deposited without preheating the substrate.
    • 表现出低噪声并且具有足够高的矫顽力的磁记录介质包括具有包括具有六方密闭堆积结构的铁磁晶粒和主要是介于晶粒之间的氧化物的非磁性晶界区域的颗粒结构的磁性层。 底层具有体心立方晶格结构。 具有六方最密堆积结构的非磁性中间层包括设置在磁性层和底层之间的Ru,Os和/或Re。 Δ不一致的程度达到= 10%以下,例如在 2.5%至7.0%,其中d 1是磁性层中晶粒的晶格间距,d 2是晶体的晶格面间距 中间层的晶粒。 晶粒尺寸等于或大于8nm的晶粒的比例至多为包含在中间层中的晶粒的10%,并且晶粒尺寸的标准偏差为至多1.4nm。 在不预热基底的情况下沉积这些层。