通过扫描电子显微镜评估页岩中的孔隙性的相对方法
Federico Medina1, Ignacio Jausoro1, María Alejandra Floridia Addato1
1YPF Tecnología S.A., Av. del Petróleo s/n entre 129 y 143, Berisso 1925, Buenos Aires, Argentina.
概括
这项研究引入了使用场辐射扫描电子显微镜 (FESEM) 的相关方法,以准确地测量大面积的纳米级毛孔性. 该方法通过分析多个图像尺度来增强代表性,揭示毛孔大小分布和裂存在.
科学领域:
- 地质学和材料科学 地质学和材料科学
- 纳米技术和显微镜学
背景情况:
- 场发射扫描电子显微镜 (FESEM) 提供了高分辨率,但在分析大样本区域以代表孔隙性方面是有限的.
- 精确的纳米级孔隙性评估对于理解材料特性和地质构造至关重要.
研究的目的:
- 开发和验证一种相关成像策略,用于计算大样本面积 (高达3毫米×3毫米) 的纳米尺度孔隙.
- 在分析较大的样本量时克服FESEM的代表性限制.
主要方法:
- 采用多尺度成像方法,从一个大面积 (3毫米×3毫米) 开始,逐渐选择较小的感兴趣区域 (ROI) (600微米×600微米,然后150微米×150微米).
- 图像根据矿物学和有机物质含量相关联,以将不同分辨率的孔径大小信息联系起来.
- 累积的多孔度图和毛孔大小分布函数被用于分析.
主要成果:
- 相关方法成功计算了大面积的纳米级孔隙性,提高了代表性.
- 累积毛孔图有效地显示了不同毛孔大小的贡献,并使裂检测成为可能.
- 在研究条件下计数小孔的实际极限被确定为大约30-40纳米.
结论:
- 提出的相关方法提供了一种高效的计算方法,用于在宏观尺度上对纳米尺度的孔隙性进行评估.
- 这种技术通过解决其固有的面积限制,提高了基于FESEM的孔径分析的可靠性.
- 这些发现提供了有关毛孔尺寸分布和检测极限的见解,这些都与材料特性有关.
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