• 한국수자원학회논문집
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• 제32권4호
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• pp.501-510
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• 1999

북한강 수계의 농업소유역에 대하여 하천수(2년)와 지하수(1년) 수질을 모니터링하여 분석하였다. 농업소유역의 주요한 비점원 오염물질인 총질소, 질산성 질소, 총인, BOD, TSS 및 대장균 농도를 주기적으로 측정하였다. 계절에 따른 수질의 변화 및 지하수와 하천수 수질과의 관계 비교를 통하여 토지이용이 수질에 미치는 영향을 분석하였다. 연구유역의 지하수 수위와 총질소, 질산성 질소의 농도의 벼농사와 밀접한 관련이 있었고 지하수와 하천수의 질소농도의 변화도 밀접한 관련이 있음이 나타나 벼농사가 하천의 질소농도에 많은영향을 주는 것으로 나타났다. 그러나 토지이용(벼농사)과 지하수 및 하천수의 총인, BOD, 대장균 농도 사이에는 일정한 관계를 발견할 수 없었다. 본 연구결과는 농업소유역의 수질변화를 이해하고 소하천의 수질관리정책을 개발하는데 유용하게 활용될 수 있을 것이다.

• 한국농공학회지
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• 제23권3호
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• pp.78-87
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• 1981

This study was attempted to get dimensionless unit hydrograph by linear model which can be used to the estimation of flood for the development of Agricultural water resources and laid emphasis on the application of dimensionless unit hydrographs for the ungaged watersheds by applying linear model. The results summarized through this study are as follows. 1.Peak discharge is found to be Qp= CAR (C =0. 895A-o.145) having high significance between peak discharge, Qp and effective rainfall, R within the range of small watershed area, 84 to 470km2. consequently, linearity was acknowledged between rainfall and runoff. Reasonability is confirmed for the derivation of dimensionless unit hydrograph by linear model. 2.Through mathematical analysis, formula for the derivation of dimensionless unit hydrograph was derived. qp--p=(tp--t)n-1[e-(n-1)](tp--t-1) 3.Moment method was used for the evaluation of storage constant, K and shape parameter, n for the derivation of dimensionless unit hydrograph. Storage constant, K is more closely related with the such watershed characteristics as length of main stream and slopes. On the other hand, the shape parameter, n was derived with such watershed characteristics as watershed area, river length, centroid distance of the basin and slopes. 4.Time to peak discharge, Tp could be expressed as Tp=1. 25 (√s/L)0.76 having a high significance. 5.Dimensionless unit hydrographs by linear model stood more closely to the observe dimensionless unit hydrographs On the contrary, dimensionless unit hydrographs by S.C. S. method has much difference in comparison with linear model at the falling limb of hydrographs. 6.Relative errors in the q/qp at the point of 0.8 and 1.2 for the dimensionles ratio by linear model and S. C. S. method showed to be 2.41, 1.57 and 4.0, 3.19 percent respectively to the q/qp of observed dimensionless unit hydrographs. 7.Derivation of dimensionless unit hydrograph by linear model can be accomplished by linking the two empirical formulars for storage constant, K, and shape parameter, n with derivation formular for dimensionless unit hydrograph for the ungaged small watersheds.

• 한국농공학회지
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• 제34권3호
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• pp.43-52
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• 1992

Design low flows were derived from the decision of a best fitting probability distribution and of an optimum transformation method can be contributed to the planning of water utilization and management of various hydraulic structures during dry season in the main river systems in Korea. The results were analyzed and summarized as follows. 1.Basic statistics for the selected watersheds were calculated as one of means for the analysis of extremal distribution. 2.Parameters for the different frequency distributions were calculated by the method of moment. 3.Type m extremal distribution was confirmed as a best one among others for the frequency distribution of the low flows by x$^2$ goodness of fit test. 4.Formulas for the design low flows of the Type m extremal distribution with two and three parameters were dervied for the selected watersheds. 5.Design low flows for the Type m extremal distribution when a minimum drought is zero or larger than zero were derived for the selected watersheds, respectively. 6.Design low flows of the Type m extremal distribution with two parameters are appeared to be reasonable when a minimum drought approaches to zero and the observed low flows varied within a relating small range while those with three parameters are seemed to be consistent with the probability distribution of low flows when a minimum drought is larger than zero and the observed low flows showed a wide range.

• 한국관개배수논문집
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• 제1권2호
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• pp.22-28
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• 1994

The calculation method for the Drought index based on the principal hydrological factors, such as precipitation, reservoir storage and river discharge, can estimate the duration and intensity of drought. It is not easy to establish an universal criteria o

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2023년도 학술발표회
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• pp.95-95
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• 2023

Common hydrological problems of developing countries include poor data management, insufficient measuring devices and ungauged watersheds, leading to small or unreliable data availability. This has greatly affected the adoption of artificial intelligence techniques for flood risk mitigation and damage control in several developing countries. While climate datasets have recorded resounding applications, but they exhibit more uncertainties than ground-based measurements. To encourage AI adoption in developing countries with small ground-based dataset, we propose data augmentation for regression tasks and compare performance evaluation of different AI models with and without data augmentation. More focus is placed on simple models that offer lesser computational cost and higher accuracy than deeper models that train longer and consume computer resources, which may be insufficient in developing countries. To implement this approach, we modelled and predicted streamflow data of the Asa River Watershed located in Ilorin, Kwara State Nigeria. Results revealed that adequate hyperparameter tuning and proper model selection improve streamflow prediction on small water dataset. This approach can be implemented in data-scarce regions to ensure timely flood intervention and early warning systems are adopted in developing countries.

