Abstract

Abstract Moisture variation in porous media depends mainly on the pore characteristics. This article used the micro-computed tomography (micro-CT) (a non-destructive imaging technique to generate a three-dimensional virtual model) and the Brooks–Corey model to deduce the moisture migration in sand. Relationship between capillary rise height and time (h–t) was achieved by numerical simulation in the capillary suction process, where the parameters fractal dimension, porosity, and air–water interfacial area were obtained by the micro-CT scanning. Meanwhile, experiments of capillary rise in sand column were performed using four different sizes washed sand, and the capillary heights at different times were recorded. Results show that the capillary suction is decided by the aperture size and phase morphology simultaneously, and particle size has obvious effect on capillarity, and the wetting front lowers with the increase in grain size and the decrease in rising rate. Parameters air entry pressure and pore-size distribution index obtained by micro-CT scanning technology and empirical formula are accurate. Method of combing micro-CT images and Brooks–Corey model can predict well the capillary suction of porous media. It is also proved that the capillary suction is decided by the aperture size and phase morphology simultaneously.

Highlights

  • Moisture variation in porous media depends mainly on the pore characteristics

  • The quantity of macropore increases with the increase in grain diameter (Figure 5), while the fractal dimension decreases with the increase in particle diameter (Table 1)

  • Micro-computed tomography (CT) technology is introduced to predict the capillary suction in porous media like sand

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Summary

Introduction

Abstract: Moisture variation in porous media depends mainly on the pore characteristics. Relationship between capillary rise height and time (h–t) was achieved by numerical simulation in the capillary suction process, where the parameters fractal dimension, porosity, and air–water interfacial area were obtained by the micro-CT scanning. Method of combing micro-CT images and Brooks–Corey model can predict well the capillary suction of porous media. The Washburn equation was used frequently to model the capillary rise in porous media. Prediction of capillary suction in porous media based on micro-CT technology and B–C model 907 or on different kinds of particles. CT technology and Brooks–Corey model are introduced to predict the capillary suction in porous media like sand. The use of micro-scale simulation method could be better to analyze the properties of porous media and the state of internal fluid. When using MRT-LBM for flow simulation, stronger steady-state viscous flow solutions could be generated under a wider range of relaxation parameters (or viscosity settings)

Capillary phenomenon in porous media
Visco-inertial time stage
Purely inertial time stage
Capillary suction modeling
Micro-CT scanning
Constant head permeability test
Capillary absorption test
Simulated results
Conclusion
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