日本第一个咸水层二氧化碳封存试点项目的经验教训

Z. Xue, T. Matsuoka
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引用次数: 21

摘要

在全球范围内进行二氧化碳地质封存时,需要回答几个关键问题。二氧化碳应该如何储存在地下?是否可以假设在含盐地层中捕获二氧化碳?是否可以将二氧化碳长期安全地保留在地下?日本在长冈进行的第一个试点规模的二氧化碳封存项目就是为了回答这些问题。注入地点位于东京以北200公里的长冈市的南长冈天然气田。超临界二氧化碳被注入岸上1100米深的含盐含水层。在18个月的时间里,二氧化碳以每天20至40吨的速度注入,累计注入量为10,400吨。通过时移测井、井间地震层析成像、三维地震测量和地层流体采样等一系列监测活动,成功监测了砂岩储层中的CO2运动。本文概述了从现场和实验室研究中获得的结果,以检查CO2在储层中的时空分布和各种捕获机制。通过电阻率、声波纵波速度和中子孔隙度的变化,3口观测井中有2口的CO2突破得到了清晰的识别。井间地震层析成像得到的速度差层析图显示,注入井周围有明显的异常区域。在前两次监测中,随着注入CO2量的增加,低速带沿地层上倾方向优先扩展,在后续监测中,低速带在含CO2带周围的变化较小。不幸的是,由于二氧化碳注入,三维地震结果没有明显变化。这个试点规模的项目表明,可以将二氧化碳注入深盐水含水层,而不会对健康、安全或环境产生不利影响。长冈项目还为开发经济上可行、环境上有效的减少日本碳排放的方案提供了独特的数据。
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Lessons from the First Japanese Pilot Project on Saline Aquifer CO2 Storage
Several key questions need to be answered when CO2 geological storage is to be undertaken worldwide. How should CO2 be stored underground? Can trapping be assumed in saline formations and can CO2 be retained for long periods safely in the subsurface? The first Japanese pilot-scale CO2 sequestration project in Nagaoka was undertaken to provide answers to these questions. The injection site is located at the Minami-Nagaoka gas field in Nagaoka City, 200km north of Tokyo. Supercritical CO2 was injected into an onshore saline aquifer at a depth of 1,100m. CO2 was injected at a rate of 20 to 40 tonnes per day over an 18-month period, with a cumulative amount of 10,400 tonnes. A series of monitoring activities, which consisted of time-lapse well logging, crosswell seismic tomography, 3D seismic survey and formation fluid sampling, was carried out successfully to monitor CO2 movement in the sandstone reservoir. This paper presents an overview of the results obtained from both field and laboratory studies to examine the spatial-time distribution of CO2 and various trapping mechanisms in the reservoir. CO2 breakthrough at two of the three observation wells was clearly identified by changes in resistivity, sonic P-wave velocity and neutron porosity from time-lapse well logging. Each velocity difference tomogram obtained by crosswell seismic tomography showed a striking anomaly area around the injection well. As the amount of injected CO2 increased, the low-velocity zone expanded preferentially along the formation up-dip direction during the first two monitoring surveys and less change around the CO2-bearing zone could be confirmed from the following surveys. Unfortunately there was no significant change in 3D seismic results due to CO2 injection. The pilot-scale project demonstrated that CO2 can be injected into a deep saline aquifer without adverse health, safety or environmental effects. The Nagaoka project also provides unique data to develop economically viable, environmentally effective options for reducing carbon emissions in Japan.
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