• KSCE Journal of Civil and Environmental Engineering Research
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• v.6 no.4
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• pp.69-78
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• 1986

The floodwave propagation resulting from the earth dam-break is studied. DBF(Dam-Break Floodwave) model based on the dynamic wave equation is presented by introducing Preissmann scheme and double sweep algorithm. DBF model is applied to the Teton dam, and the numerical results have good agreements with the data observed in the peak elevation profile, the peak discharge, the flood travel time and the flooded area.

• Water for future
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• v.27 no.4
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• pp.95-104
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• 1994

The sinuosity model has been developed to simulate to developed to simulate the floodwave in meandering channels by solving the extended Saint-Venant equation with the Preissmann scheme. The suggested model is compared with three conventional floodplain routing methods in terms of governing equations, mass conservation error and floodwave analysis. The sinuosity model produces the mass conservation error of 1.5-1.8%, however the separate channel model produces 9.1% and 27.4% for sinuosity of 1.5 and 2.0, respectively. The model has been used to simulate flow in an idealized meandering river with a floodplain. The attenuation ratio and the travel time ratio are found to increase as the floodplain roughness and width increase and as the sinuosity factor decreases. The model is expected to contribute the floodwave analysis in sinuous channel with compound corss sections.

• Journal of Korea Water Resources Association
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• v.31 no.2
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• pp.189-198
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• 1998

Five dam-break floodwave models are t재 field data sets. The models included FLDWAV, SMPDBK, HEC-1, Tr66, and HEC Dimensionless Graph. The field data sets documented the disasters at Teton dam, and Yeunchun dam. The FLDWAV results are uesd to test the sensitivity of the floodwave to variations in Manning's roughness coefficient, breach size, and bottom slope. The HEC-1 analysis includes testing the sensitivity of the results to model parameters. The TR66 model and FLDWAV, with channel routing by TR66 in both cases. SMPDBK and the Dimensionless Graph procedure are applied without particular difficulties being encountered in both real world cases. It is necessary to analyze numerical limit of existing numerical models and then to apply the relatively accurate numerical model in real basin. It is found that FLDWAV model is superior in numerical accuracy and stability to any other model. This study will contribute to improve defect of numerical models and develop more precise numerical model for a efficient and rapid dam breach flood disaster predict.

• Water for future
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• v.20 no.4
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• pp.285-294
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• 1987

The floodwave analysis for unsteady supercritical flow is performed. The numerical model. based on dynamic wave equation is presented by introducing the general Preissmann scheme and fore-sweep algorithm.The model is applied to Buffalo-Creek floods for proving its validity, and the simulation results have good agreements with those computed by DAMBRK and the observed data. It is also applied to Hyogi dam-break. The outflow hydrograph is derived based on the observed data and the analysis for the floodwave propagation is investigated.

• Water for future
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• v.23 no.4
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• pp.467-476
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• 1990

Numerical model for the floodwave propagation on dry bed which is resulting from the instantaneous failure of a dam has been developed by moving Hartree scheme. The numerical simulation result of the model has good agreements with the observed data by WES in terms of stage hydrograph and characteristics profiled. The model would contribute effectively to forecast the flood on dry bed resulting from instantaneous dam-break.

• Proceedings of the Korea Water Resources Association Conference
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• 2005.09b
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• pp.1231-1232
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• 2005

• Water for future
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• v.28 no.5
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• pp.163-174
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• 1995

A diffusion hydrodynamic model named "DFLOW-2" for the floodwave analysis from levee-break in protected lowland has been developed. The model has been applied to Ilsan levee-break, which occurred on September 12-13, 1990 in the downstream of the Han River. An unsteady flow analysis has been made in the reach from Indokyo to Junryu. Overflow through broken levee has been treated as internal boundary condition in the channel. A post-processor has been also developed to demonstrate the simulation results. The velocity distributions and inundated depths have been presented. The computed results have good agreements with observed data in terms of inundation depth, flood arrival time and flooded areas.ded areas.

