CO2 Sequestration: Studying Caprock And Fault Sealing Integrity, The CS-D Experiment In Mont Terri

A. Zappone, A. Rinaldi, M. Grab, A. Obermann, M. Claudio, C. Nussbaum, S. Wiemer
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引用次数: 7

Abstract

A key challenge for CO2 geological storage is the integrity of the caprock. This challenge is addressed by executing a decameter-scale experiment at the Mont Terri Underground Rock Laboratory in Switzerland, under the umbrella of ELEGANCY (Enabling a Low-Carbon Economy via Hydrogen and CCS). ELEGANCY is an European project aiming at advance sustainable geo-energy processes through studies on risk mitigation, characterization and public perception, whose achievements will benefit the fields of carbon dixode sequestration. The experiment will investigating the mechanisms and the physical parameters governing the migration of CO2-rich brine through a faults. In particular, the test seeks to understand the conditions for slip activation (seismic vs. aseismic slip) and the stability of clay faults, as well as the coupling between fault slip, pore pressure, fluid migration and possible induced “micro” seismicity. To this end, we will inject CO2-rich brine into the fault core for a period of about eight months, while monitoring its geo-mechanical response. Additional tracer and transmissivity tests will be conducted at regular time intervals to determine the fluid path evolution of the injected fluid and to infer the potential evolution of CO2 from the brine. Numerical simulation work assist the different phases of the field experiment.
二氧化碳封存:盖层与断层封闭性的研究,蒙特特里的CS-D实验
二氧化碳地质储存的一个关键挑战是盖层的完整性。这一挑战是通过在瑞士蒙特特里地下岩石实验室进行的十米尺度的实验来解决的,该实验是在elegance(通过氢和CCS实现低碳经济)的保护下进行的。“优雅”是一个欧洲项目,旨在通过对风险缓解、特征描述和公众认知的研究来推进可持续地能源进程,其成果将有利于二氧化碳封存领域。实验将探讨富co2卤水通过断层运移的机理和物理参数。特别是,该测试旨在了解滑动激活(地震与地震滑动)的条件和粘土断层的稳定性,以及断层滑动、孔隙压力、流体运移和可能诱发的“微”地震活动之间的耦合。为此,我们将向断层核心注入富含co2的盐水,为期8个月左右,同时监测其地球力学响应。额外的示踪剂和透射率测试将在固定的时间间隔进行,以确定注入流体的流体路径演变,并推断盐水中二氧化碳的潜在演变。数值模拟工作辅助了现场试验的不同阶段。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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