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REACTIVE TRANSPORT: EXPERIMENTS AND PORE-NETWORK MODELLING

机译:反应运输:实验和孔网建模

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Dissolution and deposition phenomena are key issues in the CO2 geological storage.In the past few years,it has been proven that CO2 injection can lead to important pore structure modifications which mainly depend on the thermodynamic conditions,the rock and fluid composition and the flow regime.Predicting these modifications and their impact on the reservoir permeability and porosity is crucial for the success of CO2 sequestration projects. This paper presents an experimental and numerical study to evaluate in a comprehensive manner the impact of the deposition regimes on the relationships between permeability and porosity.Experiments have been performed in glass micromodels to visualize deposition mechanisms for different regimes.A reactive transport model using the porenetwork approach has been developed to simulate the deposition phenomenon in the case of a single-phase flow.This numerical model is based on solving the macroscopic convection-diffusion equation.Its macroscopic coefficients,mean velocity,dispersion coefficient and apparent reaction term,are obtained for each unit cell of the pore network by solving analytically a set of equations describing the reactive transport at microscopic scale.The regimes that govern the deposition phenomena are numerically investigated.It is demonstrated that deposition patterns depend on both scales of the reactive transport, microscopic and macroscopic,each one being characterized by relevant dimensionless numbers.
机译:溶解和沉积现象是CO2地质储存的关键问题。过去几年,已证明二氧化碳注射会导致重要的孔隙结构改性,主要取决于热力学条件,岩石和流体组成和流动制度。预测这些修改及其对储层渗透性和孔隙度的影响对于CO2封存项目的成功至关重要。本文提出了一种实验和数值研究,以全面的方式评估沉积制度对渗透性和孔隙度之间的关系的影响。已经在玻璃微模中进行了实验,以使不同的制度的沉积机构进行可视化。使用Porenetwork的反应运输模型已经开发了方法以模拟单相流的情况下的沉积现象。该数值模型基于求解宏观对流扩散方程。获得宏观系数,平均速度,分散系数和表观反应术语通过分析地求解孔网络的每个单元电池,所述一组方程描述了微观规模的反应性传输。控制沉积现象的制度在数值上进行了研究。沉积图案依赖于反应性,微观和的两种尺度。宏观,每个人都有特征由相关的无量纲数ZED。

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