• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.958-962
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• 2006

하수처리수를 농업용수로 관개함에 있어서, 관개 유입수 및 논 담수에서의 수질은 작물이나 인체에 미치는 영향이 크다. 따라서 하수재처리수를 농업용수로 사용함에 있어서 수질 기준이 필요하게 되었으며, 이에 환경부에서 $\ulcorner$하수처리 재이용 수질 권고기준$\lrcorner$을 마련하게 되었다. 본 연구에서는 환경부에서 제시한 하수처리 재이용 수질 권고기준에 제시된 수질기준과 본 시험에 사용된 하수처리장 방류수 및 하수재 처리수의 수질을 비교하여 하수처리수의 농업용수 재이용의 적합성을 판단하였으며, 수질 모니터링을 실시하여 논에서의 수질 정화효율을 알아보았다. 본 시험을 위하여 경기도 수원시 하수처리장 인근에 시험포장을 설치하였으며, 하수처리장 방류수와 하수재처리수(여과, 소독, 저류)를 이용하여 논벼 작물 생육시험을 실시하였다. 하수처리장 방류수 수질과 하수재처리수의 수질을 분석한 결과, 수질 기준을 만족하는 것으로 나타났다. 또한, 4년간 실시된 논 유입수 및 담수의 수질 모니터링 결과 논에서의 수질 정화 효율은 TN의 경우 $40{\sim}65%$, TP의 경우 $15{\sim}60%$로 나타났다. 이는 배출수를 통한 하천이나 호소로의 유입에 있어서 환경개선효과를 기대할 수 있을 것이다. 농작업시 인체에 미치는 보건위생정도를 평가하기 위하여 지표미생물의 농도를 분석하였으며, 하수 재이용에 따른 농업용수 활용에 있어 인체에 크게 문제가 되지 않는 것으로 나타났다.

• Journal of Advanced Marine Engineering and Technology
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• v.35 no.4
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• pp.373-378
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• 2011

The freeze desalination cycle with seawater heat pump system is simulated and designed for the basic data for the design of freeze desalination system. The basic model of seawater heat pump system is refrigeration cycle and indirect freeze desalination method is used for seawater desalination. The cycle performance of seawater heat pump such as COP, compressor work, condensing capacity was analyzed and the desalination performance such as fresh water productivity and energy per unit fresh water productivity was compared with respect to the seawater temperature of condenser inlet and ice ratio in the evaporator. The compressor work and condensing capacity decreased with respect to the decrease of seawater inlet temperature. The energy per unit fresh water productivity in case of $8^{\circ}C$ seawater inlet temperature showed 28.9% lower than that of $20^{\circ}C$.

• Journal of the Korean Society for Marine Environment & Energy
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• v.20 no.1
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• pp.1-11
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• 2017

Nakdong River Estuary is affected by the dam, barrage construction and dredge and reclaim worked artificially. So, we have studied the area input both freshwater and sea water to understand marine environment of Nakdong River estuary related to the effect of artificial work from 2013 to 2015. As a result, The discharge flow to the estuary remarkably decreased before barrage construction and the average of salinity at the estuary increased. So, the brackish water zone reduced under the influence of decreased discharge flow. The major sources of nitrate and silicate were freshwater, phosphate supplied from bottom and the open sea water. The concentration of phosphate and dissolved oxygen (DO) decreased remarkably in spring and summer. we investigated that phosphate in freshwater was removed under the influence of the estuary dam and phosphate in sea water was removed under the influence of phytoplankton. The low concentration of DO was due to decomposition of the organic compound by microorganism after phytoplankton blooms. Generally, the concentrations of chlorophyll-a in summer was higher than spring and fall. Therefore, the change of ecosystem in Nakdong river estuary was due to decrease of freshwater influx, the other change is facing because of the barrage.

• Korean Journal of Ecology and Environment
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• v.39 no.1 s.115
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• pp.41-51
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• 2006

The influence of land use and pollutant source on water quality was investigated using 3-yrs monitoring data major influent stream in Hwaong reservoir watershed. The seven water quality station (N1, N2, J1, J3, J4, E2, E3) were used analysis of land use and pollutant effect, and six water quality station (N3, N4, J2, J5, E1, E4) were used analysis of waster quality status. Water quality parameter were positively correlated with residential and forest, negatively with paddy and upland especially during dry period. During wet period, correlation between land use and water quality was less apparent. Population and livestock density was correlated well to water quality parameter than just number of population and livestock. The watersheds studied are mainly non-urban and their land uses are similar to typical watershed of other estuarine reservoirs, therefore, the correlation developed in this study might be helpful to manage other estuarine reservoir watersheds.

