• Proceedings of the KSEEG Conference
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• 2003.04a
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• pp.139-142
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• 2003

지구물리학적 연구에서 있어서 가장 중요한 목적 중의 하나는 지각과 상부 맨틀의 상세한 구조를 규명하는 것이다. 3성분의 지진기록을 이용하여 관측소 하부의 지각구조를 연구하는 몇 가지 방법들이 개발되었으며, 수신함수분석(receiver function analysis)이 가장 널리 사용되고 있다 (Phinney, 1964: Burdick and Langston, 1977: Owens and Crosson, 1988). 수신함수는 원거리 지진의 P파와 관측소 하부의 Moho면에서 전환된 Ps 전환파를 이용하여 관측소 하부의 지각구조를 계산하는 것이다. (중략)

• Journal of the Earthquake Engineering Society of Korea
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• v.14 no.5
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• pp.53-64
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• 2010

Seismic fragility curves of structures represent the probability of exceeding the prescribed structural damage state for a given various levels of ground motion intensity, such as peak ground acceleration (PGA). This means that seismic fragility curves are essential to the evaluation of structural seismic performance and assessments of risk. Most of existing studies have not considered the near- and far-fault earthquake effect on the seismic fragility curves. In order to evaluate the effect of near- and far-fault earthquakes, seismic fragility curves for PSC box girder bridges subjected to near- and far-fault earthquakes are calculated and compared. The seismic fragility curves are strongly dependent on the earthquake characteristics such as fault distance. This paper suggests that the effect of near- and far-fault earthquakes on seismic fragility curves of PSC box girder bridge structure should be considered.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.468-468
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• 2012

레이더 강우를 적극적으로 활용하기 위해서는 레이더 강우에 포함된 각 오차들에 대한 특성을 파악하고 정량화하는 것이 무엇보다 중요하다. 본 연구에서는 레이더 반사도의 오차구조를 파악하고 그러한 오차구조를 갖는 반사도로부터 표출한 CAPPI의 거리오차를 보정하였다. 이러한 거리오차 파악을 위해서는 참 값으로 가정할 수 있는 기준 반사도가 필요하며 본 연구에서는 VPR 모형으로부터 기준 반사도인 지상 반사도를 추정하였다. 그 결과 일정한 VPR 모형을 적용하게 되면 거리와 상관없이 오차는 일정하고 오직 고도에 의해서만 영향을 받는다. 그러나 일정 고도에서의 반사도 표출 방법인 CAPPI는 지구곡률효과로 인해 실제로 거리가 멀어 질수록 관측 고도가 높아진다. 이에 따라서 오차는 거리가 멀어질수록 커지게 된다. 이는 실제 호우사상에 적용한 결과에서도 유사하게 나타났다. 강릉 기상 레이더의 경우 1.5km CAPPI는 약 100km까지 1.5km 고도를 유지하다 그 이상부터 고도가 점점 높아진다. CAPPI의 오차를 거리에 따라 분포시킨 결과에서도 100km까지는 어느 정도 일정한 오차를 보이다 그 이상부터 오차가 점점 증가하는 것으로 나타났다. CAPPI의 오차를 2차원 평면으로 나타낸 결과에서도 호우가 전반적으로 퍼져있는 시점부터 원거리에서 큰 오차를 보이고 있다. 이는 오차의 평균에서 더욱 명확히 나타났다. 이와 같이 CAPPI는 원거리 자료에서 오차가 크게 나타나고 있다. 이에 CAPPI에 포함된 거리오차를 VPR 모형을 이용하여 보정하였다. 그 결과 원거리에서의 오차가 감소하였음을 확인하였다.

• The Journal of Korean Institute of Electromagnetic Engineering and Science
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• v.24 no.3
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• pp.316-323
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• 2013

This paper deals with the near-field to far-field calculation for far-field characteristics of antenna and electromagnetic compatibility(EMC) testing. Since the conventional EMC testing process is inefficient such as measurements of the wide band signals and mega structures, Stratton-Chu formula is used to predict the far-field emission by simple and direct process. The usefulness of Stratton-Chu formula is verified by comparing to the analytic solution of the uniform distribution aperture in free-space. In order to inspect the far-fields and to get the near-field values, full-wave simulation solver is utilized. Through the full-wave simulation about the patch antenna, calculated far-field results from Stratton-Chu formula are proven. The predicted magnitudes of the far-field are in error by less than 6 %.

