한국해양대학교

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무작위 잡음이 포함된 탄성파 트레이스에서의 Q-factor 산출

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dc.contributor.author 권준석 -
dc.date.accessioned 2019-12-16T02:41:44Z -
dc.date.available 2019-12-16T02:41:44Z -
dc.date.issued 2017 -
dc.identifier.uri http://repository.kmou.ac.kr/handle/2014.oak/11351 -
dc.identifier.uri http://kmou.dcollection.net/jsp/common/DcLoOrgPer.jsp?sItemId=000002330127 -
dc.description.abstract Recently, there are various seismic explorations to develop resources like oil and gas. The existence of resources can be analyzed through interpreting the data which is obtained in the seismic explorations, and the seismic section of high resolution is necessary for the analysis. The seismic section of high resolution is the most important element about the interpretation of the data such as seismic property analysis, and there are many researches about the seismic section of high resolution. Especially, there are researches to obtain the seismic section of high resolution by the analysis of seismic attenuation. The analysis of seismic attenuation is used to recognize the increase of resolution of the seismic section and the existence of hydrocarbon. On this study, I would like to analyze the seismic attenuation by the estimation of Q-factor because Q-factor is the important element to recognize the existence of resources in the reservoir, it is used for analysis of characters of medium, and it is the effective method for analysis of quality of the seismic section resolution and AVO. To estimate Q-factor I simulate the real geological structure, add random noise and employ Spectral ratio method and Peak frequency shift. Spectral ratio method is often used for the estimation of Q-factor because it is less effected by S/N. Also, it estimates Q-factor by analysis ratio of amplitude spectrum between reference data and sample data. Peak frequency shift is the method to estimate Q-factor through frequency variation which is reflected. I set different geological structures in many times and add random noise in two methods. In the result of the research, the deviation of Q-factor through Peak frequency shift is less than the other and it appears the accuracy in research of the seismic attenuation. Thus, I assume that Peak frequency shift is the more effective method to obtain the seismic section of high resolution. Recently, there are various seismic explorations to develop resources like oil and gas. The existence of resources can be analyzed through interpreting the data which is obtained in the seismic explorations, and the seismic section of high resolution is necessary for the analysis. The seismic section of high resolution is the most important element about the interpretation of the data such as seismic property analysis, and there are many researches about the seismic section of high resolution. Especially, there are researches to obtain the seismic section of high resolution by the analysis of seismic attenuation. The analysis of seismic attenuation is used to recognize the increase of resolution of the seismic section and the existence of hydrocarbon. On this study, I would like to analyze the seismic attenuation by the estimation of Q-factor because Q-factor is the important element to recognize the existence of resources in the reservoir, it is used for analysis of characters of medium, and it is the effective method for analysis of quality of the seismic section resolution and AVO. To estimate Q-factor I simulate the real geological structure, add random noise and employ Spectral ratio method and Peak frequency shift. Spectral ratio method is often used for the estimation of Q-factor because it is less effected by S/N. Also, it estimates Q-factor by analysis ratio of amplitude spectrum between reference data and sample data. Peak frequency shift is the method to estimate Q-factor through frequency variation which is reflected. I set different geological structures in many times and add random noise in two methods. In the result of the research, the deviation of Q-factor through Peak frequency shift is less than the other and it appears the accuracy in research of the seismic attenuation. Thus, I assume that Peak frequency shift is the more effective method to obtain the seismic section of high resolution. -
dc.description.tableofcontents 1. 서 론 1 1.1 개요 1 2. 탄성파 감쇠 이론 3 2.1 탄성파 감쇠의 정의 3 2.2 탄성파 Q-factor(Quality factor) 7 2.3 Spectral ratio method(SRM) 12 2.4 Peak frequency shift(PFS) 16 3. 탄성파 감쇠 수치모형실험 및 적용 22 3.1 탄성파 감쇠 수치모형실험 22 3.1.1 탄성파 감쇠 수치모형실험 구성 22 3.1.2 탄성파 감쇠 수치모형실험 방법 24 3.1.3 탄성파 감쇠 수치모형실험 결과 27 3.1.3.1 심도에 따른 Q-factor 증가 모델 27 3.1.3.2 심도에 따른 Q-factor 감소 모델 50 3.1.3.3 급격한 변화가 있는 Q-factor 모델 58 3.2 현장 자료 적용 65 3.2.1 현장 관측자료 취득 및 처리 65 3.2.2 현장 관측자료 적용 및 분석 71 4. 결론 74 감사의 글 76 References 78 Bibliography 82 -
dc.format.extent 94 -
dc.language kor -
dc.publisher 한국해양대학교 대학원 -
dc.title 무작위 잡음이 포함된 탄성파 트레이스에서의 Q-factor 산출 -
dc.type Dissertation -
dc.date.awarded 2017-02 -
dc.contributor.alternativeName Kwon, Jun Seok -
dc.contributor.department 대학원 해양에너지자원공학과 -
dc.contributor.affiliation 한국해양대학교 대학원 -
dc.description.degree Master -
dc.subject.keyword Q-factor, Peak Frequency Shift, Spectral ratio method, 무작위 잡음, 탄성파 감쇠 -
dc.type.local Text -
dc.title.translated Q-factor estimation of seismic trace including random noise -
dc.identifier.holdings 000000001979▲000000006780▲000002330127▲ -
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