• 한국지형학회지
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• 제28권4호
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• pp.15-30
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• 2021

This study analyzed the changes in land-cover and sedimentary environment before and after flooding through drone images and sediment analysis for the Seomjin River Chimsil Wetland. The results showed that the area of some land-covers such as sand bar, grass, and trees were continuously changed. The acidity level of the sediments in the Seomjin River Chimsil Wetland was weakened gradually by flooding and EC was also decreased. The levels of organic matter, effective phosphoric acid, and CEC, however, were fluctuating depending on branches, which seems to be the result of landization as new sedimentary environment was developed and vegetation was settled after the flood. Average mean size of river sediments was found to be fine sand, and it exhibited various particle size characteristics from granule to medium silt depending on the location. As the sedimentary environment changed due to the effects of floods and typhoons, the particles were granulated or grain refined depending on the position. In the Seomjin River Chimsil Wetland, there were factors that could interfere with geomorphic development and sedimentary environment, contamination sources in and around the wetland, and natural threat factors. Therefore, in this study, a conservation and management plan was proposed to remove these threat factors and to preserve the scarcity, naturalness, and dynamics of Seomjin River Chimsil Wetland.

• 한국해양공학회:학술대회논문집
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• 한국해양공학회 2006년 창립20주년기념 정기학술대회 및 국제워크샵
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• pp.431-434
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• 2006

This study reviews the properties of coastal ocean and Seomjin River estuary spaces then define some MGIS(Marine Geographic Information System) related terminologies for clarifying the scope of MGIS boundaries. Therefore, we show the three-dimensional circulation of MGIS-based Seomjin River Estuary integrating three-dimensional POM model and observed data.

• 한국주거학회논문집
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• 제11권3호
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• pp.43-51
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• 2000

This study aims to find the characteristics of the folk houses in the upper area of Seomjin river in the view point of generating housing floor plans by their human and natural elements of environment. Because they are formed differently as them and have the characteristics as the houses in the upper area of Seomjin river. Seomjin river flows from mid-west area of the Korean peninsula to the southern sea. This is about 212.3km long and the fourth in the south of the Korean peninsula. It is surrounded high mountains in the upper area and makes open field in the mid and lower area of river. The study is surveyed and analyzed to the folk houses of the middle and lower class people in the area of Seomjin river. Because they have been formed by their natural and human elements of environment gradually. They are 35 houses - 13 in Jinan-kun, 4 in Imsil-kun, 10 in Namwon city, 10 in Sunchang-kun. They are analyzed by their floor plans and their spatial relations. The result of this study is that they are made by their natural and human elements of environment. There are some houses with semi-several wings and with storage that are appeared in the mountain village. It reflects that they are surrounded by high mountains. And there are some houses with wooden floor room that are appeared in the area of river little in the area of mountain. To prevent wind from the river the houses are layouted as a form . open ㄴ type, open ㄷ type, and their wall is made of stone and planted bamboo trees around their houses.

• 한국해양생명과학회지
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• 제5권2호
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• pp.99-106
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• 2020

섬진강 및 영산강 하구의 환경변화에 따른 식물플랑크톤의 상관성을 조사하기 위해, 2016년 4월부터 11월까지 매월 현장조사를 수행하였다. 조사 정점에서 용존무기질소(DIN, dissolved inorganic nitrogen)와 규산염(DSi, dissolved silicate)은 강으로부터 유입되는 담수의 영향을 강하게 받았다. 특히 섬진강하구에서는 DIN과 DSi가 내측에서 점차적으로 외해로 확산되는 특성을 보였으나, 영산강 하구는 복잡한 지형학적 특징으로 내측과 외해와 잘 섞이지 않았다. 식물플랑크톤 분류군별 지표색소를 활용하여 분류군별 분포를 조사하였다. 규조류 지표색소인 fucoxanthin은 섬진강, 영산강 하구에서 각각 평균 0.61±1.00 ㎍ l^-1, 0.76±1.22 ㎍ l^-1로 나타나, chlorophyll a 이외 다른 색소에 비해 2배 이상 높은 농도를 나타내었다. 와편모조류 지시색소 peridinin은 현미경 검경결과와 와편모조류의 출현양상과 유사한 경향을 보였다. 소형 녹조류, 은편모조류, 남조류는 현미경으로 관찰되지 않았으나, 각각의 지표색소 chlorophyll b, alloxanthin, zeaxanthin은 일정하게 검출되어, 하구역 내 상기와 같은 종의 출현가능성을 시사하였다. 결과적으로 본 연구의 색소분석을 통하여, 하구역 상류의 환경 특성이 연안내만생태에 영향을 미칠 수 있다는 것을 밝혔다. 특히 영산강 하구는 인공적인 배수갑문의 독특한 특성으로, 대량방류되는 담수에 의하여 연안내만에서 관찰되는 담수종이 일시적으로 분포하였다.

