• Title/Summary/Keyword: 목포해역

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Numerical Simulation of Tides of Gwangyang Bay Using Moving Boundary Treatment (이동경계를 고려한 광양만의 조석ㆍ조류 모의)

  • 민인기;오병철;전인식
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 2003.08a
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    • pp.158-163
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    • 2003
  • 한반도 서ㆍ남해안은 크고 작은 만과 해빈, 삼각주, 하구, 조간대 등 다양한 연안해역이 잘 발달 되어 있다 평균조차는 서해안 남부에서 약 3m로 북쪽으로 갈수록 증가하여 군산 부근에 6m, 인천 부근에서 약 8m에 달하며, 남해안의 평균조차는 부산 1.2m, 진해 2.1m, 충무 2.6m, 삼천포 3.0m, 여수 3.3m, 완도 3.5m, 목포 3.7m로 조석 간만의 차가 크게 나타나서 연안해역에 폭넓은 조간대가 형성되어 있다. (중략)

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Management of water quality by estimated the point source in Mokpo inner bay (점 오염원 조사를 통한 목포 내항의 수질관리)

  • Kim, Do-Hee;Lee, Ha-Ju
    • Proceedings of KOSOMES biannual meeting
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    • 2006.05a
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    • pp.121-128
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    • 2006
  • The results of COD researched on August of 2004 were 6.8 ppm in North Mokpo inner Bay, 4.4 ppm in front of YongSang Bank and 4.6 ppm in front of ShinAn Beach Hotel which is over III level Marine-Environmental Standard. The other five stations sea water quality of Mokpo inner bay were reached II-III level. Concentration of total nitrogen range from 1.23 ppm to 3.56 ppm and total phosphorous was range from 0.07 ppm to 0.12 ppm which were II-III level. This results show that the Mokpo inner bay is unsuitable for aquaculture and growth of fish and for use of marine resort, it can be only available for industrial and harbour use. In results of estimated point source flow into Mokpo inner bay, the occupation ratio from YoungSang river in total inflow of TN and TP were up to 49-89 % respectively. It is indicate that in order to improve the water quality of MokPo inner bay have to control the discharge from YoungSang river first of all, then control the discharge from North Harbour domestic wastewater treatment, InAm river and NamHae domestic wastewater treatment.

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Seasonal and Year-to-year Variations of Water Quality in Mokpo Harbor Area by the Long-term Monitoring (목포항 주변 해역에서 장기 모니터링을 통한 수질의 계절 및 년간변동)

  • Park, Joong-Hyun;Park, Seong-Yoon;Lee, Yong-Hwa;Choi, Da-Mi;Lee, Sang-Yong
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.11 no.2 s.23
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    • pp.97-102
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    • 2005
  • Seasonal and year-to-year variations of water quality were observed at six stations in Mokpo Harbor area between 1997 and 2004. Water quality(salinity, pH, DIN and DIP) was variable between years. Salinity was significantly low in 1998, while nutrient concentrations were significantly higher in 1998 than other years. Water temperature, salinity, DO, COD and DIP concentrations exhibited clear seasonal variations, and these seasonal trends reflected seasonal changes in fresh water discharge from Youngsan river mouth. Water temperature, COD and DIP were significantly higher in August, while salinity and DO reached minimum values in August. In the station 1(Youngsan river mouth), waters with low salinity are subject to high nutrient inputs from Youngsan river, while in the station 6 (outside from Mokpo harbor) waters are primarily oceanic Relationship between water quality parameters indicates that salinity is the primary factor influencing the COD, DO, pH, Chlorophyll a and nutrient concentrations in Mokpo harbor area.

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Management of Water Quality by the Point Source in Mokpo Inner Bay (점 오염원 조사를 통한 목포 내항의 수질관리)

  • Kim, Do-Hee
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.12 no.4 s.27
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    • pp.273-283
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    • 2006
  • The results of COD concentration on August of 2004 were 6.80 ppm in North Mokpo Inner Bay, 4.42 ppm un front of YongSang Bank and 4.60 ppm in front of ShinAn Beach Hotel which is over III level Marine Environmental Standard. The others researched five stations sea water quality of Mokpo inner bay are reached II-III level. The concentration of total nitrogen range from 1.23 ppm to 3.56 ppm and total phosphorous concentration was range from 0.07 ppm to 0.12 ppm which are to be II-III level. This results show that the Mokpo inner bay is unsuitable for aquaculture and for use of marine resort, it can be only avaliable for industrial and harbour port use. In this study, we researched 12 point source flow into Mokpo Inner bay. The rate from YoungSang river in total inflow of TN was up to 70-93 % and rate of TP was up to 31-91 % respectively. In this results, we have to control the discharge from YoungSang river first of all then control the discharge from North Harbour domestic wastewater treatment, InAm river and NamHae domestic wastewater treatment in order to improve the water quality of Mokpo Inner bay.

