• 한국정보통신학회논문지
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• 제18권3호
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• pp.643-650
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• 2014

TOF(Time-Of-Flight) 센서에 의해 획득된 정보로부터 3차원 깊이 영상(depth image)을 추출하기 위한 위상 연산기 하드웨어를 구현한다. 설계된 위상 연산기는 DCORDIC(Differential COordinate Rotation DIgital Computer) 알고리듬의 벡터링 모드를 이용하여 아크탄젠트 연산을 수행하며, 처리량과 속도를 늘리기 위해 잉여 이진 수체계와 파이프라인 구조를 적용하였다. 고정 소수점 MATLAB 시뮬레이션을 통해 검증하고 최적 데이터 비트 수 및 반복 횟수를 결정하였으며, MATLAB/Simulink와 FPGA 연동을 통해 하드웨어 동작을 검증하였다. TSMC $0.18-{\mu}m$ CMOS 공정으로 테스트 칩을 제작하였으며, 테스트 결과 정상 동작함을 확인하였다. 약 82,000 게이트로 구현되었고, 400MHz@1.8V로 동작하여 400 MS/s의 연산 성능을 갖는 것으로 평가되었다.

• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2005년도 춘계학술대회
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• pp.638-642
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• 2005

For gas hydrate exploration, long offset multichannel seismic data acquired using by the 4km streamer length in Ulleung basin of the East Sea. The dataset was processed to define the BSRs (Bottom Simulating Reflectors) and to estimate the amount of gas hydrates. Confirmation of the presence of Bottom Simulating reflectors (BSR) and investigation of its physical properties from seismic section are important for gas hydrate detection. Specially, faster interval velocity overlying slower interval velocity indicates the likely presences of gas hydrate above BSR and free gas underneath BSR. In consequence, estimation of correct interval velocities and analysis of their spatial variations are critical processes for gas hydrate detection using seismic reflection data. Using Dix's equation, Root Mean Square (RMS) velocities can be converted into interval velocities. However, it is not a proper way to investigate interval velocities above and below BSR considering the fact that RMS velocities have poor resolution and correctness and the assumption that interval velocities increase along the depth. Therefore, we incorporated Migration Velocity Analysis (MVA) software produced by Landmark CO. to estimate correct interval velocities in detail. MVA is a process to yield velocities of sediments between layers using Common Mid Point (CMP) gathered seismic data. The CMP gathered data for MVA should be produced after basic processing steps to enhance the signal to noise ratio of the first reflections. Prestack depth migrated section is produced using interval velocities and interval velocities are key parameters governing qualities of prestack depth migration section. Correctness of interval velocities can be examined by the presence of Residual Move Out (RMO) on CMP gathered data. If there is no RMO, peaks of primary reflection events are flat in horizontal direction for all offsets of Common Reflection Point (CRP) gathers and it proves that prestack depth migration is done with correct velocity field. Used method in this study, Tomographic inversion needs two initial input data. One is the dataset obtained from the results of preprocessing by removing multiples and noise and stacked partially. The other is the depth domain velocity model build by smoothing and editing the interval velocity converted from RMS velocity. After the three times iteration of tomography inversion, Optimum interval velocity field can be fixed. The conclusion of this study as follow, the final Interval velocity around the BSR decreased to 1400 m/s from 2500 m/s abruptly. BSR is showed about 200m depth under the seabottom