مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

559
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

SEISMIC MODELING IN ACOUSTIC AND VISCOACOUSTIC ISOTROPIC MEDIA IN THE TAU-P DOMAIN

Author(s)

KAZEMI MALIHE SADAT | GHASSEM ALASKARI MOHAMMAD KAMAL | JAVAHERIAN ABDOLRAHIM | Issue Writer Certificate 

Pages

  33-43

Abstract

ACOUSTIC WAVES propagated in gas and LOSSY MEDIA are less attenuated and more reliable than elastic waves. Accordingly, the detection and measurement of ACOUSTIC WAVES are more precise than for elastic waves. Consequently, reservoir characterization using processing techniques and seismic data inversion are based on propagations of ACOUSTIC WAVES. The wave field in acoustic media is described by a scalar quantity rather than by a vector. The tau-p transformations in the near field for the acoustic and elastic wave equations are similar, as they both yield the eikonal equation in isotropic media. The reflection and transmission behaviors of waves, however, differ considerably in each of the two media. In acoustic media, all P-wave energy is conserved and as a result it can be used for near offset tau-p modeling.Fryer (1980) developed a reflection method for modeling the VSP DATA in tau-p domain. The main idea of using tau-p domain is to investigate the amplitude variations as a function of near offset, changes of phase, estimation of attenuation factor (1/Q) and separation of primary multiples. Laboratory measurements and well log data have shown that the Q factor depends on the type of media and also the percentage of saturation. Therefore, Q is a very strong factor for characterization of reservoir gas zones. Due to its sensitivity, this factor is used in our two different modeling programs.In this study, the VSP modeling was used in the t-x and the tau-p domains. One of the most important parameters in this modeling is the velocity model. To generate the velocity model and synthetic seismograms, a computer program was developed in t-x and tau-p domains. Then, for two exploration wells, the VSP models were compared using real data. Based on the above algorithm, a software package was developed using a finite difference method in the tau-p domain. The slowness-time reflectivity method was used to calculate tau-p synthetic seismograms with the inclusion of the attenuation factor (1/Q) in LOSSY MEDIA. For large acoustic impedance contrasts, the attenuation factor occurs as an amplitude decay and phase rotation for some range of high frequencies. First, the upcoming and downgoing VSP synthetic data for side locations along each well were modeled and compared with the VSP real data. Second, the normal incident seismic sections based on well logs were compared with the tau-p sections derived from the acoustic and viscoacoustic media. The VSP DATA and seismic modeling techniques were used for the detection of gas zones in two wells in one of the south Iranian reservoir. The models of traveltime and amplitude changes of VSP DATA in the tau-p and in the t-x domains proved to be effective techniques for detection of gas zones from the VSP seismic data. Using this technique, gas zones in the reservoir can be very reliably detected using ACOUSTIC WAVES. The aforementioned procedure were applied in verification of different media.A comparison of the VSP DATA generated in the tau-p and the t-x procedures can yield valuable results. Results show that modeling in the tau-p domain using a localized slant stack is faster and more reliable than are conventional methods. Additionally, wave energy characteristics and amplitude changes of seismic waves in two different acoustic and viscoacoustic media were investigated using a 2D acoustic wave algorithm in LOSSY MEDIA. By using acoustic, viscoacoustic and anisotropic models in the tau-p domain and comparing them with normal reflections and VSP DATA, one can detect saturated gas zones. The synthetic VSP in the tau-p domain definitely helped to verify changes in amplitudes and phases in two VSP well data sets investigated here. Using this technique, it was found that reservoir gas zone can be reliably detected by ACOUSTIC WAVES. Furthermore, it was established that these waves can be used for better comparison with real VSP DATA in the reservoir gas zones.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    KAZEMI, MALIHE SADAT, GHASSEM ALASKARI, MOHAMMAD KAMAL, & JAVAHERIAN, ABDOLRAHIM. (2009). SEISMIC MODELING IN ACOUSTIC AND VISCOACOUSTIC ISOTROPIC MEDIA IN THE TAU-P DOMAIN. IRANIAN JOURNAL OF GEOPHYSICS, 3(1), 33-43. SID. https://sid.ir/paper/133867/en

    Vancouver: Copy

    KAZEMI MALIHE SADAT, GHASSEM ALASKARI MOHAMMAD KAMAL, JAVAHERIAN ABDOLRAHIM. SEISMIC MODELING IN ACOUSTIC AND VISCOACOUSTIC ISOTROPIC MEDIA IN THE TAU-P DOMAIN. IRANIAN JOURNAL OF GEOPHYSICS[Internet]. 2009;3(1):33-43. Available from: https://sid.ir/paper/133867/en

    IEEE: Copy

    MALIHE SADAT KAZEMI, MOHAMMAD KAMAL GHASSEM ALASKARI, and ABDOLRAHIM JAVAHERIAN, “SEISMIC MODELING IN ACOUSTIC AND VISCOACOUSTIC ISOTROPIC MEDIA IN THE TAU-P DOMAIN,” IRANIAN JOURNAL OF GEOPHYSICS, vol. 3, no. 1, pp. 33–43, 2009, [Online]. Available: https://sid.ir/paper/133867/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top
    telegram sharing button
    whatsapp sharing button
    linkedin sharing button
    twitter sharing button
    email sharing button
    email sharing button
    email sharing button
    sharethis sharing button