A New Modelling Approach to Simulate CO2 Movement and Containment Coupled With Geochemical Reactions and Geomechanical Effects for an Offshore CO2 Storage in Malaysia

W. Yong, A. I. Azahree, S. S. Ali, F. Azuddin, S. M. Amin
{"title":"A New Modelling Approach to Simulate CO2 Movement and Containment Coupled With Geochemical Reactions and Geomechanical Effects for an Offshore CO2 Storage in Malaysia","authors":"W. Yong, A. I. Azahree, S. S. Ali, F. Azuddin, S. M. Amin","doi":"10.2118/195432-MS","DOIUrl":null,"url":null,"abstract":"\n This paper presents a two-way coupled modelling approach to simulate CO2 movement and containment with geochemical reactions and geomechanical effects. CO2storage simulation studies cover three main disciplines, reservoir engineering, geochemistry and geomechanics. This new approach of coupled modelling simulation, by simultaneously simulate both effects of geochemistry and geomechanics, is considered as a more representative and better predictive modelling practice.\n The integration of geochemistry and geomechanics effects is important for CO2 sequestration modelling. There are a number of published studies on coupled modelling for CO2 storage. However, the majority of the studies has only covered dynamic-geomechanics or dynamic-geochemistry interaction, without considering any direct geomechanics-geochemistry interaction in a reservoir condition. It is crucial to understand the integrated effects when injected CO2 dissolves into formation water and interacts with formation rock. Depending on in-situ conditions, the formation water with dissolved CO2 could weak or strengthen the formation stress due to geochemical reactions of formation minerals. Therefore, coupled modelling is needed to ensure the long-term safetyof CO2containment at a CO2 storage site with the interactions among geomechanical, geochemical and dynamic fluid flow, and especially to understand the slow and not experimentally accessible mineral reactions.\n In this paper, a high CO2 content gas field in Malaysia with high temperature (~150°C) and high pressure (~350 bar) has been studied using integrated coupled modelling approach. The simulation input parameters are first investigated and collected from literature and laboratory studies. A two-way coupled modelling simulation with the consideration of geochemistry and geomechanics effects is desirable because it allows the updates of reservoir properties back and forth in every time step. Different CO2trapping mechanisms, long term fate analysis, subsidence and heaving analysis, and changes of porosity and permeability are investigated. The time frame of simulation studies consists of CO2 injection period (15 years) and post CO2 injection period (500 years).\n During the first 15 years of CO2 injection, 95% of injected CO2 is structurally trapped, 4% of CO2is soluted in formation water and 1% is trapped by mineralization. About 0.04m of heaving is observed at the injection area while about 0.05m of subsidence is observed at the production area. In the investigation of long-term CO2fate, it is observed that CO2 gas will be trapped between the lighter hydrocarbon gas layer and aquifer due to density difference.","PeriodicalId":103248,"journal":{"name":"Day 4 Thu, June 06, 2019","volume":"10 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Day 4 Thu, June 06, 2019","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2118/195432-MS","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3

Abstract

This paper presents a two-way coupled modelling approach to simulate CO2 movement and containment with geochemical reactions and geomechanical effects. CO2storage simulation studies cover three main disciplines, reservoir engineering, geochemistry and geomechanics. This new approach of coupled modelling simulation, by simultaneously simulate both effects of geochemistry and geomechanics, is considered as a more representative and better predictive modelling practice. The integration of geochemistry and geomechanics effects is important for CO2 sequestration modelling. There are a number of published studies on coupled modelling for CO2 storage. However, the majority of the studies has only covered dynamic-geomechanics or dynamic-geochemistry interaction, without considering any direct geomechanics-geochemistry interaction in a reservoir condition. It is crucial to understand the integrated effects when injected CO2 dissolves into formation water and interacts with formation rock. Depending on in-situ conditions, the formation water with dissolved CO2 could weak or strengthen the formation stress due to geochemical reactions of formation minerals. Therefore, coupled modelling is needed to ensure the long-term safetyof CO2containment at a CO2 storage site with the interactions among geomechanical, geochemical and dynamic fluid flow, and especially to understand the slow and not experimentally accessible mineral reactions. In this paper, a high CO2 content gas field in Malaysia with high temperature (~150°C) and high pressure (~350 bar) has been studied using integrated coupled modelling approach. The simulation input parameters are first investigated and collected from literature and laboratory studies. A two-way coupled modelling simulation with the consideration of geochemistry and geomechanics effects is desirable because it allows the updates of reservoir properties back and forth in every time step. Different CO2trapping mechanisms, long term fate analysis, subsidence and heaving analysis, and changes of porosity and permeability are investigated. The time frame of simulation studies consists of CO2 injection period (15 years) and post CO2 injection period (500 years). During the first 15 years of CO2 injection, 95% of injected CO2 is structurally trapped, 4% of CO2is soluted in formation water and 1% is trapped by mineralization. About 0.04m of heaving is observed at the injection area while about 0.05m of subsidence is observed at the production area. In the investigation of long-term CO2fate, it is observed that CO2 gas will be trapped between the lighter hydrocarbon gas layer and aquifer due to density difference.
一种新的模拟方法,以模拟二氧化碳的运动和遏制,加上地球化学反应和地质力学效应,为马来西亚的海上二氧化碳储存
本文提出了一种基于地球化学反应和地质力学效应的双向耦合建模方法来模拟CO2的运动和封存。二氧化碳储存模拟研究涵盖三个主要学科:油藏工程、地球化学和地质力学。这种同时模拟地球化学和地质力学效应的耦合建模模拟方法,被认为是一种更有代表性和更好的预测建模方法。地球化学和地质力学效应的整合对于CO2封存模型是重要的。有许多已发表的关于二氧化碳储存的耦合建模的研究。然而,大多数研究只涉及动力-地质力学或动力-地球化学相互作用,而没有考虑储层条件下的直接地质力学-地球化学相互作用。了解注入的CO2溶入地层水并与地层岩石相互作用时的综合效应至关重要。由于地层矿物的地球化学反应,含溶解CO2的地层水可能会减弱或增强地层应力,这取决于原位条件。因此,在地质力学、地球化学和动力流体流动的相互作用下,需要建立耦合模型,以确保CO2储存点CO2封存的长期安全,特别是要了解缓慢且实验上无法获得的矿物反应。本文采用综合耦合建模方法对马来西亚一个高温(~150°C)高压(~350 bar)的高CO2含量气田进行了研究。首先从文献和实验室研究中调查和收集仿真输入参数。考虑地球化学和地质力学影响的双向耦合建模模拟是可取的,因为它允许在每个时间步中来回更新储层性质。研究了不同的co2捕获机制、长期命运分析、沉陷起伏分析以及孔隙度和渗透率的变化。模拟研究的时间框架包括CO2注入期(15年)和CO2注入后期(500年)。在注入二氧化碳的前15年,95%的注入二氧化碳被构造捕获,4%的二氧化碳被地层水溶解,1%的二氧化碳被矿化捕获。注入区隆起约0.04m,采出区下沉约0.05m。在长期CO2fate调查中发现,由于密度差,CO2气体将被困在轻质烃气层和含水层之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信