• Title/Summary/Keyword: 외해 구조물

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Plane Experiment Study on Drainage Capacity of Sluice Gate by Slope and Length of Apron (Apron 경사 및 길이에 따른 수문구조물 배수능 평면실험 연구)

  • Yoon, Kwang-Seok;Yeo, Kyu-Dong
    • Proceedings of the Korea Water Resources Association Conference
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    • 2005.05b
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    • pp.1031-1035
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    • 2005
  • 조력발전 건설사업에서 우선적으로 고려되어야 할 사항은 조수간만에 의해 외해부와 조지부 사이를 이동하는 해수를 적절히 소통시키는 것이다. 즉, 조력발전소에서 수문구조물의 목적은 주어진 조건 하에서 계획된 유량을 충분히 그리고 안전하게 배제시키는 것이다. 본 연구에서는 수문구조물에 대한 Apron의 길이와 경사의 변화에 의한 외해 조위와 시화호 수위차 조건에 따른 유량계수를 구해 배수능력과 유$\cdot$출입부, 외해, 시화호 및 큰가리섬 주위의 흐름 특성을 검토하고자 하였다. 이를 위해 시화호를 실험대상으로 하여 구조물을 중심으로 외해측으로 1,000m, 시화호측으로 500m, 폭 1,500m의 범위를 선정하였다. 수리모형을 1대50의 축척비로 제작하였다. 표 1은 실험별 Apron과 수문구조물의 제원을 나타내며, 수문구조물은 7기로 이루어졌다. 시화호의 흐름은 관성력과 중력이 지배력이 되며, 이때 상사법칙은 Froude 상사법칙을 적용할 수 있다. 실험III은 실험II에서 Apron의 경사를 1대10에서 1대5로 수정한 실험으로 수위조건은 외해측 -2.530 EL.m이고, 시화호측은 -1.603EL.m이다. 유량계수를 산정하기 위하여 6개 실험조건을 기본계획에서 제시된 수위-조위 조건에서 수위차 및 통수유량을 분배하여 결정하였고 유량계수 산정식에 따라 구조물의 유입부와 유출부에서 유속-면적법에 의해서 유량을 측정하였다. 그리고 국부평면 실험모형에서의 전체적인 해류의 흐름을 분석하기 위해 2차원 유속을 측정하였다. 또한, 유$\cdot$출입부 안정성을 검토하기 위해 Apron 지점과 수문구조물 지점에 3점법으로 유속을 측정하였으며, 색소를 이용하여 유황을 관찰하였다. 시화호와 외해의 수위차가 1.011 m일 때의 전체 수문구조물을 통과하는 유량을 비교한 결과, 실험II 및 실험III의 통과유량은 각각 $10,924m^3/s$$10,075m^3/s$로서 실험 I의 $2,757m^3/s$에 비해 통수능이 많이 개선되었음을 알 수 있다.

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Development of Hybrid Three Dimensional Beach Deformation Model and Its Application (복합 3차원 해빈변형모델의 구축과 그 적용)

  • Shin Seung-Ho;Hong Keyyong
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.7 no.4
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    • pp.199-206
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    • 2004
  • Construction of a large offshore structure in coastal area may cause serious morphological changes for a wide region ranging from shoreline to offshore behind the structure. Shin et at. [2000] and Shin and Hong [2004] identified the sediment transport patterns behind the large offshore structure through a series of three dimensional movable bed experiments. In present study, a hybrid three dimensional beach deformation model was suggested based on those sediment transport mechanisms revealed by experimental results of the preceding studies. The model was verified by the results of the three dimensional moveable bed experiments and they agreed well not only in reappeared tombolo in shoreline side but also in the erosion and deposition region behind offshore structure. In addition, the model was applied to real beach deformation problem, which was occurred by construction of artificial offshore islands, and it validates the applicability of the model.

