• Title/Summary/Keyword: 굴절파

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Parabolic Approximation Model for Wave Deformation Prediction in the Shallow Water (천해파랑 변형예측을 위한 포물형 근사 모델)

  • 이동수;김숭경
    • 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)

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Atomization Technology of Liquid Fuels (액체연료의 미립화 기술(1))

  • 류정인
    • 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.

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Numerical Study of Wave Prediction Using a Ray Tracing Technique (파향선 추적기법을 이용한 파랑예측에 관한 연구)

  • 조원철
    • 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.

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Determination of photorefrative constants in LiNbO$_3$ using second harmonic generation (제2고조파발생을 이용한 LiNbO$_3$의 중요 광굴절상수측정)

  • 김봉기;이범구
    • Korean Journal of Optics and Photonics
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    • v.12 no.3
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    • pp.230-234
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    • 2001
  • We report a simple method for determining photovoltaic constant and conductivities of any photorefractive crytals which have no inversion symmetry by utilizing the electric field dependence of non-phase-matched second harmonic generation. New theoretical expression for the electric field dependence of Maker fringes is derived and space charge field can be determined using this from the observed change of intensity of second harmonic wave. The photovoltaic constant, dark conductivity and photoconductivity are easily deduced from an analysis of the measured relaxation behavior of space-charge field at two different light intensities. We demonstrate this method for $LiNbO_3$ at 514.5 nm.4.5 nm.

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Nonlinear guided-wave properties in planar waveguides with two nonlinear bounding thin films (비선형 박막으로 둘러싸인 평면 광도파로에서의 비선형 도파광 특성)

  • 정종술;송석호;이일항
    • Korean Journal of Optics and Photonics
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    • v.7 no.2
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    • pp.136-141
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    • 1996
  • We present a novel description of TE nonlinear guided waves in planar waveguides with two nonlinear bounding thin films. The nonlinear dispersion relations of the nonlinear waveguides are obtained by adopting the nonlinear transfer matrix. The optical properties obtained from these equations include: the power dependence of mode indices, the transition of the field maximum location, and the power distribution. The planar waveguide with self-focusing nonlinear layers shows the optical bistability of power-dependent mode indices, and the critical powers for the optical bistability increase with decreasing thickness of the nonlinear layers. The power distributions display the optical bistabilities, similar to those of nonlinear Fabry-Perot etalon.

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Geophysical Surveys for the Detection of Gallery and Geomembrane at the Imcheon Abandoned Mine (임천 폐광산의 지하갱도와 인공차수막의 탐지를 위한 지구물리탐사)

  • 김지수;한수형;이경주;최상훈
    • Economic and Environmental Geology
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    • v.36 no.6
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    • pp.501-510
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    • 2003
  • Several geophysical surveys(electrical resistivity, electromagnetic, seismic refraction, CPR) were conducted to primarily investigate the gallery and the geomembrane at an abandoned mine(Imcheon mine). The subsurface structure mapped from seismic refraction survey mainly consists of three velocity layers(>1000 m/s, 1000∼2000 m/s,<2000 m/s). Top of the bedrock, whose velocities exceed 2000 m/s, appears to be at depth of 7.5∼10m. Higher resistivities (of ten thousands-hundred of thousands ohm-m) are interpreted to be associated with a open(cavities) gallery. The events at depth of approximately 0.5∼0.7m in GPR sections are probably caused by high-density-poly-ethylene geomembrane. Taking into consideration of the differences in the spatial resolution between georadar and electrical surveys, the events of geomembrane correspond to the top of the high resistivities at depth of about 2m. The segments, characterized with the higher conductivities in the electromagnetic data and the lower resistivities in the electrical resistivity data, are probably associated with surface water or tear zone of geomembrane.

Geophysical surveys for delineation of leachate flows from AMD and buried rock wastes in Kwangyang abandoned mine (광양 폐광산의 산성광산배수의 유동경로 및 폐광석 탐지를 위한 지구물리탐사)

  • 김지수;한수형;윤왕중;김대화;이경주;최상훈;이평구
    • Economic and Environmental Geology
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    • v.36 no.2
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    • pp.123-131
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    • 2003
  • Geophysical surveys(electrical resistivity, self-potential, seismic refraction, GPR) were conducted to investigate the physical properties of the subsurface, and to delineate the flow channel of leachate from a AMD(acid mine drainage), buried rock wastes and tailings, and drainage pipes at an abandoned mine(Kwangyang mine). Especially in rainy season the sites appear to be abundant in AMD leachate, characterized by electrical conductivities of 0.98-1.10 ms/S. Electrical resistivity sections indicate that the leachate flows running in two directions at southern part rise up through the narrow fracture zones at the central part and contaminates the surrounding soil and stream. Such schematic features at the anomalous zone are well correlated with negative peaks in self-potential data, the limited penetration depth in GPR data and low velocity zone in seismic refraction data. Shallow high-resistivity zone is associated with the buried rock wastes which cause the diffractions in GPR image. In addition, the events at depth of approximately 1-1.25 m in GPR sections must be the metal pipes through which AMD is drained off to the inner bay.