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JP5394552B2 - Substrate for perpendicular magnetic recording medium and magnetic recording medium - Google Patents
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JP5394552B2 - Substrate for perpendicular magnetic recording medium and magnetic recording medium - Google Patents

Substrate for perpendicular magnetic recording medium and magnetic recording medium Download PDF

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JP5394552B2
JP5394552B2 JP2012207827A JP2012207827A JP5394552B2 JP 5394552 B2 JP5394552 B2 JP 5394552B2 JP 2012207827 A JP2012207827 A JP 2012207827A JP 2012207827 A JP2012207827 A JP 2012207827A JP 5394552 B2 JP5394552 B2 JP 5394552B2
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孝 森川
博一 湯浅
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本発明は、垂直磁気記録媒体用基板の検査方法、垂直磁気記録媒体用基板の製造方法、及び垂直磁気記録媒体の製造方法に関する。   The present invention relates to a method for inspecting a perpendicular magnetic recording medium substrate, a method for producing a perpendicular magnetic recording medium substrate, and a method for producing a perpendicular magnetic recording medium.

近年のHDD(ハードディスクドライブ)に代表される磁気記録装置では、2.5インチ径磁気ディスクにして、1枚辺り80GBを超える情報記憶容量が求められるようになってきた。HDD用の磁気記録媒体である磁気ディスクにおいて、これらの所要に応えるためには、1平方インチ辺り100Gビット(100Gbit/inch)を超える情報記憶密度を実現することが求められている。このような高記録密度で安定した記録再生を行うには磁気記録再生方式として垂直磁気記録方式を採用することが望ましいと考えられている。垂直磁気記録方式で用いられる垂直磁気記録媒体では、例えば、軟磁性層及び磁気記録層等の磁性層が基板上に形成される。 In recent magnetic recording apparatuses represented by HDD (Hard Disk Drive), a 2.5-inch diameter magnetic disk is required to have an information storage capacity exceeding 80 GB per sheet. In order to meet these requirements in a magnetic disk that is a magnetic recording medium for HDD, it is required to realize an information storage density exceeding 100 Gbits (100 Gbit / inch 2 ) per square inch. In order to perform stable recording and reproduction at such a high recording density, it is considered desirable to adopt a perpendicular magnetic recording system as a magnetic recording and reproducing system. In a perpendicular magnetic recording medium used in the perpendicular magnetic recording system, for example, a magnetic layer such as a soft magnetic layer and a magnetic recording layer is formed on a substrate.

垂直磁気記録媒体において、電磁変換特性を高めるためには、磁性層に含まれる磁性粒子の磁気的異方性を制御する必要がある。例えば、基板の主表面と平行な面内において、基板の円周方向の磁気的異方性を磁性粒子に付与することは、ノイズの原因となるため、好ましくない。また、例えば、軟磁性層において、磁気的異方性が円周方向を向くことはノイズの原因となるため、好ましくない。   In the perpendicular magnetic recording medium, it is necessary to control the magnetic anisotropy of the magnetic particles contained in the magnetic layer in order to improve the electromagnetic conversion characteristics. For example, giving magnetic anisotropy in the circumferential direction of the substrate to the magnetic particles in a plane parallel to the main surface of the substrate is not preferable because it causes noise. Further, for example, in the soft magnetic layer, it is not preferable that the magnetic anisotropy is directed in the circumferential direction because it causes noise.

ここで、磁性層の磁性粒子の磁気的異方性は、基板表面における微細構造の影響を受けると考えられる。そのため、面内方向における磁気的異方性を低減するためには、基板表面の微細構造を適切に制御することが望まれる。また、基板表面の微細構造を制御するためには、基板の表面形状を適切な指標を用いて評価する必要がある。   Here, it is considered that the magnetic anisotropy of the magnetic particles in the magnetic layer is influenced by the fine structure on the substrate surface. Therefore, in order to reduce the magnetic anisotropy in the in-plane direction, it is desired to appropriately control the fine structure of the substrate surface. Further, in order to control the fine structure of the substrate surface, it is necessary to evaluate the surface shape of the substrate using an appropriate index.

従来、長手記録方式用で磁気記録を行う磁気記録媒体用基板の表面形状に対し、線密度あるいはラインデンシティと呼ばれる指標(以下、LDという)を用いて評価を行う方法が知られている(例えば、特許文献1、2参照。)。LDは、例えば、AFM(原子間力顕微鏡)で基板主表面を測定することによって得られる基板の半径方向一深さ方向の断面図において、1μmあたりに存在するテクスチャの山の数(あるいは谷の数)、又は基準線と交差する回数の半分等として定義される。長手記録方式用で磁気記録を行う磁気記録媒体において、基板のLDは、高いほど電磁変換特性がよいと考えられている。   2. Description of the Related Art Conventionally, there is known a method for evaluating the surface shape of a magnetic recording medium substrate that performs magnetic recording in the longitudinal recording method, using an index called linear density or line density (hereinafter referred to as LD) (for example, LD). Patent Documents 1 and 2). The LD is the number of texture peaks (or valleys) present per 1 μm in a cross-sectional view in the radial direction depth direction of the substrate obtained by measuring the substrate main surface with an AFM (atomic force microscope), for example. Number), or half the number of times it intersects the reference line. In a magnetic recording medium that performs magnetic recording for the longitudinal recording method, it is considered that the higher the LD of the substrate, the better the electromagnetic conversion characteristics.

しかし、LDによる評価は、磁気記録媒体用基板の主表面に、テクスチャと呼ばれる無数の微小な溝を形成する場合に用いられるものである。このテクスチャは、溝に沿った結晶成長を促すことにより、磁性粒子の磁化容易軸を円周方向に配向させやすくするものである。   However, the evaluation by LD is used when an infinite number of minute grooves called textures are formed on the main surface of the magnetic recording medium substrate. This texture facilitates crystal growth along the grooves, thereby making it easy to orient the easy axis of magnetization of the magnetic particles in the circumferential direction.

