• 한국물환경학회지
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• 제34권5호
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• pp.470-486
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• 2018

This study is to investigate the allochthonous load and water quality of a typical river-reservoir, Paldang during spring (March ~ May) of 17 years (2001 ~ 2017). Phosphorus loading from point sources seems to have been reduced by 74 % in the 2010s. As a result, trophic state of the Paldang reservoir, eutrophic during the 2000s, has returned to the lmesotrophic state. Along with decrease in phosphorus concentration, standing crops of algae (Chl.a) decreased, and concentration of biodegradable organic material decreased to the past level. Concentration of total suspended solids has decreased, and it is due to the decrease of phytoplankton standing crops since the mid-2000s. As transparency increased, it is estimated that euphotic area increased by 22 % and euphotic capacity expanded by 27 %. In the river/transition zone of Paldang, concentration of organic matter increases slightly due to algal growth, but concentration of all water quality items decreases in the lacustrine zone. Although algal growth rate revealed positive correlation with concentration of phosphorus, it was insignificant. Algal growth appeared to be dependent on renewal of phosphorus by flow, than either flow rate or phosphorus concentration. The empirical model including inflow phytoplankton concentration fit well with observed values, and indicates the Paldang reservoir is greatly influenced by allochthonous loads.

• 한국환경과학회지
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• 제24권6호
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• pp.743-753
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• 2015

In this study, it is an object to develop a regression model for the estimation of TOC (total organic carbon) concentration using investigated data for three years from 2010 to 2012 in the Gam Stream unit watershed, and applied in 2009 to verify the applicability of the regression model. TOC and $COD_{Mn}$ (chemical oxygen demand) were appeared to be derived the highest correlation. TOC was significantly correlated with 5 variables including BOD (biological oxygen demand), discharge, SS (suspended solids), Chl-a (chlorophyll a) and TP (total phosphorus) of p<0.01. As a result of PCA (principal component analysis) and FA (factor analysis), COD, TOC, SS, discharge, BOD and TP have been classified as a first factor. TOCe concentration was estimated using the model developed as an independent variable $BOD_5$ and $COD_{Mn}$. R squared value between TOC and measurement TOC is 0.745 and 0.822, respectively. The independent variable were added step by step while removing lower importance variable. Based on the developed optimal model, R squared value between measurement value and estimation value for TOC was 0.852. It was found that multiple independent variables might be a better the estimation of TOC concentration using the regression model equation(in a given sites).

• 물과 미래
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• 제10권1호
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• pp.53-70
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• 1977

The analysis performed here is aimed to increase the familiarity of hydrologic process especially for the small basins which are densely gaged. Kyung An and Mu Shim river basins are selected as a representative basin according to the criteria which UNESCO has established back in 1964 and being operated under the auspice of Ministry of Construction. The data exerted from these basins is utilized for the determination of characteristics of procipitation and runoff phenomena for the small basin, which is considered as a typical Korean samall watershed. The study found that the areal distribution of preciptation did not show any significant deviation from the point rainfall. Since the area studied is less than 20 km#, the pointrainfall may be safely utilized as a representative value for the area. Also the effect of elevation on the precipitation has a minor significance in the small area where the elevation difference is less than 200m. The methodology developed by Soil Conservation Service for determination of runoff value from precipitation is applied to find the suitability of the method to Korean river basin. The soil cover complex number or runoff curve number was determined by comsidering the type of soil, soil cover, land use and other factors such as antecedent moisture content. The average values of CN for Kyung An and Mushim river basins were found to be 63.9 and 63.1 respectively under AMC II, however, values obtained from soil cover complex were less than those from total precipitation and effective precipitation about 10-30%. It may be worth to note that an attention has to be paid in application of SCS method to Korean river basin by adjusting 10-30% increase to the value obtained from soil cover complex. Finally, the design flood hydrograph was consturcted by employing unit hydrograph technique to the dimensionless mass curve. Also a stepwise multiple regression was performed to find the relationship between runoff and API, evapotranspiration rate, 5 days antecedentprecipitation and daily temperature.

• 한국환경복원기술학회지
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• 제8권4호
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• pp.52-67
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• 2005

The flora of the studied basin in the upper Keum River was listed as 237taxa; 63families, 162genera, 212species, 22varieties and 3forms. Based on the list of the ecosystem disturbance plants by the Ministry of Environment, 4taxa were recorded in the studied basin : Paspalum distichum(Gramineae), Paspalum distichum var. indutum(Gramineae), Ambrosia artemisiifolia var. elatior(Compositae), Ambrosia trifida(Compositae). Naturalized plants was listed as 54taxa; 16families, 41genera, 51species, 3varieties and naturalization index was 22.8percent of 1/4 the vascular plants. Upper Keum River was dominant floristic : indicator species were Salix gracilistyla community, Phragmites japonica community, native plants were Morus alba community, Spiraea prunifolia for. simpliciflora community, planting plants were Populus euramericana community, naturalized plants were Solidago serotina community, Helianthus tuberosus community.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2005년도 학술발표회 논문집
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• pp.52-59
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• 2005

The goal of this project is to estimate the instream flow of the Han River Basin to ensure the adequate supply of suitable quality water for preservation and enhancement of aquatic ecosystems. A applied model is Physical Habitant Simulation System(PHABSIM) of Instream Flow Incremental Methodology(IFIM). The parameters which are needed to simulation by PHABSIM such as flow depth, velocity distribution and channel cover with cross section data are obtained by field survey. The Habitat Suitability Criteria with the application of univariate curve on Zacco platypus as a target species was able to be established by conducting the field investigation. The estimated results of ecological recommended instream flow by this study has important meanings that the future river management have to seriously take into account for the natural environment and functions of river system.

