使用代数拓方法对地质样本内部3D结构的定量描述
Mikhail Chernyavskiy1, Vasilii Timoshenko1, Andrey Morkovkin2
1Faculty of Physics, Lomonosov Moscow State University, 1-2 Leninskie Gory, Moscow, Russia, 119991.
Scientific reports
|July 2, 2025
概括
本研究介绍了一种使用积分几何学和代数拓学分析地质样本纹理的定量方法. 这种方法提供了内部空间结构的精确表征,以改善分类和分析.
科学领域:
- 地质地质地质地质地质地
- 材料科学 材料科学 材料科学
- 计算几何学的计算几何学
背景情况:
- 地质样本形态学的定性描述缺乏准确性和细节性.
- 需要使用定量方法来进行紧,可比,物理信息丰富的样本表征.
- 积分几何学和代数拓学为分析复杂的空间结构提供了强大的工具.
研究的目的:
- 开发一种定量方法来表征地质样本的内部空间结构和纹理.
- 应用积分几何和代数拓来详细分析岩石样本中的X射线密度相.
- 创建基于整体几何特征的地质样本阶段的分类器.
主要方法:
- 地质样品的细分成X射线密度阶段.
- 整体几何学的应用用于定量特征提取.
- 利用代数拓学进行细分阶段的结构分析.
- 基于整体几何特征的分类器的开发.
主要成果:
- 开发了一种新的方法,用于在地质样本中定量表征空间结构和纹理.
- 一个X射线密度相的分类器表现出稳定的运行.
- 对代数拓学特征的详细分析提供了具有地质意义的解释.
- 这种方法在一个meimechite样本上成功地被证明.
结论:
- 开发的方法可以在地质样本中准确,定量地描述内部空间结构.
- 这种方法允许根据样品的纹理对样品进行分类和比较.
- 这种方法广泛适用于各种科学领域的自然和合成物质,甚至财产分布.
关键词:
岩石的特征 岩石的特征整体几何学的整体几何学.这就是Meimechit的意思.明科夫斯基函数的函数多个Otsu细分的细分.贝蒂的数字是贝蒂数字.康托泽罗山脉是一个巨大的山脉.这是一个X-μCTCT.更多相关视频
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