• Journal of Korea Water Resources Association
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• v.38 no.12 s.161
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• pp.1061-1072
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• 2005

A hydrological grey model is developed to forecast short-term river runoff from the Naju watershed located at upstream of the Youngsan estuary dam in Korea. The runoff of the Naju watershed is measured in real time at the Naju streamflow gauge station, which is a key station for forecasting the upstream inflow and operating the gates of the estuary dam in flood period. The model's governing equation is formulated on the basis of the grey system theory. The model parameters are reparameterized in combination with the grey system parameters and estimated with the annealing-simplex method In conjunction with an objective function, HMLE. To forecast accurately runoff, the fifth order differential equation was adopted as the governing equation of the model in consideration of the statistic values between the observed and forecast runoff. In calibration, RMSE values between the observed and simulated runoff of two and six Hours ahead using the model range from 3.1 to 290.5 $m^{3}/s,\;R^2$ values range from 0.909 to 0.999. In verification, RMSE values range from 26.4 to 147.4 $m^{3}/s,\;R^2$ values range from 0.940 to 0.998, compared to the observed data. In forecasting runoff in real time, the relative error values with lead-time and river stage range from -23.4 to $14.3\%$ and increase as the lead time increases. The results in this study demonstrate that the proposed model can reasonably and efficiently forecast runoff for one to six Hours ahead.

• Journal of the Korean Society for Marine Environment & Energy
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• v.12 no.4
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• pp.248-254
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• 2009

Budgets of fresh water, salt, DIP and DIN in the Youngsan river estuary were estimated seasonally in order to clarify the characteristics of material cycling and flux of nutrients with a simple box model. Inflow volumes of freshwater into system was approximately $36.481{\times}10^6{\sim}663.634{\times}10^6m^3/month$ and existing water mass of freshwater in system calculated by salt budget was approximately $2.515{\times}10^6{\sim}5.812{\times}10^6m^3$. Mean residence time of freshwater was calculated to be about 0.26~2.03 day. water exchange $1,248{\times}10^6{\sim}9,489{\times}10^6m^3/month$ assumed with salinity between estuary and adjacent ocean. Inflow mass of DIN and DIN were approximately 76.63~1,149.91 ton/month and 2.91~61.22 ton/month, respectively. Residence times of DIP and DIN were calculated to be 0.45~1.10 day and 0.28~1.92 day, respectively. The ratio of water residence time versus DIP, DIN residence time was calculated that freshwater residence time was longer than DIP, DIN residence time except for summer season. Thus, We assume that circulation of Nutrients in the system will happen rapidly except for summer season. Specially DIP in Winter could assume to outer input source existence because of seawater inflow in system and high DIP concentration in open sea.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.26 no.2
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• pp.96-109
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• 2021

Since terrestrial input plays a major role in coastal primary production, an understanding of land-ocean coupling (LOC) is key to understand coastal ecological changes. In this study, the LOC has been classified into three stages (i.e., the baseflow, plume event and residual flow). In order to characterize its pattern in Nakdong River estuary, multi-platform data were obtained from remote sensing (geostationary ocean color image (GOCI)), in-situ measurement (marine environment information system (MEIS)), on-site measurement (discharge data and meteorological data). The MEIS data were grouped into three stages of LOC using principal component analysis (PCA), and the LOC (2013 ~ 2018) was examined at each stage using multi-platform data. In the Nakdong River estuary, the maximum value of chlorophyll-a (chl-a) was unexpectedly appeared during the plume event. It is assumed that there was no significant increase in turbidity, expected during the typical plume event, together with the weak flushing effect, caused the enhanced phytoplankton growth. Compared with other estuaries, LOC is common in estuaries affected by freshwater inflow, but LOC has different pattern depending on the size of the plume. While estuaries that form small plumes of about 10 km (low freshwater discharge and weak flushing effect) observed high chl-a in the plume event because the phytoplankton can response to the increased nutrient more rapidly. estuaries that form large plumes of more than 100 km est (high freshwater discharge and strong flushing effect) follow the typical LOC pattern conceptualized in this study (high chl-a in the residual flow).

