• 제목/요약/키워드: Intermediate depth

검색결과 262건 처리시간 0.029초

항주파고의 특성에 관한 연구 (A study on the characteristics of shipwaves)

  • 강성진;김선규;손창배;김종성;홍정혁;김창제
    • 한국항해항만학회지
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    • 제31권5호
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    • pp.339-344
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    • 2007
  • 항주파는 해안침식, 호안 결괴, 하역곤란 및 어선 등 소형선박의 동요를 발생시키며, 최근에는 고속으로 항행하는 수상오토바이, 모터보트 및 여객선 등이 수영객, 낚시꾼 및 어로작업중인 어민에게 위협이 되고 있다. 본 연구에서는 실험 및 이론적으로 항주파고의 전파특성을 검토하였으며 상대수심이 얕은 수역에서 발생한 항주파가 천해역으로 전파하는 경우 파고증가율이 커지며, 수심이 얕을수록 유속이 느린 흐름이 존재하여도 파가 진행하지 못함을 알 수 있다.

제한수역에서의 동유체력에 대한 고찰 (On the Characteristics of Hydrodynamic Forces in a Restricted Water)

  • 조일형;최항순
    • 대한조선학회논문집
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    • 제29권1호
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    • pp.55-60
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    • 1992
  • 본 논문에서는 선형포턴셜이론을 이용하여 제한수로에 놓인 2차원 주상체에 작용하는 동유체력과 운동응답의 특성을 고찰하였다. 유체영역을, 수로입구영역 그리고 수로영역으로 구분하여 우선 각 영역에서 해를 독립적으로 구한 다음 이를 인접영역의 해와 정합시켜 완전해를 구하였다. 수로의 길이보다 대략 4배가 긴 파장의 입사파는 수로내 유동을 공진시킨다. 이때 주상체에 작용하는 부가질량은 음의 값을 갖게 되며 동유체감쇠력은 급격한 변화를 보이고 주상체의 수평운동은 최대가 됨을 밝혔다.

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Investigation on site conditions for seismic stations in Romania using H/V spectral ratio

  • Pavel, Florin;Vacareanu, Radu
    • Earthquakes and Structures
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    • 제9권5호
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    • pp.983-997
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    • 2015
  • This research evaluates the soil conditions for seismic stations situated in Romania using the horizontal-to-vertical spectral ratio (HVSR). The strong ground motion database assembled for this study consists of 179 analogue and digital strong ground motion recordings from four intermediate-depth Vrancea seismic events with $M_w{\geq}6.0$. In the first step of the analysis, the influence of the earthquake magnitude and source-to-site distance on the H/V curves is evaluated. Significant influences from both the earthquake magnitude and hypocentral distance are found especially for soil class A sites. Next, a site classification method proposed in the literature is applied for each seismic station and the soil classes are compared with those obtained from borehole data and from the topographic slope method. In addition, the success and error rates of this method are computed and compared with other studies from the literature. A more in-depth analysis of the H/V results is performed using data from seismic stations in Bucharest and a comparison of the free-field and borehole H/V curves is done for three seismic stations. The results show large differences between the free-field and the borehole curves. As a conclusion, the results from this study represent an intermediary step in the evaluation of the soil conditions for seismic stations in Romania and the need to perform more detailed soil classification analysis is highly emphasized.

Bi-stability in a vertically excited rectangular tank with finite liquid depth

  • Spandonidis, Christos C.;Spyrou, Kostas J.
    • Ocean Systems Engineering
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    • 제2권3호
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    • pp.229-238
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    • 2012
  • We discuss the bi - stability that is possibly exhibited by a liquid free surface in a parametrically - driven two-dimensional (2D) rectangular tank with finite liquid depth. Following the method of adaptive mode ordering, assuming two dominant modes and retaining polynomial nonlinearities up to third-order, a nonlinear finite-dimensional nonlinear modal system approximation is obtained. A "continuation method" of nonlinear dynamics is then used in order to elicit efficiently the instability boundary in parameters' space and to predict how steady surface elevation changes as the frequency and/or the amplitude of excitation are varied. Results are compared against those of the linear version of the system (that is a Mathieu-type model) and furthermore, against an intermediate model also derived with formal mode ordering, that is based on a second - order ordinary differential equation having nonlinearities due to products of elevation with elevation velocity or acceleration. The investigation verifies that, in parameters space, there must be a region, inside the quiescent region, where liquid surface instability is exhibited. There, behaviour depends on initial conditions and a wave form would be realised only if the free surface was substantially disturbed initially.

