扫描磁显微镜使用高灵敏度室温道磁阻传感器用于地质应用
Hirokuni Oda1, Kosuke Fujiwara2, Naoto Fukuyo1,3
1Research Institute of Geology and Geoinformation, Geological Survey of Japan (GSJ), National Institute of Advanced Industrial Science and Technology (AIST), Central 7, 1-1-1 Higashi, Tsukuba 305-8567, Ibaraki, Japan.
高灵敏道磁电阻 (TMR) 装置使地质样品的先进磁显微镜成为可能. 这些室温传感器与扫描SQUID显微镜相比,提供更高的性能,用于详细的磁图像.
科学领域:
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
- 显微镜的使用方法
背景情况:
- 磁显微镜对于分析地质薄片至关重要.
- 室温磁传感器比冷系统具有潜在的优势.
- 道磁阻 (TMR) 装置对磁场检测具有很高的灵敏度.
研究的目的:
- 使用高灵敏度室温TMR设备报告磁显微镜.
- 为了评估TMR传感器对薄地质段的性能.
- 将TMR传感器结果与扫描SQUID显微镜 (SSM) 数据进行比较.
主要方法:
- 使用高灵敏度室温TMR设备进行磁性成像.
- 获得了垂直磁化玄武岩薄部分的磁图像.
- 配置的TMR传感器与X和Y轴平行,起飞距离不同.
- 使用磁点源进行传感器评估和与SSM进行比较.
主要成果:
- TMR传感器提供了地质薄段的详细磁图.
- 在高空间分辨率区域观察到TMR和SSM之间的轻微差异.
- 与SSM相比,TMR传感器的测量显示了显著更大的峰值磁场,磁时刻和双极倾斜.
- 半最大全宽度 (FWHM) 在两种传感器类型的起飞时线性增加.
结论:
- 高灵敏度TMR设备适用于地质样品的磁显微镜.
- 与SSM相比,TMR传感器显示出与SSM相比增强磁性表征的潜力.
- 差异可能源于TMR传感器的垂直活性区域,噪音和漂移.
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