• 한국농공학회:학술대회논문집
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• 한국농공학회 2003년도 학술발표논문집
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• pp.519-522
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• 2003

The purpose of this study is to analyze various hydraulic characteristics using SMS (Surface Water Modelling System) RMA2 model. It is based on 2-D finite element method. River reaches (13.8km) from Gyeongan gauge station to the inlet of Paldang lake was selected. Finite element was made by RIMGIS Data, and the analysis of river-changes was operated by unsteady flow. The sediment concentration and bed change was simulated using SED2D model.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2003년도 학술발표논문집
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• pp.479-482
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• 2003

Landsat-TM images were applied for evaluating the spatial variations of flow and water quality at the Saemankeum areas. For supervised classifications, the results from hydrodynamic modeling and water quality data were compared to the reflectance characteristics of the satellite images. Multiple regression analyses indicated that suspended sediment, transparency, salinity, total nitrogen, and total phosphorus showed a good relationship to the signature. Supervised classifications showed spatial variations of the water environments at the areas under construction. The results showed the satellite imagery may be applied for the project areas with a reasonable degree of accuracy.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2005년도 학술발표논문집
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• pp.272-277
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• 2005

Initial mixing characteristics in near field regions were analyzed by FLOW-3D, for analyzing mixing behavior of submerged discharge from freshwater lake in sea water. FLOW-3D model was applied to the region near Geum-ho dike for its verification. Simulation results from FLOW-3D were compared to the observed data for the verification periods. FLOW-3D showed resonable prediction results compared to the observed data, except underestimation in area near outfall. Particularly, FLOW-3D showed a good prediction for movement of buoyancy jets. In addition, FLOW-3D model was applied to the region near Saemangeum dike, which is to be constructed in near future. It was expected that the results of model application to Saemangeum area could provide substantial information in planning submerged discharge facilities. Based on the model applications to Saemangeum area, it was recommended that outfall should be located to the distance which gave an enough depth of outfall from water surface.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2000년도 학술발표회 발표논문집
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• pp.637-642
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• 2000

In order to control the water quality of freshwater lake in tidal reclaimed land, it is needed to evaluate accurate amount of pollutant loadings from reclaimed paddy field. This study was carried out to investigate the pollutant loading from a reclaimed paddy field. Site of the study was a paddy field located in Taeho reclaimed land, with an areas of 38.5 hectares. The runoff loadings of Total-Nitrogen, Total-Phosphorus, and Chemical Oxygen Demand were 49.5 kg/㏊/yr, 3.2 kg/㏊/yr and 154.0 kg/㏊/yr, respectively. The runoff loadings in Total-Nitrogen and Total-Phosphorus from this study were much higher values than the pollutant load factor of Total-Nitrogen and Total-Phosphorus from the paddy field published by the Ministry of Environment.

• Mycobiology
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• 제47권3호
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• pp.273-279
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• 2019

A new species, Pythium subutonaiense, isolated from aquatic environments (lake) in China is being described based on morphological characters and molecular evidence. The isolates grew at temperatures between $5^{\circ}C$ and $38^{\circ}C$, and the optimum temperature was $30^{\circ}C$, with a radial growth rate of 17.6 mm at $25^{\circ}C$ per day. It is homothallic and characterized by globose to sub-globose shaped and mostly terminal or sometimes catenulate hyphal swellings, filamentous non-inflated sporangia, and smooth oogonia with hypogynous and monoclinous antheridia that contained one plerotic oospore. In phylogenetic analysis, inferred based on the internal transcribed spacer region of the ribosomal RNA gene and mitochondrial cytochrome c oxidase subunit 1 gene, the new species formed a distinct lineage in Pythium clade B. Differences between the new species and phylogenetically related and morphologically similar species are discussed.

• 한국환경농학회지
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• 제7권2호
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• pp.102-110
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• 1988

