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      https://www.riss.kr/link?id=A102475444

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      The distribution of dissolved oxygen (DO) and its variability in Chunsu Bay were studied. Monthly hydrographic survey and realtime monitoring for water quality conditions were carried out in study area. Vertical distribution of DO shows the formation of hypoxia in the bottom water in the vicinity of the artificial dyke and net cage aquaculture site in summer. Annual mean of DO was 8.4 mg/l, with minimum monthly mean of 6.9 mg/l in July and maximum of 11.2 mg/l in March. Temporal variation of DO at bottom water around the net cage aquaculture site shows pronounced oscillatory characteristics with range of 0.5~7.0 mg/l. Coherency analyses between the tidal range and DO concentration shows that variation of DO is significantly coherent with tidal range at semi-diurnal period with 1~3.5 hours phase-lags. A simple DO budget model was set up to account for the formation of the extreme hypoxic conditions in Chunsu Bay. The governing equation is based on the mass-balance for kinetic process with simplified parameter of source and sink terms of DO. the source term is represented by replenishment through the vertical and horizontal diffusion and mixing. the sink terms comprise function of sediment oxygen demand (SOD) and carbonaceous biochemical oxygen demand (CBOD). The result of numerical solution indicates the dominant role of SOD as the overriding factor against the oxygen supply.
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      The distribution of dissolved oxygen (DO) and its variability in Chunsu Bay were studied. Monthly hydrographic survey and realtime monitoring for water quality conditions were carried out in study area. Vertical distribution of DO shows the formation ...

      The distribution of dissolved oxygen (DO) and its variability in Chunsu Bay were studied. Monthly hydrographic survey and realtime monitoring for water quality conditions were carried out in study area. Vertical distribution of DO shows the formation of hypoxia in the bottom water in the vicinity of the artificial dyke and net cage aquaculture site in summer. Annual mean of DO was 8.4 mg/l, with minimum monthly mean of 6.9 mg/l in July and maximum of 11.2 mg/l in March. Temporal variation of DO at bottom water around the net cage aquaculture site shows pronounced oscillatory characteristics with range of 0.5~7.0 mg/l. Coherency analyses between the tidal range and DO concentration shows that variation of DO is significantly coherent with tidal range at semi-diurnal period with 1~3.5 hours phase-lags. A simple DO budget model was set up to account for the formation of the extreme hypoxic conditions in Chunsu Bay. The governing equation is based on the mass-balance for kinetic process with simplified parameter of source and sink terms of DO. the source term is represented by replenishment through the vertical and horizontal diffusion and mixing. the sink terms comprise function of sediment oxygen demand (SOD) and carbonaceous biochemical oxygen demand (CBOD). The result of numerical solution indicates the dominant role of SOD as the overriding factor against the oxygen supply.

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      참고문헌 (Reference)

      1 O'Connor, D. J, "Water Quality Models: Chemical, Physical and Biological Constituents. In: Estuarine Modeling: An Assessment, EPA Water Pollution Control Research Series" Section 702/ 102-169, 1972

      2 Caddy, J., "Toward a comparative evaluation of human impacts on fishery ecosystems of enclosed and semienclosed seas" 1 : 57-96, 1993

      3 Kuo, A. Y., "Spatial and temporal variabilities of Hypoxia in the Rappahannock River" 14 (14): 113-121, 1991

      4 Karim M. R., "Simulation of eutrophication and associated occurrence of hypoxic and anoxic condition in a coastal bay in Japan" 45 : 280-285, 2002

      5 Shi, Z., "Settling velocities of fine suspended particles in the Changjiang Estuary, China" 22 (22): 245-251, 2003

      6 Covar, A. P., "Selecting the Proper Reaeration Coefficient for use in Water Quality Models" 19-22, 1976

      7 Tengberg, A., "Resuspension and its effects on organic carbon recycling and nutrient exchange in coastal sediments: in situ measurements using new experimental technology" 285 : 119-142, 2003

