An experimental investigation of matrix components and grain size influence on the permeability in porous medium containing hydrate

被引:11
作者
Chen, Ye [1 ,2 ]
Gao, Yonghai [1 ,2 ]
Chen, Litao [1 ,2 ]
Li, Hao [1 ,2 ]
Liu, Kai [1 ]
Sun, Baojiang [1 ,2 ]
机构
[1] China Univ Petr East China, Sch Petr Engn, Qingdao 266580, Shandong, Peoples R China
[2] Natl Engn Lab Subsea Equipment Testing & Detect T, Qingdao 266580, Shandong, Peoples R China
基金
中国国家自然科学基金;
关键词
GAS-PRODUCTION; METHANE; SEDIMENT; MODELS;
D O I
10.1007/s00231-018-02542-5
中图分类号
O414.1 [热力学];
学科分类号
摘要
Natural gas hydrate is a kind of potential alternative energy, widely distributed in deep water deposits. Permeability is one of the most important factors during this underground energy extraction, determining production efficiency and economic benefits. Based on special characteristics of natural gas hydrate, a set of experimental apparatus is designed to study the influence of matrix components and grain size on permeability in porous medium with different hydrate saturation. The results suggest that the permeability of porous medium containing hydrate is significantly smaller than that of conventional sample. Under the same hydrate saturation, larger grain size can always improve the sample permeability. According to the curves' shape of the permeability variations over time, grain size effect should be divided into two grades by particle size. Moreover, the existence of clay can greatly weaken the permeability of sand sample. Generally, the sample permeability decreases with the increase of clay content. When the matrix content is dominated by clay, the weakening effect is greatly reduced. At last, a modified empirical relation formula is fitted by related experimental data on the basis of Masuda model.
引用
收藏
页码:1563 / 1570
页数:8
相关论文
共 33 条
  • [1] Chen Fang, 2011, Marine Geology & Quaternary Geology, V31, P95, DOI 10.3724/SP.J.1140.2011.05095
  • [2] Original component of grain size index in core sediment from southwestern slope of the South China Sea and its paleoenvironmental implication
    Chen, MH
    Zheng, F
    Lu, J
    Xiao, SB
    Yan, W
    Chen, Z
    Xiang, R
    Wei, GJ
    Zhang, LL
    [J]. CHINESE SCIENCE BULLETIN, 2005, 50 (09): : 896 - 902
  • [3] [程家望 Cheng Jiawang], 2016, [地球物理学进展, Progress in Geophysiscs], V31, P2072
  • [4] Helgerud M. B., 2001, THESIS
  • [5] Huang L., 2016, THESIS
  • [6] Natural gas production from hydrate decomposition by depressurization
    Ji, C
    Ahmadi, G
    Smith, DH
    [J]. CHEMICAL ENGINEERING SCIENCE, 2001, 56 (20) : 5801 - 5814
  • [7] New method of assessing absolute permeability of natural methane hydrate sediments by microfocus X-ray computed tomography
    Jin, Yusuke
    Hayashi, Junko
    Nagao, Jiro
    Suzuki, Kiyofumi
    Minagawa, Hideki
    Ebinuma, Takao
    Narita, Hideo
    [J]. JAPANESE JOURNAL OF APPLIED PHYSICS PART 1-REGULAR PAPERS BRIEF COMMUNICATIONS & REVIEW PAPERS, 2007, 46 (5A): : 3159 - 3162
  • [8] Pore-scale modeling of flow in particle packs containing grain-coating and pore-filling hydrates: Verification of a Kozeny-Carman-based permeability reduction model
    Katagiri, Jun
    Konno, Yoshihiro
    Yoneda, Jun
    Tenma, Norio
    [J]. JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING, 2017, 45 : 537 - 551
  • [9] Permeability of Laboratory-Formed Methane-Hydrate-Bearing Sand: Measurements and Observations Using X-Ray Computed Tomography
    Kneafsey, Timothy J.
    Seol, Yongkoo
    Gupta, Arvind
    Tomutsa, Liviu
    [J]. SPE JOURNAL, 2011, 16 (01): : 78 - 94
  • [10] Kvenvolden K.A., 2001, GLOBAL OCCURRENCE NA