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An Experimental Study of Sediment Transport Patterns behind Offshore Structure (외해 구조물 배후의 표사이동에 관한 실험적 연구)

  • Shin Seung-Ho;Hong Keyyong
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.7 no.4
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    • pp.207-215
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    • 2004
  • Recently, securing a vast land in the land region becomes more difficult and efforts to seek its alternation in the sea area have been increased. As a consequence, the coastal region has been faced to extensive beach erosion problems. In planning offshore structures such as artificial islands, it is necessary to forecast the influence of the structure construction exerting on the beach erosion of the adjacent coast. In the present study, the sediment movement pattern behind offshore structure was examined through a series of three dimensional movable bed experiments, so as to develop the numerical model which forecasts morphological change including beach erosions. The experimental results reveal that the sediment movement patterns of the beach line side and the depth region are separated at a certain boundary line. In details, at the beach side including swash zone the sediment movement becomes dominant, which is governed by a relation between depth contours and incident wave directions, while at the depth region the bed load and suspended load due to the orbit motion of waves are carried by nearshore currents, and both movements are clearly separated at a specified boundary that is related to partial standing wave from the beach. It is expected that these results can be effectively used for verification of a numerical model on morphological change of the coast.

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Experimental Study for Beach Process by Construction of Offshore Structure (외해구조물 건설에 따른 해빈 변형에 관한 실험적 연구)

  • 이중우
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.12 no.2
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    • pp.96-106
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    • 2000
  • Though the recent years, large scale structures have been built on offshore for utilization of coastal ocean space as offshore airport and marine terminals. Sometimes, those big scale structures, however, happened to act as significant barriers against waves and severe beach erosion would take place on the coast. The present study deals nearshore topography changes affected by construction of an offshore structure with different distance from the shore. The series of three dimensional movable bed experiments have been examined in detail. Moreover, in order to make clear the relation of nearshore currents and local erosions behind offshore structure, the nearshore currents are calculated by Boussinesq equation model and compared with the same scale condition of the physical model experiments.

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Helmholtz 공명원리를 이용한 해수교환형 방파제의 성능해석

  • 조일형
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 1998.09a
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    • pp.84-87
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    • 1998
  • 본 연구에서는 음향학에서 음파를 제어하는데 주로 이용되는 헤름홀츠 공명장치의 원리를 방파제에 응용하였다. 외해에서 발생된 입사파는 Fig.1에 보여진 입구를 가진 공명 구조물(Resonant Structure)을 만나면 에너지 일부는 입구를 통하여 방사(Radiate)되며 또 일부 에너지는 입구를 통하여 공명 구조물 안으로 방사된다. 공명 구조물 안으로 들어온 파의 주파수와 공명 구조물의 고유 주파수(Natural Frequency)들 중 첫 번째 공진 모드(Resonance Mode)의 주파수가 일치되면 구조물 내부에서의 파는 크게 증폭된다. (중략)

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Wave Field Analysis around Permeable Breakwaters (투과성 방파제 주변의 파랑장 해석)

  • 곽문수;이기상;편종근
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 2002.08a
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    • pp.49-55
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    • 2002
  • 항만을 계획함에 있어서 방파제는 가장 대표적인 계획요소로서 주된 목적은 외해로부터 내습하는 파랑을 차단하여 항내의 정온수역을 확보하는 것이다. 그러나 불투과성 방파제의 경우는 페쇄성이라는 특성 때문에 연안에서의 물질순환 체계가 구조물 건설전의 환경과는 근본적으로 달라져 심각한 환경부작용이 초래되어 왔다. 육상으로부터 유입된 유기물질이 외해로 확산되지 못하고 항내에서 누적됨으로서 부영양화가 일어나며 항외에서의 산소를 포함하고 있는 해수의 유입이 차단됨으로서 항내는 만성적인 산소부족현상이 발생하게 된다. (중략)

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A Study on the development of the aquaculture fishcage for the open sea (외해용 양식 구조물 개발에 관한 연구)

  • Shin, Jong-Keun;Jeong, Seong-Jae;Yoon, Ji-Hyun
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • v.29 no.1
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    • pp.285-290
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    • 2005
  • Until now, korean aquaculture industry has been grown largely from a quantitative viewpoint. However, an increase of quantity has caused lots of problems producing a derived effect recently. Nearly 82% of korean aquaculture farms had been installed mainly at inshore of the southern sea and also sewage, factory wastes, high density of fishcage at the limited area and autoinfection have deteriorated inshore fisheries. The offshore have been on the rise for the solution to these problems since it has clear seawater reduces the environmental pollution with much current. As a matter of fact, the existing inshore fishcage facilities have trouble advancing to the offshore due to the rough environmental conditons such as a high sea, strong currents etc.; therefore, it is necessary to develop a new cultivating equipment fit the open sea conditons. In this research, the theoretical study and experimental analysis have been carried out for the fishcage design of the structure which is able to use at the open sea.

