• Journal of Plant Biology
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• 제17권2호
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• pp.53-62
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• 1974

A study was made on the primary production of Lake Changjamot during the spring season of 1973 by menas of the oxygen method. The stratification of temperature and dissolved oxygen were formed in May with the stratified structure of phytoplankton. The range of Secchi disc transparency was from 0.8m to 2.3m during the nine months of this investigation, which was begun in January, 1973. The value was lowest in early June when the phytoplankton blooming reached the peak. The concentration of PO4-P, NH3-N, NO3-N and NO3-N was reduced at the beginning of the phytoplankton blooming and increased again after May except PO4-P. It might have been caused by the inflow of the nitogenous fertilizer from the surrounding agricultural area since May when farming was started. The total amount of chlorophyll-a in the entire water column varied from 25mg/$m^2$ to 277mg/$m^2$ from January till September with the maximum value occurring in early June. These values show a considerable eutrophication of the in comparison with the data obtained in 1969. The daily gross production in the lake varied from a low of 655mgC/$m^2$ to a high of 2,859 mgC/$m^2$ during the spring season and this corresponds to the variation of the amount of chlorophyll. The total amount of daily respiration varied from 650mg C/$m^2$ in winter to 2,307 mg C/$m^2$ in late spring and exceeds gross primary production especially in late May showing the negative balance of daily production and consumption of organic material at that time. In conclusion, Lake Changjamot is a fairly productive and a moderately autotrophic lake and has been eutrophicated much during the past four years.

• 한국물환경학회지
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• 제35권1호
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• pp.28-34
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• 2019

This study analyzed the occurrence pattern of Dolichospermum (= Anabaena) in the Bukhan river from March 2012 to December 2014 in order to identify the genotypes of Dolichospermum. Furthermore, 16S rRNA were analyzed to identify the genotypes of Dolichospermum that occurred in 2015 which were then compared to the reference sequence deposited at NCBI. During this period, the occurrence of Dolichospermum was highly correlated to water temperature. In the year 2012 and 2013, Dolichospermum appeared in Lake Cheongpyeong (CP), Sambong (SB), and Lake Paldang (P2) between July and August. However, in 2014, it appeared in SB and P2, but not in CP. This reduction in appearance was attributed to the decreased inflow to Lake Uiam as a result of low rainfall in 2014 as compared to 2012. In July 2015, the Dolichospermum 16S rRNA genotype was confirmed in five locations; Lake Cheongpyeong (CP), Seojong (SJ), Songchon Sewage Treatment Plant (SC), Joan (P4), and Lake Paldang (PD). Anabaena crassa of spiral clone, A. planctonica of linear clone, and A. circinalis of spiral clone exhibited high genetic similarity with the reference sequence. The 16r RNA genotype showed approximately 3 % sequence variation between the locations and were more similar to each other in locations that were closer.

• 한국물환경학회지
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• 제27권4호
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• pp.445-460
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• 2011

The objective of this study was to construct and assess the applicability of the EFDC model for Saemangeum Reservoir as a 3D hydrodynamic and water quality modeling tool that is necessary for the effective management of water quality and establishment of conservation measures. The model grids for both reservoir system only and reservoir-ocean system were created using the most recent survey data to compare the effects of different downstream boundary conditions. The model was applied for the simulations of temperature, salinity, water quality variables including chemical oxygen demand (COD), chlorophyll-a (Chl-a), phosphorus and nitrogen species and algal biomass, and validated using the field data obtained in 2008. Although the model reasonably represented the temporal and spatial variations of the state variables in the reservoir with limited boundary forcing data, the salinity level was underestimated in the middle and upstream of the reservoir when the flow data were used at downstream boundaries; Sinsi and Garyuk Gates. In turn, the error caused to increase the bias of water quality simulations, and inaccurate simulation of density flow regime of river inflow during flood events. It is likely because of the loss of momentum of sea water intrusion at downstream boundaries. In contrast to flow boundary conditions, the mixing between sea water and freshwater was well reproduced when open water boundary condition was applied. Thus, it is required to improve the downstream boundary conditions that can accommodate the real operations of the sluice gates.

