日本地球惑星科学連合2015年大会

講演情報

口頭発表

セッション記号 S (固体地球科学) » S-EM 固体地球電磁気学

[S-EM34] 地磁気・古地磁気・岩石磁気

2015年5月24日(日) 10:00 〜 10:45 102A (1F)

コンビーナ:*望月 伸竜(熊本大学大学院先導機構)、松島 政貴(東京工業大学大学院理工学研究科地球惑星科学専攻)、座長:望月 伸竜(熊本大学大学院先導機構)

10:15 〜 10:30

[SEM34-02] 磁性体薄膜ドットを用いたSQUID顕微鏡計測における位置決め手法の提案

*河合 淳1小田 啓邦2宮城 磯治2 (1.金沢工業大学、2.産業技術総合研究所)

キーワード:スクイド顕微鏡, 岩石薄片試料, 位置決め, 磁性ドット, 薄膜

We have developed a scanning superconducting quantum interference device (SQUID) microscope (SSM) for imaging magnetic field distribution of geological rock samples. The rock sample, which is processed into a thin section and glued on a glass with non-magnetic resin, is placed on a XY table under the SQUID microscope, and is scanned. The distance between the SQUID and the sample can be calibrated with magnetic field generated with a dc-current applied to a thin and long wire. However, the position of the sample for the SQUID must be determined in another way. Positioning the magnetic field image for the structure of the sample is necessary for analysis of the magnetic field distribution. We propose a positioning method using a thin-film magnetized circular dot as a magnetic dipole marker.
Considering expected special resolution of about 200 μm or smaller, we designed four kinds of single circular dots with different diameter, which are 10 μm, 50 μm, 75 μm, 100 μm. We adopted FeCo as a material for the dot. A 500-nm-thick FeCo layer was deposited on a silicon substrate with DC-sputtering and was formed into circular dots with lift-off process. After forming the dots, the Si substrate was diced into square chips with the size of 3.5 mm × 3.5 mm, where each chip has a single dot. Scanning the 25-μm dot with the SQUID microscope, we obtained dipole-like field of ~10 nT, which is large enough as a magnetic maker.
We plan to attach this chip with the dot adjacent to the sample on the sample holder. Finally, we can superimpose the magnetic field pattern on an optical image of the sample.