3D CSEM modeling and time-lapse sensitivity analysis for subsurface CO2 storage

Author:

Bhuyian Anwar H.1,Landrø Martin1,Johansen Ståle E.1

Affiliation:

1. Norwegian University of Science and Technology, Department of Petroleum Engineering and Applied Geophysics, Trondheim, Norway..

Abstract

Monitoring a time-lapse geophysical anomaly due to variation in the pore-fluid contents of a subsurface reservoir is critical for further development and management. However, it may be difficult to detect the changes in P-wave responses beyond a certain level of saturation. A comprehensive 3D finite-difference time domain (FDTD) forward modeling, based on idealized subsurface resistivity structures, demonstrates the possibility of marine controlled-source electromagnetic (CSEM) surveying to monitor the movement of subsurface [Formula: see text] storage. We focused on CSEM sensitivity studies with respect to variations in geometry and/or saturation of [Formula: see text] storage, evaluation of the effects of reservoir depths and lithology, and detection of [Formula: see text] leakage from the main storage. A 100% lateral expansion from the initial diameter (1500 m) of a typical [Formula: see text] plume with thickness and resistivity of 100 m and 80 Ωm, respectively, at 850 m below seafloor, results in 41% electric field (E-field) magnitude increase at 2500 m source-receiver offset for 0.5 Hz source frequency. In comparison, a 300% vertical expansion of a 50 m thick plume with diameter and resistivity of 2500 m and 80 Ωm, respectively, gives only a 7% E-field magnitude anomaly. An increase of the aspect ratio of a [Formula: see text] plume with diameter and thickness of 1750 and 130 m, respectively, by 110%, without volumetric change, results in a 20% E-field magnitude increase. The E-field magnitude differences due to [Formula: see text] saturation change by 20% in clay-rich (10% clay) and clean reservoirs are almost identical; thus, a time-lapse anomaly in a clay-rich reservoir might be detectable. A gradual inverse variation of offset and frequency can differentiate the responses of a 50 m thick shallow [Formula: see text] accumulation, 200 m below the seafloor, from the main [Formula: see text] plume at 850 m below the seafloor and allow for early warning of [Formula: see text] leakage.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3