これに対し、面内方向における磁気的異方性を低減することが望ましい垂直磁気記録媒体において、基板にテクスチャを形成することは必ずしも必要ではない。そのため、指標としてLDを用いた場合、垂直磁気記録媒体用基板の評価を適切に行うことはできないおそれがある。   In contrast, in a perpendicular magnetic recording medium in which it is desirable to reduce the magnetic anisotropy in the in-plane direction, it is not always necessary to form a texture on the substrate. Therefore, when LD is used as an index, there is a possibility that the perpendicular magnetic recording medium substrate cannot be properly evaluated.

また、基板の表面の断面は、単純な山と谷で構成されてはおらず、高さ深さや幅が不揃いである。そのため、どの程度の高さ、深さ、又は幅を有する形状を山又は谷と判断するかによって、LDの値が変化してしまう。従って、LDは、定義自体が曖昧さを含んでいるとも言える。また、定義の取り方によってLDの値自体が変化してしまうとすれば、絶対的な指標としては使いにくい。   Further, the cross section of the surface of the substrate is not composed of simple peaks and valleys, and the height depth and width are not uniform. Therefore, the value of LD changes depending on how high, deep, or width the shape is determined as a mountain or a valley. Therefore, it can be said that the definition of LD includes ambiguity. Also, if the LD value itself changes depending on the definition, it is difficult to use as an absolute index.

そのため、垂直磁気記録媒体用基板の表面形状の評価を、より適切な指標を用いて行うことが望まれている。また、適切な指標を用いて行う評価により検査された垂直磁気記録媒体用基板や垂直磁気記録媒体を提供することが望まれている。本発明は、上記の課題を解決できる垂直磁気記録媒体用基板の検査方法、垂直磁気記録媒体用基板の製造方法、及び垂直磁気記録媒体の製造方法を提供することを目的とする。   For this reason, it is desired to evaluate the surface shape of the perpendicular magnetic recording medium substrate using a more appropriate index. It is also desirable to provide a perpendicular magnetic recording medium substrate or a perpendicular magnetic recording medium that has been inspected by evaluation using an appropriate index. An object of the present invention is to provide a method for inspecting a perpendicular magnetic recording medium substrate, a method for producing a perpendicular magnetic recording medium substrate, and a method for producing a perpendicular magnetic recording medium that can solve the above-described problems.

本願発明者は、鋭意研究により、磁性粒子の磁気的異方性に影響を与える基板表面の微細構造としては、基板表面における山や谷の数又は密度だけだはなく、山や谷の幅が重要であることを見出した。そして、山や谷の幅を反映した指標として、基板の断面形状の波形をフーリエ変換した指標を用いることが有効であることを見出した。そして、これらの知見に基づき、本発明に至った。本発明は、以下の構成を有する。   The inventor of the present application has intensively studied that the fine structure of the substrate surface that affects the magnetic anisotropy of the magnetic particles includes not only the number or density of peaks and valleys on the substrate surface, but also the width of the peaks and valleys. I found it important. And it discovered that it was effective to use the parameter | index which carried out the Fourier transform of the waveform of the cross-sectional shape of a board | substrate as a parameter | index reflecting the width | variety of a peak or a valley. And based on these knowledge, it came to this invention. The present invention has the following configuration.

(構成1)垂直磁気記録方式で情報を記録する垂直磁気記録媒体の製造に用いられる垂直磁気記録媒体用基板の形状を検査する垂直磁気記録媒体用基板の検査方法であって、主表面が研磨された円盤状の基板の断面形状を測定する断面形状測定段階と、断面形状測定段階で測定された断面形状の波形をフーリエ変換することにより、断面形状の波形を波長と強度との関係に変換するフーリエ変換段階と、フーリエ変換段階で得られた波長と強度との関係に基づいて基板の合否を判定する判定段階とを備える。フーリエ変換段階は、例えば、断面形状の波形に対して乗じる必要に応じた窓関数を用いて、フーリエ変換を行う。   (Configuration 1) A perpendicular magnetic recording medium substrate inspection method for inspecting the shape of a perpendicular magnetic recording medium substrate used for manufacturing a perpendicular magnetic recording medium for recording information by a perpendicular magnetic recording method, wherein a main surface is polished. The cross-sectional waveform is measured to measure the cross-sectional shape of the disc-shaped substrate, and the waveform of the cross-sectional shape measured in the cross-sectional shape measurement step is Fourier transformed to convert the waveform of the cross-sectional shape into a relationship between wavelength and intensity. A Fourier transform stage, and a determination stage for judging pass / fail of the substrate based on the relationship between the wavelength and the intensity obtained in the Fourier transform stage. In the Fourier transform stage, for example, the Fourier transform is performed using a window function according to the necessity to multiply the waveform of the cross-sectional shape.

窓関数とは、ある有限区間以外で0となる関数である。他の関数や信号(データ)に窓関数が掛け合わせられると、区間外は0になり、有限区間内だけが残るので、数値解析が容易になる。構成1において、窓関数としては、例えば矩形窓又はハミング窓の関数を用いることができる。   The window function is a function that becomes 0 outside a certain finite interval. When another function or signal (data) is multiplied by a window function, the outside of the interval becomes 0 and only the finite interval remains, so that numerical analysis becomes easy. In Configuration 1, for example, a rectangular window function or a Hamming window function can be used as the window function.

