• Geophysics and Geophysical Exploration
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• v.10 no.4
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• pp.314-321
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• 2007

Recently, multi-dimensional joint inversion of geophysical data based on fundamentally different physical properties is being actively studied. Joint inversion can provide a way to obtaining much more accurate image of the subsurface structure. Through the joint inversion, furthermore, it is possible to directly estimate non-geophysical material properties from geophysical measurements. In this study, we developed a new algorithm for jointly inverting dc resistivity and seismic traveltime data based on the multiple constraints: (1) structural similarity based on cross-gradient, (2) correlation between two different material properties, and (3) a priori information on the material property distribution. Through the numerical experiments of surface dc resistivity and seismic refraction surveys, the performance of the proposed algorithm was demonstrated and the effects of different regularizations were analyzed. In particular, we showed that the hidden layer problem in the seismic refraction method due to an inter-bedded low velocity layer can be solved by the joint inversion when appropriate constraints are applied.

• Proceedings of the Korean Society for Noise and Vibration Engineering Conference
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• 2009.10a
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• pp.429-430
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• 2009

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 1996.10a
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• pp.172-175
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• 1996

외해로부터 해안선부근으로 이동하는 파랑은 해저협곡 및 대륙붕과 같은 해저지형의 변화, 방파제와 같은 해안구조물과의 상호간섭 및 파랑상호간의 비선형효과 등에 의해 굴절, 회절, 천수 및 쇄파 등과 같은 변화를 경험한다. 파랑변형의 원인이 되는 여러 변화 중에서 흥미 있고 연구할 가치가 있는 물리적 현상중의 하나는 Bragg 반사이다. (중략)

• Proceedings of the Optical Society of Korea Conference
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• 2007.02a
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• pp.233-234
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• 2007

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 1992.08a
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• pp.84-89
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• 1992

파랑변형 예측모델로서는 타원형 편미분 방정식 형태인 완경사 방정식(Berkhoff, 1972)이 있으며 이는 파랑의 굴절, 회절, 반사등의 변형을 재현할 수 있으나 수치해석상 어려운점이 있으며 많은 기억용량과 계산시간이 소요되어 일반적이지 못한 단점이 있다.(중략)

• Proceedings of the Korean Society for Noise and Vibration Engineering Conference
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• 2013.04a
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• pp.327-328
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• 2013

• Journal of the korean Society of Automotive Engineers
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• v.15 no.4
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• pp.59-68
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• 1993

본 강좌는 지금까지 밝혀진 미립화 방법과 그 실용예를 언급하고 초음파 미립화 기구를 소개하고자 한다. 1. 서론. 2. 미립화 방법과 그 실용예. 3. 음파. 4. 음압 level과 음의 강도 level의 관계. 5. 초음파의 반사, 투과 및 굴절. 6. 정상파.

• 한국문화재보존과학회:학술대회논문집
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• 2004.03a
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• pp.36-36
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• 2004

• Proceedings of the Korean Magnestics Society Conference
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• 2016.05a
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• pp.64-64
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• 2016

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.8 no.3
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• pp.236-245
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• 1996

A wave prediction model is used to estimate the wave spectrum at Ulsan Bay. The Wave model includes the refraction of wave rays according to water depth changes in transient and shallow waters. The calculation of wave refraction is performed from three wave directions : east, southeast and south. Three target locations are selected and the wave spectrum at each location is computed for several uniform wind speeds and directions. The computation results of wave spectrum are compared with PNJ(Pierson, Newmann and James) nomogram and Bretschneider nomogram as well. The model could be used in selection of proper harbor site and in construction of coastal facilities, providing fundamental data in design.