利用弗里德尔对来解释复杂地质材料的扫描3DXRD数据.
Jean-Baptiste Jacob1, Jonathan Wright2, Benoît Cordonnier2
1The Njord Centre, Departments of Geosciences and Physics University of Oslo Norway.
概括
这项研究提出了一个新的处理策略,用于同步扫描3D X射线衍射 (s3DXRD) 数据的同步扫描. 该方法准确地定位大,变形材料中的衍射事件,揭示内部结构和矿物成分.
科学领域:
- 材料科学 材料科学 材料科学
- 地质地质地质地质地质地
- 晶体学 晶体学是指结晶学.
背景情况:
- 使用s3DXRD数据处理大型,高度变形的多相材料面临重大挑战.
- 准确地描述内部结构和矿物成分对于理解材料的行为至关重要.
研究的目的:
- 为s3DXRD数据引入一种新的处理策略.
- 为了能够精确地定位衍射事件和详细的谷内分析.
- 为了应对分析大,变形,多相材料的挑战.
主要方法:
- 利用弗里德尔对 (对称布拉格反射) 来精确定位衍射事件.
- 在大型数据集 (高达10^8峰值) 中开发新模块,以实现高效的弗里德尔对匹配.
- 在voxel网格上实现相位分配和晶体方向和单元细胞参数的局部拟合.
主要成果:
- 在破碎的花岩样本和合金密封件上成功演示了该技术.
- 描述了复杂的地质材料,揭示了内部结构和矿物成分.
- 在高度变形的材料中恢复了内部纹理和残余应变信息.
结论:
- 开发的处理策略有效地处理大型,复杂的s3DXRD数据集.
- 该方法可以进行详细的谷内分析和准确的材料表征.
- 这种技术对于研究晶体岩石和其他高度变形材料的内部结构和变形非常有价值.
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