新疆准东地区场地尺度二氧化碳地质封存联合深部咸水开采潜力评估

马鑫, 李旭峰, 文冬光, 罗兴旺, 刁玉杰, 杨国栋, 尹书郭, 曹伟. 新疆准东地区场地尺度二氧化碳地质封存联合深部咸水开采潜力评估[J]. 水文地质工程地质, 2021, 48(6): 196-205. doi: 10.16030/j.cnki.issn.1000-3665.20201043
引用本文: 马鑫, 李旭峰, 文冬光, 罗兴旺, 刁玉杰, 杨国栋, 尹书郭, 曹伟. 新疆准东地区场地尺度二氧化碳地质封存联合深部咸水开采潜力评估[J]. 水文地质工程地质, 2021, 48(6): 196-205. doi: 10.16030/j.cnki.issn.1000-3665.20201043
MA Xin, LI Xufeng, WEN Dongguang, LUO Xingwang, DIAO Yujie, YANG Guodong, YIN Shuguo, CAO Wei. A study of the potential of field-scale of CO2 geological storage and enhanced water recovery in the eastern Junggar area of Xinjiang[J]. Hydrogeology & Engineering Geology, 2021, 48(6): 196-205. doi: 10.16030/j.cnki.issn.1000-3665.20201043
Citation: MA Xin, LI Xufeng, WEN Dongguang, LUO Xingwang, DIAO Yujie, YANG Guodong, YIN Shuguo, CAO Wei. A study of the potential of field-scale of CO2 geological storage and enhanced water recovery in the eastern Junggar area of Xinjiang[J]. Hydrogeology & Engineering Geology, 2021, 48(6): 196-205. doi: 10.16030/j.cnki.issn.1000-3665.20201043

新疆准东地区场地尺度二氧化碳地质封存联合深部咸水开采潜力评估

  • 基金项目: 国家重点研发计划项目(2019YFE0100100);国家自然科学基金项目(41702284;41602272);中国地质调查局地质调查项目(DD20160307);湖北省自然科学基金项目(2019CFB451);冶金矿产资源高效利用与造块湖北省重点实验室开放基金项目(2020zy003)
详细信息
    作者简介: 马鑫(1986-),男,高级工程师,主要从事二氧化碳地质储存与利用技术研究。E-mail:maxin@mail.cgs.gov.cn
    通讯作者: 杨国栋(1986-),男,博士,讲师,主要从事二氧化碳地质储存与资源化利用、土壤与地下水污染调查与修复研究。E-mail:ygdguodong@126.com
  • 中图分类号: P641.5

A study of the potential of field-scale of CO2 geological storage and enhanced water recovery in the eastern Junggar area of Xinjiang

More Information
  • 二氧化碳地质封存联合深部咸水开采技术(CO2-EWR)被认为是有效的碳减排途径之一。在新疆准东地区率先开展CO2-EWR技术,可在实现CO2减排的同时获得咸水,在一定程度上缓解当地的水资源短缺问题,取得环境经济双重效益。以往研究大多以概化模型为主,缺乏工程实践依托,根据准噶尔盆地东部CO2源汇匹配适宜性评价结果,基于我国首个CO2-EWR野外先导性工程试验场地资料,构建拟选CO2-EWR场地西山窑组三维(3D)非均质模型开展了场地尺度CO2-EWR技术潜力研究。研究表明,拟选场地CO2理论封存量为1.72×106(P50)t,动态封存量为2.14×106 t。采用CO2-EWR技术可实现CO2动态封存量11.18×106 t,较单独CO2地质封存提升5.22倍,同时可增采咸水资源10.17×106 t,CO2采水比率为1∶0.91。同时,该技术可有效缓解因CO2大量注入引起的储层压力累积,提高CO2封存效率,增加咸水开采潜力。本研究可为新疆准东地区实施规模化CO2地质封存联合深部咸水开采工程提供理论依据和技术支撑。

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  • 图 1  准噶尔盆地CO2源汇匹配

    Figure 1. 

    图 2  拟选准东CO2-EWR工程场地模型

    Figure 2. 

    图 3  研究区三维静态地质模型

    Figure 3. 

    图 4  情景设置

    Figure 4. 

    图 5  CO2累计注入量与储层平均压力变化

    Figure 5. 

    图 6  单井CO2注入量与整体注入速率的变化

    Figure 6. 

    图 7  气相CO2饱和度空间分布

    Figure 7. 

    图 8  溶解态CO2空间分布

    Figure 8. 

    图 9  方案2中CO2累计注入量与产水量

    Figure 9. 

    图 10  方案1和2中各注入井井底压力

    Figure 10. 

    图 11  CO2累计采出量与采出速率

    Figure 11. 

    图 12  采出CO2与采出咸水体积比(1 bar,25 ℃)

    Figure 12. 

    表 1  基于静态地质建模的CO2埋存量

    Table 1.  CO2 storage capacity from static geological modeling

    计算参数P10P50P90
    封存系数/%[32]1.22.44.1
    封存体积/(106 m31.222.434.16
    封存质量/(106 t)0.861.722.94
      注:基于蒙特卡罗模型计算的深部咸水层CO2有效封存系数可信度为90%时定义为P10,CO2有效封存系数可信度为50%时定义为P50,CO2有效封存系数可信度为10%时定义为P90。不同的可信度对应不同的CO2有效封存系数。
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出版历程
收稿日期:  2020-10-05
修回日期:  2021-01-14
刊出日期:  2021-11-15

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