• 환경생물
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• 제24권2호
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• pp.160-165
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• 2006

The purpose of this study was to ascertain the prey composition and utilization of the Eurasian otter, Lutra lutra, in the ecosystem conservation region of the Seomjin River. The study was conducted for a 12-month period from March 2003 to February 2004 by spraints analysis and an investigation using artificial holts. We found seasonal variation in the number of spraints and composition of prey items. Fish were the main prey items throughout the period (82%), and other prey items included birds (14%), amphibians (2%) and arthropods (1%). In addition to prey identification, we investigated habitat utilization by otters through spraints distribution. The traces of otters were discovered in five of the six total artificial holts. However, the utilization of the artificial holts in the study area seemed to be limited as evidenced by the low frequency of traces in the holts.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2023년도 학술발표회
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• pp.526-526
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• 2023

Water circulation plays a crucial role in regulating the salinity of estuaries, which is essential for the survival of estuarine organisms. Changes in freshwater inflows or sea level can have significant impacts on the distribution and abundance of species within these ecosystems. To better understand these dynamics, this paper presents a study of water circulation and salinity distribution in Seomjin River estuary using the Finite Volume Coastal Ocean Model (FVCOM) numerical model. An extreme scenario was simulated to assess the potential impact of tidal currents and river flow discharge on circulation and salinity distribution. The results of this study have important implications for managing estuarine ecosystems and conserving their associated biodiversity.

• 한국방재학회 논문집
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• 제9권1호
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• pp.115-121
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• 2009

섬진강 하류의 하상변동 특성 분석 및 하상변동을 예측함으로서, 하도 및 유역관리에 효과적으로 이용하도록 하였다. 하상변동 특성 분석에 필요한 자료(단면, 하상구성물질, 기점수위, 조도계수 등)는 섬진강하천정비기본계획에서 실측 및 분석한 것을 활용하였다. 또한 하상변동 예측은 HEC-6 모형으로 수행하였다. 본 연구의 주요 연구 결과를 요약하면 다음과 같다. 섬진강 하류 하상변동의 주요인은 수문인자의 변화에 따른 것이라기보다는 과도한 하상골재 채취 때문으로 판단된다. 마찰속도와 대표 입경의 관계와 무차원소류력과 대표입경의 관계를 토대로 하도안정성을 정성적으로 분석한 결과 섬진강 하류 하상은 대부분의 구간에서 상승하는 경향을 나타내고 있다. 섬진강 하도의 대부분의 지점에서 2003년의 하상구성물질은 1989년에 비해 자갈의 구성비가 높아지고 모래의 구성비가 작아졌다. 하상변동을 예측한 결과 섬진강 하류의 하상은 하구에서 약 9 km 지점까지 1.5 m 내외로 상승하고, $9{\sim}21\;km$ 구간은 1 m 내외로 상승과 저하가 반복되며, $22{\sim}25\;km$ 구간은 0.5 m 내외로 하강할 것으로 예상된다. 이러한 결과로 볼 때 섬진강 하류 구간의 하상은 대체로 점점 상승할 것으로 판단된다. 다만, 본 연구의 하상변동 예측은 인위적인 골재채취가 없다는 가정 하에 수행된 것이므로, 과거와 같이 하상에서 대규모 골재채취가 진행되면 본 연구의 예측 결과와는 상이하게 하상이 저하되는 결과를 초래할 것이다.

