土工基础 ›› 2020, Vol. 34 ›› Issue (4): 563-566.

• 测试技术 • 上一篇    

含水合物细粒土的渗透特性

马慧龙1,阴良魁2,汪华军3,颜荣涛1   

  1. (1.桂林理工大学 广西建筑新能源与节能重点实验室,广西桂林 541004;2.中国科学院科技创新发展中心,北京 100000;3.湖北中民建筑工程有限公司,湖北潜江 433199)
  • 收稿日期:2020-02-24 修回日期:2020-03-02 出版日期:2020-08-20 发布日期:2020-08-16
  • 作者简介:马慧龙(1993-),男,硕士,研究方向为水合物等。
  • 基金资助:
    国家自然科学基金(No.11562007,No.11962004)

Permeability Fine-Grained Soils with Natural Gas Hydrate

MA Huilong1, YIN Liangkui2, WANG Huajun3, YAN Rongtao1   

  1. (1.Guangxi Key Laboratory of New Energy and Building Energy Saving, Guilin University of Technology, Guilin, 541004;
    2.Innovation and Development Center, Chinese Academy of Sciences, Beijing 100000;
    3.Hubei Zhongmin Construction Engineering Co. Ltd., Qianjiang 433199)
  • Received:2020-02-24 Revised:2020-03-02 Online:2020-08-20 Published:2020-08-16

摘要: 含水合物储层的渗透率是影响开采水合物效率的重要物理参数。为了研究水合物赋存对赋存沉积物渗透性的影响规律,参照南海神狐海域水合物赋存区的沉积物的颗粒级配,配制了试验土体,并合成了含四氢呋喃水合物细粒土,并且基于稳态法测试了含不同水合物饱和度沉积物试样的渗透率。试验结果表明,该试验含水合物细粒土的渗透率介于11.41 mD和61.63 mD之间;随着水合物饱和度增加,含水合物细粒土的相对渗透率明显下降,主要是由于水合物的形成填充了沉积物孔隙,减小了孔隙率,此外,水合物还有可能阻塞流体渗流关键通道,从而减小了渗流率;采用现有渗流模型对试验结果进行了对比,发现与Masuda模型(N=3)最为近似。

关键词: 含水合物细粒土, 四氢呋喃水合物, 渗透率, 饱和度, 模型

Abstract: The permeability of porous material is an important physical parameter that affects the exploitation of natural gas hydrate. In order to study the effect of natural gas hydrate on the permeability of the hydrate deposition, this paper presents the laboratory tests of fine-grained soil samples containing natural gas hydrate. The gradation of the fine-grained soils contained tetrahydrofuran hydrate was similar to the grain size distribution of soils in in Shenhu area of the South China Sea. Then, the permeability of fine-grained soil samples with different hydrate saturations was tested based on the steady state method. The test results show that the permeability of fine-grained soil containing hydrate in this test is between 11.41 mD and 61.63 mD. As the hydrate saturation increases, the relative permeability of the hydrate containing fine-grained soil decreases significantly, mainly due to the hydrate formation that fills the pores of the sediment and reduces the porosity. In addition, hydrates may also block the porous fluid seepage, thereby reducing the permeability. The test results were compared using the existing permeability model, and it was found that the result was close to the Masuda Model (N=3).

Key words: Fine Grained Soil with Natural Gas Hydrate, Tetrahydrofuran Hydrate, Permeability, Degree of Saturation, Model

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