微观结构
成岩作用
磁导率
地质学
压实
溶解
碳酸盐岩
矿物学
碳酸盐
数字化
计算
材料科学
岩土工程
计算机科学
复合材料
工程类
冶金
算法
化学工程
膜
生物
计算机视觉
遗传学
作者
Dulcie Head,Tiziana Vanorio
摘要
Abstract Rocks are naturally heterogeneous; two rock samples with identical bulk properties can vary widely in microstructure. Understanding how the microstructure and bulk properties of rocks then evolve during experiments and computations simulating diagenesis is inherently a multiscale problem. The advent of modern 3‐D printing has provided an unprecedented opportunity to link those scales by combining the strengths of digital and experimental rock physics. In this study, we take a computerized tomography‐scanned model of a natural carbonate pore space then iteratively digitally manipulate, 3‐D print, and measure the flow properties in the laboratory. This approach allows us to access multiple scales digitally and experimentally and test hypotheses about how changes in rock microstructure due to compaction and dissolution affect bulk transport properties in a repeatable manner.
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