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A Study on the Assessment of Environment Stress in Mokpo Approaching Channel (목포항 출입항로의 환경스트레스 평가에 관한 연구)

  • KIM Chol-Seong;JONG Jae-Yong;Park Sung-Hyun
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.12 no.3 s.26
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    • pp.211-218
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    • 2006
  • Recently, many ships such as fishing boats, cargo ships, high speed ferry boats are visiting Mokpo harbor. In particular, many marine accidents have been occurred at this area due to the narrow channel, a thick fog, the existing of the shallow waters etc. However there is no suitable ships' routeing system which takes account of today's traffic situations in this area. This study aims at the settling of hazardous factors to mitigate the danger to vessels in Mokpo harbor and to secure the safety of maritime environment.

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The Changes of Coastal Water Level due to the Development of Mokpo Harbor and Construction of Daebul Industrial Complex (목포항 개발 및 대불 산업단지 조성에 따른 연안해역 해면변화)

  • 정명선;이중우
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 1991.06a
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    • pp.37-44
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    • 1991
  • 영산강 하구언 방조제의 건설로 인한 항만 및 이의 인접해역 해면의 변화는 예상한 바 있으며 실제 여러개소에서 월 2회정도의 주기로 목포 구항부근 상업지역에서 해면상승에 따라 주기적으로 침수되는 현상이 나타나고 있다 목포항의 영산강 하구언 방조제 조성으로 인한 조류성분중 최고기록을 가진 수로에서는 6kts 정도로 감소된 것으로 보고되고 있으나 주위자연환경 변화에 따른 수면 상승 및 해수면의 주기적인 변화 등에 대한 상세한 언급 및 깊이 있는 분석은 회피되어왔다. 수자원의 효율적관리를 위해 하구언 방조제는 이미 건설되었고 앞으로 대규모의 항만개발과 대불산업단지조성을 위해 추가 3개의 만입해안해역에 댐으로 해역을 막아 매립공사를 추진하고 있다 그러나 이 지역에 대한 분석은 타당성의 여부만을 강조한 상업적 용역이 이루어지고 있고 장래 개발에 대해 학술적이고 실질적인 문제점 추출과 해결방아네 대해서는 무시하거나 경시한 바가 많다 더구나 태풍 저기압 등과 같은 자연재해를 고려한 분석은 시도되지 못하고 있다 따라서 개발전후의 현상에 대한 상세한 자료 및 현장 조사와 극한 상태를 고려하여 개발에 따른 수위상승 부진동, 조류 수질등 이해역의 변화요소를 수집하고 분석하며 과학적 접근방법에 기초를 둔 수치모델의 실험을 포함하여 현장관측 및 측정자료를 검증하는 것이 필수적이라고 사료되어 종합분석의 한단계로 여기서는 하구언 및 하구간척(Land Reclamatic of Estuary barren)으로 해역축소에 따른 해면변화의 실제현상을 조사하여 정리하고 이를 수치모델을 통해 시뮬레이션하여 보았다 이는 종합개발의 좋은 기초자료로 이용됨은 물론이로 이지역의 개발에 기여할 것으로본다.적절하게 가정된 지반의 응력-변형률 관계와 간극수압특성에 의하여 고려되었다. 그 결과 응력 및 변위가 심하게 발생하는 지역은 황색 점토층이었으며 이로부터 황색 점토층에서 부터 파괴면이 생성되어 다른 지역으로 전파되었음을 유추할 수 있었다.form trap with 2.88[eV] deep of injected space charge from the chathode in the crystaline regions. The origin of ${\alpha}$$_2$ peak was regarded as the detrapping process of ions trapped with 0.9[eV] deep originated from impurity-ion remained in the specimen during production process of the material, in the crystalline regions. The origin of ${\beta}$ peak was concluded to be due to the depolarization process of "C=0"dipole with the activation energy of 0.75[eV] in the amorphous regions. The origin of ${\gamma}$ peak was responsible to the process combined with the depolarization of "CH$_3$", chain segment, with the activation energy of ca

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A Study on the Establishment of Allowable Criteria for Sailing Ships at Offshore Wind Farms (해상풍력발전단지해역 선박 통항 허용기준 설정에 관한 연구)

