• Effect of permeable and anisotropic coal reservoirs on CO2-ECBM
    編號:186 稿件編號:144 訪問權限:僅限參會人 更新:2022-05-13 17:05:41 瀏覽:397次 口頭報告

    報告開始:2022年05月27日 11:30 (Asia/Shanghai)

    報告時間:10min

    所在會議:[S10] Resource Development and Utilization of Underground Space [S10-2] Resource Development and Utilization of Underground Space-2

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    摘要
    Gas driving water can cause staged inhibition on CH4 production, and reservoir permeability has a critical influence on it. Taking the Shizhuangnan coalbed methane development block in Qinshui Basin as the research background, the impacts of permeability and horizontal anisotropy on CH4 production and CO2 sequestration are simulated numerically and then discussed adequately, and the displacement profile in the processes of gas driving water is analyzed. The results show that the reservoirs with low permeability or weak horizontal anisotropy are harmful to enhancing CBM recovery, but beneficial to CO2 sinking. With the rise of permeability and anisotropy, the hysteresis time and staged inhibition time are observably shortened, and the staged inhibition level is markedly weakened, while the CH4 output and CO2 injection volume are significantly increased. However, high permeability and strong anisotropy easily tend to premature CO2 breakthrough and the producers' shut-off, resulting in cumulative CH4 production, CO2 injection, and storage volume lower than expected. Upregulating the limit of CO2 breakthrough concentration appropriately can effectively ameliorate the situation. Additionally, along the displacement direction, the displacement profile consists of sequential CO2 enriched zone, CO2-CH4 enriched zone, CH4 enriched zone, H2O enriched zone. Ultimately, for field projects, the producers in the dominant seepage direction possess more potential of enhanced recovery in the short term, while those in the inferior seepage direction avoid becoming invalid only if a long-time injection measure is taken into the injectors.
     
    關鍵字
    the staged inhibition, permeability, horizontal anisotropy, dominant seepage direction
    報告人
    Ziliang WANG
    China University of Mining and Technology

    稿件作者
    Ziliang Wang Key Laboratory of Coalbed Methane Resources & Reservior Formation Process, Ministry of Education, and School of Resources and Geosciences, China University of Mining and Technology
    Shuxun Sang Jiangsu Key Laboratory of Coal-Based Greenhouse Gas Control and Utilization, Carbon Neutrality Institute, and School of Resources and Geosciences, China University of Mining and Technology
    Xiaozhi Zhou Key Laboratory of Coalbed Methane Resources & Reservior Formation Process, Ministry of Education, and School of Resources and Geosciences, China University of Mining and Technology
    Xudong Liu Key Laboratory of Coalbed Methane Resources & Reservior Formation Process, Ministry of Education, and School of Resources and Geosciences, China University of Mining and Technology
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