このようにした場合、フーリエ変換によって得られた波長と強度との関係において、波長は、例えば、断面形状測定段階で測定した断面形状に含まれる山や谷の幅を反映する。また、強度は、それぞれの波長に対応する幅の山や谷の数を反映する。そのため、例えば、幅が小さな山や谷が多い場合、小さな波長領域の強度が大きくなる。また、幅が大きな山や谷が多い場合、大きな波長領域の強度が大きくなる。   In this case, in the relationship between the wavelength and the intensity obtained by Fourier transform, the wavelength reflects, for example, the width of a peak or valley included in the cross-sectional shape measured in the cross-sectional shape measurement stage. The intensity reflects the number of peaks and valleys with a width corresponding to each wavelength. Therefore, for example, when there are many peaks and valleys with a small width, the intensity of the small wavelength region is increased. In addition, when there are many peaks and valleys with a large width, the intensity in a large wavelength region increases.

これにより、例えば、基板表面の微細構造として、山や谷の数や密度だけだはなく、特定の幅の山や谷の数や密度を把握できる。また、判定段階において、特定の幅の山や谷の数や密度に基づく評価を行うことができる。   Thereby, for example, as the fine structure of the substrate surface, not only the number and density of peaks and valleys but also the number and density of peaks and valleys having a specific width can be grasped. In the determination stage, evaluation based on the number and density of peaks and valleys having a specific width can be performed.

従って、構成1のようにすれば、基板表面の山や谷の幅や、特定の幅の山や谷の数や密度を反映した、より適切な指標により、垂直磁気記録媒体用基板の表面形状の評価を行うことができる。そして、例えばこの評価に基づく検査を行うことにより、例えば、面内方向における磁気的異方性が小さな磁気記録層を有する垂直磁気記録媒体を適切に製造できる。また、これにより、磁気記録層の電磁変換特性を適切に高めることができる。   Therefore, according to Configuration 1, the surface shape of the substrate for the perpendicular magnetic recording medium can be determined by a more appropriate index reflecting the width of the peaks and valleys of the substrate surface, and the number and density of peaks and valleys of a specific width. Can be evaluated. For example, by performing an inspection based on this evaluation, for example, a perpendicular magnetic recording medium having a magnetic recording layer with a small magnetic anisotropy in the in-plane direction can be appropriately manufactured. Thereby, the electromagnetic conversion characteristics of the magnetic recording layer can be appropriately enhanced.

尚、断面形状測定段階は、例えば、原子間力顕微鏡(AFM)により断面形状を測定する。この測定は、1μmあたり256点以上のサンプリング点を含む測定精度で行うことが好ましい。測定に必要な解像度は、磁気記録層の磁性粒子の結晶粒径によるが、このような精度で測定すれば、測定に必要なコストを上げることなく、十分な精度で測定を行うことができる。   In the cross-sectional shape measurement step, the cross-sectional shape is measured by, for example, an atomic force microscope (AFM). This measurement is preferably performed with measurement accuracy including 256 or more sampling points per 1 μm. The resolution required for the measurement depends on the crystal grain size of the magnetic particles in the magnetic recording layer, but if measured with such accuracy, the measurement can be performed with sufficient accuracy without increasing the cost required for the measurement.

測定された全範囲の波長とは、例えば、測定可能範囲の下限値以上、測定上意味がある上限値以下の範囲である。断面形状測定段階においてAFMを用いて測定を行う場合、測定上意味がある上限値とは、例えば、断面形状測定段階における測定の長さの1/4の波長である。これは、AFMによる測定において、測定の長さの1/4以上の波長成分は、平坦度補正等の要素によって変化し、真の表面形状を反映しないためである。   The measured wavelength of the entire range is, for example, a range not less than the lower limit value of the measurable range and not more than the upper limit value that is meaningful in measurement. When measurement is performed using the AFM in the cross-sectional shape measurement stage, the upper limit value meaningful in measurement is, for example, a wavelength that is ¼ of the measurement length in the cross-section shape measurement stage. This is because in the measurement by the AFM, the wavelength component of ¼ or more of the measurement length changes depending on factors such as flatness correction and does not reflect the true surface shape.

また、測定された全範囲の波長は、例えば、磁性層あるいは軟磁性層に含まれる磁性粒子の平均粒径の0.6〜120倍であってもよい。このようにした場合も、例えば磁性粒子の磁気的異方性に影響を与える可能性が高い基板表面の形状を適切に評価できる。磁性粒子の平均粒径は、例えば、200万倍で撮影したTEM写真から任意の50nm×50nmの領域を選び、領域内に含まれる個々の磁性粒子を抽出し、それぞれの長径・短径の平均値を算出することにより、求めることができる。領域内に含まれる個々の磁性粒子とは、例えば、粒子全体が単結晶になっている磁性結晶粒子である。   Further, the measured wavelength in the entire range may be, for example, 0.6 to 120 times the average particle diameter of the magnetic particles contained in the magnetic layer or the soft magnetic layer. Even in this case, for example, the shape of the substrate surface that is highly likely to affect the magnetic anisotropy of the magnetic particles can be appropriately evaluated. The average particle size of the magnetic particles is, for example, an arbitrary 50 nm × 50 nm region is selected from a TEM photograph taken at 2 million times, and individual magnetic particles contained in the region are extracted, and the average of the major axis and minor axis of each is selected. It can be obtained by calculating the value. The individual magnetic particles included in the region are, for example, magnetic crystal particles in which the entire particle is a single crystal.

磁性粒子の平均粒径は、基板上に形成される磁性層において算出されると考えられる予測値であってよい。この予測値は、例えば、基板上に磁性層を形成した試料を予め作成して上記の算出を行うことにより、得ることができる。   The average particle diameter of the magnetic particles may be a predicted value that is considered to be calculated in the magnetic layer formed on the substrate. This predicted value can be obtained, for example, by preparing a sample in which a magnetic layer is formed on a substrate and performing the above calculation.