• Proceedings of the Optical Society of Korea Conference
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• 2003.07a
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• pp.196-197
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• 2003

광섬유형 센서는 전자기적 간섭에 강하고 높은 감도와 원거리 측정 등의 장점뿐만 아니라 낮은 삽입 손실, 높은 기계적인 신뢰성, 원거리 측정과 같은 장점을 가지고 있어 광통신 기술뿐 아니라 기초과학및 응용 과학분야의 계측에 활발히 이용되고 있다. 온도센서의 경우 센서의 재료가 온도에 견디는 정도에 따라 측정범위가 좌우되므로 광섬유형 센서의 경우 넓은 온도범위에서 측정이 가능하며 다양한 구조의 센서구현이 용이하다. (중략)

• Geophysics and Geophysical Exploration
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• v.23 no.1
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• pp.13-21
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• 2020

The acquisition and processing of long-offset data are essential for imaging deep geological structures in marine seismic surveys. It is challenging to derive an accurate subsurface image by employing conventional data processing to long-offset data owing to the normal moveout (NMO) stretch and non-hyperbolic moveout phenomena induced by seismic anisotropy. In 2017, the Korea Institute of Geoscience and Mineral Resources conducted a simultaneous two-dimensional multichannel streamer and ocean-bottom seismic survey using a 5.7-km streamer and an ocean-bottom seismometer to identify the deep geological structure of the Ulleung Basin. Herein, the actual geological subsurface structure was obtained via the sequential iterative updating of the velocity and anisotropic parameters of the long-offset data obtained using a multichannel streamer, and anisotropic prestack Kirchhoff migration was performed using the updated velocity and anisotropic parameters as input parameters. As a result, the reflection energy in the long-offset traces, which showed non-hyperbolic moveout owing to seismic anisotropy, was well aligned horizontally and NMO stretches were also reduced. Thus, a more precise and accurate migrated image was obtained, minimizing the distortion of reflectors and mispositioned reflection energy.

• Proceedings of the Korean Vacuum Society Conference
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• 1996.02a
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• pp.56-56
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• 1996

• Journal of the Korean Society for Nondestructive Testing
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• v.28 no.5
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• pp.416-420
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• 2008

In EMAT field, spiral RF coils are much more widely used when compared with solenoid coils. In the field of the magnetostrictive strip transducers for long range ultrasonic testing of cylindrical structures, however, solenoid coils has been used. This seems to be attributed to the difficulty in fabricating low frequency (i.e., large size) spiral coils. In this paper, we describe a method for fabricating spiral coil magnetostrictive strip guided wave transducers from FFC (flexible flat cable). It is demonstrated through a comparison experiment that the spiral coil transducer has much superior performance (sensitivity, SNR, and guided wave direction control capability) than the previous transducer with solenoid coils.

• The Journal of the Acoustical Society of Korea
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• v.34 no.6
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• pp.455-462
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• 2015

It is well known that warm eddy is frequently developed through the year in the East Sea. The warm eddy may affect sound propagation due to changes of sound velocity structures in the sea water. To verify the effects of the warm eddy for long-range sound propagation, transmission loss and performance surface, which were used mean direct signal excess range generated by sound propagation modeling using re-analyzed climatology data on March 23th in 2007 were analysed. From these analyses, we found that characteristics of sound propagation in the sea water are changed by the warm eddy, and boundaries of the warm eddy act as a barrier for long-range sound propagation. Furthermore, these disadvantages of the eddy related to sound propagation were increased when the sea bottom depth is shallow.

• Magazine of the Korea Institute for Structural Maintenance and Inspection
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• v.17 no.4
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• pp.27-35
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• 2013