• Journal of Korea Water Resources Association
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• v.31 no.4
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• pp.415-427
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• 1998

FIAS (Flood Inundation Analysis System) using Arc/Info is developed and applied to the South Han River basin. The DWOPER model is revised and expanded to handle simultaneous multiple overtopping and/or breaking and to estimate the inundation depth and extents. The model is applied to an actual levee overtopping case, which occurred on August 23~27, 1995 in the South Han River. Stage hydrographs inside and outside of the levee are compared, then inundated discharges from overbank spilling are computed. The Graphic User Interface is developed with AML(Arc/Info Macro Language). Two-and three-dimensional inundation maps by Arc/Info are presented. The computed inundation extends agree with observations in terms of inundation depth and flooded area. Keywords : River, Floodwave, Flood Inundation, Geographic Information System.

• Journal of Korea Water Resources Association
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• v.31 no.3
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• pp.337-345
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• 1998

DAMBRK-U model is developed for the evaluation of overtopping risk of dam and levee and for the estimation of uncertainty in floodwave simulation. The original algorithm is revised and expanded to include Monte-Carlo analysis to estimate them. The model is tested by applying to hypothetical channels of widening, uniform and narrowing geometry. Larger variation in discharge and water depth are expected at narrower sections of a river. It is calibrated by applying to the Hantan River, where severe damages from Yunchun dam-break and levee overtopping occurred on July, 1996. Overtopping risk of dam is calculated for various discharge conditions for Yunchun-dam, and that of levee is also calculated by comparing levee height with flood level at Hantan recreation area. Simulation results show that the overflow depth of flood level is 1,266~0.782 m and the overflow risk turns out to be 100%.

• Proceedings of the Korea Water Resources Association Conference
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• 2005.05b
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• pp.1021-1025
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• 2005

물리적 파괴력을 가진 하천의 유수 및 토사가 주택, 농경지, 시설 등에 피해를 입히는 것을 방지하거나 저감하기 위해서는 홍수방어 및 조절 계획에 따라 구조적 대책과 비구조적 대책을 적절히 강구해야 한다. 구조적 대책 중에서도 제방은 기본적이고도 중요한 역할을 차지한다. 하천제방이 붕괴되었을 때 발생하는 홍수범람구역의 정확한 추정과 홍수파가 제내지에서 거동하는 양상을 파악하는 것은 홍수피해를 저감하는 데 있어서 매우 중요한 과제이다. 이는 홍수전에는 치수사업 계획시 좀더 정확한 경제성 분석을 하는데 필요한 입력자료와 효율적인 계획수립에 있어서 그 범위를 결정하는 중요한 역할을 하며, 홍수시에는 신속한 대피를 유도하고, 긴급한 수방대책을 수립하는데 적용할 수 있기 때문이다. 제내지 범람 홍수파에 대한 수치해석은 여러 차례 수행된 바 있으나, 범람홍수파의 수리특성 규명이나 수치모형 검증을 위한 수리실험은 거의 수행되지 않은 것으로 알려져 있다. 제방붕괴의 원인에 따라 붕괴형태나 과정은 많은 차이를 보이겠으나 제방이 붕괴되는 과정에서 홍수류가 제내지로 어떠한 양상으로 유입되는지를 분석하기 위하여 국내외에서 수행된 실험을 분석한 후, 제내지 범람 수리실험 방안을 수립하였다. 본 논문은 제방붕괴에 의한 홍수범람에 대한 대피체계를 설립하기 위한 기초자료를 제공학기 위해 수행되었으며, 수리실험은 홍수터에서 홍수의 거동을 연구하기 위해 실시되었다. 본 논문에서는 제방붕괴와 홍수터에서의 홍수파 유속, 최대수심, 수면곡선의 관계에 대하여 연구하였다.