3차원 인체 해부도 작성을 위한 칼라 볼륨 데이터의 입체 영상 재구성 (Reconstruction of Color-Volume Data for Three-Dimensional Human Anatomic Atlas)

  • 김보형;이철희
    • 대한의용생체공학회:의공학회지
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    • 제19권2호
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    • pp.199-210
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    • 1998
  • 본 논문에서는 전산화된 인체 해부도의 필수 기능인 3차원 볼륨 가시화 기법을 제시한다. 오브젝트순서에 기반한 광선 추적과 런-길이 인코딩의 장점을 이용한 이진 볼륨 렌더링 기법은 경계 추출된 칼라 슬라이스로 구성된 볼륨 데이터를 이용하여, 특정 하드웨어의 도움없이 일반 PC에서 대화식 수준의 속도로 3차원 가시화를 수행한다. 이 방법은 이진 볼륨 렌더링을 위해 필요한 이진 깊이 화상의 구성을 간소화하고 새루운 법선 벡터 계산 방법을 적용하여 렌더링 시간의 향상을 꾀하였다. 이와 함께 화질의 손실 없이 관련 데이터의 양을 줄이는 3D경계 인코딩 방법도 제시한다. 본 논문에서 제시한 렌더링 방법의 대화식 수준의 속도와 인코딩 방법의 정보 저장면에서의 효율성은 PC에서 운용될 수 있는 의학 해부도 응용 프로그램의 개발을 보다 가속화할 것이다.

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해저구조물에 대한 비선형분산파의 변형 (Deformation of Non-linear Dispersive Wave over the Submerged Structure)

  • 박동진;이중우
    • 한국항만학회지
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    • 제12권1호
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    • pp.75-86
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    • 1998
  • To design a coastal structure in the nearshore region, engineers must have means to estimate wave climate. Waves, approaching the surf zone from offshore, experience changes caused by combined effects of bathymetric variations, interference of man-made structure, and nonlinear interactions among wave trains. This paper has attempted to find out the effects of two of the more subtle phenomena involving nonlinear shallow water waves, amplitude dispersion and secondary wave generation. Boussinesq-type equations can be used to model the nonlinear transformation of surface waves in shallow water due to effect of shoaling, refraction, diffraction, and reflection. In this paper, generalized Boussinesq equations under the complex bottom condition is derived using the depth averaged velocity with the series expansion of the velocity potential as a product of powers of the depth of flow. A time stepping finite difference method is used to solve the derived equation. Numerical results are compared to hydraulic model results. The result with the non-linear dispersive wave equation can describe an interesting transformation a sinusoidal wave to one with a cnoidal aspect of a rapid degradation into modulated high frequency waves and transient secondary waves in an intermediate region. The amplitude dispersion of the primary wave crest results in a convex wave front after passing through the shoal and the secondary waves generated by the shoal diffracted in a radial manner into surrounding waters.

