Abstract

Direct numerical simulation and pore-network modeling are common approaches to study the physics of two-phase flow through natural rocks. For assessment of the long-term performance of geological sequestration of CO2, it is important to model the full drainage-imbibition cycle to provide an accurate estimate of the trapped CO2. While direct numerical simulation using pore geometry from micro-CT rock images accurately models two-phase flow physics, it is computationally prohibitive for large rock volumes. On the other hand, pore-network modeling on networks extracted from micro-CT rock images is computationally efficient but utilizes simplified physics in idealized geometric pore elements. This study uses the lattice-Boltzmann method for direct numerical simulation of CO2-brine flow in idealized pore elements to develop a new set of pore-level flow models for the pore-body filling and snap-off events in pore-network modeling of imbibition. Lattice-Boltzmann simulations are conducted on typical idealized pore-network configurations, and the interface evolution and local capillary pressure are evaluated to develop modified equations of local threshold capillary pressure of pore elements as a function of shape factor and other geometrical parameters. The modified equations are then incorporated into a quasi-static pore-network flow solver. The modified model is applied on extracted pore-network of sandstone samples, and saturation of residual trapped CO2 is computed for a drainage-imbibition cycle. The modified model yields different statistics of pore-level events compared with the original model; in particular, the occurrence of snap-off in pore-throats is reduced resulting in a more frontal displacement pattern along the main injection direction. Compared to the original model, the modified model is in closer agreement with the residual trapped CO2 obtained from core flow experiments and direct numerical simulation.

Highlights

  • Physics of two-phase flows in natural rocks plays an important role in addressing many current issues in subsurface water and energy resource assessment

  • We aim to apply Direct numerical simulation (DNS) of two-phase flow using the LB code developed by Chen et al (2018) on pore elements of PNs extracted from natural rocks to assess the physical assumptions used for pore-level events during imbibition

  • It is standard practice in LB simulation to use dimensionless parameters normalized with lattice units and convert to physical units when needed

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Summary

Introduction

Physics of two-phase flows in natural rocks plays an important role in addressing many current issues in subsurface water and energy resource assessment. Recent advances in X-ray computed tomography (CT) scanning has provided high resolution images needed to reconstruct the 3D pore structure of rock. This non-destructive technology is able to produce images of pore space and fluids in real rocks at micron resolution for larger rock samples compared to its early days (Andrä et al, 2013; Blunt et al, 2013; Wildenschild and Sheppard, 2013; Schlüter et al, 2014; Bultreys et al, 2016; Balcewicz et al, 2021). PN modeling extracts a simplified network of pore elements from the real geometry of pore spaces and solves the Navier-Stokes equations in the simplified geometry

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