MFM analysis of magnetic inhomogeneity in recorded area for perpendicular magnetic recording media by simultaneous imaging of perpendicular and in-plane magnetic field gradient
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作者:
Yoshimura, Satoru
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Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, JapanAkita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Yoshimura, Satoru
[1
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Egawa, Genta
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Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, JapanAkita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Egawa, Genta
[1
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Miyazawa, Tasuku
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Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, JapanAkita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Miyazawa, Tasuku
[1
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Li, Zhenghua
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Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, JapanAkita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Li, Zhenghua
[1
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Saito, Hitoshi
[1
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Bai, Jianmin
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机构:Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Bai, Jianmin
Li, Guoqing
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机构:Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
Li, Guoqing
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[1] Akita Univ, Ctr Geoenvironm Sci, Fac Engn & Resource Sci, Akita 0108502, Japan
A new MFM method which can measure the perpendicular and in-plane magnetic field gradient simultaneously was developed. The measuring direction of in-plane magnetic field can be easily changed only by selecting the scanning direction of MFM tip with respect to the sample. This method was used to successfully estimate the magnetic domain structure of recorded area on CoCrPt-SiO2 perpendicular magnetic recording media. When the scanning direction is along the down-track direction, the component of strong magnetic field gradient along the down-track direction can be observed with high spatial resolution at the bit transition. On the other hand, when the scanning direction is along the corss-track direction, the new MFM method is effective to mask the component of magnetic field from homogeneous recorded bits, and consequently the components of magnetic field from bended recorded bits at the track edge can be observed. The simultaneous measurement of perpendicular and in-plane magnetic field is useful to evaluate the magnetic inhomogeneity of recorded area such as bit transition and track edge.
机构:
Akita Univ, Venture Business Lab, Akita 0108502, Japan
Lanzhou Univ, Minist Educ, Key Lab Magnetism & Magnet Mat, Lanzhou 730000, Peoples R ChinaAkita Univ, Venture Business Lab, Akita 0108502, Japan
Li, Zhenghua
Egawa, Genta
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Akita Univ, Grad Sch Engn & Resource Sci, Ctr Geoenvironm Sci, Akita 0108502, JapanAkita Univ, Venture Business Lab, Akita 0108502, Japan
Egawa, Genta
Yoshimura, Satoru
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Akita Univ, Grad Sch Engn & Resource Sci, Ctr Geoenvironm Sci, Akita 0108502, JapanAkita Univ, Venture Business Lab, Akita 0108502, Japan
Yoshimura, Satoru
Li, Guoqing
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S Western Univ, Sch Phys Sci & Technol, Chongqing 400715, Peoples R ChinaAkita Univ, Venture Business Lab, Akita 0108502, Japan
Li, Guoqing
Asano, Hidefumi
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Nagoya Univ, Grad Sch Engn, Dept Crystalline Mat Sci, Chikusa Ku, Nagoya, Aichi 4648603, JapanAkita Univ, Venture Business Lab, Akita 0108502, Japan
Asano, Hidefumi
Saito, Hitoshi
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Akita Univ, Grad Sch Engn & Resource Sci, Ctr Geoenvironm Sci, Akita 0108502, JapanAkita Univ, Venture Business Lab, Akita 0108502, Japan