• Journal of Korea Water Resources Association
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• v.33 no.S1
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• pp.203-208
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• 2000

• Proceedings of the Korea Water Resources Association Conference
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• 2001.05a
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• pp.194-199
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• 2001

• Current Research on Agriculture and Life Sciences
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• v.16
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• pp.37-44
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• 1998

The estimation of PMP (Probable Maximum Precipitation) and the analysis of characteristics of PMF (Probable Maximum Flood) according to the types of time distribution of rainfall and variations of base flow for the determination of design flood of major hydraulic structures in the watershed area of Wi stream were analysed. The PMP was estimated by the hydro-meteorological method suggested by the guideline of the World Meteorological Organization(WMO). The Blocking method was cited to transpose from PMP to PMS (Probable Maximum Storm) with time distribution. The unit hydrograph, applied for the estimation of PMF was derived by Clark's method. The summaryzed results : (1) The 72 hrs duration PMP in the area is 477.3mm which is 80mm less than the PMP map in Korea and 134 mm lager than the maximum precipitation of 342.9mm in Taegu, near the Wi stream watershed. (2) According to the types of time distribution and variations of base flow, the ranges of PMF for advanced type, central type and delayed type are 3,145.3~3,348.3cms, 3,774.6~3,977.7cms and 3,814.6~4,017.3cms, respectively. Those mean that peak discharge of advanced type is 600cms less than the central type and delayed type. (3) Delayed type among three types by Blocking method has been estimated the largest PMF of 4,017.3cms, and the advanced type has been estimated the smallest PMF of 3,145.3cms. The mean value of the peak PMF of 3,653.6cms may probably be resonable PMF in the Wi stream watershed. The mean PMF could probably be 1.7 times lager than the result of Gajiyama's equation. It is equivalent to the flood of return period 1,000 to 10,000 yrs.

• Journal of the Korean Association of Geographic Information Studies
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• v.9 no.1
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• pp.34-45
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• 2006

In this study comparison estimates travel times with observed travel time. In generally, peak flood discharges decrease become travel times longer. It is closely related to storage constant for the watershed routing of a flood. There are so many empirical formulas available for the estimation of travel time, storage coefficients and lag time but results computed generally show great different depending on individual formulas. When calculated flood discharge depend on the travel times varying the discharge. In this study the Wichun travel time shorter optimization travel time than observed travel time for the rusa and memi. There are showed good results for flood discharges, water level and velocity of the memi at the Younggok.

• Korean Journal of Ichthyology
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• v.29 no.3
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• pp.190-196
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• 2017

The egg and larval development of pale chub, Zacco platypus were determined by observation of laboratory reared larvae from hatching. The experimental adult fish were collected in Wicheon of Nakdong river in June 2016, The eggs and larvae were reared in the experimental tanks, and observed their morphological change. The egg diameter ranged from 1.68 to 1.78 mm ($mean{\pm}SD$, $1.73{\pm}0.07mm$, n =30). The eggs were hatch 70 hours after fertilization. The total length (TL) of the newly hatched larvae ranged from 5.39 to 5.42 mm ($5.40{\pm}0.02mm$, n=10). On the 8 days after hatching, 10 fin rays were formed in caudal fin at 7.89~7.93 mm TL ($7.91{\pm}0.02mm$, n=10). On the 44 days after hatching, the juveniles ranged from 16.1~16.5 mm TL ($16.3{\pm}0.28mm$, n=10).

• Journal of Korea Water Resources Association
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• v.33 no.2
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• pp.159-167
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• 2000

The purpose of this study is to estimate the stochastic monthly runoff model for the Kunwi south station of Wi-stream basin in Nakdong river system. This model was based on the theory of Box-Jenkins multiplicative ARlMA and the state-space model to simulate changes of monthly runoff. The forecasting monthly runoff from the pair of estimated effective rainfall and observed value of runoff in the uniform interval was given less standard error then the analysis only by runoff, so this study was more rational forecasting by the use of effective rainfall and runoff. This paper analyzed the records of monthly runoff and effective rainfall, and applied the multiplicative ARlMA model and state-space model. For the P value of V AR(P) model to establish state-space theory, it used Ale value by lag time and VARMA model were established that it was findings to the constituent unit of state-space model using canonical correction coefficients. Therefore this paper confirms that state space model is very significant related with optimization factors of VARMA model.

• Proceedings of the Korea Water Resources Association Conference
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• 2009.05a
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• pp.1384-1388
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• 2009

