• Title/Summary/Keyword: Coastal water

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The Change of Coastal Water Area due to the Development of Mokpo Harbor and Construction of Daebul Industrial Complex(II) (木浦港 開發 및 大佛産業團地 造成에 따른 沿岸海域 變化(II) - 海上環境을 中心으로 -)

  • 이중우;정명선;민병언
    • Journal of the Korean Institute of Navigation
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    • v.16 no.1
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    • pp.37-64
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    • 1992
  • A study on the changes of the oceanographical environment caused by Mokpo coastal zone development was carried out. Special emphasis was placed on the clarification of the water level changes and coastal current structure and influence of the environmental factors on the coastal area. In order to understand the structure oceangraphical environemnt, such as water temperature, salinity, suspended solids, pH, dissolved oxygen, chemical oxygen demand, biochemical oxygen demand, distribution of bottom sediment, tide and current were measured. To investigated the structure of tide and current for the future development, a numerical analysis was carried out. In certain zones, it was found to be flooding problems near the lowlying commercial area.

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Characteristics of Cochlodinium polykrikoides Bloom in Southeast Coastal Waters of Korea, 2008 (2008년 남해동부해역의 Cochlodinium polykrikoides 적조발생 특성)

  • Lim, Weol-Ae;Lee, Young-Sik;Park, Jong-Gyu
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.14 no.3
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    • pp.155-162
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    • 2009
  • To characterize the initiation, propagation and termination of Cochlodinium polykrikoides blooms in the southeast coastal waters of Korea, 2008, we analyzed the data set of phytoplankton composition, physical and chemical water properties, and meterological data. C. polykrikoides bloom in 2008 were long lasting and restricted to the coastal area with a low density. Our results indicate that C. polykrikoides blooms were affected by the atypical cold waters occurring in east-south coastal water in the early July. The cold water masses probably protected the free living cells of C. polykrikoides from entering into the coastal area from offshore waters as a pelagic seed population. The low density blooms of small scale established possibly by the germination of C. polykrikoides cyst in shallow coastal bottom could have not spread over because of the weak wind and low nutrient concentrations caused by severe drought in July and September.

Characteristic of Coastal Soil Improvement by MICP Technology Using Sea Water (해수를 사용한 MICP 기술의 연안 지반 개량시 발생하는 특성 분석)

  • Sojeong Kim;Jinung Do
    • Journal of the Korean Geosynthetics Society
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    • v.22 no.2
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    • pp.13-21
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    • 2023
  • Mean sea level has recently been rising due to global warming causing coastal erosion. As Korea is peninsula, the land loss due to coastal erosion is critical. An approach in this study is cementing the coastal area using bacteria, which is called microbially induced carbonate precipitation (MICP). This study tried to see how fresh water and sea water work with MICP as a solvent. Ureolytic activity during the MICP reaction was measured with deionized and sea water. A soil column was prepared to evaluate the strength of MICP-treated sand. Sands were treated by MICP with surface percolation method. As the treatmen t style was different with other conventional methods, several methods were proposed to properly evaluate the MICP-treated sand surface. A micro-scale evaluation was performed to assess the mineral structure treated by different solvents. As results, sea water rendered the ureolytic reaction slower. A needle penetrometer worked well to evaluate the MICP-treated sand surface. This study confirmed the utilization of sea water is feasible as the solvent of MICP.

A Waste Load Allocation Study for Water Quality Management of the Incheon Coastal Environment (인천해안의 수질관리를 위한 오염부하량 할당에 관한 연구)

  • Kim, So-Yeon;Choi, Jung-Hyun;Na, Eun-Hye;Park, Seok-Soon
    • Journal of Korean Society of Environmental Engineers
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    • v.27 no.1
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    • pp.43-51
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    • 2005
  • This paper presents a waste load allocation study for the Incheon coastal environment, where a computer model, called AQUASEA, was applied. A finite element mesh was constructed and refined to cover the complicated geometry of Incheon coastal sea. The tidal height at 13 places of Incheon coastal boundary and flow of the Han River were given as an input condition to the tidal simulation. All pollution sources that discharge into Incheon coast were given as input data to the water quality simulation. The modeled parameters include tidal flow and COD(Chemical Oxygen Demand). The model was calibrated and verified with the field measurements. The model results showed reasonable agreements with field measurements in both tidal flow and water quality. Systems analysis showed that the pollution load from the Han River caused recognizable impacts on the water quality of Incheon coast from Yeomhwa waterway to northern area of Younghungdo. The loads from Incheon City affected water quality from the area below Youngjongdo to the area above Jawalldo. The discharge from the Sihwa Lake caused discernible impacts on the coastal zone from the dike outlet to the Incheon harbor, and pollution loads from Kyungkido affected the sea near the Oido. An effective water quality management plan was developed from the waste load allocation analysis of the validated model, that the maximum waste loads can be discharged without violating the water quality standard given in the Incheon coastal environment.