• 한국물환경학회지
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• 제27권5호
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• pp.699-709
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• 2011

The uses of multi-dimensional hydrodynamic and water quality models are increasing to support a sustainable management of large dam reservoirs in Korea. Any modeling study requires selection of a proper spatial dimension of the model based on the characteristics of spatial variability of concerned simulation variables. For example, a laterally averaged two-dimensional (2D) model, which has been widely used in many large dam reservoirs in Korea, assumes that the lateral variations of hydrodynamic and water quality variables are negligible. However, there has been limited studies to give a justification of the assumption. The objectives of this study were to present the characteristics of spatial variations of water quality variables through intensive field monitoring in Daechung Reservoir, and provide information on a proper spatial dimension for different water quality parameters. The monitoring results showed that the lateral variations of water temperature are marginal, but those of DO, pH, and conductivity could be significant depending on the hydrological conditions and local algal biomass. In particular, the phytoplankton (Chl-a) and nutrient concentrations showed a significant lateral variation at R2 (Daejeongri) during low flow periods in 2008 possibly because of slow lateral mixing of tributary inflow from So-oak Stream and wind driven patchiness.

• Proceedings of the National Institute of Ecology of the Republic of Korea
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• 제3권1호
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• pp.13-22
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• 2022

In this study, we investigated the water quality and fish community of the Gudam Wetland, a riverine wetland in the middle-upper reaches of the Nakdong River, during March-October 2020. The main results were as follows: average annual flow rate: 45.0±23.7 m³/s, flow velocity: 0.4±0.3 m/s, water depth: 1.4±0.4 m, water temperature: 17.5±0.8℃, pH: 7.8±0.2, electrical conductivity: 121.6±19.0 ㎲/cm, dissolved oxygen concentration: 11.4±0.9 mg/L, suspended solids concentration: 3.8±2.0 mg/L, and the water quality was classified as Ia (very good). A total of 754 individual fish belonging to 4 orders, 7 families, and 19 species were investigated. Cyprinidae was the dominant group, with 13 species. The dominant species was Zacco platypus (39.3%), followed by Pseudogobio esocinus (17.5%). There were 8 (42.1%) endemic Korean species and 1 exotic species, Micropterus salmoides. Four species were carnivores, six were insectivores, and nine were omnivores. Regarding tolerance to environmental changes, 6 species were tolerant, 11 had intermediate tolerance, and 2 were sensitive. Fish community analysis revealed dominance of 0.57, diversity of 2.04, evenness of 0.69, and richness of 2.72, indicating a diverse and stable fish community. The fish assessment index showed that the assessment class was B (average 62.5), which was higher than that of major streams of the Nakdong River (class C). For sustainable conservation of the Gudam Wetland, management strategies such as minimizing aggregate collection and preventing inflow of non-point pollutants are required.

• Ocean and Polar Research
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• 제45권3호
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• pp.173-183
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• 2023

The barren ground phenomenon in Korea began to occur and spread in the southern coast region and in Jeju Island in the 1980s, and since the 1990s, the damage has become serious in the east coast region as well. Korea has enacted the fisheries resource management act to manage such barren ground through the installation of sea forests among projects for the creation of fishery resources. Until now, projects related to the identification of the cause of barren ground have focused on the density of crustose coralline algae, sea urchins and seaweed, so the original cause of barren ground has not yet been identified. In order to manage barren ground, it is necessary to identify the cause of barren ground. To identify these causes, it is necessary to comprehensively consider i) studies on spatial characteristics such as rock mass distribution, slope and water depth, ii) studies on ecological and oceanographic characteristics such as water temperature, salinity, El Niño, and typhoons etc, iii) studies on organisms such as crustose coralline algae, macroalgae, and sea urchins, and iv) studies on coastal use such as living and industrial sewage inflow. Next, as with regard to legislative policy proposals , it is necessary to prepare self-management measures by the government, local governments, and fishermen as well as address management problems related to the use of sea forests by fishermen after their creation . In addition, when creating a sea forest, a management model for each resource management plan is required, and evaluation indicators and indexes that can diagnose the cause of barren ground and guidelines for barren ground measures should be developed.