래스터 기반 DEM 모델을 이용한 수문지형인자의 산정은 DEM의 해상도(셀크기)에 영향을 받으며, 이러한 DEM의 해상도에 따른 불확실성은 강우-유출모델의 결과에 전파되어 모델의 모의결과에 오차를 발생시키는 원인이 된다. 또한 흐름경로의 결정은 수문모델링에서 DEM으로부터 수계를 형성하고 유역을 생성 및 분할하는데 있어 결정적인 역할을 하며, 각 셀의 경사는 흐름방향을 결정하고 흐름길이는 흐름경로를 따라 측정된 거리로서 결정된다. 이러한 모든 일련의 과정들은 셀간의 연산을 통해 이루어지며, 이러한 점에서 DEM의 해상도에 따른 DEM 처리연산 및 수문지형인자의 변동성은 중요한 고려사항이라 할 수 있다. DEM의 해상도에 따른 영향을 규명하기 위해서는 주요 수문지형인자를 대상으로 DEM의 해상도에 따른 민감도를 분석하는 것이 일반적이며, 따라서 본 연구에서는 위천, 황강 및 금호강 유역에 대해 DEM의 셀크기에 따른 유역면적, 유로연장과 최원유로연장, 유역평균경사와 같은 수문지형인자의 변동성을 분석하였다. 셀크기가 증가함에 따라 유로연장 및 최원유로연장이 감소하는 추세는 보이고 있지만 셀크기의 증가로 인해 반드시 흐름길이 및 유로연장이 감소 또는 증가되는 것은 아니며, 더 많은 유역에 대한 적용을 통해 유로연장에 대한 변동을 규명할 필요가 있을 것으로 판단된다. 또한 유역평균경사는 대체로 셀크기 $10\sim30m$에서 가장 큰 감소를 보이고 있으며, 셀크기 30m 이상에서는 감소크기가 점차 완만하게 나타난다. 그리고 셀크기가 증가할수록 유역평균경사에 대한 누가빈도곡선의 기울기는 점차 급해지고 누가빈도가 증가할수로 각 셀크기간의 유역평균경사의 감소에 큰 영향을 미침을 알 수 있다. 이는 비록 유역평균경사에 대한 누가빈도분포의 추세가 모든 해상도에 대해 유사하게 나타나고 있지만 급경사부에 대해서는 데이터 축약으로 인해 유역평균경사에 있어 상당한 감소를 발생시킬 수 있기 때문이라 판단된다.

• Journal of Korea Water Resources Association
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• v.38 no.7 s.156
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• pp.555-564
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• 2005

In this study, a simple rainfall-runoff model was proposed by using the hydraulic routing model that requires relatively few parameters. The parameters of this model were estimated by the watershed characteristics data, and were applied to the Soyang watershed and Ui stream watershed by using the kinematic wave for overland flow and dynamic wave routing for channel routing. In order to demonstrate validity, the proposed approach was compared to the HEC-1 model for the Soyang watershed. As the results of modeling have shown, the hydraulic model shows reasonable results similar to that of the HEC-1 model. This model also represents good results for the Ui stream watershed. Hence, even if this model is a simple rainfall-runoff model using general methodology, it is competitive to the natural watershed. However, it is still difficult to estimate the roughness coefficient and the catchment width, and therefore this model is in need of such supplements.

• Journal of Korea Water Resources Association
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• v.30 no.3
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• pp.279-291
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• 1997

This study is to evaluate the accuracy and practicality of the existing four conceptual models, two linear models of Clark and Nash model and two nonlinear models of Laruenson and WBN model, and to select an appropriate model to simulate the rainfall-runoff process in a given catchment. The variability of parameters for linear models is generally larger than that of nonlinear models. The errors in peak discharge are similar among the four conceptual models buy the errors in time to peak are quite different. Nonlinear models produce better results for time distribution than linear models. A comparison of the conceptual models to predict overall hydrograph using Friedman two-way analysis of variance by rank test indicates that nonlinear models are slightly better than linear models.

• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.334-338
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• 2011

일반적으로 유역에서 발생하는 토양손실은 붕괴사면과 표면침식, 토사류 붕괴에 의한 운반, 하상의 침식등 자연적인 요인과 도로건설, 산림의 벌채, 단지개발 등 인위적인 원인으로 발생할 수 있다. 토양손실의 발생은 농업생산성을 떨어뜨리고 목초지를 손상시키며, 물의 흐름을 방해하여 홍수위 상승, 저수지의 저수용량 감소, 고탁수 등 다양한 문제를 야기 시킨다. 이러한 문제를 해결하기 위해선 우선 토양손실 발생의 위험지역을 선정하고 그 지역을 집중적으로 관리하는 적절한 관리 대책의 마련이 필요하다. 이에 본 연구에서는 낙동강유역 전체를 대상유역으로 선정하고 토양손실 발생에 영향을 주는 여러 요소중 도시화나 농경지 확장 등 인간의 인위적인 개발로 인해 쉽게 변경될 수 있는 토지이용도를 이용하여 세부적으로 분석하였다. 토지이용도를 구성하고 있는 총 8가지의 토지이용항목 중 다른 항목들에 비해 분포면적이 매우 작은 녹지, 습지, 나지를 제외한 5가지의 항목(시가화, 논, 밭, 산림, 수역)의 분포면적을 통해 토지 이용특성에 따른 유사발생의 연관성을 파악하였으며 유역별 유사발생 위험순위를 평가하였다. 유사발생 위험순위 평가결과, 전체 낙동강유역내 유사발생 위험성이 높은 표준유역들로 구성되어있는 중권역은 내성천, 위천합류점, 합천댐유역, 안동댐유역으로 모두 높은 순위를 차지했다. 내성천유역, 위천합류점 유역, 합천댐유역은 구성하고 있는 표준유역의 절반 이상이 높은 순위들로 구성되어 있으며 안동댐유역은 구성하고 있는 소수의 표준유역이 유역내 최상위 순위를 차지하였다.