• 한국환경복원기술학회지
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• 제6권4호
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• pp.52-61
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• 2003

This study was carried out to analyze the effects of stormwater retention and infiltration pond on reduction of flood peak and volume in a experimentally developed ecological pond. The experimental site has 542$m^2$ watershed area, 1,310mm yearly-averaged rainfall. And the area of the retention pond is 60$m^2$, the maximum water depth is 0.5m, the maximum and average storage is 15$m^3$and 9.3$m^3$d. And the area of infiltration pond is 58$m^2$, and the water depth varies 0.2m~0.5m. The monitoring system consists of one rainfall gage, one Parshall flume and acoustic water level gage, two rectangular weirs and acoustic water level gage for discharge gaging, and one data recording unit. Data from ten storm events in total, three storm events in year 2000 and seven storm events in year 2001, were collected. From the data the evaporation rate was achieved with the water balance equation, and the result shows 5.0mm/day in average. The result from the analysis of the effects on reduction of flood peak and volume, is that 14% reduction of flood volume and 15% reduction of flood peak in retention pond and 49% reduction of flood volume in infiltration pond.

• 한국방재학회:학술대회논문집
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• 한국방재학회 2008년도 정기총회 및 학술발표대회
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• pp.743-746
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• 2008

Recently, due to the effect of global warming and extreme rainfall, the magnitude of flood disaster and the frequency of flood is rapidly increasing. In order to mitigate the damage of human and property from this kind of meteorological phenomenon and manage water resources scientifically, effective operation of dam and reservoir is very important. In case of Andong dam which was not performed a flood control function needs to develop new types of dam safety management measure because of recent extraordinary flood by typhoons. In case of Andong dam and Imha dam, I am using HEC-5 model in order to apply reservoir simulation. In this case, complex conditions among 100-year floods , 200-year floods and PMF was used. Also, I modified the maximum outflow 3,800m3/s into 3,490m3/s and applied this modified discharge in order to secure freeboard in the downstream. In an analysis that I applied modified outflow by 100-year floods and 200-year floods to, the result showed that river didn't overflow in Andong area but some other places have relatively low freeboard. In the cases that I modified maximum outflow, results showed that freeboard of levee is larger than existed simulation. In the simulation that I applied 200-year floods and PMF to and under a condition connected with PMF, results showed overflowing the levees. Because of the difference between the frequency of dam outflow and the design flood in river, it is required to improve the existed flood plan in the downstream of Andong dam. As a result of this study, the optimal operation of reservoir systems can be proposed to mitigate the flood damage in the downstream of Andong dam and also can be used to establish the flood plans.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2015년도 학술발표회
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• pp.173-173
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• 2015

The flood water level in tidal river is determined by the joint effects of flood discharge and tidal water levels at downstream boundary. Due to the variable tidal boundary conditions, the evaluated design water levels associated with a certain flood event can be significantly different. To avoid determining of design water levels just by a certain tidal boundary condition and remove the influence of variability in boundary condition from the evaluation of design water levels, a probabilistic approach is considered in this study. This study focuses on the development of a method to evaluate the realistic design water levels in tidal river with taking into account the combined effects of river discharge and tidal level. The flood water levels are described by the joint probability of two driving forces, river discharge and tidal water levels. The developed method is applied to determine design water levels for the tidal reach of the Han River. An unsteady flow model is used to simulate the flow in the reach. To determine design water levels associated with a certain flood event, first, possible boundary conditions are obtained by sampling starting times of tidal level time series; then for each tidal boundary condition, corresponding peak water levels along the channel are computed; and finally, design water levels are determined by computing the expectations of the peak water levels. Two types of tides which are composed by different constituents are assumed (one is composed by $M_2$, and the other one is composed by $M_2$ and $M_2$) at downstream boundary, and two flood events with different maximum flood discharges are considered in this study. It is found that (a) the computed design water levels with two assumed tides have no significant difference for a certain flood event, though variability of peak water levels due to the tidal effect is considerably different; (b) tidal effect can reach to the Jamsil submerged weir and the effect is obvious in the downstream reach of the Singok submerged weir; (c) in the tidally affected reach, the variability of peak water levels due to the tidal effect is greater if the maximum flood discharge is smaller.

• Korean Journal of Hydrosciences
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• 제4권
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• pp.51-63
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• 1993

This study is to verify the applicability of statistical models in predicting flood frequency at the stage gaging stations of which the flow is under natural condition in the Han River basin. The results of the study show that the statistical flood frequency models were proven to be fairly reasonable to apply in practice, and also were compared with sampling variance to calibrate the statistical efficiency of the estimators of the T year floods Q(T) by two different flood frequency models. As a result, it was showed that for return periods greater than about T = 10 years the annual exceedance series estimators of Q(T) has smaller sampling variance than the annual maximum series estimators. It was showed that for the range of return periods the partial duration series estimators of !(T) has smaller sampling variance than the annual maximum series estimate only if the POT model contains at least 2N(N : record length) items or more in order to estimate Q(T) more efficiently than the ANNMAX model.