남해연안해역에 있어서 식물플랑크톤 군집의 계절변동 특성과 기초생산 1. 가뭄시 여수해만의 수질환경과 식물색소량 분포특성

  • 윤양호;김성아
    • Journal of Environmental Science International
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    • v.5 no.3
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    • pp.347-359
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    • 1996
  • A study was carried out on the distribution of chlorophyll a and water quality in the dry season in Yosuhae bay and adjoining sea, Southern Korea, in July of 1994. Concentration of salinity and phosphate were lower in the outer bay than in the inner bay. While nitrate and silicate were higher in the former than in the latter. We were identified with coastal waters of origin from China with the lower salinity in outer bay. The China coastal water was characteristic of high nutrients and phytoplankton biomass, such as chlorophyll a. The principal component analysis-(PCA) on the analytical data proved that high density of phytoplankton biomass , occurred under the condition of low salinity and high concentration of nissoived Inorganic nutrients. It is thought that the thermoharine structure and biological produtions of Yosuhae bay were controlled by the China coastal water in the outer bay.

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A study of Robust Diagnostic Model of residual current in coastal sea (연안해역에서 잔차류의 Robust진단 model에 관한 연구)

  • 신문섭;홍성근
    • Proceedings of the Korea Water Resources Association Conference
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    • 1996.05a
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    • pp.683-688
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    • 1996
  • The purpose of this study is to find seasonal variation of the water circulation in the Chenbuk coastal sea region. Chenbuk coastal sea is investigated with use of a robust diagnostic numerical model. Water circulations in four seasons are calculated diagnostically from the observed water temperature and salinity data and wind data from Kunsan mereorologcal station.

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Topographic Relief Mapping on Inter-tidal Mudflat in Kyongki Bay Area Using Infrared Bands of Multi-temporal Landsat TM Data

  • Lee, Kyu-Sung;Kim, Tae-Hoon
    • Korean Journal of Remote Sensing
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    • v.20 no.3
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    • pp.163-173
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    • 2004
  • The objective of this study is to develop a method to generate micro-relief digital elevation model (DEM) data of the tidal mudflats using multi-temporal Landsat Thematic Mapper (TM) data. Field spectroscopy measurements showed that reflectance of the exposed mudflat, shallow turbid water, and normal coastal water varied by TM band wavelength. Two sets of DEM data of the inter-tidal mudflat area were generated by interpolating several waterlines extracted from multi-temporal TM data acquired at different sea levels. The waterline appearing in the near-infrared band was different from the one in the middle-infrared band. It was found that the waterline in TM band 4 image was the boundary between the shallow turbid water and normal coastal water and used as a second contour line having 50cm water depth in the study area. DEM data generated by using both TM bands 4 and 5 rendered more detailed topographic relief as compared to the one made by using TM band 5 alone.

A Numerical Experiment of Tide Changes due to the Development of Land Reclamation near the Youngsan River (영산강지구 대단위간척지 개발로 인한 조석변화에 대한 수치실험)

  • Lee, J.W.;Shin, S.H.
    • Journal of Korean Port Research
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    • v.5 no.2
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    • pp.65-75
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    • 1991
  • Tidal current and water level change in coastal waters are formulated in terms of mathematical models. A systematic discussion of the derivation of a set of governing equations, expressing conservation of mass and momentum is presented. A simplification is introduced by integrating all variables and equations over the total water depth, the Solution of the formulated problem is achieved by using the finite difference method(FDM). The applied study area is taken from Mokpo harbor and its adjacent coastal water which have significant hydrographical changes due to the construction of the estuary barrage and land reclamation work of estuary barren. Some comparisons with the observed current and water level changes the numerical solutions are found to be considerably fit well for the recent coastal water motion.

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An Experimental Study on the Behavior of Muddy Water Lumps Caused by Dropping Soil in Coastal Areas (해역에서 토사침하에 따른 탁수괴 거동에 관한 연구)

  • 신문섭;이종남
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.2 no.4
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    • pp.223-230
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    • 1990
  • Suspended materials during maritime construction works may cause surrounding environmental changes Therefore, it is important to know the behavior of the muddy water lumps caused by dropping soil in coastal areas. Two-dimensional behaviors of the muddy water moving along the inclined boundaries are investigated experimentally, which are the change of height, length, and moving velocity, the properties of movement at the head of muddy water, the coefficient of entrainment and shape, and the accumulation shape. The shape of the muddy water lumps was similar with the slope thermal. Therefore, the moving characteristics were found to be described using turbulence theory.

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