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퇴적물 원격분류를 위한 개선된 초동신호결정 알고리즘 개발

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Alternative Title
Development of an improved algorithm of the first arrival detection for the remote classification of seabed sediments
Abstract
In seismic exploration, the first arrival detection is the task of determining the first signal arrivals as accurately as possible. The accurate detection of the first arrivals needs to calculate the static corrections in a fundamental stage of seismic data processing. For the seismic data with a low signal-to-noise ratio, the first arrival automatic detection method is an important step but it is not easy. Determining of the first arrivals is similar to finding the bathymetry in the ocean exploration.
In the set of seismic traces, the method of the first arrival detection is divided in a way directly or using an automated algorithm. When using the former method, users should read the figure for each trace, which takes first arrival travel time. This method is time-consuming; also, the picking error can be relatively large. Therefore, this method is usually both inefficient and unreliable. The latter method aims to pick the first arrival time automatically. It is intend to reduce the picking errors using an automatic picking algorithm.
First arrival detection algorithms can be divided into several types of methods, including the coherence method, the neural network method, and the cross-correlation method. Coherence and neural network methods assume the existence of patterns in the first arrivals. Cross-correlation methods are considered to be most appropriate for the near-surface surveys since their algorithms are based on trace-by-trace evaluation of the first arrival times.
For first arrival detection, it has been used with a variety of ways of energy ratio (ER), modified energy ratio (MER), and short-term average/long-term average ratio (STA/LTA) such as a cross-correlation method.
The energy ratio method is based on sliding time windows; however, the conventional method based on sliding time windows is not stable. The modified energy ratio method was designed to overcome this disadvantage. The peak of the modified energy ratio is much closed to the time of first arrival on noise-free seismograms.
The STA/LTA ratio method is similar to Coppens’ algorithm. The difference is to do the ratio of two averages of energy between a short-term window and a long-term window, which is denoted as the STA/LTA, instead of calculating the ratio of energy of seismogram of the two windows in Coppens’ algorithm. The basic idea of this method detects first arrival time when the STA/LTA ratio exceeds a pre-defined threshold. This method is well suited for the first arrival detection, but not for providing accurate arrival times due to the delay associated with the length of the short-term average window.
In this study, it is proposed an improved algorithm that can determine first arrivals even in low SNRs signals by combining ER, MER, STA/LTA, exponentially weighted low-pass filter, and Kalman filter precisely. In addition, it is developed and introduced basic signal analysis and processing application which applied to improved algorithm. It is proposed the depth of submarine cable installation, attenuation of the surface related multiple, combining the two types of seismic data, and preliminary result of seabed characterizing based on similarity index using first arrivals of the developed algorithm and application.
Key to the effectiveness of the improved algorithm is the manual selection of the first arrival on the initial trace. Thus, the Kalman filter or the exponentially weighted low-pass filter can be used to predict the first arrival time of the next trace in advance.
The ER method showed that the first arrival is determined to be approximately 2.0 to 3.0 ms earlier than actual first arrival time due to the noise of the upper water layer. The MER method yielded better results than the ER method. However, the first arrival is determined to be approximately 0.5 ms earlier than actual first arrival time. The STA/LTA method showed more consistent results than the ER method and the MER method. However, the first arrival is determined to be approximately 1.0 ms earlier than actual first arrival time. The improved first arrival detection algorithm showed sound results in finding the first arrival time correctly.
Author(s)
임문수
Issued Date
2018
Awarded Date
2018.2
Type
Dissertation
Keyword
퇴적물 원격분류 초동신호 remote classification first arrival
Publisher
부경대학교
URI
https://repository.pknu.ac.kr:8443/handle/2021.oak/14211
http://pknu.dcollection.net/common/orgView/200000010825
Alternative Author(s)
Moon-Soo Lim
Affiliation
부경대학교 대학원
Department
대학원 응용지질학과
Advisor
김대철
Table Of Contents
1. 서 론 1
2. 초동신호결정 알고리즘 4
2.1 개요 4
2.2 ER (Energy Ratio) / MER (Modified Energy Ratio) 5
2.3 STA/LTA (Short-Term Average/Long-Term Average) 8
2.4 지수가중 저주파통과필터 11
2.5 칼만필터 13
2.6 초동신호결정 소프트웨어 개발 14
2.6.1 소프트웨어의 구성 16
2.6.2 탄성파 자료 20
2.6.3 자료변환 21
2.6.4 트레이스 뷰어(Trace viewer) 24
2.6.5 주파수 분석(Frequency analysis) 27
2.6.6 초동신호결정 30
2.6.7 개선된 초동신호결정 알고리즘 36
2.6.8 자료처리 어플리케이션 38
2.7 결과 41
3. 초동신호 결과의 응용 48
3.1 해저케이블 매설심도 산정 48
3.2 해저면 기인 다중반사파 저감방안 52
3.2.1 SRM (Surface related multiple) 모델링 52
3.2.2 SRM 찾기 55
3.2.3 SRM 저감방안 56
3.3 고주파 및 저주파 탄성파자료 융합 58
3.4 유사도지수를 이용한 퇴적물 원격분류 64
3.4.1 개요 64
3.4.2 유사도지수(Similarity Index) 66
3.4.3 K-L (Karhunen-Loève) 변환 66
3.4.4 유사도지수 68
3.4.5 연구지역 69
3.4.6 재료 및 방법 72
3.4.6.1 고해상 탄성파탐사(High-resolution seismic profiles) 72
3.4.6.2 표층퇴적물 및 수중카메라 75
3.4.7 결과 78
3.4.7.1 표층퇴적물 및 수중카메라 분석결과 78
3.4.7.2 유사도지수 계산 84
3.4.7.3 퇴적물 원격분류 94
4. 고찰 101
5. 결론 105
참고문헌 107
감사의 글 113
APPENDICES 114
Degree
Doctor
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대학원 > 응용지질학과
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