• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.28-28
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• 2019

강 하구의 민물과 바닷물이 만나 형성되는 기수역 생태계는 독특한 환경적 가치를 지니고 있다. 낙동강 하구는 우리나라의 대표적인 철새 도래지로 풍부한 생태자원을 지닌 곳이지만, 하굿둑 건설로 기수역이 사라진 이후 기수역 생태계가 갖고 있는 고유의 생태적인 특성이 감소하였다. 한편, 낙동강 하굿둑 건설은 염해피해 방지 및 부산, 울산, 창원 등의 지역에 추가적인 용수공급을 가능하게 도왔다. 이에 낙동강 기수역 생태계 복원을 위한 하굿둑 개방과 용수공급 및 염해피해 방지 등을 위한 하굿둑 운영에 대한 논의가 지속되어 왔다. 낙동강 하구관리에 대한 합리적인 의사결정을 위해서는 하굿둑 건설 및 운영에 따른 편익과 동시에 낙동강 하구 기수역의 생태 환경적 가치도 함께 고려해야한다. 이에 본 논문에서는 낙동강 하구의 기수역 생태 복원에 초점을 맞추어 이와 관련된 환경적 가치를 조건부 가치측정법이라는 경제학적 기법을 적용하여 추정하고자한다. 전국 800가구를 무작위로 추출하여 일대일 개별면접을 통해 낙동강 기수역의 생태복원에 대한 지불의사액을 조사하였다. 이 정보는 낙동강 하구관리에 대한 의사결정시 활용할 수 있다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.24 no.1
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• pp.106-127
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• 2019

This study aims to understand spatio-temporal variations of macrozoobenthos community in Han River (HRE), Geum River (GRE), and Nakdong River estuaries (NRE) of Korea, sampled by National Survey of Marine Ecosystem. The survey was seasonally performed at a total of 20 stations for three years (2015-2017). Sediment samples were taken three times with van Veen grab of $0.1m^2$) areal size and sieved through a 1 mm pore size mesh on site. A total of 1,008 species were identified with 602 species in HRE, 612 in GRE, and 619 in NRE, showing similar number of species between estuaries. Mean density was $1,357ind./m^2$, showing the high in NRE ($1,357ind./m^2$), mid in GRE ($1,357ind./m^2$), and low in HRE ($1,127ind./m^2$). Mean biomass was $116.8g/m^2$, showing similar variations to density ($174.2g/m^2$ in NRE, $129.0g/m^2$ in GRE, $49.0g/m^2$ in HRE). Polychaeta dominated in number of species and density in three estuaries. Biomass-dominated taxon was Mollusca in HRE and GRE, and Echinodermata in NRE. Polychaetous species dominated all three estuaries over 4% of density, such as Dispio oculata, Heteromastus filiformis and Aonides oxycephala in HRE, Heteromastus filiformis and Scoletoma longifolia in GRE, and Pseudopolydora sp. and Aphelochaeta sp. in NRE, showing various density between estuaries. Community structure was determined by various environmental variables among estuaries such as mean grain size and sorting (HRE), salinity and mean grain size (GRE), and salinity, dissolved oxygen, loss on ignition and mud content (NRE). Our study demonstrates the application of different measures to manage ecosystems in three estuaries. HRE needs to alleviate sedimentary stressors such as sand mining, land-filling, dike construction. Management of GRE should be focused on fresh water control and sedimentary stressors. In NRE, monitoring of dominant benthos and process study on hypoxia occurrence in inner Masan Bay are necessary.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2018.11a
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• pp.36-37
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• 2018

낙동강 하구역의 퇴적환경은 육성기원 퇴적물과 해성기원 퇴적물에 따라 다양하고 복잡하게 이루어진다. 낙동강 하굿둑이 건설된 이후의 퇴적환경 특성을 파악하기 위하여 해양공학회(2003)와 수자원공사(2016)의 자료를 수집 분석하였다. 2003년과 2016년의 표층퇴적물 분석결과, 낙동강 하구는 전반적으로 사질퇴적물이 우세하고 분급도가 양호하고 중앙입경 보다 조립질의 퇴적물이 우세하게 분포되는 것으로 나타났다. 기존 연구결과와 금회 연구결과로부터 2003년 이후 낙동강 하구 퇴적환경은 평형상태를 이루고 있는 것으로 판단되며, 낙동강 하굿둑 유출 유사량과 외해측 파랑에 의한 영향이 크게 받고, 창조시의 약화된 유속으로 인하여 니질퇴적물의 이동이 줄어든 것으로 판단된다. 또한, 니질퇴적물이 우세한 구간은 사주와 갯골 부근의 간사지로, 이로 인한 낙동강 하구역의 퇴적우세 현상은 지속될 것으로 판단된다

• Proceedings of the Korea Committee for Ocean Resources and Engineering Conference
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• 2004.05a
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• pp.298-302
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• 2004

본 연구에서는 낙동강 하구역 해역에서의 폭풍 해일의 특성 및 이를 고려한 외해 압사파랑특성을 고찰하고 연안사주 전면의 입사파랑과 퇴적 특성과의 상호 관계를 고찰하였으며 천해역의 파랑변형을 예측할 수 있는 다방향 불규칙파 묘형을 구성하고 폭풍 해일고를 수심조건에 고려함으로써 하구역 해역에서의 파랑 변형계산을 2차원 평면수치모의실험을 수행하였다. 낙동강 하구역에서 서측에 위치하는 진우도 전면해역이 무명도 전면해역보다 약 1.0배에서 2.0배 크게 파고분포를 나타내었다. 이는 입사하는 파랑의 공간 분포가 사주전면에서 공간적으로 차이가 남을 나타내는 것으로 사주의 퇴적작용에 영향을 줄 것이라고 판단된다.

