曲折
微尺度化学
水文地质学
多孔介质
磁导率
多孔性
地质学
各向同性
材料科学
岩土工程
微观结构
岩石物理学
相对渗透率
流体力学
机械
矿物学
复合材料
光学
数学
化学
物理
数学教育
膜
生物化学
作者
Philipp Eichheimer,Marcel Thielmann,Wakana Fujita,Gregor J. Golabek,Michihiko Nakamura,Satoshi Okumura,Takayuki Nakatani,Maximilian O. Kottwitz
出处
期刊:Solid Earth
[Copernicus Publications]
日期:2020-06-25
卷期号:11 (3): 1079-1095
被引量:9
标识
DOI:10.5194/se-11-1079-2020
摘要
Abstract. Fluid flow on different scales is of interest for several Earth science disciplines like petrophysics, hydrogeology and volcanology. To parameterize fluid flow in large-scale numerical simulations (e.g. groundwater and volcanic systems), flow properties on the microscale need to be considered. For this purpose experimental and numerical investigations of flow through porous media over a wide range of porosities are necessary. In the present study we sinter glass bead media with various porosities and measure the permeability experimentally. The microstructure, namely effective porosity and effective specific surface, is investigated using image processing. We determine flow properties like tortuosity and permeability using numerical simulations. We test different parameterizations for isotropic low-porosity media on their potential to predict permeability by comparing their estimations to computed and experimentally measured values.
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