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.2135-2139
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• 2007

현재 한국농촌공사에서는 농업용수의 효율적인 관리를 위하여 물관리자동화사업을 시행하고 약 8만ha를 대상으로 418개의 수리시설을 전동화하였다. 물관리자동화사업에서의 물관리는 공급자 위주로서 이미 결정되어진 물의 양을 시기에 따라 적절하게 공급하여 주며 이를 계측하고 제어하기 위한 시설이다. 그러나 현재 실제로 물관리가 일어나는 곳을 말단포장으로서 급수물꼬의 개폐에 따라 농업용수의 공급과 단절이 이루어지고 있다. 이러한 사실에 착안하여 본 연구에서는 급수물꼬를 논의 담수심에 따라 자동으로 개폐시키는 자동물꼬, 논의 담수심과 수로의 유황상황을 체크하여 정보전달을 수행하는 수로수위측정 및 담수심 측정장치, 상기의 논과 수로의 유황정보에 의하여 논에 물을 공급하는 태양광 전동수문, 수로의 수위증감에 따라서 수로의 수압을 일정하게 형성시켜 용수공급을 원활하게 해주며 또 기존의 제수문과는 다르게 항상 수위를 일정하게 유지하면서도 하류방향으로 물을 공급해주는 무동력 자동수문을 개발하여 시스템으로서 구성하여 설치하였다. 현재 담수심 측정 및 수로수위측정장치로부터의 정보전달은 무선으로 하며 이 정보를 기초로 하여 태양광 전동수문의 모터제어부에서 판단을 하여 수문의 개폐를 지시한다. 또한 무동력 자동수문의 경우에는 부력부가 별도로 설치되어 있어서 주수부를 통하여 수로내 수위와 같은 레벨로 물이 유입되고 이를 플로트가 감지하여 수문비 후방에 설치되어 있는 밸런스 웨이트를 제어하여 수문을 개폐한다. 본 무동력 자동수문은 수위를 유지하는 설정수심을 자유로이 변경할 수 있도록 주수부를 개량하였으며 부력부에 오물유입이 되지 않도록 스크린을 주수부의 물유입장소에 설치하였다. 현재까지 시스템의 작동상황에 대한 성능은 양호하다. 다만 향후의 문제점으로서 시스템이 설치된 지역과 설치되지 않은 지역과의 용수사용량을 비교분석하는 작업으로 본 시스템의 경제적 효과 및 효율성을 증명할 필요가 있으며 본 시스템의 실용화시 시스템 사용방안에 대해서는 대규모 평야부와 저수지 지구의 물공급특성이 다르기 때문에 이를 감안한 시스템 구성을 할필요가 있다.

• Korean Journal of Microbiology
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• v.36 no.4
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• pp.285-291
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• 2000

To investigate the variations of physicochemical factors and microbial populations in seven stations at water region of Gangjin bay, nutritive salts, water temperature, transparency, suspended solid, salinity, COD, DO, pH, heterotrophic bacteria, fungi and fecal coliform were analysed four times from February to October, 1999. Total fecal coliform and heterotrophic bacterial population during investigation periods ranged 16.1~166.0 CFU/ml and $5.0{\times}10^3$~$13.1{\times}10^3$CFU/ml, respectively. Stational mean values of these bacterial population showed higher densities at the inlet of fresh water inflow than those of other stations. When the aspects of abiotic and biotic parameters measured were analyzed, ecosystem of Gangjin bay was regulated by factors such as inflow of fresh water, nutrient salts, salinity and variation of water temperature during four seasons.

• Journal of the Korean Society of Marine Environment & Safety
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• v.21 no.6
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• pp.617-636
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• 2015

The Mokpo coastal waters receive discharges from three artificial lakes(Youngsan, Youngam, Geumho) and other terrigenous freshwater inflows(streams, sewage treatment effluent, fresh groundwater), which exhibit very high concentrations of nutrients and/or organic matters. To understand spatial distributions of nutrients(DIN, DIP, DSi) and other water quality parameters(Chl-a, water temperature, salinity, DO, COD, SS), field surveys were conducted at 10 stations in the Mokpo harbor and adjacent estuaries on May, July, September, and November 2008 within 10 days following discharge events from artificial lakes. In this study, the freshwater flow rate influxed by the operation of sea dike sluice had significant influence on water qualities of the Mokpo coastal waters, although nutrient concentrations in other freshwater sources such as streams, sewage treatment effluent, and fresh groundwater were much higher. As a result of statistical analysis, DIN, COD, and Chl-a had a negative correlation with salinity. Therefore it was shown that discharge extents, time, and nutrients from the Youngsan lake were major impact factors dominating the spatial characteristics of nutrients and other water quality parameters in the Mokpo harbor and adjacent waters. However, despite non-discharge from the Youngsan Lake on September of this investigated period, it was observed that the nutrient addition was taking place in the lower layer of the estuary suggesting nutrient supply through different pathways. This result has emphasized the need to implement the combined assessment about the cumulative impacts on the Youngsan Estuary environment and ecosystem due to freshwater inputs derived from the artificial lakes as well as other terrigenous inflows, or benthic releases.