• 수산해양교육연구
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• 제28권1호
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• pp.172-179
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• 2016

The study of Mobile MGIS (Marine Geographic Information System) based on the Android Mobile Platform is mainly performed on effective methodologies which transform real world data to computing world data. Mobile GUI system has its own target on reliable data service by acquisition of geometric information using EFDC (Environmental Fluid Dynamics Code) Model, accurate measurement and graphical visualization. Even simple visualizations can aid in the interpretation of complex hydrodynamic relationships that are frequently encountered in the marine environment. The Mobile MGIS provides an easy way for hydrodynamics geoscientists to construct complex visualizations that can be viewed with free software. This study proposes a Mobile GUI MGIS using EFDC Model result of Seomjin River estuary. Finally, we design a Seomjin River estuarine Coastal Waters Mobile MGIS integrating above data models. It must adds more ecological information and the various service item for approach more easily in order to user.

• 한국수산과학회지
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• 제37권4호
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• pp.323-329
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• 2004

In situ particle size and volume concentration of suspended sediment was measured at the mouth of Seomjin River Estuary In February 2001, using an optical instrument, 'LISST-100'. Time variation of in situ particle size and concentration shows: (1) during ebb tide, Seomjin River supplies relatively fine-grained particles with less-fluctuated, compared to during flood tide, and well-behaved concentrations following the tidal cycle; and (2) during flood tide, relatively coarse-grained particles with highly variable in size distribution and concentration flow upstream from Kwangyang Bay. This explains a poor correlation $(r^{2}=0.10)$ between sediment concentration and beam attenuation coefficient during flood and a high degree of correlation $(r^{2}=0.80)$ during ebb tide. Relatively fine grained and well defined, monotonous size distribution may promote the correlation between concentration and beam attenuation coefficient due to optical homogeneity of particles during ebb tide. Abundance of large aggregates with time-varying size and shape distributions may be mainly responsible for variations in optical properties of the sediment during flood tide, and thus may confound the relationship between the two variables. The difference in particle sizes and shapes between flood and ebb tides can also be observed on SEM images.

• 한국어류학회지
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• 제20권3호
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• pp.179-189
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• 2008

섬진강과 동해로 유입하는 하천인 오십천, 양양남대천 및 주수천에서 2007년 3월부터 10월까지 은어를 채집하여 체장분포와 생식소 성숙도를 조사 비교하였다. 조사 결과 산란시기에 수온은 $17{\sim}23^{\circ}C$사이였으며, 평균 수온이 높은 섬진강산 은어는 9월 하순 부터 11월 초순 사이에 산란이 이루어졌고, 동해로 유입하는 하천에 서식하는 은어집단들은 그보다 1개월 빠른 8월 하순부터 10월 중순에 주로 산란이 이루어졌다. GSI와 HSI의 변화 역시 수온변화와 유사하게, 섬진강산의 은어가 동해안산의 은어보다 먼저 증가하였다. 동일시기에 성숙한 암컷 생식소의 조직학적 관찰에서도 섬진강에 서식하는 은어집단에서 동해안에 분포하는 은어집단에 비해 늦게 산란기에 도달하는 것을 확인하였다. 포란수는 조사지점별로 차이를 보이지 않았으며 체장에 비례하여 증가하였다. 조사된 은어의 집단별 체장의 차이는 하천의 길이에 따라 증가하였으며, 하천규모가 긴 섬진강(유로연장: 223.86 km, 유역면적: $4,911.89km^2$), 오십천(55.76 km, $393.78km^2$), 양양남대천(54 km, $474.09km^2$), 주수천 (21.1 km, $141.47km^2$) 순으로 $194{\pm}15.3mm$, $185{\pm}15.5mm$, $142{\pm}11.8mm$, $136{\pm}16.7mm$를 나타내 차이를 보였다.