多孔介质
消散
流离失所(心理学)
机械
跳跃
多孔性
流体力学
磁滞
微模型
级联
比例(比率)
流量(数学)
统计物理学
材料科学
地质学
物理
化学
热力学
岩土工程
心理学
量子力学
色谱法
心理治疗师
作者
Steffen Berg,Holger Ott,Stephan A Klapp,Alex Schwing,R. Neiteler,Niels Brussee,Axel Makurat,L. Leu,Frieder Enzmann,Jens-Oliver Schwarz,Michael Kersten,Sarah Irvine,Marco Stampanoni
标识
DOI:10.1073/pnas.1221373110
摘要
Newly developed high-speed, synchrotron-based X-ray computed microtomography enabled us to directly image pore-scale displacement events in porous rock in real time. Common approaches to modeling macroscopic fluid behavior are phenomenological, have many shortcomings, and lack consistent links to elementary pore-scale displacement processes, such as Haines jumps and snap-off. Unlike the common singular pore jump paradigm based on observations of restricted artificial capillaries, we found that Haines jumps typically cascade through 10–20 geometrically defined pores per event, accounting for 64% of the energy dissipation. Real-time imaging provided a more detailed fundamental understanding of the elementary processes in porous media, such as hysteresis, snap-off, and nonwetting phase entrapment, and it opens the way for a rigorous process for upscaling based on thermodynamic models.
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