• Geophysics and Geophysical Exploration
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• v.5 no.1
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• pp.64-67
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• 2002

• Proceedings of the Korean Magnestics Society Conference
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• 2005.12a
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• pp.94-96
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• 2005

포항방사광가속기의 전자빔수명을 연장하기 위한 3차 하모닉 초전도 RF 공동기를 개발하고 있다. 저장링 빔물리 계산에 따르면 3차 하모닉 초전도 RF 공동기를 설치할 경우 점자빔의 수명이 약2.3배 증가하는 것으로 나타났다. 또 이 공동기를 설치할 경우 란다우 (Landau) 감쇄 (damping)에 의한 빔의 안정화도 개선되는 효과가 있다. 본 논문은 이것을 실현하기 위한 초전도 RF 공동기의 전자기장 분포와 고차원 전자장 계산을 통하여 최적의 공동기의 모양 결정과 설계 특성에 대한 것을 보고 하고자 한다.

• Geophysics and Geophysical Exploration
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• v.3 no.2
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• pp.48-52
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• 2000

We have calculated and analyzed the electromagnetic responses of buried conductive pipes due to a horizontal magnetic dipole source on the pound using a three-dimensional (3-D) finite element method to provide useful guidelines for designing electromagnetic pipe locator and for field operation of the system. For single buried pipe, the horizontal component and the horizontal difference of the vertical component of magnetic field show peaks above the pipe. When comparing the width of response curves of both cases around the peak, horizontal difference of vertical component of magnetic field shows much narrower peak, 2 times narrower at a half of maximum amplitude, than that of horizontal component of magnetic field. Accordingly, we can pinpoint the horizontal location of pipe on the ground more accurately by measuring the horizontal difference of vertical component of magnetic fold. Moreover, it will have a merit in determining the depth of pipe, because the equation for depth estimation is defined just above the pipe. When there are two buried pipes separated by two meters with each other, the response of horizontal difference of vertical component of magnetic field has two separate peaks each of which is located above the pipe whereas horizontal magnetic field response has only one peak above the pipe just below the transmitter. Thus, when there exist more than a buried pipe, measuring the horizontal difference of vertical magnetic field can effectively detect not only the pipe under transmitter but also adjacent ones. The width of response curves also indicates higher resolving ability of horizontal difference of vertical component of magnetic field.

• Geophysics and Geophysical Exploration
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• v.14 no.1
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• pp.1-6
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• 2011

As a check on calibration and drift in each discrete sub-system of a commercial frequency-domain airborne electromagnetic system, we aim to use causality constraints alone to predict in-phase from wide-band quadrature data. There are several possible applications of the prediction of in-phase response from quadrature data including: (1) quality control on base level drift, calibration and phase checks; (2) prediction and validation of noise levels in in-phase from quadrature measurements and vice versa and in future; and (3) interpolation and extrapolation of sparsely sampled data enforcing causality and better frequency-domain-time-domain transformations. In practice, using tests on both synthetic and measured Resolve helicopter-borne electromagnetic frequency domain data, in-phase data points could be predicted using a scaled Hilbert transform with a standard deviation between 40 and 80 ppm. However, relative differences between base levels between flight could be resolved to better than 1 ppm, which allows an independent quality control check on the accuracy of drift corrections.

• KIPE Magazine
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• v.21 no.2
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• pp.29-34
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• 2016

• Journal of the Korean Geophysical Society
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• v.5 no.2
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• pp.99-109
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• 2002

Among the geophysical exploration methods, electromagnetic method(EM) has the broadest range of instrumental systems and remarkable range of applications. There are a lot of available techniques and instruments which have different depth of investigation and resolution depending on the operating frequency and source-receiver configuration. Furthermore, it is very easy to apply on the engineering and environmental problems since modern EM equipments are remarkably portable, considering their sophistication. Even though electromagnetic theory is very complex and not easy to understand, rapid avances in recent computer technology have made it possible to conduct accurate forward modeling and inversion of various EM exploration data. Here, we are going to provide brief theoretical principles, survey techniques and case histories of some selected EM methods that can be applied to geotechnical and environmental problems in Korea.

• Geophysics and Geophysical Exploration
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• v.6 no.4
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• pp.207-214
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• 2003

To analyze soil properties with depth in rice field, we compared resistivity distributions obtained from soil analysis with one dimensional inversion of small loop electromagnetic (EM) data. Although it didn't show consistency exactly between the two resistivity distributions, low resistivity zones in soil analysis, appeared to agree with low resistivity zones in EM result. Therefore, small loop EM method can be applied to obtain rapidly the soil properties such as salt accumulation in a rice field. If research on soil property and EM responses of unsaturated zone would be conducted consistently, small loop EM method can be used effectively to detect salt accumulated zone in agricultural area.

• 한국지구물리탐사학회:학술대회논문집
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• 2011.10a
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• pp.55-56
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• 2011

• Defense and Technology
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• no.9 s.271
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• pp.39-49
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• 2001

미래에는 정보전자전을 대비해서 전자기펄스탄(EMP 탄), 탄소섬유탄, 고섬광 발생탄과 같이 물리화학적 파괴 능력을 갖는 특수 전용 탄두들이 소요될 것이다. 세계 대전의 가능성은 희박하나 지역분쟁이 발생했을 때 전후방과 군과 민이라는 구분이 없어지고, 전쟁상황이 실시간으로 전파되기 때문에 다양한 비살상 탄두가 주요 전술탄두로 등장할 수 있다. 따라서 전자기 펄스탄(EMP 탄), 탄소섬유탄과 같은 대 정보.전자전 탄두들이 우리가 미래를 대비하는 하나의 수단이 되리라 확신한다.

• Electronics and Telecommunications Trends
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• v.21 no.2 s.98
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• pp.170-183
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• 2006

모뎀 진단/감시 장치(DM)는 기지국 DM 데이터 수집부와 단말 DM 데이터 수집부로각각 구분되어 DM 장치 내에서 기지국/단말 모뎀 플랫폼을 수용한다. 기지국 변조기, 기지국 동기, 기지국 채널 디코더, 기지국 복조기의 데이터는 기지국 DM 데이터 수집부에서 수집하고, 단말 변조기, 단말 동기, 단말 채널 디코더, 단말 복조기의 데이터는 단말 DM 데이터 수집부에서 수집하여 각각 수집된 데이터를 호스트 PC에서 분석하여 물리 계층 송수신 데이터 및 각종 통계 정보를 사용자 및 운용자가 확인할 수 있도록GUI로 화면에 표시해 준다. 모뎀 진단/감시 장치(DM)는 무선 전송 시스템(HM20)MIMO 구조 기지국/단말 모뎀의 물리 계층에 대한 상태 진단 및 감시 기능을 수행하여 모뎀 개발 과정에서 개발자에게 디버깅을 쉽게 하기 위한 장치로 사용된다. 또한 기지국 모뎀과 단말 모뎀의 유지 보수시 오류 발견을 위한 장치로 사용하기 위함이다.