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금호지구 저습답의 암거배수효과에 관한 연구(I) (Studies on Wet Paddy Field Underdrainage Improvement in the Gum-Ho Area (I))

  • 김조웅;김시원
    • 한국농공학회지
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    • 제22권4호
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    • pp.82-95
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    • 1980
  • This paper complies the results of the studies so far made on the subsoil improvement of subsurface drainage systems for wet paddy fields (those were located in the Gum-Ho area in Kyung Buk province) which had poor permeability and a high water table. In general, a drainage problem is an excess of water on the ground surface which can effect the productivity and bearing capacity of the soil. With drain pipe systems, (According to their depths and spacing) it may be possible to correct that problem. The experimentation consisted of three test plots, two of which included drain pipe systems with varing depths and width spacing of the pipes. The third plot (C) was an ordinary plot being exempt of a drain pipe system. In detail, the depth of plot A was 80 cm, and the width spacings began at 2. Om and increased by 2. Om up to 10. 0m. The depth of plot B was 60cm and the width spacing was the same as plot A. These tests were performed to research specific details; such as crop yeild, bearing capacity of the soil, the amount of underdrainage, surface cracks, root distribution, the water table level, the consumptive water depth and the soil moisture content. The test period lasted three years, from 1977 thru 1979. The results obtained were as follows: 1. During the test period, the weather conditions for the area tested were in accordance with the annual average for that area. Furthermore the precipitation factor during the spring cultivation season, the intermediate drainage period and the harvest drainage period was of optimum conditions for controling surface cracks, because of less precipitation than evaporation. 2. The difference in the level of the ground water table in plots A and B was hardly noticable, but the difference in the test plots and the ord. plot was greatly noticable. The test plots (A, B) were 30 to 40cm lower than the ordinary plot. On the whole, the ground water table of the ord. plot always stayed at a level of 15-20cm beneath the surface of the soil, the ground water table of the test plot A showed The difference in the depth of the pipe lower than the test plot B, while the test plots showed a remarkable descending effect. 3. The soil temperature in plot A was slightly core than in plot B with a difference of 0. 47$^{\circ}$C, but plot A was 1. 6$^{\circ}$C higher than the ord. plot during the flooding period, but after drainage the temperature difference climed to 2. 0$^{\circ}$C. 4. During the 3rd test year, the values of the cracks were recorded with the values of 59cm in plot A, 42cm in plot B and 15cm in the ordinary plot. Plots A and B had increased 2.5 times the value of the first year while the ordinary plot had remained the same. 5. The root weight of the rice was measured at a value of 77.2 gr. for plot A, 73.5 gr. for plot B and 65.3 gr. for the ord. plot. Therefore, the root growths in plots A and B were much more energetic than in the ord. plot. 6. The consumptive water depth measured during the 3rd year resulted in the values of 26. 0mm per day for plot A, and 24.9 mm per day for plot B, respectively. Therefore, both plot A and plot B maintained the optimum consumptive water depths, but the ordinary plot only obtained the value of 12.3 mm per day, which clearly showed less than the optimum consumptive water depth which is 20 to 30 mm/day. 7. The soil moisture content is in direct relationship to the ground water level. During drainage, test plot A decreased in its ground water level much more rapidly than the other two plots. Therefore, plot A had a much less soil moisture content. But this decreased water level could be directly effected by the weather conditions. 8. The relationship between the bearing capacity and the soil moisture content were directly inversely proportional. It can be assumed that the occurence of soil creaks is limited by the soil moisture content. Therefore, the greater the progress of the surface creaks resulted in a greater bearing capacity. So, tast plot A with a greater amount of surface cracks than the other test plots resulted in a greater bearing capacity. But, the bearing capacity at the harvest season could be effected by the drainage during the intermediate drainage period and by the weather conditions. 9. Comparing the production of the test plots to the ord. plot; there was an increased value of 840kg for plot A, 755kg for plot B and 695kg for the ord. plot in the rough rice. Therefore, plot A had an increase of 20% over the ordinary plot. The possibility of producing double crops was investigated. The effects on barley production in the test plots showed a value of 367kg per 10 acres, which substantiated the possibility of double crops because that value showed an increased value over the average yearly yield for those uplands. 10. So as a result, it can be recommended that by including a drain pipe system with the optimum conditions of an (80cm centimeter) depth and a (l0m) spacing will have a definite positive effect on the over all production capacity and quality of wetpaddy fields.