• 스마트미디어저널
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• 제11권9호
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• pp.56-63
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• 2022

최근 기후변화에 의한 수온상승, 과다한 영양염류의 유입 및 하천환경의 변화로 인한 주요하천 및 호소에 대한 조류발생 빈도 및 범위가 증가하고 있다. 이상조류에는 녹조와 적조가 있다. 녹조현상은 물속의 클로로필(Chl-a) 등의 남조류가 과다 성장하여 물의 색이 짙은 녹색으로 변하는 현상으로, 미량의 냄새물질과 독소를 생성하여 수질악화와 식수안전에 대한 우려가 급증하고 있다. 본 연구는 생활주변 환경의 생태하천과 호소에서 측정된 수질정보를 원격지에서 1:1 실시간모니터링 및 제어하기 위하여 디지털트윈의 3D 가상세계를 구축하고, 사물인터넷(IOT) 센서기반의 수질정보 센서측정기를 개발하며, AI의 머신러닝 기반 수집데이터 분석을 토대로 녹조 등 수질오염의 발생원인과 확산패턴을 예측하여 조류경보와 수질예보를 할 수 있는 스마트 수질환경 서비스 플랫폼 구축을 제안하고자 한다.

• 한국막학회:학술대회논문집
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• 한국막학회 1997년도 제5회 하계 Workshop (97 한,카 국제공동 Workshop, 고도 수처리를 위한 막분리 공정)
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• pp.207-231
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• 1997

The use household water purifier is continuously increasing due to the distrust of the piped, rap water, which may be caused by the deterioration of water quality and water supply facilities in Korea. The water purifier distributing in the domestic market is the membrane type that composes of membrane as a basic filter, sediment filter as a prefilter and activated carbon filter instead of one purifying water system. The membrane type using as a water cleaning system is mainly the method of micro filtration(NIF) as well as ultra filtration(UF) and reverse osmosis(RO). The types of MF and UF are using to remove suspended solids and virus, and RO is using to remove ionic compound in chemical organic compounds. At the beginning the household water purifier was imported as end-product or assembled by only importing module from small businesses in Korea. Therefore, people was hard to confide in the product quality because the sales policy and management of water purifier by small business were not effectively organized. However, the defects of water purifier having up to now ate improving by the efforts of special branches of water purifier and large enterprises, and new great products are developing and producing. To develop the best quality product of water purifier in Korea, it should be considered seasonal water characteristrics rather than any other condition. For example, the water purifier can be affected by the water temperature change, increase of suspended solids in the rainy season and inflow of raw water having concentration in a dry season. The subject we have to investigate in the future is to develop the water purifying system adaptable in Korea which can treat the water quality using close analyses of local and seasonal water characteristics.

• 생태와환경
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• 제41권2호
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• pp.206-215
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• 2008

