• 한국지진공학회논문집
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• 제1권4호
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• pp.29-35
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• 1997

MM진도(Modified Mercalli Intensity) V이상의 한반도 지진자료에 의거하여 서울 수도권일원 $(위도 37.0^{circ}~37.8^{circ} N, 경도 126.5^{circ}~127.5^{circ} E)$ 의 확률론적인 지진위험도가 점지진원방법에 의해 추정되었다. 전지진자료를 이용하여 추정된 지진위험도는 비교적 완전하다고 여겨지는 조선시대이후의 지진자료를 이용하여 추정된 지진위험도보다 더 낮다고 추정되었다. 수평지반가속도 0.1g 이상의 파괴적인 지진은 90% 초과확률로서 전지진자료와 조선시대이후의 지진자료가 이용되었을 때 각각 500년과 200년 기간에 발생한다.

• 지질공학
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• 제24권2호
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• pp.171-178
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• 2014

In seismic reflection data processing, the crossdip correction effectively focuses the stacking energy near the sharp bends of a crooked survey line. Additionally, approximate 3-D information on the reflector (e.g., true crossdip angle and lateral continuity) are locally investigated as a by-product of the crossdip correction procedure. Improvement of the signal-to-noise ratio and estimation of reflector crossdip attitude are tested, in terms of both common midpoint bin direction and processing-line type, using synthetic seismic reflection data. To effectively image the reflection energy near bends in seismic survey lines, straight-line binning is preferred to slalom-line binning.

• Journal of Advanced Marine Engineering and Technology
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• 제32권8호
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• pp.1309-1314
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• 2008

Seismic data is often contaminated with high-energy, spatially aliased noise, which has proven impractical to attenuate using Fourier techniques. Wavelet filtering, however, has proven capable of attacking several types of localized noise simultaneously regardless of their frequencies. In this study a 2-D stationary wavelet transform is used to decompose seismic data into its wavelet components. A threshold is applied to these coefficients to attenuate high amplitude noise, followed by an inverse transform to reconstruct the seismic trace. The stationary wavelet transform minimizes the phase-shift errors induced by thresholding that occur when the conventional discrete wavelet transform is used.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 2002년도 추계 학술발표회 논문집
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• pp.35-42
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• 2002

Frequency responses for most of the local seismic sensors in Korea have been roughly checked by mutual comparison of Fourier spectra of seismic records from accelerometer and seismometer, both of which are installed at the same location. Especially, because the frequency content of the seismic energy is usually above 1 Hz for local earthquakes, the reliability of low frequency response could have not been evaluated. Fortunately a recent large earthquake, Ms=7.2 on 02/06/29 containing dominant low frequency energy makes it possible to check the low frequency response of the seismic sensors, especially EpiSensor and JC-V100. Considering two types of sensor pairs, (STS-2 and EpiSensor, JC-V100 and EpiSensor), the low frequency response of EpiSensor is confirmed first by comparison with STS-2 which has proved low frequency response. Second, reliable low frequency limit of instrumentally corrected seismic data from JC-V100 data is estimated to be about 0.03 Hz by comparison with EpiSensor data.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2007년도 공동학술대회 논문집
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• pp.209-214
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• 2007

In Korean geology that crystalline rock is dominant, the properties of subsurface including the anisotropy are distributed complexly and changed abruptly. Because of such geological environments, cross-hole seismic traveltime tomography is widely used to obtain the high resolution image of the subsurface for the engineering purposes in the geotechnical sites. However, because the cross-hole tomography has a wide propagation angle coverage relatively, its data tend to include the seismic velocity anisotropy comparing with the surface seismic methods. It can cause the misinterpretation that the cross-hole seismic data including the anisotropic effects are analyzed and treated with the general processing techniques assuming the isotropy. Therefore, we need to consider the seismic anisotropy in cross-hole seismic traveltime tomography. The seismic anisotropic tomography algorithm, which is developed for evaluation of the velocity anisotropy, includes several inversion schemes in order to make the inversion process stable and robust. First of all, the set of the inversion parameters is limited to one slowness, two ratios of slowness and one direction of the anisotropy symmetric axis. The ranges of the inversion parameters are localized by the pseudo-beta transform to obtain the reasonable inversion results and the inversion constraints are controlled efficiently by ACB(Active Constraint Balancing) method. Especially, the inversion using the Fresnel volume is applied to the anisotropic tomography and it can make the anisotropic tomography more stable than ray tomography as it widens the propagation angle coverage.

• Earthquakes and Structures
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• 제9권5호
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• pp.983-997
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• 2015

This research evaluates the soil conditions for seismic stations situated in Romania using the horizontal-to-vertical spectral ratio (HVSR). The strong ground motion database assembled for this study consists of 179 analogue and digital strong ground motion recordings from four intermediate-depth Vrancea seismic events with $M_w{\geq}6.0$. In the first step of the analysis, the influence of the earthquake magnitude and source-to-site distance on the H/V curves is evaluated. Significant influences from both the earthquake magnitude and hypocentral distance are found especially for soil class A sites. Next, a site classification method proposed in the literature is applied for each seismic station and the soil classes are compared with those obtained from borehole data and from the topographic slope method. In addition, the success and error rates of this method are computed and compared with other studies from the literature. A more in-depth analysis of the H/V results is performed using data from seismic stations in Bucharest and a comparison of the free-field and borehole H/V curves is done for three seismic stations. The results show large differences between the free-field and the borehole curves. As a conclusion, the results from this study represent an intermediary step in the evaluation of the soil conditions for seismic stations in Romania and the need to perform more detailed soil classification analysis is highly emphasized.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 2000년도 추계 학술발표회 논문집 Proceedings of EESK Conference-Fall 2000
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• pp.49-56
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• 2000