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도면 자동 벡터화를 위한 선의 굵기 인식이 가능한 세선화의 전처리 기법 (A Preprocessing Scheme of Thinning Capable of Lines' Thickness Recognition for the Automated Vectorizing of Maps)

  • 전일수;원남식;부기동
    • 한국지리정보학회지
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    • 제2권2호
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    • pp.1-8
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    • 1999
  • 세선화 결과에서 원래 선의 굵기 정보는 도면 자동 벡터화 시스템을 구현하는데 유용하게 사용될 수 있다. 본 연구는 세선화 결과에서 원래 선의 굵기 정보를 표현할 수 있는 세선화의 전처리 기법을 제안하였다. 제안된 기법에서는 입력 도면에서 선을 구성하는 각 화소들에 대해서 그것이 주변화소들로부터 둘러싸인 정도를 나타내는 깊이를 계산하고, 세선화 결과에서 골격선의 깊이 정보를 보고 원래 선의 굵기를 알 수 있게 하였다. 제안된 기법을 구현하여 등고선에 대해 실험한 결과, 골격선의 깊이 정보로부터 그 선이 주곡선인지 계곡선인지 쉽게 구별할 수 있었다.

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축대칭 함몰지형 위를 진행하는 파의 변형에 관한 완경사 방정식의 해석 해 (Analytic Solution to Mild Slope Equation for Transformation of Waves Propagating over an Axi-symmetric Pit)

  • 정태화;서경덕
    • 한국해안해양공학회지
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    • 제18권4호
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    • pp.308-320
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    • 2006
  • 축대칭 함몰지형 위를 진행하는 파에 관한 완경사 방정식의 해석 해를 유도하였다. 함몰지형 내부에서의 수심은 함몰지형 중심으로부터의 거리의 덕에 비례하여 변한다. 변수 분리법을 사용하여 지배 방정식을 상미분 방정식으로 전환하였으며, Hunt(1979)의 근사식을 사용하여 방정식의 계수들을 양함수의 형태로 변환하였다. 마지막으로 Frobenius 급수를 사용하여 해석 해를 유도하였다. Hunt 근사식의 특성 상 본 연구에서 유도된 해석 해는 천해와 심해에서는 정확하고 중간수심에서는 덜 정확하다. 해석 해의 타당성을 검토하기 위하여 수치 모델 결과와 비교하였다. 또한 해석 해를 이용하여 함몰지형의 형상과 상대수심 등을 변화시키면서 다양한 조건에 대한 파랑 변형을 검토하였다.

라인 레이저 기반 3차원 스캐너에서 투영을 이용한 고속 3D 메쉬 생성 (Fast 3D mesh generation using projection for line laser-based 3D Scanners)

  • 이경미;유훈
    • 한국정보통신학회논문지
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    • 제20권3호
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    • pp.513-518
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    • 2016
  • 본 논문은 라인 레이저 기반 3차원 스캐너에서 투영을 이용한 고속 메쉬 생성 방법을 제안한다. 3차원 공간에서의 메쉬를 생성하기 위한 가장 알려진 방법은 3차원의 점을 4차원으로 변환하고 4차원 컨벡스 헐(convex hull)을 구축하는 방법을 활용한다. 이런 방법은 많은 수의 점 데이터를 가지는 3D 스캔 결과에서는 메쉬를 만들 때 시간이 많이 요구된다. 제안하는 방법에서는 라인 레이저 스캐너에서 중간에 얻어지는 (${\theta}$, y, z)축의 점 정보를 투영하여 얻어진 (${\theta}-y$) 2차원 깊이 지도를 메쉬 생성에 활용한다. 제안된 방법은 2D 영역에서 수행되기 때문에 메쉬를 구성하는 시간이 상당히 단축된다. 제안하는 방법을 평가하기 위해서 라인 레이저 기반 스캐너의 중간 데이터를 이용하여 실험을 진행하였다. 실험 결과는 제안된 방법이 기존방법보다 고속 메시 생성에서 우수함을 보여준다.