대호(大湖) 방조제(防潮堤) 축조(築造) 후(後) 담수호(淡水湖)의 수질(水質)을 조사(調査)하여 염농도 및 일반수질변화가 관개용수원에 미치는 영향을 규명(糾明)하고자 '84년(年) 에서 '88년(年) 5월(月) 까지의 조사결과(調査結果)를 요약(要約)하면 다음과 같다. 1. 대호(大湖) 담수호(淡水湖)의 수온분포(水溫分布)는 암거탄구 설치지점(設置地點)인 -14m 상부에는 계절변화(季節變化)에 따른 기온(氣溫)의 영향으로 변화(變化)$(6-25^{\circ}C)$가 많았으며, 암거탄구 이하에서는 $11.9^{\circ}C$로 년중(年中) 변화(變化)가 없었다. 2. 방조제(防潮堤) 앞 제일 깊은곳의 연도별(年度別) 수질변화는 pH7.6 $EC16,800-1,472{\mu}m$ hos/cm, DO 9.2-10.8ppm, BOD 1.3-2.5ppm, COD 2.4-5.3ppm, T-N 0.22-2.29pp, T-P는 0.01-0.10ppm을 나타내었다. 3. 대호(大湖) 담수층(淡水層)의 평균 수질성적('88년)은 pH 7.6, $EC1,745{\mu}m$ hos/cm, DO 10.8ppm, BOD 1.8pp, COD 2.4pp, T-N 0.52ppm, T-P 0.05ppm으로 전(全) 지점(地點)에서 비슷한 경향(傾向)이었다. 4. 담수층(淡水層)(6m)에서의 염도변화(鹽度變化)는 체절(締切) 전(前) 29,000ppm에서 '84년(年) 3월(月) 11,000ppm '85년(年) 3월(月) 4,300ppm, '86년(年), '87년(年) 3월(月)에는 2,000ppm, '88년 3월(月)에는 900ppm 까지 낮아졌다. 호내(湖內) 평균(平均) 염도(鹽度) 29,000ppm 정도에서 '88년(年) 3월(月) 1,200ppm 까지 낮아졌다. 또한 암거탄구 상부의 평균염도('87년(年))는 1,300ppm 정도였으며, 탄구아래는 해수(海水)와 같은 30,000ppm정도였다. 5. 담수층(淡水層)에서 가장 높은 염도를 나타낸 지점(地點)은 방조제(防潮堤) 앞 부근이며, '84년(年)에는 5,835ppm 이었다. 6. 조사시기별(調査時期別) 염도변화(鹽度變化)는 갈수기인 '87년(年) 5월(月) 2,000ppm에서 홍수기 후 8월(月) 800ppm, 풍수기인 9월(月)에는 485ppm까지 낮아졌다. 7. 염분약층(鹽分躍層) 깊이는 암거탄구 지점(地點)인 -l4m까지 유지(維持)되어 담수호화(淡水湖化)가 진행(進行)되었다. 그러므로 대호(大湖) 담수층(淡水層)의 수질은 농업용수원(農業用水源)으로는 큰 문제가 없으며, 삽교호로부터 제염용수(除鹽用水)의 공급(供給)도 불필요할 것으로 사료된다.

• 농촌계획
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• 제23권2호
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• pp.55-65
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• 2017

This study is to estimate the circuity factors which can be used to assess for public facilities accessibility and analyze traffic in the area. We set the range of the administrative districts by Si Gun Gu unit and Eup Myeon Dong unit (more subdivided unit than Si Gun Gu unit). The average circuity factor in Si Gun Gu unit is 1.364 (maximum 2.953 and minimum 1.711). The region indicated the highest value of circuity factor is wando-gun in jeollanam-do, which area consists of 4 island and is connected to the bridges. Having to use the bridges for using public facilities hinders its accessibility. In the case of Eup Myeon Dong unit, the average circuity factor is 1.353 (maximum 2.950 and minimum 1.154). The region indicated the highest value of circuity factor is buksan-myeon in chuncheon-si, Gangwon-do. This region also has to use bridges for using public facilities because there is the largest lake, called Soyangho. This circuity factor is used to analyze the location of public facilities and assess vulnerability of accessibility. And also the factor can be applied to some policies, such as rural public service planning based on spatial big data.

• 한국해양환경ㆍ에너지학회지
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• 제20권2호
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• pp.76-83
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• 2017

본 연구에서는 시화호 유역 하천수의 일반수질 및 중금속의 변화 및 유출특성을 파악하기 위하여 시화호로 유입되는 하천수 중 일반수질 및 중금속의 분포 특성, 토지이용형태에 따른 농도비교 및 하천을 통한 유출부하량 조사를 실시하였다. 시화호 유역 하천을 토지이용형태에 따라 산업지역, 도심 및 농업지역으로 구분하여 일반수질 농도 비교를 실시하였을 때, 하천수 중 DO, SS, POC, $NO_3$와 Chl-a는 농업지역이 산업 및 도심지역에 비해 높은 농도를 보였으며 COD, DIN, $PO_4$, TN, TP, DOC와 TOC는 산업지역이 상대적으로 높은 농도를 보였다. 하천수 내 수질 및 중금속 분석항목에 따라 약간의 차이가 존재하지만, 3월~5월 조사시기에 상대적으로 농도가 높고 7월~8월에는 강우에 의한 영향으로 농도가 감소하는 결과를 보였다. 하천유량과 농도를 이용하여 계산된 일반수질의 유출부하량은 SS 1,172 kg/d, TN 151 kg/d, TP 11.1 kg/d, TOC 389 kg/d이었고, 농업지역인 장전보가 전체 유출부하량에서 47.5%(TP)~75.1%(SS)를 차지하고 있었다. 하천수 내 Cu, Zn, Cd은 산업단지 하천을 통한 유출부하량이 전체의 92%를 초과하고 있는 것을 알 수 있었으며, Zn>Cu>Ni>Pb>Co>Cd의 순으로 나타났다.