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Impact of the coastal structures on the water circulation near Gusipo coast, Yellow Sea, Korea (서해 구시포 해안에서 해수유동에 미치는 구조물의 영향)

  • Kim, Cha-Kyum;Park, Il Heum
    • Journal of Korea Water Resources Association
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    • v.55 no.11
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    • pp.865-875
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    • 2022
  • Field measurements and numerical simulations using EFDC model were performed to quantify the changes of water circulation near Gusipo coast located in the Yellow Sea of Korea to estimate the impact of the construction of the coastal structures (jetty, groin, Gusipo port and bridge). The model predicted tide and tidal currents agreed reasonably well with the measurements. The maximum currents during spring tide near the Gusipo Beach (GB) have the range of 20~40 cm/sec whereas those off the GB range from 60 to 80 cm/sec. The typical patterns of tidal current show parallel with the local isobath. Tidal currents flow northeastward during the flood tide whereas the currents during the ebb tide flow southwestward. The current speeds at shielded waters after the construction of coastal structures strongly decreased as compared with those before the construction. The tidal volume due to the construction of coastal structures was estimated using the depth averaged velocity for 24 hours of spring tide. Tidal volume after construction of coastal structures was compared with initial state (before construction). Tidal volume at present state (after construction of jetty, groin, Gusipo port and bridge) decreased by 28.4% as compared with that of the initial state. The volume after construction of jetty and groin decreased by 21.3%, and the volume after construction of Gusipo port and bridge decreased by 9.8%.

Experimental Study on Hydraulic Characteristics of Wave Dissipating New Armor Unit (새로운 소파블록의 수리특성에 관한 실험적 연구)

  • 김인철;박영우;유철희;권혁민
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 2003.08a
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    • pp.87-97
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    • 2003
  • 외해로부터 내습하는 파랑을 차단하므로서 해안의 세굴, 침식 등을 방지하고 항내의 정온을 유지하고 항만시설물을 보호하기 위하여 축조되는 방파제, 호안 등의 구조물 형식에는 경사제, 직립제, 혼성제 등 여러 가지가 있다 이 중 경사제는 표면을 파력에 충분히 대항할 수 있는 크기의 사석이나 콘크리트 블록을 쌓아 파랑을 경사면에서 쇄파시켜 에너지를 소멸시킴으로서 소파기능을 발휘한다. (중략)

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Transport of Sandy Sediments in the Yellow Sea off Tae-An Peninsula, Korea (한반도 황해 중부 태안반도 근해 사질퇴적물의 이동)

  • 최동림;김성렬
    • 한국해양학회지
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    • v.27 no.1
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    • pp.66-77
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    • 1992
  • Tidal sand ridges and sand waves are well developed in the Yellow Sea off Tae-An Peninsula, Korea. Their transport directions were inferred based on high resolution seismic profiles, surficial sediment characteristics and tidal regime. Tidal sand ridges are asymmetric, with long axes parallel to or slightly oblique to the dominant NE-SW tidal current direction. They show steep south and/or southeast flanks, which are in concordance with the apparent direction of internal cross-bedding in the south. Holocene sediments occur in accordance with distributional patterns of tidal sand ridges. These features indicate that Holocene active tidal sand ridges move toward the open sea in southeast, south and southwest direction. Sand waves which are distributed in flat sea floor with depth of about 40-60m show also asymmetric forms with a steep east-to-northeast face. Surficial sediments in the sand wave field are characterized by well sorted fine sands compared with poorly sorted adjacent areas. The sand waves appear to undergo easterly or northeasterly landward movement.

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