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中国南海天然气水合物开采储层水合物相变与渗流机理: 综述与展望

秦绪文, 陆程, 王平康, 梁前勇. 2022. 中国南海天然气水合物开采储层水合物相变与渗流机理: 综述与展望[J]. 中国地质, 49(3): 749-769. doi: 10.12029/gc20220306
引用本文: 秦绪文, 陆程, 王平康, 梁前勇. 2022. 中国南海天然气水合物开采储层水合物相变与渗流机理: 综述与展望[J]. 中国地质, 49(3): 749-769. doi: 10.12029/gc20220306
QIN Xuwen, LU Cheng, WANG Pingkang, LIANG Qianyong. 2022. Hydrate phase transition and seepage mechanism during natural gas hydrate production tests in the South China Sea: A review and prospect[J]. Geology in China, 49(3): 749-769. doi: 10.12029/gc20220306
Citation: QIN Xuwen, LU Cheng, WANG Pingkang, LIANG Qianyong. 2022. Hydrate phase transition and seepage mechanism during natural gas hydrate production tests in the South China Sea: A review and prospect[J]. Geology in China, 49(3): 749-769. doi: 10.12029/gc20220306

中国南海天然气水合物开采储层水合物相变与渗流机理: 综述与展望

  • 基金项目:
    国家自然科学基金重大项目课题(51991365)资助
详细信息
    作者简介: 秦绪文, 男, 1977年, 博士, 研究员, 长期从事海域天然气水合物研究工作; E-mail: qinxuwen@163.com
  • 中图分类号: P744;P618.13

Hydrate phase transition and seepage mechanism during natural gas hydrate production tests in the South China Sea: A review and prospect

  • Fund Project: Supported by the National Natural Science Foundation of China (No.51991365)
More Information
    Author Bio: QIN Xuwen, male, born in 1977, doctor, researcher, engaged in marine gas hydrate research; E-mail: qinxuwen@163.com .
  • 研究目的

    中国地质调查局先后于2017年、2020年在南海北部神狐海域成功实施两轮水合物试采,创造了产气时间最长、产气总量最大、日均产气量最高等多项世界纪录,了解和掌握南海天然气水合物开采储层相变与渗流机理,有助于进一步揭示该类型水合物分解机理、产出规律、增产机制等,可为中国海域水合物资源规模高效开采提供理论基础。

    研究方法

    基于两轮试采实践,笔者通过深入研究发现,储层结构表征、水合物相变、多相渗流与增渗、产能模拟与调控是制约水合物分解产气效率的重要因素。

    研究结果

    研究表明,南海水合物相变具有分解温度低,易在储层内形成二次水合物等特点,是由渗流场-应力场-温度场-化学场共同作用的复杂系统;多相渗流作用主要受控于未固结储层的物性特征、水合物相变、开采方式等多元因素影响,具有较强的甲烷吸附性、绝对渗透率易突变、气相流动能力弱等特点;围绕南海水合物长期、稳定、高效开采目标,需要在初始储层改造基础上,通过实施储层二次改造,进一步优化提高储层渗流能力,实现增渗扩产目的。

    结论

    随着天然气水合物产业化进程不断向前推进,还需要着力解决大规模长时间产气过程中温度压力微观变化及物质能源交换响应机制以及水合物高效分解、二次生成边界条件等难题。

  • 加载中
  • 图 1  研究区地质图

    Figure 1. 

    图 2  水合物储层样品的典型矿物表面

    Figure 2. 

    图 3  南海神狐海域泥质粉砂储层矿物组分图(a)和黏土矿物含量图(b)

    Figure 3. 

    图 4  基于(a) N2吸附和(b) NMR的泥质粉砂储层孔径分布和孔隙类型(Li et al., 2022)

    Figure 4. 

    图 5  六个水合物储层样品的原始灰度图(a)、二值化图(b)及压力场分布图(c)(Bian et al., 2020)

    Figure 5. 

    图 6  水合物样品孔隙度和渗透率拟合示意图(a)以及样品在不同正方向上的进相与渗透率拟合曲线(b)(Bian et al., 2020)

    Figure 6. 

    图 7  果胶在0、1、2、3、4、5、10和20 ns的构型(其中蓝色代表水分子,蓝色虚线代表氢键,绿色代表甲烷,红色代表果胶)

    Figure 7. 

    图 8  水基体系不同盐度条件下天然气水合物分解条件(a)和不同盐度条件下沉积物基体系中水合物分解条件(b)(Geng et al., 2021)

    Figure 8. 

    图 9  甲烷水合物实验数据压力与温度图:a—水基体系;b—沉积物基体系, 其中实线表明实验方法与数据的可靠性(Geng et al., 2021)

    Figure 9. 

    图 10  不同模型计算的水合物饱和度与渗透率/初始渗透率的关系图

    Figure 10. 

    图 11  地层压力、水合物平衡压力随时间分布以及分解区储层温度和压力的分布(a—距离出口3 m, b—距离出口5 m, c—距离出口8 m)

    Figure 11. 

    图 12  不同压差下天然气(a)和二次水合物生成(b)的产量曲线图

    Figure 12. 

    图 13  泥质粉砂甲烷吸附特性图

    Figure 13. 

    图 14  改进的Langmuir和DR模型拟合不同实验样品结果图(a—KT4-16; b-KT4-17;c—KT4-18;d—KT4-16)(Qi et al., 2022)

    Figure 14. 

    图 15  泥质粉砂储层微观孔隙结构与压力变化关系图

    Figure 15. 

    图 16  泥质粉砂与常规砂岩煤层气、致密砂岩气-水两相相对渗透率曲线对比图(Lu et al., 2021)

    Figure 16. 

    图 17  水合物分解区泥质粉砂储层水力压裂断裂特征CT扫描图(Lu et al., 2021)

    Figure 17. 

    图 18  Hydrate Smart平台界面(Sun et al., 2021)

    Figure 18. 

    图 19  首轮水合物试采生产动态特征与地层温压变化关系图

    Figure 19. 

    表 1  世界主要国家水合物试采情况

    Table 1.  NGH production tests in major countries

    下载: 导出CSV

    表 2  不同样品孔隙半径参数对照

    Table 2.  Comparison of pore radius parameters between samples

    下载: 导出CSV

    表 3  六个水合物样品和两个砂岩岩心的三维分形维数计算(Bian et al., 2020)

    Table 3.  Calculated 3D fractal dimensions of six hydrate samples and two sandstone cores (Bian et al., 2020)

    下载: 导出CSV
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收稿日期:  2022-05-26
修回日期:  2022-06-06
刊出日期:  2022-06-25

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