• 한국습지학회지
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• 제21권3호
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• pp.191-198
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• 2019

도시지역의 높은 불투수면은 강우시 지표 유출량을 증가시키고 지하침투량을 줄이면서 물순환을 왜곡시킨다. 왜곡된 물순환은 도시침수와 가뭄, 비점오염유출로 인한 수질오염 및 수생태계 훼손 등의 다양한 도시환경 문제 등을 유발시킨다. 기후변화는 도시강우의 계절적 편중현상을 더욱 심화시키고 도시 미기후에 영향을 줌으로써 도시침수와 가뭄의 강도 및 빈도를 증가시킨다. LID(Low Impact Development) 기법은 도시내 자연적 물순환 체계를 회복함으로써 물로 인하여 발생하는 도시환경문제를 줄일 수 있는 기법으로 다양하게 적용되고 있다. 본 연구에서는 도시지역 내 적용된 다양한 LID 기법의 장기 모니터링 결과를 활용하여 LID 적용 이후 수문특성의 변화와 물순환 회복에 기여도를 평가하기 위하여 수행되었다. LID 시설의 높은 저류량과 침투능력은 강우시 첨두유출 저감과 유출지연에 크게 기여하는 것으로 나타났다. LID 시설에서 강우시 평균 유출저감효과는 60% 이상으로 나타났으며, 유역면적 대비 LID 시설 면적비(Surface area of Catuchment area, SA/CA)와 LID 저류 용량은 첨두유출 저감과 유출지연 효과에 영향을 끼치는 중요한 인자로 평가되었다.

• 한국수자원학회논문집
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• 제35권3호
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• pp.307-319
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• 2002

본 연구에서는 WGR 강우모형으로부터 모의된 공간적으로 분포된 강우자료를 수정Clark방법으로 유출 해석하여 면적평균강우의 추정에 따른 오차와 유출오차사이의 관계론 고찰해 보았다. 이러한 관계는 강우관측소의 밀도를 다양하게 변화시켜가며 아울러 호우의 방향을 여러 가지 경우로 가정하여 살펴보았으며, 그 결과를 정리하면 다음과 같다. (1) 면적평균강우의 추정오차 및 이에 따른 유출오차는 강우관측소의 밀도가 높아짐에 따라 지수함수적으로 줄어들고 있으며, 어떤 밀도 이상이 되면 그 감소 폭이 크게 둔화되는 것으로 나타났다. (2) 면적평균강우의 추정오차는 강우관측소의 밀도가 작을수록 유출에 보다 큰 영향력을 미치고 있음을 알 수 있었다. 그러나 면적평균 강우-유출의 관계에서는 그 오차의 비가 1.0이하로 유역면적평균강우 추정시의 오차가 유출에 감소되어 전달되는데 비해 첨두유출량에는 그대로 또는 경우에 따라 증폭되어 전달됨을 파악할 수 있었다. (3) 호우의 방향성에 따른 강우오차는 크게 영향 받지 않는 것으로 판단된다. 그러나, 유출오차는 호우의 방향이 유역의 배수방향에 일치하는 경우에 더 크게 나타나고 있으며, 특히 수문곡선의 형상적인 측면에서보다는 첨두유출량에 더 많은 영향력을 미치고 있는 것으로 보여진다.

• 한국물환경학회지
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• 제27권2호
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• pp.228-234
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• 2011

The goal of water quality management on stream and watershed is to focus not on discharged loads management but on a water quality management. Discharged loads management is not goal of water quality management but way for perform with total maximum daily loads management. It is necessary to estimate the relation between non-point source with stromwater runoff (NPSSR) and water quality to select a watershed where it is required to manage NPSSR for water quality improvement. To evaluate the effects of NPSSR on stream's water quality, we compare the aspects of water quality in dry and wet seasons using flow duration curve analysis based on flow rate variation data by actual surveying. In this study we attempt to quantify the variation characteristic of water quality and estimate the Inflow characteristic of pollution source with water quality and flow rate monitoring on 10 watersheds. We try to estimate water quality and flow rate by regression analysis and try again regression analysis with each high and low water quality data more than estimations. An analysis of relation between water quality and flow rate of 10 watersheds shows that the water quality of the Nonsan and the Ganggyeong streams had been polluted by NPSSR pollutants. Other eight streams were important point source more than NPSSR. It is wide variation range of $BOD_5$ also high average concentration of $BOD_5$. We have to quantify water quality variation by cv1 in wet season and cv365 in dry season with comparing the estimate of high water quality and low water quality. This method can be used to indicator for water quality variation according to flow rate.

