A reactive transport model for geochemical mitigation of CO2 leaking into a confined aquifer

被引:6
|
作者
Druhan, Jennifer L. [1 ]
Vialle, Stephanie [1 ]
Maher, Kate [1 ]
Benson, Sally [2 ]
机构
[1] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA
[2] Stanford Univ, Dept Energy Resources Engn, Stanford, CA 94305 USA
来源
12TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES, GHGT-12 | 2014年 / 63卷
关键词
CO2; storage; caprock defect; sealant; reactive transport; WATER-ROCK INTERACTIONS; DEEP SALINE; FRIO-FORMATION; STORAGE; SEQUESTRATION; LEAKAGE; TEXAS; INTRUSION; IMPACTS; CEMENT;
D O I
10.1016/j.egypro.2014.11.495
中图分类号
O69 [应用化学];
学科分类号
081704 ;
摘要
Long-term storage of anthropogenic CO2 in the subsurface generally assumes that caprock formations will serve as physical barriers to upward migration of CO2. However, as a precaution and to provide assurances to regulators and the public, monitoring is used detect any unexpected leakage from the storage reservoir. If a leak is found, the ability to rapidly deploy mitigation measures is needed. Here we use the TOUGHREACT code to develop a series of two-dimensional reactive transport simulations of the hydrogeochemical characteristics of a newly formed CO2 leak into an overlying aquifer. Using this model, we consider: (1) geochemical shifts in formation water indicative of a leak; (2) hydrodynamics of pumping wells in the vicinity of a leak; and (3) delivery of a sealant to a leak through an adjacent well bore. Our results demonstrate that characteristic shifts in pH and dissolved inorganic carbon can be detected in the aquifer prior to the breakthrough of supercritical CO2, and could offer a potential means of identifying small and newly formed leaks. Pumping water into the aquifer in the vicinity of the leak provides a hydrodynamic control that can temporarily mitigate the flux rate of CO2 and facilitate delivery of a sealant to the location of the caprock defect. Injection of a fluid-phase sealant through the pumping well is demonstrated by introduction of a silica-bearing alkaline flood, resulting in precipitation of amorphous silica in areas of neutral to acidic pH. Results show that a decrease in permeability of several orders of magnitude can be achieved with a high molar volume sealant, such that CO2 flux rate is decreased. However, individual simulation results are highly contingent upon both the properties of the sealant, the porosity-permeability relationship employed in the model, and the relative flux rates of CO2 and alkaline flood introduced into the aquifer. These conclusions highlight the need for both experimental data and controlled field tests to constrain modelling predictions. (C) 2014 The Authors. Published by Elsevier Ltd.
引用
收藏
页码:4620 / 4629
页数:10
相关论文
共 50 条
  • [1] Geochemical assessment of CO2 perturbation in a shallow aquifer evaluated by a push-pull field experiment
    Rillard, Jean
    Gombert, Philippe
    Toulhoat, Pierre
    Zuddas, Pierpaolo
    INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2014, 21 : 23 - 32
  • [2] Merits of pressure and geochemical data as indicators of CO2/brine leakage into a heterogeneous, sedimentary aquifer
    Trainor-Guitton, Whitney
    Mansoor, Kayyum
    Sun, Yunwei
    Carroll, Susan
    INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2016, 52 : 237 - 249
  • [3] Intrusion of CO2 and impurities in a freshwater aquifer - impact evaluation by reactive transport modelling
    Jacquemet, Nicolas
    Picot-Colbeaux, Geraldine
    Chan Quang Vong
    Lions, Julie
    Bouc, Olivier
    Jeremy, Rohmer
    10TH INTERNATIONAL CONFERENCE ON GREENHOUSE GAS CONTROL TECHNOLOGIES, 2011, 4 : 3202 - 3209
  • [4] Well-based, geochemical leakage monitoring of an aquifer immediately above a CO2 storage reservoir by stable carbon isotopes at the Ketzin pilot site, Germany
    Nowak, Martin
    Myrttinen, Anssi
    Zimmer, Martin
    Wiese, Bernd
    van Geldern, Robert
    Barth, Johannes A. C.
    EUROPEAN GEOSCIENCES UNION GENERAL ASSEMBLY 2013, EGUDIVISION ENERGY, RESOURCES & THE ENVIRONMENT, ERE, 2013, 40 : 346 - 354
  • [5] Reactive transport simulation study of geochemical CO2 trapping on the Tokyo Bay model - With focus on the behavior of dawsonite
    Okuyama, Yasuko
    Todaka, Norifumi
    Sasaki, Munetake
    Ajima, Shuji
    Akasaka, Chitoshi
    APPLIED GEOCHEMISTRY, 2013, 30 : 57 - 66
  • [6] Reactive transport modeling of leaking CO2-saturated brine along a fractured pathway
    Ahmad, Nawaz
    Worman, Anders
    Bottacin-Busolin, Andrea
    Sanchez-Vila, Xavier
    INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2015, 42 : 672 - 689
  • [7] Impact of rock mineralogy on reactive transport of CO2 during carbon sequestration in a saline aquifer
    Rezk, Mohamed Gamal
    Ibrahim, Ahmed Farid
    JOURNAL OF PETROLEUM EXPLORATION AND PRODUCTION TECHNOLOGY, 2025, 15 (01)
  • [8] Coupled geomechanical and reactive geochemical model for fluid, heat flow and convective mixing: application for CO2 geological sequestration into saline aquifer with heterogeneity
    Zhang, Ronglei
    Winterfeld, Philip H.
    Yin, Xiaolong
    Wu, Yu-Shu
    Xiong, Yi
    INTERNATIONAL JOURNAL OF GLOBAL WARMING, 2017, 13 (02) : 197 - 236
  • [9] Geochemical impacts of leaking CO2 from subsurface storage reservoirs to an unconfined oxidizing carbonate aquifer
    Wang, Guohui
    Qafoku, Nikolla P.
    Lawter, Amanda R.
    Bowden, Mark
    Harvey, Omar
    Sullivan, Charlotte
    Brown, Christopher F.
    INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2016, 44 : 310 - 322
  • [10] Reactive transport LBM model for CO2 injection in fractured reservoirs
    Tian, Zhiwei
    Xing, Huilin
    Tan, Yunliang
    Gu, Sai
    Golding, Suzanne D.
    COMPUTERS & GEOSCIENCES, 2016, 86 : 15 - 22