      8 Sloth, N. P., "Resilience of pelagic and benthic microbial communities to sediment resuspension in a coastal ecosystem" 42 : 405-415, 1996

      9 Howarth, R. W., "Regional nitrogen budgets and reverine N & P fluxes for the drainage to the North Atlantic Ocean: Natural and Human influences" 35 : 75-139, 1996

      10 Thomann, R. V, "Principles of surface water quality modeling and control" Haper & Row publishers 644-, 1987

      1 O'Connor, D. J, "Water Quality Models: Chemical, Physical and Biological Constituents. In: Estuarine Modeling: An Assessment, EPA Water Pollution Control Research Series" Section 702/ 102-169, 1972

      2 Caddy, J., "Toward a comparative evaluation of human impacts on fishery ecosystems of enclosed and semienclosed seas" 1 : 57-96, 1993

      3 Kuo, A. Y., "Spatial and temporal variabilities of Hypoxia in the Rappahannock River" 14 (14): 113-121, 1991

      4 Karim M. R., "Simulation of eutrophication and associated occurrence of hypoxic and anoxic condition in a coastal bay in Japan" 45 : 280-285, 2002

      5 Shi, Z., "Settling velocities of fine suspended particles in the Changjiang Estuary, China" 22 (22): 245-251, 2003

      6 Covar, A. P., "Selecting the Proper Reaeration Coefficient for use in Water Quality Models" 19-22, 1976

      7 Tengberg, A., "Resuspension and its effects on organic carbon recycling and nutrient exchange in coastal sediments: in situ measurements using new experimental technology" 285 : 119-142, 2003

      8 Sloth, N. P., "Resilience of pelagic and benthic microbial communities to sediment resuspension in a coastal ecosystem" 42 : 405-415, 1996

      9 Howarth, R. W., "Regional nitrogen budgets and reverine N & P fluxes for the drainage to the North Atlantic Ocean: Natural and Human influences" 35 : 75-139, 1996

      10 Thomann, R. V, "Principles of surface water quality modeling and control" Haper & Row publishers 644-, 1987

      11 Diaz, R. J, "Overview of Hypoxia around the world" 30 (30): 275-281, 2001

      12 Clarke, S, "Modelling Suspended Sediment Concentrations in the Firth of Forth" 47 : 235-250, 1998

      13 DiToro, D. M, "Mathematical Models of Water Quality in Large Lakes, Part 2: Lake Erie" 90-101, 1980

      14 Lee, J. S., "Massive Sedimentation of fine sediment with organic matter and enhanced benthicpelagic coupling by an artificial dyke in semi-enclosed Chonsu Bay, Korea" 64 (64): 153-163, 2012

      15 NFRDI, "Korea Oceanographic Data Center at National Fisheries Research and Development Institute"

      16 Rouse, H., "Experiments on the mechanics of sediment suspension" Massachusetts 550-554, 1938

      17 Azarovitz, T. R., "Effects on finfish and lobster: in Oxygen depletion and associated benthic mortalities in New York Bight" NOAA 295-314, 1979

      18 Boesch, D. F, "Effects of hypoxia on continental shelf benthos: comparisons between the New York Bight and the northern Gulf of Mexico, in Modern and ancient continental shelf anoxia" spec. publ 27-34, 1991

      19 Choi, Y. H., "Development of Water Quality Predic tion Model in Chunsu Bay" Chungnam National University 2004

      20 Rutherford, J. C., "Deoxygenation in a mobile-bed river" 25 : 1487-1497, 1991

      21 노영재, "Application of Realtime Monitoring of Oceanic Conditions in the Coastal Water for Environmental Management" 한국해양과학기술원 39 (39): 148-154, 2004

      22 Park, K. A., "A numerical model study of hypoxia in the Tidal Rappahannock river of Chesapeake bay" 42 : 563-581, 1996

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