• 한국수자원학회논문집
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• 제39권3호
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• pp.261-274
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• 2006

본 연구에서는 소양강 유역을 대상으로 중장기 확률론적 댐 유입량 예측을 위해 30년 동안의 일단위 장기유출 해석을 수행하였다. 유출모형의 입력자료를 구축하기 위해 Anderson의 융설모형으로 적설에 대한 융설량을 계산하였고, Penman의 혼합기법으로 잠재증발량을 산정하였다. 또한, 기존 TOPMODEL의 적용 유역면적의 제약성을 극복하기 위해 대상유역을 적정 소유역으로 구분하고 운동파 하도홍수 추적기법을 통해 대유역 유출량을 계산할 수 있는 준분포형 TOPMODEL을 활용하였으며, 강수, 융설 및 잠재증발량을 유출모형에 입력하여 장기유출 해석을 수행하였다. 융설량 및 잠재증발량 계산결과는 관측자료의 부재로 그 정량적 평가는 수행할 수 없었지만 최대 적설깊이와 소형접시 증발량 자료와 같은 간접적 자료와의 시간적 변동성은 매우 잘 일치하였다. 이렇게 구축된 입력자료를 바탕으로 저수(1979년), 중수(1999년), 고수(1990년) 유출사상에 대한 모형의 최적 매개변수를 산정하고 준분포형 TOPMODEL의 일단위 장기유출 모의능력을 검토한 결과 계산유량과 관측유량 사이의 유출용적 상대오차가 5.64%, 상관계수가 0.91로 계산되어 비교적 정확한 유출결과를 제시하였고, 융설고려 유무에 따라 3, 4월의 유출용적 상대오차가 17% 및 4%로 감소함으로써 장기유출 계산시 모형의 정확도 향상을 위해 융설모형의 적용이 매우 필요한 것으로 나타났다.

• 국제학술발표논문집
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• The 6th International Conference on Construction Engineering and Project Management
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• pp.54-55
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• 2015

Increase of impervious areas due to expansion of housing area, commercial and business building of urban is resulting in property change of stormwater runoff. Also, rapid urbanization and heavy rain due to climate change lead to urban flood and debris flow damage. In 2010 and 2011, Seoul had experienced shocking flooding damages by heavy rain. All these have led to increased interest in applying LID and decentralized rainwater management as a means of urban hydrologic cycle restoration and Natural Disaster Prevention such as flooding and so on. Urban development is a cause of expansion of impervious area. It reduces infiltration of rain water and may increase runoff volume from storms. Low Impact Development (LID) methods is to mimic the predevelopment site hydrology by using site design techniques that store, infiltrate, evaporate, detain runoff, and reduction flooding. Use of these techniques helps to reduce off-site runoff and ensure adequate groundwater recharge. The contents of this paper include a hydrologic analysis on a site and an evaluation of flooding reduction effect of LID practice facilities planned on the site. The region of this Case study is LID Rainwater Management Demonstration District in A-new town and P-new town, Korea. LID Practice facilities were designed on the area of rainwater management demonstration district in new town. We performed analysis of reduction effect about flood discharge. SWMM5 has been developed as a model to analyze the hydrologic impacts of LID facilities. For this study, we used weather data for around 38 years from January 1973 to August 2014 collected from the new town City Observatory near the district. Using the weather data, we performed continuous simulation of urban runoff in order to analyze impacts on the Stream from the development of the district and the installation of LID facilities. This is a new approach to stormwater management system which is different from existing end-of-pipe type management system. We suggest that LID should be discussed as a efficient method of urban disasters and climate change control in future land use, sewer and stormwater management planning.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2002년도 학술발표회 논문집(II)
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• pp.1034-1040
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• 2002

A rainwater recharge model, which is combined with the quasi-three dimensional unconfined groundwater flow, is proposed in the present paper. The water budget in the catchments of the planned new campus of Kyushu University is evaluated by the present method that calculates both the surface runoff and groundwater flow simultaneously. The results obtained in the present study reveal that the calculated monthly and annual runoff discharges agree reasonably well with the observed discharge. Combining the rainwater recharge model, the two-phase groundwater flow equation is numerically solved f3r the entire area including the low land where the salt water intrusion is observed. The calculated depth of the salt-fresh interface agrees reasonably well with the observed ones at several cross sections. On the other hand, however, it is found that the calculated water budget remains uncertain because of lack of information on the accurate potential evapotranspiration including rainfall interception. In conclusion, however, it is found that the proposed method is applicable for the areas where the horizontal flow is dominant and the interface is assumed to be sharp.

