Simulation of NMR responses in sandstone and restricted diffusion

被引:11
|
作者
Guo Jiang-Feng [1 ,2 ]
Xie Ran-Hong [1 ,2 ]
Zou You-Long [1 ,2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Key Lab Earth Prospecting & Informat Technol, Beijing 102249, Peoples R China
来源
关键词
Sandstone; NMR responses; Random-Walk method; Restricted diffusion; Diffusion coefficient line; POROUS-MEDIA; RELAXATION; GEOMETRIES; INVERSION; PROBE; MAPS;
D O I
10.6038/cjg20160733
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Nuclear magnetic resonance (NMR) responses and restricted diffusion phenomenon of the fluids in sandstone were simulated by the Random-Walk method. Sandstone of different pore sizes was generated by changing digital cores' resolution, permitting to study how the fluid diffusion coefficient changes with time when the sandstone of different pore sizes were saturated with water, and to simulate the NMR responses of the either single or two phase fluids in the sandstone. Then the relationship between the fluid restricted diffusion coefficient and the T-2 relaxation time was researched, and the influence on restricted diffusion phenomenon of wetting phase fluid posed by the surface relaxivity and cementation index of the sandstone was analyzed. Finally the analysis results were used to interpret the D-T-2 distributions of the sandstone. It was concluded that the diffusion coefficient of fluid gradually decreases and tends to be constant with increase of diffusion time. The smaller pore size of the rock, the restricted diffusion phenomenon is more obvious, and the restricted diffusion has a greater influence on NMR responses. The position of the restricted diffusion coefficient line of wetting phase fluid is affected by the rock cementation index and surface relaxivity. The wetting phase fluid signal in the D-T-2 distributions deviates from the unrestricted diffusion coefficient line due to the decreasing diffusion coefficient of the wetting phase fluid, hence the restricted diffusion coefficient line of fluid should be used to recognize the wetting phase fluid in D-T-2 distributions.
引用
收藏
页码:2703 / 2712
页数:10
相关论文
共 29 条
  • [1] Correlations Between NMR-Relaxation Response and Relative Permeability From Tomographic Reservoir-Rock Images
    AlGhamdi, Tariq M.
    Arns, C. H.
    Eyvazzadeh, R. Y.
    [J]. SPE RESERVOIR EVALUATION & ENGINEERING, 2013, 16 (04) : 369 - 377
  • [2] [Anonymous], THESIS
  • [3] [蔡淑惠 CAI Shuhui], 2009, [计算物理, Chinese Journal of Computational Physics], V26, P42
  • [4] [成家杰 Cheng Jiajie], 2013, [波谱学杂志, Chinese Journal of Magnetic Resonance], V30, P336
  • [5] The inversion of NMR log data sets with different measurement errors
    Dunn, KJ
    LaTorraca, GA
    [J]. JOURNAL OF MAGNETIC RESONANCE, 1999, 140 (01) : 153 - 161
  • [6] Einstein Albert., 1956, INVESTIGATION THEORY
  • [7] Predictions of pulsed field gradient NMR echo-decays for molecules diffusing in various restrictive geometries.: Simulations of diffusion propagators based on a finite element method
    Hagslätt, H
    Jönsson, B
    Nydén, M
    Söderman, O
    [J]. JOURNAL OF MAGNETIC RESONANCE, 2003, 161 (02) : 138 - 147
  • [8] RESTRICTED DIFFUSION IN SEDIMENTARY-ROCKS - DETERMINATION OF SURFACE-AREA-TO-VOLUME RATIO AND SURFACE RELAXIVITY
    HURLIMANN, MD
    HELMER, KG
    LATOUR, LL
    SOTAK, CH
    [J]. JOURNAL OF MAGNETIC RESONANCE SERIES A, 1994, 111 (02) : 169 - 178
  • [9] Comparison of NMR simulations of porous media derived from analytical and voxelized representations
    Jin, Guodong
    Torres-Verdin, Carlos
    Toumelin, Emmanuel
    [J]. JOURNAL OF MAGNETIC RESONANCE, 2009, 200 (02) : 313 - 320
  • [10] Restricted diffusion effects on nuclear magnetic resonance DT2 maps
    Luo, Zhi-Xiang
    Paulsen, Jeffrey
    Vembusubramanian, M.
    Song, Yi-Qiao
    [J]. GEOPHYSICS, 2015, 80 (02) : E41 - E47