(構成2)フーリエ変換段階で得られた波長と強度との関係に基づき、測定された全範囲の波長の範囲について強度を積分した値である全範囲積分値と、予め設定された波長の範囲について強度を積分した値である設定範囲積分値とを算出する積分段階を更に備え、判定段階は、全範囲積分値に対する設定範囲積分値の比に基づき、基板の合否を判定する。   (Configuration 2) Based on the relationship between the wavelength and the intensity obtained in the Fourier transform stage, the entire range integrated value, which is a value obtained by integrating the intensity for the measured wavelength range, and the preset wavelength range An integration stage is further provided for calculating a set range integral value that is a value obtained by integrating the intensity with respect to. The determination stage determines pass / fail of the substrate based on a ratio of the set range integral value to the entire range integral value.

このようにした場合、設定範囲積分値は、例えば、特定の範囲の幅の山や谷の数を反映した値となる。また、全範囲積分値に対する設定範囲積分値の比は、例えば、測定領域内の山や谷の総数に対する特定の範囲の幅の山や谷の数の割合を反映した値となる。   In this case, the set range integral value is a value reflecting the number of peaks and valleys of a specific range width, for example. The ratio of the set range integral value to the total range integral value is a value reflecting the ratio of the number of peaks and valleys of a specific range width to the total number of peaks and valleys in the measurement region, for example.

磁性粒子の磁気的異方性(配向性)への影響は、基板表面における山や谷の幅が一定範囲の場合に特に大きくなると考えられる。例えば、山や谷の幅が一定範囲より小さい場合、その上で成長する磁性粒子の数が少なくなるため、磁性粒子の磁気的異方性の制御に対する寄与が小さくなると考えられる。また、山や谷の幅が一定範囲より大きい場合、その山や谷は、磁性粒子にとって平坦な領域に近くなり、磁性粒子の磁気的異方性を制御する機能を発揮しにくくなると考えられる。   The influence on the magnetic anisotropy (orientation) of the magnetic particles is considered to be particularly large when the width of the peaks and valleys on the substrate surface is within a certain range. For example, when the width of the peaks and valleys is smaller than a certain range, the number of magnetic particles growing on the peaks and valleys is reduced, so that the contribution to the control of the magnetic anisotropy of the magnetic particles is considered to be small. In addition, when the width of the peaks and valleys is larger than a certain range, the peaks and valleys are considered to be close to a flat region for the magnetic particles, and it is considered difficult to exhibit the function of controlling the magnetic anisotropy of the magnetic particles.

そのため、このようにすれば、磁性粒子の磁気的異方性への影響が大きい山や谷の割合を適切に評価できる。また、これにより、垂直磁気記録媒体用基板の表面形状の評価を、より適切に行うことができる。   Therefore, in this way, it is possible to appropriately evaluate the ratio of peaks and valleys that have a large influence on the magnetic anisotropy of magnetic particles. This also makes it possible to more appropriately evaluate the surface shape of the perpendicular magnetic recording medium substrate.

尚、磁性粒子の磁気的異方性への影響は、例えば、山や谷の幅が磁性粒子の平均粒径の1〜3倍の場合に特に大きくなると考えられる。そのため、積分段階は、磁性粒子の平均粒径の1〜3倍に対応する波長の範囲について、設定範囲積分値を算出することが好ましい。判定段階は、例えば、全範囲積分値に対するこの設定範囲積分値の比が予め設定した値以下の場合に、基板が合格であると判定する。   In addition, it is thought that the influence on the magnetic anisotropy of a magnetic particle becomes large especially when the width | variety of a peak or a valley is 1-3 times the average particle diameter of a magnetic particle, for example. Therefore, it is preferable that the integration step calculates a set range integral value for a wavelength range corresponding to 1 to 3 times the average particle diameter of the magnetic particles. In the determination step, for example, when the ratio of the set range integral value to the total range integral value is equal to or less than a preset value, it is determined that the substrate is acceptable.

また、断面形状測定段階は、基板の半径方向に沿った断面形状を測定することが好ましい。このようにすれば、基板の円周方向の磁気的異方性に対する影響が大きな山や谷の形状を適切に評価できる。また、これにより、基板の円周方向の磁気的異方性を適切に低減できる。   Moreover, it is preferable that the cross-sectional shape measurement step measures a cross-sectional shape along the radial direction of the substrate. In this way, it is possible to appropriately evaluate the shapes of peaks and valleys that have a large influence on the magnetic anisotropy in the circumferential direction of the substrate. Thereby, the magnetic anisotropy in the circumferential direction of the substrate can be appropriately reduced.

(構成3)垂直磁気記録方式で情報を記録する垂直磁気記録媒体に用いられる垂直磁気記録媒体用基板の製造方法であって、主表面が研磨された円盤状の基板を準備する準備工程と、構成1又は2に記載の垂直磁気記録媒体用基板の検査方法により、準備工程で準備される基板を検査する検査工程とを備える。このようにすれば、例えば、構成1又は2と同様の効果を得ることができる。また、主表面上に形成される磁性層において面内方向の磁気的異方性が生じにくい垂直磁気記録媒体用基板を適切に製造できる。   (Configuration 3) A method for manufacturing a substrate for a perpendicular magnetic recording medium used for a perpendicular magnetic recording medium that records information by a perpendicular magnetic recording method, and a preparation step of preparing a disk-shaped substrate having a main surface polished; An inspection step of inspecting the substrate prepared in the preparation step by the method for inspecting a perpendicular magnetic recording medium substrate according to Configuration 1 or 2. In this way, for example, the same effects as those of Configuration 1 or 2 can be obtained. In addition, it is possible to appropriately manufacture a perpendicular magnetic recording medium substrate in which in-plane magnetic anisotropy hardly occurs in the magnetic layer formed on the main surface.

尚、検査工程は、必ずしも全数の基板に対して検査を行う工程でなくてもよい。例えば、検査工程は、一定数の基板毎に一部の基板を検査する抜き取り検査や、品質を保持するために一定期間毎に行う検査の工程であってもよい。   The inspection process is not necessarily a process for inspecting all the substrates. For example, the inspection process may be a sampling inspection for inspecting a part of the substrates for every predetermined number of substrates, or an inspection step performed at regular intervals in order to maintain quality.