• 한국관개배수논문집
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• 제16권1호
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• pp.94-99
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• 2009

• 한국농공학회논문집
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• 제48권5호
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• pp.17-27
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• 2006

The objective of this study is to induce the design floods by the methodology of L-moment including test of homogeneity, independence and outlier of the data of annual maximum flood flows for 12 water level gaging stations of South Korea. To select appropriate distribution of the data for annual maximum flood flows, the distributions of Wakeby and Kappa are applied and the appropriateness is judged by Kolmogorov-smirnov (K-S) test. The parameters of selected Wakeby and Kappa distributions are calculated by the method of L-moment and the design floods are induced. Through the comparative analysis using the relative root mean square errors (RRMSE) and relative absolute errors (RAE) of design floods, the result shows that the design floods by Wakeby distribution are closer to the observed data than those obtained by the Kappa distribution.

• 한국농공학회논문집
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• 제51권4호
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• pp.49-55
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• 2009

This paper is to induce design floods through L-moment with 3 and 4 parameter Kappa distributions including test of independence by Wald-Wolfowitz, homogeneity by Mann-Whitney and outlier by Grubbs-Beck on annual maximum flood flows at 9 water level gaging stations in Han, Nakdong and Geum Rivers of South Korea. After analyzing appropriateness of the data of annual maximum flood flows by Kolmogorov-Smirnov test, 3 and 4 Kappa distributions were applied and the appropriateness was judged. The parameters of 3 and 4 Kappa distributions were estimated by L-moment method and the design floods by water level gaging station was calculated. Through the comparative analysis using the relative root mean square errors (RRMSE) and relative absolute errors (RAE) calculated by 3 and 4 parameter Kappa distributions with 4 plotting position formulas, the result showed that the design floods by 4 parameter Kappa distribution with Weibull and Cunnane plotting position formulas are closer to the observed data than those obtained by 3 parameter Kappa distribution with 4 plotting position formulas and 4 parameter Kappa distribution with Hazen and Gringorten plotting position formulas.

• 한국습지학회지
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• 제13권2호
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• pp.219-229
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• 2011

본 연구는 강우특성과 홍수피해액과의 관계를 히스토그램분석을 이용해 분석하였다. 분석대상의 공간적 범위는 전국 및 16개의 광역자체단체로 하였으며 시간적 범위는 1994년에서 2009년까지 16개년도의 홍수피해 자료를 이용하였다. 분석결과, 홍수로 인한 총 피해액은 대부분 발생횟수가 높은 중 소규모 호우사상에 의한 피해 비중이 가장 높게 나타나고 있음을 알 수 있었다. 또한 국내 16개 광역지자체별 홍수피해액을 비교한 결과 도(道)에 비해 광역시의 방재능력이 우수한 것으로 나타났으며, 각 지자체별로 총 피해액이 최대로 발생하는 강우 특성들이 상이하게 나타났다. 따라서 국가에서 집중해야 할 치수대책 수립 시 위의 결과들을 고려하여 대상 규모를 결정하여야 할 것으로 판단된다.

• 한국지리정보학회지
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• 제16권4호
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• pp.1-15
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• 2013

세계적으로 홍수로 인하여 인명과 재산의 피해가 발생하고 있다. 국내에서는 홍수피해를 줄이기 위하여 비구조물적 대책의 하나로 홍수범람지도를 작성하고 있으며, 홍수범람해석을 위한 다양한 모형이 연구되고 있다. 본 연구에서는 LiDAR 자료와 LISFLOOD 모형을 이용한 홍수범람해석을 수행하여 국내 하천에서의 적용성을 검토하고, 파제 시나리오에 의한 파제 위치별 범람해석 결과를 평가하였다. 범람해석 결과 최대 홍수범람면적에서는 HEC-RAS 모형에 의해 작성된 홍수범람도와 차이가 약 4% 미만으로 유사하였으며, 파제 시나리오에 의한 홍수범람해석에서는 시나리오 별로 약 0.2%~6.5%의 범람면적 차이를 나타내었다. 또한 파제 위치에 따라서 홍수범람 양상이 다르게 나타났으며, 제내지에서 범람류의 흐름방향과 하천 흐름방향의 관계에 따라 최대 홍수범람면적과 최대 침수심이 변화함을 확인할 수 있었다. 연구 결과 국내 하천에서 홍수범람해석시 LISFLOOD 모형의 적용이 가능하고, 다양한 범람상황을 고려한 홍수범람해석이 가능할 것으로 판단된다.

• Ecology and Resilient Infrastructure
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• 제3권4호
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• pp.294-301
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• 2016

금강의 지류인 치성천의 홍수범람이 빈번하게 발생하는 구간을 대상으로 하단배출형 가동보를 다단으로 배치하여 가동보 관리수위별 홍수조절 및 저류 효과를 기존 고정보의 설치 경우와 비교 분석하였다. 하단배출형 가동보 설치 지점에서의 첨두유량이 최대 97%가 감소하였고, 하류단 홍수위가 최대 82%가 감소하였다. 또한 하단배출형 가동보의 다단 배치로 구조물 상류구간에 저류와 분배 기능으로 저류량이 최대 463%가 증가하였다. 이러한 저류량과 하류단 첨두 홍수위, 유량의 관계를 통해 대상구간의 목표 저류량과 홍수 저감 수위를 위한 각 가동보의 관리수위 제안이 가능하다.