• 한국환경과학회지
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• 제16권3호
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• pp.357-367
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• 2007

Recently, eutrophication or lake and reservoir has become serious problem to man who want use that water for several purpose. In order to solve the eutrophication problem, the trophic state of that eutrophic lake and reservoir should be measured properly. For the purpose of this, various method to indicate the trophic state of lake and reservoir was developed by many researchers. This research was conducted to evaluate characteristics and eutrophication of water qualitymfor small scale reservoir in Kunsan. On-site investigation to 5 reservoirs and laboratory experiment were carried out during four seasons from November, 2003 to July, 2004. Twelve items measured field ana a laboratory. Measured data was analyzed to quantitative method by multivariate approach and eutrophication index. The result is summarized as following. 1) Showing the characteristics of water quality for reservoir in Kunsan, Okgu reservoir and Oknua reservoir was exceeded 4 grades of agricultural water standard in TP, TN and COD. This means that eutrophication was gone much, therefore, water-purity control of reservoir need. While, Mije reservoir that is used to Kunsan citizens' recreation was good in water quality. But, water quality exceeded 4 grades of agricultural Dater standard sometimes. 2) As a results of correlation analysis between variables of water qualify, Interrelation between variables which is connected with eutrophication was expressed good relationship as above 6.000 in correlation coefficients. The correlation coefficient(r) between COD and chlorophyll-a, total phosphorus and chlorophyll-a, total nitrogen and chlorophyll-a were 0.750, 0.720 and 0.600 respectively. Therefore, Change of water quality can grasp according to eutrophication progress degree. 3) If do evaluate to eutrophication by quantitative method which is proposed by OECD, US-EPA and Forsberg & Ryding, in the case of chlorophyll a, Okgu, Oknua and Daewi reservoir was eutrophic state and Mije and Geumgul reservoir was mesotrophic state. But, estimation by TN and TP showed highly eutrophic state (hypereutrophic) in all reservoirs. 4) If do evaluate by eutrophication index which is Carlson's TSI, revised carlson TSI and Walker's index, in the case of chlorophyll a, TSI values of Okgu, Oknua and Daewi reservoir is eutrophic state more than 50 and Mije and Geumgul reservoir was mesotrophic state as range of $40{\sim}50$ in TSI value. But, in the case of TP as nutrients, all reservoirs showed highly eutrophic state which was exceed to 70 in TSI value. According to above results, the water quality for small scale reservoirs in Kunsan is progressing by trophic state. therefore, for continuous use as agriculture water, we had better do establishment of management plan about water quality.

• 한국물환경학회지
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• 제27권4호
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• pp.467-474
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• 2011

In an effort to investigate water pollution characteristics of Juam lake, water samples were collected from three sites (Sites A, B, and C) of Oenam stream which is a typical tributary of rural watershed in the lake and analyzed for N concentration and the corresponding isotope ratio (${\delta}^{15}N$) of ${NO_3}^-$. Concentrations of ${NO_3}^-$ were not dramatically different among the sites; $0.8{\pm}0.2mgNL^{-1}$ (range: $0.0{\sim}4.3mgNL^{-1}$) for Site A, $1.1{\pm}0.2mgNL^{-1}$ ($0.0{\sim}4.3mgNL^{-1}$) for Site B, and $1.1{\pm}0.1mgNL^{-1}$ ($0.1{\sim}2.6mgNL^{-1}$) for Site C. Meanwhile, ${\delta}^{15}N$ tended to decrease with river flow; it was highest for Site A ($45.5{\pm}5.3$‰) followed by Site B ($19.7{\pm}2.0$‰) and Site C ($8.7{\pm}1.5$‰). Such high ${\delta}^{15}N$ values of ${NO_3}^-$ in Site A suggested that ${NO_3}^-$ derived from livestock feedlot (specifically livestock excrete of which ${\delta}^{15}N$ is higher than 10‰) is the predominant pollution sources despite mountainous area occupied the most of land-use in the watershed. Using the two-sources isotope mixing model, it was estimated that the contribution of cropping activities (i.e. fertilization) became greater in down-stream area (Sites B and C) due to the higher agricultural land-use than the up-stream area (Site A). Particularly, during the active cropping season, the low contribution of organic pollution sources indicated that domestic sewage was not the predominant pollution source. Therefore, it was suggested that agricultural sources such as livestock farming and cropping rather than mountainous and residential are the dominant sources of water pollution in the study area. These results could be effectively utilized in elucidating water pollution sources in rural areas and selecting water management practices.