(構成4)垂直磁気記録方式で情報を記録する垂直磁気記録媒体の製造方法であって、構成3に記載の垂直磁気記録媒体用基板の製造方法で製造される垂直磁気記録媒体用基板上に、少なくとも磁気記録層を形成する。このようにすれば、面内方向における磁気的異方性が小さな垂直磁気記録媒体を適切に製造できる。また、これにより、磁気記録層の電磁変換特性を適切に高めることができる。   (Structure 4) A method of manufacturing a perpendicular magnetic recording medium for recording information by the perpendicular magnetic recording method, wherein the perpendicular magnetic recording medium substrate manufactured by the method for manufacturing a perpendicular magnetic recording medium substrate according to Structure 3 is used. At least a magnetic recording layer is formed. In this way, a perpendicular magnetic recording medium having a small magnetic anisotropy in the in-plane direction can be appropriately manufactured. Thereby, the electromagnetic conversion characteristics of the magnetic recording layer can be appropriately enhanced.

本発明によれば、例えば、垂直磁気記録媒体用基板の表面形状の評価を、より適切な指標を用いて行うことができる。   According to the present invention, for example, the surface shape of a perpendicular magnetic recording medium substrate can be evaluated using a more appropriate index.

以下、本発明に係る実施形態を、図面を参照しながら説明する。図1は、本発明の一実施形態に係る垂直磁気記録媒体10の構成の一例を示す断面図である。垂直磁気記録媒体10は、垂直磁気記録方式のHDDに用いられる磁気ディスクであり、基板12、軟磁性層14、及び磁気記録層16を備える。基板12は、中心に円孔を有する円盤状のガラス基板である。このガラス基板は、例えばアルミノシリケートのアモルファスガラス基板である。また、基板12の主表面及び内外周の端面は、所定の表面粗さに研磨されている。   Hereinafter, embodiments according to the present invention will be described with reference to the drawings. FIG. 1 is a cross-sectional view showing an example of the configuration of a perpendicular magnetic recording medium 10 according to an embodiment of the present invention. The perpendicular magnetic recording medium 10 is a magnetic disk used in a perpendicular magnetic recording type HDD, and includes a substrate 12, a soft magnetic layer 14, and a magnetic recording layer 16. The substrate 12 is a disk-shaped glass substrate having a circular hole in the center. This glass substrate is, for example, an aluminosilicate amorphous glass substrate. The main surface of the substrate 12 and the inner and outer peripheral end surfaces are polished to a predetermined surface roughness.

軟磁性層14及び磁気記録層16は、基板12上に形成される磁性層である。軟磁性層14は、磁気記録層16を介してHDDの磁気ヘッドとの間に磁気回路を形成する層であり、例えば、平均粒径が7.5〜8.5nmの磁性粒子を含む。磁気記録層16は、CoCrPt等の硬磁性の磁性粒子を含む層である。磁気記録層16は、TiO2等の酸化物のマトリクス中に磁性粒子が分散するグラニュラ構造の層であってよい。また、磁気記録層16は、例えば、平均粒径が7.5〜8.5nmの磁性粒子を含む。   The soft magnetic layer 14 and the magnetic recording layer 16 are magnetic layers formed on the substrate 12. The soft magnetic layer 14 is a layer that forms a magnetic circuit between the magnetic recording layer 16 and the magnetic head of the HDD, and includes, for example, magnetic particles having an average particle diameter of 7.5 to 8.5 nm. The magnetic recording layer 16 is a layer containing hard magnetic particles such as CoCrPt. The magnetic recording layer 16 may be a layer having a granular structure in which magnetic particles are dispersed in a matrix of an oxide such as TiO 2. The magnetic recording layer 16 includes, for example, magnetic particles having an average particle diameter of 7.5 to 8.5 nm.

尚、上記では説明を簡単にするために省略したが、垂直磁気記録媒体10は、基板12と軟磁性層14との間、軟磁性層14と磁気記録層16との間、又は磁気記録層16上に、更に他の層を備えてもよい。例えば、垂直磁気記録媒体10は、軟磁性層14と磁気記録層16との間に、磁気記録層16の結晶配向を制御する配向制御層等を更に備えてもよい。また、磁気記録層16上に、例えば保護層や潤滑層等を更に備えてもよい。また、軟磁性層14はアモルファスであってもよい。   Although omitted for the sake of simplicity in the above description, the perpendicular magnetic recording medium 10 is provided between the substrate 12 and the soft magnetic layer 14, between the soft magnetic layer 14 and the magnetic recording layer 16, or the magnetic recording layer. Further layers may be provided on 16. For example, the perpendicular magnetic recording medium 10 may further include an orientation control layer for controlling the crystal orientation of the magnetic recording layer 16 between the soft magnetic layer 14 and the magnetic recording layer 16. Further, a protective layer, a lubricating layer, or the like may be further provided on the magnetic recording layer 16. The soft magnetic layer 14 may be amorphous.

図2は、基板12の製造方法の一例を示すフローチャートである。本例において、この製造方法は、最初に、主表面及び内外周の端面が所定の表面粗さに研磨された円盤状の基板を準備する(準備工程S102)。   FIG. 2 is a flowchart showing an example of a method for manufacturing the substrate 12. In this example, the manufacturing method first prepares a disk-shaped substrate whose main surface and inner and outer peripheral end faces are polished to a predetermined surface roughness (preparation step S102).

続いて、準備工程S102で準備された基板の形状の検査を行う(検査工程S104)。本例において、検査工程S104は、最初に、例えば、原子間力顕微鏡(AFM)により、半径方向に沿った基板12の断面形状を測定する(断面形状測定段階S202)。   Subsequently, the shape of the substrate prepared in the preparation step S102 is inspected (inspection step S104). In this example, the inspection step S104 first measures the cross-sectional shape of the substrate 12 along the radial direction by, for example, an atomic force microscope (AFM) (cross-sectional shape measurement step S202).

