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      셰일 저류층에서 케로젠, GOR 변화에 따른 속도 변화 및 AVO 반응 분석 = Analysis of Seismic Velocity Change and AVO Response Depending on Saturation of Kerogen and GOR in Shale Reservoirs

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      https://www.riss.kr/link?id=A101806375

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      다국어 초록 (Multilingual Abstract)

      Recently, the studies about rock physics model (RPM) in shale reservoir are widely performed. In shale reservoir, the degree of the maturity can be estimated by kerogen and GOR (Gas-Oil Ratio). The researches on the rock physics model of shale reservo...

      Recently, the studies about rock physics model (RPM) in shale reservoir are widely performed. In shale reservoir, the degree of the maturity can be estimated by kerogen and GOR (Gas-Oil Ratio). The researches on the rock physics model of shale reservoir with the amount of kerogen have been actively carried out but not with GOR. Thus, in this study, we analyzed the changes in seismic velocity and density, and AVO (Amplitude Variation with Offset) response depending on changes in GOR and the amount of kerogen. Since the shale consists of plate-like particles, it has vertical transverse isotropy (VTI). Therefore we estimated the seismic velocity and density by using Backus averaging method and analyzed AVO responses based on these estimated properties. The results of analysis showed that the changes in the velocity with the GOR variation are small but the velocity changes with the variation in kerogen amount are relatively larger. In case, GOR 180 (Litre/Litre) which is boundary between heavy oil and light oil, when volume fraction of kerogen increased from 5% to 35%, the P-wave velocity normal to the layering increased 51%. That is, it helps estimating maturity of kerogen through the velocity. Meanwhile, when rates of oil-gas mixture are large, the effect of GOR variation on the velocity change became larger. In case volume fraction of kerogen is 5%, the P-wave velocity normal to the layering was estimated 1.46 km/s2 in heavy oil (GOR 40) but 1.36 km/s2 in light oil (GOR 300). The AVO responses analysis showed class 4 regardless of the GOR and amount of kerogen because variation of poisson’s ratio is small. Therefore, shale reservoir has possibility to have class 4.

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      참고문헌 (Reference)

      1 Thomsen, L., "Weak anisotropic reflections, in Offset dependent reflectivity" 103-114, 1993

      2 Kuster, G. T., "Velocity and attenuation of seismic waves in two-phase media, Part I. Theoretical formulations" 39 : 587-606, 1974

      3 Canada Society for Unconventional Resources, "Understanding tight oil"

      4 Clark, V. A., "The effect of oil under in-situ conditions on the seismic properties of rocks" 57 (57): 894-901, 1992

      5 Carcione, J. M., "Source-rock seismic-velocity models Gassmann versus Backus" 76 : N37-N45, 2011

      6 Sayers, C. M., "Sensitivity of the elastic anisotropy and seismic reflection amplitude of the Eagle Ford Shale to the presence of kerogen" 63 (63): 151-165, 2013

      7 Batzle, M. L., "Seismic properties of pore fluids" 57 : 1396-1408, 1992

      8 Yenugu, M., "Seismic characterization of kerogen maturity, An example from Bakken shale"

      9 Carcione, J. M., "Rock-physics templates for hydrocarbon source rocks" 80 (80): D481-D500, 2014

      10 Forrest, M., "Risking seismic amplitude anomaly prospects based on database trends" 29 (29): 570-574, 2010

      1 Thomsen, L., "Weak anisotropic reflections, in Offset dependent reflectivity" 103-114, 1993

      2 Kuster, G. T., "Velocity and attenuation of seismic waves in two-phase media, Part I. Theoretical formulations" 39 : 587-606, 1974

      3 Canada Society for Unconventional Resources, "Understanding tight oil"

      4 Clark, V. A., "The effect of oil under in-situ conditions on the seismic properties of rocks" 57 (57): 894-901, 1992

      5 Carcione, J. M., "Source-rock seismic-velocity models Gassmann versus Backus" 76 : N37-N45, 2011

      6 Sayers, C. M., "Sensitivity of the elastic anisotropy and seismic reflection amplitude of the Eagle Ford Shale to the presence of kerogen" 63 (63): 151-165, 2013

      7 Batzle, M. L., "Seismic properties of pore fluids" 57 : 1396-1408, 1992

      8 Yenugu, M., "Seismic characterization of kerogen maturity, An example from Bakken shale"

      9 Carcione, J. M., "Rock-physics templates for hydrocarbon source rocks" 80 (80): D481-D500, 2014

      10 Forrest, M., "Risking seismic amplitude anomaly prospects based on database trends" 29 (29): 570-574, 2010

      11 Ruger, A., "Reflection coefficients and azimuthal AVO analysis in anisotropic media" Society of Exploration Geophysicists 10 : 39-62, 2002

      12 Avseth, P., "Quantitative seismic interpretation" Cambridge University Press 2005

      13 Aki, K., "Quantitative Seismology: Theory and Methods" WH Freeman and Co 1980

      14 Castagna, J. P., "Fluid effects on bright spot and AVO analysis"

      15 Cander, H., "Finding Sweet Spots in Shale Liquids and Gas Plays with Lessons from the Eagle Ford Shale" 2013

      16 Hwang, L. F., "Bright Spots related to High GOR Oil Reservoir in Green Canyon"

      17 Carcione, J. M., "AVO effects of a hydrocarbon sourcerock layer" 66 : 419-427, 2001

      18 Schoenberg, M., "A calculus for finely layered media" 54 : 582-590, 1989

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2026 평가예정 재인증평가 신청대상 (재인증)
      2020-01-01 평가 등재학술지 유지 (재인증) KCI등재
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      2008-12-23 학술지명변경 한글명 : 물리탐사 -> 지구물리와 물리탐사
      외국어명 : Geophysical Exploration -> Geophysics and Geophysical Exploration
      KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2005-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
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      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.15 0.15 0.15
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.14 0.15 0.311 0.07
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