• 한국환경복원기술학회지
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• 제22권6호
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• pp.115-124
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• 2019

In a climate change environment where heat damage and drought occur during a rainy season such as in 2018, a vegetation-based LID system that enables disaster prevention as well as environment improvement is suggested in lieu of an installation-type LID system that is limited to the prevention of floods. However, the quantification of its performance as against construction cost is limited. This study aims to present an experiment environment and evaluation method on quantitative performance, which is required in order to disseminate the vegetation-based LID system. To this end, a 3^rd quartile huff time distribution mass curve was generated for 20-year frequency, 60-minute probable rainfall of 68mm/hr in Cheonan, and effluent was analyzed by recreating artificial rainfall. In order to assess the reliability of the rainfall event simulator, 10 repeat tests were conducted at one-minute intervals for 20 minutes with minimum rainfall intensity of 22.29mm/hr and the maximum rainfall intensity of 140.69mm/hr from the calculated probable rainfall. Effective rainfall as against influent flow was 21.83mm/hr (sd=0.17~1.36, n=20) on average at the minimum rainfall intensity and 142.27mm/hr (sd=1.02~3.25, n=20) on average at the maximum rainfall intensity. In artificial rainfall recreation experiments repeated for three times, the most frequent quartile was found to be the third quartile, which is around 40 minutes after beginning the experiment. The peak flow was observed 70 minutes after beginning the experiment in the experiment zone and after 50 minutes in the control zone. While the control zone recorded the maximum runoff intensity of 2.26mm/min(sd=0.25) 50 minutes after beginning the experiment, the experiment zone recorded the maximum runoff intensity of 0.77mm/min (sd=0.15) 70 minutes after beginning the experiment, which is 20 minutes later than the control zone. Also, the maximum runoff intensity of the experiment zone was 79.6% lower than that of the control zone, which confirmed that vegetation unit-type LID system had rainfall runoff reduction and delay effects. Based on the above findings, the reliability of a lab-level rainfall simulator for monitoring the vegetation-based LID system was reviewed, and maximum runoff intensity reduction and runoff time delay were confirmed. As a result, the study presented a performance evaluation method that can be applied to the pre-design of the vegetation-based LID system for rainfall events on a location before construction.

• 한국물환경학회지
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• 제21권6호
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• pp.575-583
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• 2005

In this study the flow curve estimation is discussed using TANK model which is one of hydrologic models. The main interest is the accuracy of TANK model parameter estimation with respect to the sampling frequency of input data. For doing this, input data with various sampling frequencies is used to estimate model parameters. As a result, in order to generate relatively accurate flow curve, it is recommendable to measure stream flow at least every 8 days.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2005년도 학술발표회 논문집
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• pp.1199-1203
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• 2005

Combined sewer overflows(CSOs) are themselves a significant source of water pollution. Therefore, the control of urban drainage for CSOs reduction and receiving water quality protection is needed. Examples in combined sewer systems include downstream storage facilities that detain runoff during periods of high flow and allow the detained water to be conveyed by an interceptor sewer to a centralized treatment plant during periods of low flow. The design of such facilities as stormwater detention storage is highly dependant on the temporal variability of storage capacity available(which is influenced by the duration of interevent dry periods) as well as the infiltration capacity of soil and recovery of depression storage. As a result, a contiunous approach is required to adequately size such facilities. This study for the continuous long-term analysis of urban dranage system used analytical Probabilistic model based on derived probability distribution theory. As an alternative to the modeling of urban drainage system for planning or screening level analysis of runoff control alternatives, this model have evolved that offer much ease and flexibility in terms of computation while considering long-term meteorology. This study presented rainfall and runoff characteristics or the subject area using analytical Probabilistic model. Runoff characteristics manifasted the unique characteristics of the subject area with the infiltration capacity of soil and recovery of depression storage and was examined appropriately by sensitivity analysis. This study presented the average annual COSs and number of COSs when the interceptor capacity is in the range 3xDWF(dry weather flow). Also, calculated the average annual mass of pollutant lost in CSOs using Event Mean Concentration. Finally, this study presented a dicision of storage volume for CSOs reduction and water quality protection.

• 한국농공학회지
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• 제30권1호
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• pp.50-62
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• 1988

This study refers to the development of a hydrologic model simulating daily inflow and release rates for irrigation reservoirs. A daily - based model is needed for adequate operation of an irrigation reservoir sufficing the water demand for paddy fields which is closely related to meteorological conditions. Inflow rates to a reservoir need to be accurately described, which may be simulated using a hydrologic model from daily rainfall data. And the objective of this paper is to develop, test, and apply a hydrologic model for daily runoff simmulation. A well - known tank model was selected and modified to simulate daily inflow rates. The model parameters were calibrated using observed runoff data from twelve watersheds, Relationships between the parameters and the watershed characteristics were derived by a multiple regression analysis. The simulation results were in agreement with the data. The inflow model was found to simulate low flow conditions more accurately than high flow conditions, which may be adequate for water resources utilization.