尚、AFMを用いた場合、例えばJIS B0601の規定に従って、各走査線毎の粗さ曲線を求めることができる。そのため、AFMを用いれば、基板12の断面形状を適切かつ高い精度で測定できる。この測定は、1μmあたり256点以上のサンプリング点を含む測定精度で行うことが好ましい。このような精度で測定すれば、測定に必要なコストを上げることなく、十分な精度で測定を行うことができる。   When AFM is used, a roughness curve for each scanning line can be obtained in accordance with, for example, JIS B0601. Therefore, if the AFM is used, the cross-sectional shape of the substrate 12 can be measured appropriately and with high accuracy. This measurement is preferably performed with measurement accuracy including 256 or more sampling points per 1 μm. If the measurement is performed with such accuracy, the measurement can be performed with sufficient accuracy without increasing the cost required for the measurement.

断面形状の測定は、基板12の主表面の一部の領域について行う測定であってよい。断面形状測定段階S202は、例えば、基板12の半径方向に延びる500nmの測定領域に対して、断面形状の測定を行う。   The measurement of the cross-sectional shape may be a measurement performed on a partial region of the main surface of the substrate 12. In the cross-sectional shape measurement step S202, for example, the cross-sectional shape is measured for a measurement region of 500 nm extending in the radial direction of the substrate 12.

次に、測定された断面形状の波形をフーリエ変換することにより、断面形状の波形を波長と強度との関係に変換する(フーリエ変換段階S204)。フーリエ変換段階S204は、例えば高速フーリエ変換(FFT)により、フーリエ変換を行う。高速フーリエ変換とは、離散フーリエ変換(DFT)を計算機上で高速に計算するアルゴリズムである。フーリエ変換の窓関数としては、例えば矩形窓又はハミング窓の関数を用いる。   Next, the cross-sectional waveform is converted into the relationship between the wavelength and the intensity by Fourier transforming the measured cross-sectional waveform (Fourier transform step S204). The Fourier transform step S204 performs Fourier transform, for example, by fast Fourier transform (FFT). Fast Fourier transform is an algorithm for calculating discrete Fourier transform (DFT) at high speed on a computer. As the window function of the Fourier transform, for example, a rectangular window function or a Hamming window function is used.

次に、得られた波長と強度との関係について、強度を波長で積分する演算を行う(積分段階S206)。本例において、積分段階S206は、測定された全範囲の波長の範囲について強度を積分した値である全範囲積分値と、予め設定された波長の範囲について強度を積分した値である設定範囲積分値とを算出する。   Next, with respect to the relationship between the obtained wavelength and intensity, an operation for integrating the intensity with the wavelength is performed (integration step S206). In this example, the integration step S206 includes a total range integrated value that is a value obtained by integrating the intensity over the measured wavelength range and a set range integration that is a value obtained by integrating the intensity over a preset wavelength range. Value.

次に、全範囲積分値に対する設定範囲積分値の比を算出することにより設定範囲積分値を規格化する。そして、規格化された設定範囲積分値に基づき、基板12の合否を判定する(判定段階S208)。本例によれば、例えば、磁性粒子の磁気的異方性(配向性)への影響が大きい山や谷の割合を考慮して、基板12の形状を適切に評価できる。これにより、基板12の表面形状の評価を、適切な指標を用いて行うことができる。   Next, the set range integral value is normalized by calculating the ratio of the set range integral value to the entire range integral value. Then, it is determined whether the substrate 12 is acceptable based on the standardized set range integral value (determination step S208). According to this example, for example, the shape of the substrate 12 can be appropriately evaluated in consideration of the ratio of peaks and valleys that have a large influence on the magnetic anisotropy (orientation) of the magnetic particles. Thereby, evaluation of the surface shape of the board | substrate 12 can be performed using a suitable parameter | index.

尚、本例において、積分段階S206は、設定範囲積分値を求めるための波長の範囲として、基板12上に形成されるべき軟磁性層14に含まれる磁性粒子の平均粒径の1〜3倍の波長の範囲を用いる。この平均粒径は、例えば、基板12上に軟磁性層14を形成した試料を予め作成することにより、平均粒径の予測値として算出できる。軟磁性層14がアモルファスである場合は、磁気記録層16に含まれる磁性粒子の平均粒径の1〜3倍の波長の範囲を用いることができる。   In the present example, the integration step S206 has a wavelength range for obtaining the set range integral value of 1 to 3 times the average particle diameter of the magnetic particles contained in the soft magnetic layer 14 to be formed on the substrate 12. The wavelength range is used. This average particle diameter can be calculated as a predicted value of the average particle diameter by, for example, preparing a sample in which the soft magnetic layer 14 is formed on the substrate 12 in advance. When the soft magnetic layer 14 is amorphous, a wavelength range of 1 to 3 times the average particle diameter of the magnetic particles contained in the magnetic recording layer 16 can be used.

このような波長の範囲を用いた場合、全範囲積分値に対する設定範囲積分値の比は、軟磁性層14および磁気記録層16の磁性粒子に磁気的異方性を与えやすい幅の山や谷の割合を示すと考えられる。例えば、この比が大きい場合、磁性粒子に磁気的異方性を与えやすい幅の山や谷の割合が大きいと考えられる。   When such a range of wavelengths is used, the ratio of the set range integral value to the total range integral value is such that peaks and valleys with a width that easily gives magnetic anisotropy to the magnetic particles of the soft magnetic layer 14 and the magnetic recording layer 16. It is thought that the ratio of For example, when this ratio is large, it is considered that the ratio of peaks and valleys having a width that easily gives magnetic anisotropy to magnetic particles is large.