• Journal of the Korean Society for Marine Environment & Energy
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• v.12 no.3
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• pp.188-196
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• 2009

This study conducted numerical simulations to analyze the wave characteristics(distribution) depending on the directional changes of waves in the Nakdong river estuary by using SWAN(Simulating WAves Nearshore) model. The results from the tests are summarized as below. The wave height rates are generally highly distributed with the incident waves from the S, SSE, SSW, SE, SW in sequence. When the waves from the S, SSW, SSE directions are predominant, the bigger waves were observed in front of sandbars. According to the results of the wave steepness against the wave direction, at the east coast of Gadeok island(northwest of Nakdong estuary), where has mild seabed slopes, the wave height rates distribute in the range of 0.4~0.6; the wave height rates over the west coastal region of Dadeapo(southeast of Nakdong estuary) are 0.5~0.6. The wave height rate tends to be rapidly decreased over the east region of Nakdong river estuary rather than its west region.

• Journal of the Korean Society of Marine Environment & Safety
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• v.17 no.3
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• pp.185-189
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• 2011

To predict the deposition characteristic in the Nakdong river estuary, the material budget of Suspended Solid(SS) was investigated with the amount of Nakdong river discharge being set as dry season and flood season. The results of material budged of SS in dry season and flood season were 60,708 kg/day(inflow) and 306,892 kg/day(outflow), respectively.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.26 no.3
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• pp.184-195
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• 2014

After building the dyke in Nakdong River Estuary, mixing of freshwater inflow to ocean and seawater to upstream is controlled by operating the sluice gates. Mixing and convergence of seawater and freshwater by opening the sluice gates, have a major impact on the circulation of seawater in the Nakdong River Estuary. Field measurement was carried out to study the characteristics of the estuary flow and environment of each channel of the Nakdong River Estuary. Vertical salinity distribution and residual current is different from each channel by the river discharge and topographic changes.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
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• 2018.11a
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• pp.38-39
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• 2018

낙동강 하구 하류역의 지형변화는 장기간에 걸쳐 변화가 발생하고, 이러한 지형변화의 메커니즘을 파악하는 것은 하구의 관리방안과 처리방법 등을 연구하는데 있어서 매우 중요하다. 본 연구에서는 낙동강 하구 하류역의 지형변동에 관한 기초자료를 수집 분석하였으며, 이를 근거하여 지형변화 예측실험을 수행하였다. 실험결과, 하굿둑 건설과 부산신항 건설 등의 대규모 개발사업으로 인한 해수면 축소로 인한 유속감소로 인하여 전반적인 퇴적우세 현상이 지속되는 것으로 나타났다. 또한, 해빈류 실험결과 울타리선 남쪽과 동서쪽으로 지형 발달 및 성장이 지속될 것이라 판단된다.

• Journal of the Korean Society for Marine Environment & Energy
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• v.8 no.4
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• pp.186-192
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• 2005

We investigated the deposition characteristics and mass transport flux estimation of the Nakdong estuary, Korea. To understand the effects of the tidal current circulation that influences estuary terrain changes, we used a 2D numerical model to map seawater circulation under three different situations, with the level of river flow being set as none or flood. The net-water flux of the cross-sectional area between sandbars (known as dung) was estimated. From our review of previous research, we know that the development of local sandbars shifted from the west to the east side of the estuary after the construction of the Nakdong River dike. Current development is occurring mostly at the Bakhap-dung near Tadea. The seawater circulation pattern over this large-scale area of tidal na is brings changes related to the quantity of the outflow from the Nakdong River. Based on the calculated results for the net-water flux of the cross-sectional area, we see very strong accumulation in local waters around Jangjiado, Bakhapdung, and Tadae under flood river flow conditions, but accumulation in local waters around Jinudo under the other states of flow. Consequently, in the Nakdong estuary, the main sensitive regions that are affected by changes in the flow of river discharge are the local waters around Jangiado, Bakhapdung, Tadae, and Jinudo.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.20 no.4
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• pp.372-389
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• 2008

In this study, we formed a detailed grid at the estuary area of the Nakdong and collected the surface sediments. Particle size analysis and comparison with existing data were conducted to investigate the characteristics of seasonal and long-term changes in the sediments. As a result of investigation, the distribution of the sediments showed a great change per season and was greatly influenced by the quantity of outfall discharge at the Nakdong estuary barrier and the incident wave climate. The sandy sediments showed dominant movement toward the front of Jinwoodo west of the estuary area of the Nakdong due to the influence of the ENE wave, the annually-dominant wave. And the muddy sediments showed deposition by being moved toward the deep open sea along with a current. The present conditions of the sediments at the estuary area of the Nakdong showed great differences from the results of previous studies.