• 한국조명전기설비학회:학술대회논문집
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• 한국조명전기설비학회 2005년도 춘계학술대회논문집
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• pp.111-116
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• 2005

This study examined the luminance and light appearance about 14 flood lighting established bridges of 26 Han River bridges and then analyzed the result through questionnaire and so on. Through this result, we looked out for new direction of analysis research for flood lighting that consider the problem of optimum brightness and light appearance harmony at flood lighting presentation, proposed to be utilized concretely in lighting design guideline for Han River bridge.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2004년도 학술발표회
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• pp.1331-1334
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• 2004

Wet/Dry phenomena typically incorporate a number of complex flow mechanism. These include a momentum transfer and turbulent mixing caused by the delivery of water. However currently available one dimensional schemes applicable to wet/dry process cannot effectively simulate such process. Two dimensional finite element model, SU/PG, is used to simulate complex flow in this study. The Wetted Area Method in SU/PG allows elements to transition gradually between wet and dry states. The model is applicable to a straight river reach with irregular bathymetry. Wet/dry calculation using the wetted area method can simulate simple numerical test. The computed results of velocity vectors and water depth agree with those of observed. The methodology Presented in this study will contributed to two-dimensional wet/dry analysis in a river in this country.

• 한국환경과학회지
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• 제12권9호
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• pp.935-941
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• 2003

To investigate the interaction of bacteria and Microcystis isolated from a hypertrophic reservoir(Seo-Nakdong River), the response of five bacteria in relation to the different treatment of Microcystis and microcystin production by addition of dominant bacteria Staphylococcus sciuri were examined. Five bacteria (S. sciuri, S. capitis, S. epidermis, Pseudomonas aeruginosa and Aeromonas aimonicida) were identified from the reservoir. In the experiment of bacterial response, two types of bacterial growth pattern were observed. All bacteria showed active growth in heated Microcystis-added media. Especially, three species of bacteria (S. sciuri, S. capitis and P. aeruginosa) among them showed active growth in live Microcystis-added media. In Microcystis response, increase of microcystin production showed when dominant bacteria, S. sciuri was added.

• 한국수자원학회논문집
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• 제45권10호
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• pp.983-995
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• 2012

본 연구에서는 기상학적 가뭄지수인 SPI(Standardized Precipitation Index)를 이용한 가뭄 빈도해석을 통하여 남한지역에서 발생했던 과거가뭄사상의 시, 공간적 분포 특성을 정량적으로 평가하고자 한다. 가뭄의 심도별, 지역별 발생빈도를 추정하기 위하여 Drought Spell 분석을 실시하였고, 또한 남한지역을 대상으로 심한 가뭄에 대한 가뭄우심지역의 공간적 분포특성을 평가하기 위하여 가뭄의 지속기간별 가뭄빈도해석을 통해 기상관측소별 SDF (severity-duration-frequency) 곡선을 작성하고 이를 이용하여 남한지역을 대상으로 하는 가뭄우심도(Potential Drought Hazard Map)를 작성하였다. 가뭄단계별 과거의 발생빈도를 분석한 결과, 금강, 낙동강, 섬진강 유역에서 심한가뭄과 극한가뭄단계의 발생빈도가 매우 큰 것으로 나타났으며 가뭄빈도해석을 통해 작성된 SDF 곡선에서도 한강유역에 위치한 서울관측소에 비해 금강, 낙동강, 섬진강 유역에 위치한 대전, 대구, 광주 관측소의 재현기간별 가뭄심도가 심하게 나타났다. 가뭄빈도해석을 통해 작성된 가뭄우심도에서는 한강 유역과 낙동강 유역의 상류 지역에 비해 금강, 섬진강, 영산강 유역이 가뭄에 취약했던 지역으로 분석되었으며 가뭄단계별 발생빈도와 유사한 결과를 나타내었다. 계절별 가뭄우심도의 경우 봄철에 가장 자주 가뭄이 발생하였으며 짧은 지속기간의 가뭄이 자주 발생했던 것으로 나타났다.

• 한국지역지리학회지
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• 제17권6호
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• pp.666-678
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• 2011

본 연구는 한국에서 6개(한강유역, 낙동강유역, 금강유역, 섬진강 영산강유역, 동해안지역, 도서지역) 유역별로 가뭄의 변화경향을 분석하였다. 이를 위해 무 강수일과 관련된 3개의 극한강수지수를 분석하였다. 최대연속건조일수의 변화지속성은 전 기간에 걸쳐 뚜렷하지 않고 변동성이 크다. 낙동강유역과 섬진강 영산강유역이 한강유역과 금강유역에 비하여 변동폭이 크다. 최근 낙동강유역과 섬진강 영산강유역에서 그 변동폭이 더 커지고 있다. 최대연속건조기의 출현은 대부분 유역에서 가을과 겨울철에 빈번하다. 낙동강유역은 겨울철 가뭄이 특징적이다. 평균연속건조일수의 변화는 최대연속건조일수에 비하여 연 변동성이 작고 금강과 섬진강 영산강유역의 최근 증가경향은 지속적이다. 낙동강유역은 연속건조일의 평균값과 중앙값의 차가 크며, 이는 다른 유역에 비해 연속건조일의 장기간 출현가능성이 높음을 의미한다.