そのため、本例において、判定段階S208は、例えば、全範囲積分値に対する設定範囲積分値の比が予め設定した基準値以下の場合に、基板12が合格であると判定する。この基準値は、例えば0.3である。このようにすれば、例えば、磁性粒子に磁気的異方性を与えやすい幅の山や谷の割合が大きな基板12を不合格にできる。また、これにより、例えば、基板12の形状を適切に制御して、軟磁性層の磁気的異方性が半径方向に配向した状態を維持できる。   Therefore, in this example, the determination step S208 determines that the substrate 12 is acceptable when, for example, the ratio of the set range integral value to the total range integral value is equal to or less than a preset reference value. This reference value is 0.3, for example. In this way, for example, the substrate 12 having a large ratio of peaks and valleys with a width that easily gives magnetic anisotropy to the magnetic particles can be rejected. Thereby, for example, the shape of the substrate 12 can be appropriately controlled, and the magnetic anisotropy of the soft magnetic layer can be maintained in the radial direction.

(実施例)
以下、基板12の表面形状の評価を行う方法の一例を、実施例により、更に詳しく説明する。実施例1に係る基板12として、アルミノシリケートのアモルファスガラス基板を準備した。基板12は、2.5インチ型磁気ディスク用基板であり、直径は65mm、内径は20mm、ディスク厚は0.635mmである。そして、AFMにより、基板12の半径方向に延びる500nmの測定領域に対して、256点/1μmの測定精度で行った。また、この測定により得られた断面形状の波形に対し、窓関数としてハミング関数を用いて、フーリエ変換を行った。
(Example)
Hereinafter, an example of a method for evaluating the surface shape of the substrate 12 will be described in more detail with reference to examples. As the substrate 12 according to Example 1, an aluminosilicate amorphous glass substrate was prepared. The substrate 12 is a 2.5-inch magnetic disk substrate having a diameter of 65 mm, an inner diameter of 20 mm, and a disk thickness of 0.635 mm. Then, AFM was performed with a measurement accuracy of 256 points / 1 μm for a measurement region of 500 nm extending in the radial direction of the substrate 12. Further, Fourier transform was performed on the cross-sectional waveform obtained by this measurement using a Hamming function as a window function.

図3は、実施例1に係る基板12に対するフーリエ変換の結果を示すグラフである。この結果を、例えば予め用意した判定基準と比較することにより、基板12の表面の山や谷の幅を考慮して、基板12の表面形状の評価を行うことができる。例えば図2を用いて説明した積分段階S206及び判定段階S208を行うことにより、基板12の検査を行うことができる。   FIG. 3 is a graph illustrating the result of Fourier transform on the substrate 12 according to the first embodiment. By comparing this result with, for example, a determination criterion prepared in advance, the surface shape of the substrate 12 can be evaluated in consideration of the widths of peaks and valleys on the surface of the substrate 12. For example, the substrate 12 can be inspected by performing the integration step S206 and the determination step S208 described with reference to FIG.

尚、実施例1において、積分段階S206において全範囲積分値を算出する場合、測定された全範囲の波長範囲について、下限の波長は、256点/1μmの測定精度におけるサンプリング点間の距離(3.9nm)に合わせて4nmとする。また、上限の波長は、測定領域の長さ500nmの1/4である125nm(125nmは除外)とする。これは、AFMの測定において、測定の長さの1/4以上の波長成分は、測定時の平坦度補正等の要素によって変化し、真の表面形状を反映しないためである。そのため、全範囲積分値の算出は、4nm以上125nm未満の波長範囲に対して行うことが好ましい。   In the first embodiment, when the integral value of the entire range is calculated in the integration step S206, the lower limit wavelength of the measured wavelength range is the distance between sampling points (3 (3 points) at a measurement accuracy of 256 points / 1 μm. .9 nm) to 4 nm. The upper limit wavelength is 125 nm (excluding 125 nm), which is a quarter of the length of the measurement region of 500 nm. This is because, in AFM measurement, a wavelength component that is ¼ or more of the measurement length varies depending on factors such as flatness correction during measurement and does not reflect the true surface shape. Therefore, it is preferable to calculate the total range integral value for a wavelength range of 4 nm or more and less than 125 nm.

また、設定範囲積分値を算出する場合、基板12上に形成されるべき軟磁性層14に含まれる磁性粒子の平均粒径の1〜3倍の波長範囲を用いる。例えば、軟磁性層14に含まれる磁性粒子の平均半径が8nmと予測できる場合、設定範囲積分値を算出する波長範囲として、8〜24nmの波長範囲を用いる。このようにすれば、基板12の表面の微細構造のうち、磁性粒子の磁気的異方性への影響が大きい山や谷の割合を適切に考慮できる。   Further, when calculating the set range integral value, a wavelength range of 1 to 3 times the average particle diameter of the magnetic particles contained in the soft magnetic layer 14 to be formed on the substrate 12 is used. For example, when the average radius of the magnetic particles contained in the soft magnetic layer 14 can be predicted to be 8 nm, a wavelength range of 8 to 24 nm is used as a wavelength range for calculating the setting range integral value. In this way, it is possible to appropriately consider the ratio of peaks and valleys that have a large influence on the magnetic anisotropy of the magnetic particles in the fine structure of the surface of the substrate 12.

上記の波長範囲において積分を行ったところ、実施例1において、全範囲積分値は、4.14、設定範囲積分値は、1.07となった。また、その結果、全範囲積分値に対する設定範囲積分値の比は、0.26となった。   When integration was performed in the above wavelength range, in Example 1, the total range integrated value was 4.14, and the set range integrated value was 1.07. As a result, the ratio of the set range integral value to the entire range integral value was 0.26.