Instrumental observation of earth quakes in KIGAM was first attempted in the earty 1980`s by using 6 portable seismographs in the vicinity of Yang-San Faults. Now twenty-four permanent stations, which are equipped with short-period or broad-band seismometer, are included in seismic research network in KIGAM, including KSRS array station in Wonju which is consisted of 26 bore-hole stations. The seismic network of KIGAM is also linked to that of KEPRI(Korea Electric Power Research Institute)which is consisted of eight stations installed within and around the nuclear power plants. Owing to real-time data acquisition by telemetry, it became feasible to automatically locate hypocenters of the local events within fifteen minutes by computer data processing system, named KEMS(Korea Earthquake Monitoring System). Results of the hypocenter determination, together with observational data, are compiled and stored in the data base system. And they are published via web site whose URL is http://quake.kigam.re.kr KIGAM is also running t재 permanent geomagnetic stations installed in Daejun and Kyungju. The observed geomagnetic data are transmitted to Earthquake Research Centre in KIGAM by seismic network and compiled for the purpose of earthquake prediction research and other basic geophysical research.

• 산업기술연구
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• 제20권A호
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• pp.303-309
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• 2000

Seismic reflection method is applied to detect shallow location of limestone in Chechon area. The data using hammer source is compared with that of weight drop. Small size hammer and weight-drop are used as energy source and 100Hz geophones are used for data aquisition. Data processing is conducted utilizing the available processing technique of "Geobit", which is seismic data processing software developed by KIGAM. The result of above data processing, the velocity of topsoil layer is 1,250m/sec. The velocity of this area is higher than other area because loading trucks pass this area and make this layer compact. And in limestone area, hammer is proposed to energy source instead of weight drop because the energy propagates the layer very well.

• 한국지진공학회:학술대회논문집
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• 한국지진공학회 1997년도 추계 학술발표회 논문집 Proceedings of EESK Conference-Fall 1997
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• pp.41-48
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• 1997

The seismic risk in Seoul Metropolitan Area(latitude 37.0$^{\circ}$~37.8$^{\circ}$, longitude 126.5$^{\circ}$~127.5$^{\circ}$)based on all Korean earthquake data of Modified Mercalli Intensity equal to or greater than V is evaluated by extreme value method and point source method. The seismic risk estimated from all data turned out to be lower than from the data since the Chosen dynasty during which seismic data appear to be rather complete. The damaging earthquake of park horizontal ground acceleration grater than 0.1g turns out to occur with 90% probability of being exceeded in 200 years when the data since the Chosen Dynasty are used.

• 지구물리와물리탐사
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• 제27권2호
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• pp.91-107
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• 2024

단일 채널 탄성파 탐사는 소규모 자료획득 시스템으로 지하 지질구조를 파악하는 효과적인 방법이다. 영벌림거리 혹은 가까운 벌림거리를 사용하여 획득한 단일 채널 탄성파 자료는 연직 방향의 지하 지질구조를 직접 반영하므로 탄성파 단면도를 효과적으로 작성할 수 있다. 그러나 공통중간점 중합 과정을 적용할 수 없어 신호 대 잡음비가 매우 낮으므로 단면에 나타나는 반사 구조의 정밀한 해석에 있어 중합 단면 대비 불리함을 가진다. 본 연구에서는 단일 채널 탄성파 자료의 신호 대 잡음비를 향상시키기 위해 특이 스펙트럼 분석을 기반으로 한 잡음 제거 및 신호 향상 방법을 제안한다. 기존의 특이 스펙트럼 분석 방법은 행렬의 특정 특잇값을 임의로 추출하여 자료 내에 있는 무작위 잡음을 제거하는 방식으로 수행되었으나, 이는 낮은 신호 대 잡음비나 이상 잡음이 있는 자료에 적용할 수 없다. 따라서 본 연구에서는 행렬의 특잇값을 최적화하고 저계수 근사를 수행하여 무작위 및 이상 잡음을 동시에 효과적으로 제거한다. 또한, 잡음 제거로 인한 신호 손실을 보정하고 탄성파 이벤트의 수평적 연속성을 향상시키기 위해 행렬의 고유 영상에 기반한 가중치를 계산하여 탄성파 단면의 품질을 향상시킨다. 본 연구에서 제안하는 기술의 적용성 및 우수성을 확인하기 위해 북극해 척치해저고원에서 획득한 단일 채널 스파커 탄성파 자료에 대한 자료 처리 실험을 수행하였으며, 수치 예제를 통해 매우 높은 수준의 신호 대 잡음비와 최소의 신호 손실을 가진 탄성파 단면을 얻을 수 있었다. 본 연구에서 제안하는 단일 채널 탄성파 자료 처리 기술은 향후 국내 연안지역의 해양개발과 해저 지질재해를 규명하기 위한 단일 채널 및 초고해상도 탄성파 탐사에 매우 효과적으로 기여할 것으로 기대된다.