• 지구물리
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• 제6권2호
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• pp.99-105
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• 2003

Rayleigh waves which has more than 70% of the total seismic energy is the principal component of ground roll. Frequency component of a surface wave has a different propagation velocity, that is, phase velocity, which results in a different wavelength called dispersion. Rayleigh wave is one of the most common ways to use the dispersive properties of surface waves. MASW is a seismic method to evaluate shear-wave velocity information of the ground.

• 지구물리
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• 제6권2호
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• pp.49-56
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• 2003

Under the attack of storm waves, there are many destructions of coastal structures in the forms of sinking and sliding. There types of destructions will be in close relation to the dynamic behavior of sand bed around the structures. Form this point of view, in this pear, we investigate the characteristics of the pore water pressure and effective stresses in the highly saturated sand bed under oscillating water pressure theoretically. The results indicate that the oscillating water pressure induce the notable drop of strength of and bed around the structure under certain condition.

• 지구물리
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• 제4권3호
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• pp.219-226
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• 2001

본 연구에서는 주기적인 하중하에서의 철근콘크리트 기둥의 이력응답거동을 예측할 수 있는 해석적인 모델의 개발을 다루고 있다. 철근콘크리트 기둥의 비탄성 휨, 전단 및 휨-전단 변형은 개발된 모델을 통하여 주기적인 변위하에서 검토되었다. 개발된 모델들을 포함한 해석치와 실험치와의 비교분석을 통하여 본 연구에서 개발된 모델들의 검증을 실시하였고, 이 비교분석을 통하여 휨-전단간의 상호작용의 중요성을 강조하였으며, 본 연구에서 개발된 모델들의 정확성, 효율성 및 타당성을 입증하였다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 봄 학술발표회 논문집
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• pp.517-522
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• 2002

This study was carried out to understand the cause and processes of a reactivated landslide that occurred in Gonmyeong-myeon, Sacheon City, Kyeongsangnam-do. For the study, geologic mapping, geophysical exploration, boring, laboratory testing, and slope stability analyses were conducted. The landslide area has geologic conditions that are prone to slope failure, due to the past landslide. The trigger that caused the landslide was removal of lateral support by excavation of the toe of slopes.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2010년도 학술대회 초록집
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• pp.21-22
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• 2010

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2010년도 학술대회 초록집
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• pp.103-106
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• 2010

• 지구물리
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• 제9권3호
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• pp.263-272
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• 2006

Since the paleomagnetic study was introduced in Korea about 40 years ago, its scientific findings contributed to the understanding of geologic settings and tectonic processes of the Korean Peninsula and eventually to the escalation of geology and geophysics in Korea. It is worth summarizing and introducing the up-to-date paleomagnetic results produced by the representative paleomagnetic working groups in Korea, such as K. D. Min, I. S. Kim, S. J. Doh, Y. S. Lee, D. W. Suk, the late K. H. Kim and others.

• 지구물리
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• 제7권2호
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• pp.135-149
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• 2004

The present time is wanted quickness corretness position so as having more and more concern about present my position AS a doncing fan the intrenet marketed of fornation and recongnition about spatial generel is changed now is opening that present my position is where? to questing is answering through smaller (Mobile Device : Mobile Phone, PDA, GPS) then palm of the hand like this background, we know about that what is LBS?, service commercial of LBS SUCH embodiment practical use and possibilities of the future!!

• 지구물리
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• 제9권2호
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• pp.99-103
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• 2006

3D object recognition independent of translation and rotation using an ultrasonic sensor array, invariant moment vectors and SOFM(Self Organizing Feature Map) neural networks is presented. Using invariant moment vectors of the acquired 16×8 pixel data of square, rectangular, cylindric and regular triangular blocks, 3D objects could be classified by SOFM neural networks. Invariant moment vectors are constant independent of translation and rotation. The recognition rates for the training and testing data were 95.91% and 92.13%, respectively.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2005년도 공동학술대회 논문집
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• pp.267-272
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• 2005

충북 장풍, 전남 광양, 충남 임천의 세 개의 폐광산을 대상으로 물리탐사를 수행하였다. 연구는 산성광산배수에 의한 침출수의 유동경로, 매립된 광미 및 폐광석의 파악, 광산 폐수의 배수관 탐지, 갱도와 인공차수막의 효과를 파악하는데 목적을 두었다. 상관 해석 결과 물리탐사 자료는 물시료 분석 자료(수소이온농도, 전기전도도, 중금속, 황산이온)와 잘 일치하고 있다. 산성광산배수에 의한 침출수의 유동경로는 전기비저항 및 자연전위탐사로 탐지 가능한 반면에 폐광석, 산성광산배수의 배수관, 인공차수막 등은 탄성파 굴절법, 전기비저항, 지하투과레이다탐사를 통해 효과적으로 파악되었다.