使用微CTCT评估石膏岩碎片的孔裂微结构
Filip Košek1, Jan Dudák2, Veronika Tymlová2
1Institute of Geochemistry, Mineralogy, and Mineral Resources, Faculty of Science, Charles University, Albertov 6, Prague 128 00, Czech Republic.
概括
射线微型计算机断层扫描 (micro-CT) 揭示了经过气候变化的石膏岩石的内部孔隙断裂微观结构. 这种方法有效地量化了多孔性,并对内分泌生物体的微生态环境进行了描述.
科学领域:
- 地质科学 地质科学
- 地质生物学 地质生物学
- 微生物学 微生物学
背景情况:
- 经过气候变化的石膏岩石为内石生物提供了必不可少的息地.
- 了解这些岩石的内部微观结构对于描述这些息地至关重要.
研究的目的:
- 通过使用X射线微型计算机断层扫描 (微型CT) 来研究经过气候变化的石膏岩石的孔裂微结构.
- 为了估计多孔性和量化比较不同石膏样本的微观结构特征.
- 评估微CT适合在地生物学和微生物学中对石化息地进行表征的适用性.
主要方法:
- 使用X射线微型计算机断层扫描 (micro-CT) 来绘制化石膏岩样本的图像.
- 在Dragonfly软件中使用U-Net模型进行深度学习细分,用于识别和可视化多孔系统.
- 对空隙空间,毛孔网络和毛孔大小分布进行了定量分析.
主要成果:
- 微型CT显示了各种各样的石膏微型结构,包括空洞,骨折和二次气候特征.
- 该研究成功量化了多孔性,并描述了负责多孔空间的微观结构.
- 与侵入孔径测试的比较表明微CT在检测较大的孔径 (> 10μm) 中的有效性.
结论:
- 射线微型计算机断层扫描是一种有效的工具,用于检查化石膏岩石的内部微观结构.
- 这些发现对在地生物学和微生物学中对石质息地进行表征具有有希望的意义.
- 微CT提供了关于孔腔网络发展和潜在内皮质基质内连接的宝贵见解.
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