  • Ohn, Sung-Wook;Lee, Chang-Hyun;Kim, Cheol-Seong
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.24 no.7
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    • pp.841-847
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    • 2018
  • Since global energy consumption and demand for energy have dramatically risen, a focus on environmental problems and sustainability has become more important. Clean and renewable energy sources such as offshore wind power generation have received attention among new renewable energy options as alternative energy resources. Due to maintenance and operational perspectives, offshore wind farms have been planned for installation in many coastal waters. However, development of offshore wind farms faces interference from existing maritime traffic along the planned areas. In order to safely and effectively govern marine traffic in the vicinity of wind farms and inner areas, standard criteria are suggested to allow vessels to sail the internal waters of offshore wind farm areas. Therefore, the purpose of this study is to establish allowable criteria for sailing vessels and safety zones for offshore wind farms by investigating the local regulations of various offshore wind farm cases overseas. The commended inner safety zone of wind farms is proposed to be a distance of 150 % of the rotation diameter of the wind turbine rotor and a distance of 200 m from the outer wind turbine for the outer safety zone. Besides this, the allowable criteria for sailing vessels within a wind farm is proposed to have an air draft of 14.47 m south-west wind farm sea areas for a minimum margin to avoid hull contact through evaluation of the tide and height of a wind turbine. further studies will be needed to establish vessel sailing criteria among adjacent offshore wind farms as well as vessel sailing criteria within a single offshore wind farm.

A study on the relocation strategy of the control line considering the marine pollution risk index and control capacity (해양오염 위험지수와 방제능력을 고려한 방제선 재배치 전략에 관한 연구)

  • Song, Youn-Hee;Lee, Gi-Whan
    • Journal of Digital Convergence
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    • v.20 no.5
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    • pp.547-557
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    • 2022
  • The numbers of occurrences and the amount of spills of marine oil pollution have increased, and accordingly, it is necessary to secure additional control capabilities. Therefore, it was intended to present an empirical basis for improving the overall idle capacity through the relocation of control ships existing in each region. First, the marine pollution index was derived and the control capability compared to the marine pollution index of each region was compared to examine the appropriateness of the deployment of control ships. The marine oil pollution risk index was derived by multiplying the nine items that cause marine pollution by the weight derived by experts. We checked the control capacity (A) compared to the marine pollution risk index (F) for each sea area. Mokpo (F:13.4, A:1.9), Busan (F:14.3, A:6.4), and Yeosu (F:21.5, A:16.6) are the areas that lack control capabilities compared to the marine pollution risk index. On the other hand, the areas that have room for control compared to the marine pollution risk index for each sea area are Masan (F: 5.9, A:13.3), Gunsan (F:1.7, A:8.3), and Jeju (F:2.7, A:6.9). Therefore, for improving the standardized control capacity proportional to the risk of marine pollution nationwide, it is suggested that the control ships of Masan, Gunsan, and Jeju should be relocated to Mokpo, Busan, and Yeosu, which lack control capacity.

물때별 해상교통량 분석

  • Yu, Sang-Rok;Jeong, Cho-Yeong;Yun, Cheong-Geum;Jeong, Jae-Yong;Im, Jeong-Bin
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 2015.07a
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    • pp.319-321
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    • 2015
  • 특정 물때, 특정 시간대에 다수 어선의 입 출항은 해상교통관제사 및 항해사에게 많은 위험부담이 된다. 본 연구는 목포항의 물때별-시간대별에 따른 교통패턴을 분석하였다. 연구 결과, 업종별 안강망, 자망 어업에 따라 교통량의 차이를 보였다. 또한, 물때별로 최대 30%까지 교통량의 차이를 보였으며, 목포구 만곡부에서는 항로 역행의 통항패턴을 보였다. 본 연구의 결과는 해역이용자에게 입 출항시 항행참고 지침 및 교육 자료로 활용될 것으로 기대된다.

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Tidal Changes in the Harbor due to the Development of Mokpo Coastal Zone (목포해역 개발에 따른 항내 조석변화)

  • Jeong, M.S.;Jeong, D.D.;Shin, S.H.;Lee, J.W.
    • Journal of Korean Port Research
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    • v.11 no.1
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    • pp.113-120
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    • 1997
  • Tidal changes in Mokpo harbor and its adjacent coastal waters caused by the coastal development including the construction of the Youngsan, Youngam, and Gumho Estuary Barrages had been predicted previously. Since then, the construction work for these estuary barrages had been completed and it was available to get water level variations from the continuous measurement at the Mokpo tidal station. This study deals with the analysis of water level variation from the observed data by the harmonic analysis and mathematical treatment. Some comparisons between the observed water level changes and the predicted by the numerical model are made, which was not supported before. The result shows that the trend of the water level changes are following well the previously predicted variations.

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