• 물과 미래
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• 제29권5호
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• pp.223-233
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• 1996

우리나라의 강수와 유역특성을 고려하여 일강우량과 증발량의 입력자료로 일유출량을 모의발생할 수 있는 "한국 하천의 일 유출량 모형(DAWAST)"을 개발하였다. 이 모형은 개념화 모형을 기본모형으로 최적화모형, 일반화모형 및 수계화모형 등 3개의 부모형으로 구성되어 있다. 기본모형은 유역을 지표면, 불포화층과 포화층의 3개 저수층으로 단순화하고 각 저수층에서 일단위로 물수지를 분석하였다. 최적화모형은 관측유출자료가 있는 유역에서 최적화기법으로 매개변수를 보정하여 적용하고, 일반화모형은 유역특성인자로부터 매개변수를 예측하여 미계측 중, 소유역에 적용하고, 수계화모형은 유역특성인자 조사가 없거나 어려운 지점에서 최적화기법으로 분석된 수문지점의 매개변수를 전용하여 미계측 대유역에 적용하여 일유출량을 추정한다.유출량을 추정한다.

• 한국지반환경공학회 논문집
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• 제17권9호
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• pp.21-28
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• 2016

본 연구의 목적은 유역규모별 홍수침수면적을 산정하기 위한 하천지형 구축기법과 그에 따른 침수면적을 비교하는 것이다. 대상 지역은 경상북도 청도군과 의성군 내 14개소 하천이며 수치지도 DEM, ASTER DEM과 SRTM DEM을 이용하여 하천지형을 구축하였으며, HEC-GeoRAS, RAS Mapper, RiverCAD 모형을 적용하여 홍수침수해석을 수행하였다. 해석 결과와 실제 침수흔적도와 비교하였으며, 각 해석 모형들과 하천지형 구축기법에 따라 침수면적을 비교하였다. 침수흔적도와 비교한 결과 HEC-GeoRAS 모형의 결과가 이 침수흔적도의 범람면적과 대부분의 유역에서 유사한 값을 나타내었으며, SRTM DEM이 ASTER DEM보다 수치지도 DEM과 유사한 결과를 나타내었다. 중 대규모 유역의 경우 HEC-GeoRAS 모형과 Ras Mapper 모형, 소규모 유역의 경우 HEC-GeoRAS 모형과 RiverCAD 모형이 효율적인 해석 모형으로 나타났다.

• 한국수자원학회논문집
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• 제52권4호
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• pp.245-253
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• 2019

본 연구에서는 한강유역 산지소하천 미세소유역별 돌발홍수 재현기간을 산정하고, 돌발홍수 실사례를 활용하여 적합성을 평가하였다. 이를 위해 1시간 지속기간의 한계유출량과 SURR 모형으로 모의한 토양포화미흡량으로부터 돌발홍수능을 산정하였다. 이후 돌발홍수능을 초과한 과거 집중호우 사상(2002~2010년)의 강우량과 재현기간별 유역평균확률강우량을 비교하여 미세소유역별 돌발홍수 재현기간을 산정하였다. 또한, 돌발홍수 실사례(2011~2016년) 강수량으로부터 추정된 재현기간을 활용하여 적합성을 평가하였다. 돌발홍수 재현기간 산정결과 평균은 1.6년, 표준편차는 1.1로 산정되었으며, 1.1~19.9년 범위로 나타났다. 적합성 평가결과 돌발홍수 사례별 추정된 재현기간의 83%가 돌발홍수 재현기간 범위 이내로 나타났다. 본 연구에서 산정한 돌발홍수 재현기간의 적합성은 높은 것으로 판단된다.

• 한국농공학회논문집
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• 제46권7호
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• pp.71-80
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• 2004

A system for estimating daily paddy irrigation water requirements was developed to simulate daily stream flows that reflect various upstream and downstream return flows from river basin. Evapotranspiration in paddy fields was estimated using the modified Penman equation. Daily irrigation water requirements of paddy fields were calculated by multiplying the paddy area and the daily decrease in ponding depth. The system was constructed almost completely using images, grids, etc. in Visual Basic 6.0. The developed model was verified in the Damyang dam, and was used to estimate daily paddy irrigation water requirements at 12 small watersheds in Geum river basin for 20 years, from 1983 to 2002, covering paddy field areas of $3,332\~26,422$ ha. The results on the runoff analysis on the inflow to the Daecheong multi-purpose dam with various return flows were satisfactory. They were reasonable compared to the scenario where return flows were not considered.

• 한국환경과학회지
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• 제15권4호
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• pp.349-357
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• 2006

The purpose of this study is to evaluate the water pollution degree in the Mid-Nakdong River watershed regarding to landcover types using GIS method. As a result of landcover classification, rate of urban appeared highly on Daegu Metropolitan city. Also, rate of agriculture showed highly in the riparian zones of the Nakdong and Guemho River and rate of forest appeared highly in the borders of the study area. To identify the groups of watershed with similar landcover patterns using the Cluster Analysis. According to the cluster analysis, the fifty sub-watersheds were grouped in three clusters, 'Urban watershed', 'Agriculture watershed', 'Forest watershed'. The proportion of urban area in each cluster had a positive correlation with water pollution degree. Otherwise, the proportion of agriculture in the Agriculture watershed had a high positive correlation with water pollution degree. Therefore, it is necessary to estimate environmental capacity of water duality considering ecological and environmental characteristics of watershed ecosystem and expand water duality monitoring systems to small stream.