본 연구는 방조제 조성 이후 물 교환이 제한적인 시화호의 기수역에서 염분도, 수온, DO, 탁도의 시공간적 분포특성을 분석하여 기수역의 수질오염 원인을 해석하고 개선방안을 수립하기 위한 기초자료를 활용하고자 하였다. 시화호 기수역에서 염분도는 $0.1{\sim}29.9\;psu$ 그리고 수온은 $4.7{\sim}28.1^{\circ}C$의 범위로 변동이 매우 컸으며, 담수유 입량과 해수의 유입/유출 여부 및 유통량에 의해 영향을 받은 것으로 나타났다. 그리고 기수역 내 염분약층의 형성과정에는 담수유입이 주된 요인인 반면, 염분약층이 형성되는 구간은 배수갑문을 통한 해수의 유입 및 유출여부와 유통량에 의해 영향을 받는 것으로 나타났다. 기수역에서 수온과 염분도의 시공간적 분포는 DO농도와 탁도 분포에 영향을 미치는 것으로 나타났다. DO는 수온이 상승하는 4월에 기수역 중류부의 표층에서 최대 $26.5\;mg\;L^{-1}$(포화도 315%)의 농도를 보였는데, 이는 이 시기 대량 증식한 식물플랑크톤의 광합성에 의한 것으로 사료된다. 반면, 염분약층이 강하게 형성된 지점의 심층에서는 저산소층이 형성되었고, 여름으로 갈수록 확대되어 수온이 가장 높았던 7월에 가장 넓게 형성되는 것으로 나타났다. 한편 탁도는 $1.5{\sim}86.3\;NTU$의 범위로 하류에 비해 중류와 상류부에서 높은 값을 보였고, 염분약층이 형성된 구간에서 높은 경향을 보였다. 본 연구로부터 담수와 해수가 공존하는 시화호 상류 기수역에서 염분도 차이에 의해 형성되는 염분약층은 수체의 공간적인 혼합을 제한시키는 결과를 가져오고, 결국 심층의 산소고갈, 퇴적물의 증가, 식물플랑크톤의 대량증식에 의한 수체의 유기물 증가 등의 수질문제를 유발시킬 수 있는 원인으로 판단된다.

• 한국해양학회지:바다
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• 제8권4호
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• pp.357-368
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• 2003

남극 세종기지 앞에 위치한 마리안 소만의 여름 수층 구조과 부유물질 분산기작을 이해하기 위해 빙벽 앞에서 CTDT 연속측정을 하였으며, 측정기간 동안의 조석, 부유물질농도, 유속, 그리고 기상요인도 함께 분석되었다. 45 시간동안 1시간 간격으로 측정된 연속 수층 특성 분포에 의하면, 수심 0∼20 m에는 저온$.$저염$.$고탁도의 혼합 표층수가 존재하였고, 수심 20∼40 m에 고온$.$고염$.$저탁도의 최대수온층인 맥스웰 만 유입수가 나타난다. 그 아래의 수심 40∼70 m에는 주변 해수에 비해 저온$.$고탁도의 아빙하성 유출수인 중층 플름(빙하기저부)이 위치한다. 마지막으로 수심 70 m 이하에 나타나는 저층수는 저온$.$고염$.$저탁도의 특성을 보였다. 늦여름 (2 월초)에 연안의 높아진 설선에서 녹아 소만으로 유입하는 담수의 특성은 유입지역의 특성(지형, 빙하조건, 퇴적물의 구성 등)에 따라 수온과 부유물질농도에서 차이를 보였으며, 바람이 거의 불지 않는 측정시기 동안에는 저염$.$고탁도의 표층 플름이 유입지역에 제한적으로 나타났다. 지속적으로 강한 바람이 불 경우, 빙벽 앞에서 육성기원의 혼탁한 담수성 플름, 저온의 중빙하성 용승수/조수빙하 융빙수 그리고 맥스웰 만 유입수가 혼합되면서 표층에 혼합층(저온$.$저염$.$고탁도)이 발달하였다. 소만의 강수는 단기간 빙하성 유출 증가의 가장 큰 요인이며, 중빙하성 용승수의 발생은 조수빙하의 상태와 강수량이 크게 좌우하였다. 특히 많은 양의 강수로 인해 아빙하성 중층 플름의 유출량이 커지면서 중층 이하의 수심에 저염화를 초래하였다. 그러나 입자가 거의 없을 정도로 깨끗한 중앙 빙벽에서 나오는 중빙하성 용승수와 중층 플름의 유입량이 클지라도, 낮은 부유물질농도로 인해 육성기원 입자의 소만 퇴적율은 작을 것이다.