• Geophysics and Geophysical Exploration
• /
• v.15 no.4
• /
• pp.199-208
• /
• 2012

High-amplitude swell noises (HASN) are very difficult to eliminate from the marine seismic data. In this paper, we applied F-X filter and median filter in order to suppress HASN. Test data have been acquired on the northern offshore of the South Shetland Islands in December, 2010. Parts of data have been contaminated by HASN caused by bad weather during the cruise. We applied F-X filter and median filter to test data with HASN. After F-X filtering, most of non-coherent noises and small-amplitude swell noises are eliminated effectively but HASN are still remained significantly. With median filter, HASN was suppressed better than F-X filter, however some of non-coherent noises are still remains. We applied a cascade of two filters and results show HASN and non-coherent noises are suppressed effectively. After the cascade of two filtering, it is possible to define reflection layers clearly on the velocity spectrum and to produce better stacked section with a good signal-to-noise ratio.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
• /
• 2018.05a
• /
• pp.67-69
• /
• 2018

해수욕장의 침식 및 퇴적은 입사파랑, 파에 의한 흐름, 조석류 및 바람에 의해 이동하며, 특히 하천을 끼고 있는 해수욕장의 경우 하천으로부터 표사를 공급받게 된다. 이러한 해수욕장의 침식 및 퇴적을 유발시키는 외력인자인 파랑, 조석 및 조류, 하천유량자료를 수집하여 분석하였으며, 해양수산부에서 수행하고 있는 진하해수욕장의 연안침식 실태조사자료를 수집 분석하여 사빈의 침식 및 퇴적변화를 파악하였다.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
• /
• 1993.07a
• /
• pp.34-37
• /
• 1993

지금까지의 항만정온도 평가시에는 주로 회귀연도 50연의 설계파를 입사파로 사용하여 대상수역에서의 파고비를 구한 후 평상시의 파랑에 대해서도 이 비율이 선형적으로 적용 가능한 것으로 가정하고 사용하였다. 그러나, 설계액와 평상시 파랑은 주기외 파고가 달라서 파랑경사가 다르므로 위와 같이 파고비가 선형적으로 비례한다고 가정하는 것은 실제와 상당한 차이를 야기시킬 수 있다. (중략)

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
• /
• 1994.07a
• /
• pp.33-38
• /
• 1994

• Geophysics and Geophysical Exploration
• /
• v.21 no.1
• /
• pp.54-60
• /
• 2018

The data acquired from seismic exploration can be used to detect the existence of oil and gas resources through appropriate processing and interpretation. The seismic attributes indicating the existence of resources are extracted from amplitude information, where the Q-factor representing intrinsic attenuation plays an useful role of hydrocarbon indicator. So, the accuracy of Q-factor estimation is very important to investigate the existence of resources. In this study, we calculated the Q-factor and analyzed the error rate through a numerical example. To mimic real data, random noise was added to the synthetic data. With the noise-added data, the Q-factor was estimated and the error rate was analyzed by using the spectral ratio method (SRM) and peak frequency shift method (PFSM). Both methods provided a relatively accurate Q-factor when the signal-to-noise ratio was 90 dB. However, the peak frequency shift method (PFSM) produced better results than the spectral ratio method (SRM) as the level of random noise increased.

• Geophysics and Geophysical Exploration
• /
• v.8 no.1
• /
• pp.41-49
• /
• 2005

We have developed a random heterogeneous velocity model with bimodal distribution in methane hydrate-bearing Bones. The P-wave well-log data have a von Karman type autocorrelation function and non-Gaussian distribution. The velocity histogram has two peaks separated by several hundred metres per second. A random heterogeneous medium with bimodal distribution is generated by mapping of a medium with a Gaussian probability distribution, yielded by the normal spectral-based generation method. By using an ellipsoidal autocorrelation function, the random medium also incorporates anisotropy of autocorrelation lengths. A simulated P-wave velocity log reproduces well the features of the field data. This model is applied to two simulations of elastic wane propagation. Synthetic reflection sections with source signals in two different frequency bands imply that the velocity fluctuation of the random model with bimodal distribution causes the frequency dependence of the Bottom Simulating Reflector (BSR) by affecting wave field scattering. A synthetic cross-well section suggests that the strong attenuation observed in field data might be caused by the extrinsic attenuation in scattering. We conclude that random heterogeneity with bimodal distribution is a key issue in modelling hydrate-bearing Bones, and that it can explain the frequency dependence and scattering observed in seismic sections in such areas.

• Proceedings of the KIEE Conference
• /
• 2003.04a
• /
• pp.405-408
• /
• 2003

국내철도는 많은 철도선로를 전철화하고 있다. 25kV-60Hz 전철화구간에서 운행하는 전기차량으로 인하여 고조파에 대한 문제가 있다 이를 해결하기 위하여 AT급전방식에서의 고조파 특성을 해석하고 차량에서 발생하여 변전소로 유입되는 고조파를 저감시키기 위한 대책설비가 필요하다 여기에서는 지금까지 고조파 해석에 사용된 3종류의 고조파 해석모델과 기존선 전철화 과정에서 고조파 대책설비 설계에 대한 3가지 예를 보인다.

• Geophysics and Geophysical Exploration
• /
• v.21 no.2
• /
• pp.94-102
• /
• 2018

To characterize virtual reflection images of deep subsurface by the method of seismic interferometry, we analyzed effects of offset range, ambient noise, missing data, and statics on interferograms. For the analyses, seismic energy was simulated to be generated by a 5 Hz point source at the surface. Vertical components of particle velocity were computed at 201 sensor locations at 100 m depths of 1 km intervals by the finite difference method. Each pair of synthetic seismic traces was cross-correlated to generate stacked reflection section by the conventional processing method. Wide-angle reflection problems in reflection interferometry can be minimized by setting a maximum offset range. Ambient noise, missing data, and statics turn to yield processing noise that spreads out from virtual sources due to stretch mutes during normal moveout corrections. The level of processing noise is most sensitive to amplitude and duration time of ambient noise in stacked sections but also affected by number of missing data and the amount of statics.

• Journal of Korean Electronics
• /
• v.25 no.11
• /
• pp.45-46
• /
• 2005

• Electrical & Electronic Materials
• /
• v.17 no.12
• /
• pp.20-23
• /
• 2004