The velocity dispersion and attenuation of marine hydrate-bearing sediments

被引:13
|
作者
Zhang Ru-Wei [1 ,2 ]
Li Hong-Qi [1 ]
Wen Pen-Fei [2 ]
Zhang Bao-Jin [2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China
[2] Minist Land & Resources, Guangzhou Marine Geol Survey, Key Lab Marine Mineral Resources, Guangzhou 510075, Guangdong, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2016年 / 59卷 / 09期
关键词
Gas hydrate; Effective medium theory; BISQ model; Velocity dispersion; Seismic wave attenuation; SEISMIC-WAVE ATTENUATION; GAS-HYDRATE; METHANE HYDRATE; WELL;
D O I
10.6038/cjg20160924
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
P-wave and S-wave velocity will increase when the concentration of gas hydrate increases, and the attenuation will vary too. The analysis of velocity dispersion and attenuation for hydrate-bearing sediments ( GHBS) would contribute to the estimate of gas hydrate concentration. Based on effective medium theory (EMT), we study the nonlinear variation feature of P-wave and S-wave velocity for marine unconsolidated hydrate-bearing sediments. Moreover, we use BISQ model to replace Gassmann equation in the EMT, and research the velocity dispersion and attenuation of hydrate-bearing sediments in the full frequency band. Based on this model, the velocity and attenuation always increase with the increasing amount of gas hydrate, and the rock porosity and clay content doesn't make any differences to the attenuation. After the numeral modeling, we apply the sonic logging (20 kHz) and VSP (100 Hz) data from Ocean drilling Program (ODP) leg 164 to obtain the concentration of gas hydrate stability zone (GHSZ). In the application, the average hydrate concentration of GHSZ from hole 995 in ODP leg 164 is about 5% similar to 7%, consistent with the pressure core sample (PCA) data, Helgerud et al.'s research conclusions, and the prediction data from neural network (NN). Due to the velocity dispersion, the estimated hydrate concentration from VSP data is lower than the estimated results from sonic logging data. The prediction results of three hydrate stations (SH2, SH3 and SH7) from Shenhu area also coincide with the PCA, South China Sea. Moreover, based on the peak frequency method, the effective seismic quality factors (Q) of the BSR are estimated from the inline prestack seismic gathers. The Q-values suggest the effective saturation of gas hydrate estimated by this model fluctuates between 15%similar to 30%. The results of numeral modeling and applications indicate that the velocity dispersion and attenuation of GHBS always vary with the concentration of hydrate. The study of velocity dispersion and attenuation feature for GHBS in the full frequency band would contribute to the estimate of gas hydrate concentration.
引用
收藏
页码:3417 / 3427
页数:11
相关论文
共 36 条
  • [1] Implication of seismic attenuation for gas hydrate resource characterization, Mallik, Mackenzie Delta, Canada
    Bellefleur, G.
    Riedel, M.
    Brent, T.
    Wright, F.
    Dallimore, S. R.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2007, 112 (B10)
  • [2] The effect of methane hydrate morphology and water saturation on seismic wave attenuation in sand under shallow sub-seafloor conditions
    Best, Angus I.
    Priest, Jeffrey A.
    Clayton, Christopher R. I.
    Rees, Emily V. L.
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2013, 368 : 78 - 87
  • [3] Bottom-simulating reflectors: Seismic velocities and AVO effects
    Carcione, JM
    Tinivella, U
    [J]. GEOPHYSICS, 2000, 65 (01) : 54 - 67
  • [4] Estimation of seismic attenuation of gas hydrate bearing sediments from multi-channel seismic data: A case study from Krishna-Godavari offshore basin
    Dewangan, P.
    Mandal, R.
    Jaiswal, P.
    Ramprasad, T.
    Sriram, G.
    [J]. MARINE AND PETROLEUM GEOLOGY, 2014, 58 : 356 - 367
  • [5] Direct measurement of in situ methane quantities in a large gas-hydrate reservoir
    Dickens, GR
    Paull, CK
    Wallace, P
    [J]. NATURE, 1997, 385 (6615) : 426 - 428
  • [6] DYNAMIC POROELASTICITY - A UNIFIED MODEL WITH THE SQUIRT AND THE BIOT MECHANISMS
    DVORKIN, J
    NUR, A
    [J]. GEOPHYSICS, 1993, 58 (04) : 524 - 533
  • [7] Elasticity of marine sediments: Rock physics modeling
    Dvorkin, J
    Prasad, M
    Sakai, A
    Lavoie, D
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (12) : 1781 - 1784
  • [8] Dvorkin J., 2004, Leading Edge, V23, P730, DOI [10.1190/1.1786892, DOI 10.1190/1.1786892]
  • [9] Estimating the amount of gas hydrate and free gas from marine seismic data
    Ecker, C
    Dvorkin, J
    Nur, AM
    [J]. GEOPHYSICS, 2000, 65 (02) : 565 - 573
  • [10] Sediments with gas hydrates: Internal structure from seismic AVO
    Ecker, C
    Dvorkin, J
    Nur, A
    [J]. GEOPHYSICS, 1998, 63 (05) : 1659 - 1669