判定段階S208においては、この比を基準値(例えば0.3)と比較することにより、基板12の合否を判定する。これにより、主表面上に形成される磁性層において基板の円周方向の磁気的異方性が生じにくい基板12を適切に判定できる。そのため、実施例1によれば、基板12の表面形状の評価を適切に行うことができる。   In the determination step S208, the pass / fail of the substrate 12 is determined by comparing this ratio with a reference value (for example, 0.3). Thereby, it is possible to appropriately determine the substrate 12 in which the magnetic anisotropy in the circumferential direction of the substrate hardly occurs in the magnetic layer formed on the main surface. Therefore, according to Example 1, the surface shape of the substrate 12 can be appropriately evaluated.

また、実施例1の基板12上に軟磁性層14を形成して、軟磁性層の磁気的異方性を測定したところ、半径方向に配向していた。そのため、判定段階S208で合格と判定された基板12を用いることにより、基板の円周方向の磁気的異方性を適切に制御できることも確認できた。   Further, when the soft magnetic layer 14 was formed on the substrate 12 of Example 1 and the magnetic anisotropy of the soft magnetic layer was measured, it was oriented in the radial direction. For this reason, it was confirmed that the magnetic anisotropy in the circumferential direction of the substrate can be appropriately controlled by using the substrate 12 determined to be acceptable in the determination step S208.

以上、本発明を実施形態を用いて説明したが、本発明の技術的範囲は上記実施形態に記載の範囲には限定されない。上記実施形態に、多様な変更又は改良を加えることが可能であることが当業者に明らかである。その様な変更又は改良を加えた形態も本発明の技術的範囲に含まれ得ることが、特許請求の範囲の記載から明らかである。   As mentioned above, although this invention was demonstrated using embodiment, the technical scope of this invention is not limited to the range as described in the said embodiment. It will be apparent to those skilled in the art that various modifications or improvements can be added to the above embodiment. It is apparent from the description of the scope of claims that embodiments with such changes or improvements can be included in the technical scope of the present invention.

本発明は、例えば垂直磁気記録媒体用基板に好適に用いることができる。   The present invention can be suitably used, for example, for a perpendicular magnetic recording medium substrate.

本発明の一実施形態に係る垂直磁気記録媒体10の構成の一例を示す断面図である。1 is a cross-sectional view showing an example of the configuration of a perpendicular magnetic recording medium 10 according to an embodiment of the present invention. 基板12の製造方法の一例を示すフローチャートである。5 is a flowchart showing an example of a method for manufacturing the substrate 12. 実施例1に係る基板12に対するフーリエ変換の結果を示すグラフである。6 is a graph showing the result of Fourier transform on the substrate 12 according to Example 1;

10・・・垂直磁気記録媒体、12・・・基板、14・・・軟磁性層、16・・・磁気記録層 DESCRIPTION OF SYMBOLS 10 ... Perpendicular magnetic recording medium, 12 ... Substrate, 14 ... Soft magnetic layer, 16 ... Magnetic recording layer

Claims (5)

垂直磁気記録方式で情報を記録する垂直磁気記録媒体の製造に用いられる垂直磁気記録媒体用基板であって、
主表面が研磨された円盤状の基板であって、
主表面にテクスチャが形成されておらず、
前記基板の主表面の断面形状を測定し、測定した前記断面形状の波形をフーリエ変換することにより、前記主表面の断面形状の波形を波長と強度との関係に変換して、フーリエ変換により得られた前記波長と強度との関係に基づき、測定された全範囲の波長の範囲について前記強度を積分した値である全範囲積分値と、予め設定された波長の範囲について前記強度を積分した値である設定範囲積分値とを算出した場合に、前記全範囲積分値に対する前記設定範囲積分値の比が、0.3以下であり、
前記全範囲の波長は、4nm以上、125nm未満の範囲の波長であり、
前記設定範囲積分値を算出する前記波長の範囲は、8〜24nmの波長範囲であることを特徴とする垂直磁気記録媒体用基板。
A perpendicular magnetic recording medium substrate used for manufacturing a perpendicular magnetic recording medium for recording information by a perpendicular magnetic recording method,
A disk-shaped substrate whose main surface is polished,
No texture is formed on the main surface,
The cross-sectional shape of the main surface of the substrate is measured, and the waveform of the cross-sectional shape thus measured is Fourier transformed to convert the waveform of the cross-sectional shape of the main surface into a relationship between wavelength and intensity, and obtained by Fourier transform. Based on the relationship between the measured wavelength and intensity, an integrated value of the entire range, which is a value obtained by integrating the intensity with respect to the measured wavelength range, and a value obtained by integrating the intensity with respect to a preset wavelength range. When the set range integral value is calculated, the ratio of the set range integral value to the total range integral value is 0.3 or less,
The wavelength of the entire range is a wavelength in the range of 4 nm or more and less than 125 nm,
The perpendicular magnetic recording medium substrate according to claim 1, wherein the wavelength range for calculating the set range integral value is a wavelength range of 8 to 24 nm.
軟磁性層を有する垂直磁気記録媒体の製造に用いられることを特徴とする請求項に記載の垂直磁気記録媒体用基板。 The perpendicular magnetic recording medium substrate according to claim 1 , wherein the perpendicular magnetic recording medium substrate is used for manufacturing a perpendicular magnetic recording medium having a soft magnetic layer. 前記基板の材料はガラスであることを特徴とする請求項1または2に記載の垂直磁気記録媒体用基板。 The perpendicular magnetic recording medium substrate according to claim 1 or 2, wherein the material of said substrate is glass. 前記ガラスは、アモルファスのアルミノシリケートガラスであることを特徴とする請求項に記載の垂直磁気記録媒体用基板。 4. The perpendicular magnetic recording medium substrate according to claim 3 , wherein the glass is amorphous aluminosilicate glass. 請求項1からのいずれかに記載の垂直磁気記録媒体用基板上に、少なくとも磁性層を形成したことを特徴とする磁気記録媒体。 On the substrate for a perpendicular magnetic recording medium according to any one of claims 1 to 4, a magnetic recording medium characterized by forming at least a magnetic layer.
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