• Journal of the Korean Association of Geographic Information Studies
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• v.10 no.1
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• pp.124-135
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• 2007

The purpose of this study is to analyze the hydraulic behavior in a stream reach using SMS RMA-2 model with a series of dynamic boundary conditions of main stream and lateral flows simulated by WMS HEC-1 program. For the stream reach (10.5 km) between Gongdo and Pyeongtaek water level gauge stations of Anseongcheon, the model simulated two dimensional flow characteristics by applying dynamic flow conditions of rainfall frequencies of 50, 100, 500, and 1,000 years for the main stream and three tributaries. The temporal flow behavior successfully simulated and the results showed that the distribution of mean velocity and water level within the stream reach increased according to the increase of flow frequency. Especially, the flow velocity sensibly increased at the near downstream of lateral inflow as the width of main stream is narrower.

• Proceedings of the Korea Water Resources Association Conference
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• 2007.05a
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• pp.1277-1281
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• 2007

1차원 수치해석망은 수위관측소와 우량관측소를 경계로 광역모형을 구성하고 HEC-RAS를 이용하여 부정류 해석을 실시하였다. 그 결과로 얻은 유량과 수위자료는 2차원 해석 모형인 RMA-2의 경계조건으로 적용하였다. 또한 수치지형도를 이용하여 2차원 격자망을 구성하고 RMA-2를 적용하여 수리특성을 분석하였다. 광역모형의 구성에 의한 HEC-RAS 부정류 해석 결과 제방설치 전과 후의 수리특성의 변화는 그리 크게 나타나지 않았다. 또한 RMA-2 해석 결과 계획홍수량 초과하는 홍수에서 대상유역에서 제방설치 전과 후의 변화는 통수단면적의 감소에 따른 빠른 흐름과 수위의 변화를 가져왔으나 그 크기는 현저하지 않음을 보여준다.

• Journal of the Korean Society of Industry Convergence
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• v.8 no.4
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• pp.213-220
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• 2005

The Youngwal 1, Youngwal 2 and Youngchun gaging stations are observed flood flow and low flow during Mar. 2004~Oct. 2004. They are observed water stages and flow velocities for flood and low flow. The observed data are used to derived rating curve and equations. The HEC-RAS model is applied for hydraulic modeling in gauging stations. The model is designed to perform one-dimensional hydraulic calculations for an river improvement plan in a full network of natural and constructed channels, and is comprised of a graphical user interface(GUI), separate hydraulic analysis components, data storage and management capabilities, graphics and reporting facilities.

• Proceedings of the Korean Society of Agricultural Engineers Conference
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• 2002.10a
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• pp.293-296
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• 2002

The purpose of this study is to evaluate the hydrological impact due to temporal land cover change urbanization of Anseong-cheon watershed $(585.09km^2)$. WMS (Watershed Modeling System) HEC-1 was adopted, and burned DEM with $200{\times}200m$ resolution and soil map reclassified by hydrologic soil groups were prepared. Land cover for 1985, 1990, 1995 and 2000 were classified by maximum likelihood method, using Landsat MSS and TM imageries. Calibration and verification of HEC-1 were conducted using 4 storm events. Peak flow at Pyeong taek station increased $25.9m^3/sec$ during the past 15 years due to paddy and forest decrease. Streamflow impact by just paddy area decrease and forest area decrease were also analysed keeping watershed CN values unchanged of the given year, respectively.

• Journal of the Korean Ceramic Society
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• v.37 no.12
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• pp.1192-1197
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• 2000

Si-Mg 첨가물, LiOH, NaOH로부터 제조한 슬러리의 수열반응으로 헥토라이트 점토를 합성하였다. 수열합성의 온도와 반응시간에 따른 합성헥토라이트 점토의 화학적 조성과 결정형태를 조사하였고, 합성헥토라이트 0.2~1.0% 수분산액의 투과도와 입경을 UV-VIS 분광광도계와 투과전자현미경으로 각각 측정하였다. 합성헥토라이트 수분산액의 투과도와 유동성은 25$0^{\circ}C$, 6시간의 합성조건과 Si/Mg/Li/Na=8.0/5.4/0.6/0.6의 조성에서 최대치를 나타내었고, Mg/Si=5.4/8.0의 슬러리 조성으로부터 합성된 헥토라이트(Hec-6)가 최적의 투명성과 용액점도를 나타내었다. 또한 Hec-6의 수분산액은 높은 전단력에서 낮은 점도의 졸상으로 전화됨으로서 요변성을 나타내었고, 1.0% Hec-6/sodium carboxymethyl cellulose(50/50) 혼합용액은 전단력이 1.0 s$^{-1}$ 이상에서 1.0% Hec-6 수분산액보다 더욱 높은 점도를 나타냄으로서 점도의 상승효과가 나타났다.

• Proceedings of the Korea Contents Association Conference
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• 2012.05a
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• pp.115-116
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• 2012

본 연구는 미호천의 홍수위 안정성 검토를 위하여 HEC-HMS를 이용해 첨두홍수량을 산정하였다. HEC-RAS를 적용하여 200년빈도의 홍수량에 대해 홍수위를 검토 하였다. 홍수위 분석 결과는 대체척으로 유역의 상류구간은 안전성을 확보하였으나 병천천 합류후 하류구간의 2지점은 위험단면으로 평가 되었다.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.13 no.5
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• pp.157-163
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• 1993

The present study focuses on simulating river profile changes downstream of the Daecheong multipurpose dam by using the computer program HEC-6, which was developed by the United States Army Corps of Engineers. The dam locates at the Keum river, a typical alluvial stream, whose bed material is composed mostly of fine and medium sands. The study reveals that after the completion of dam, a 15 km long reach downstream from the regulatory dam was severely degraded by about 2~3 m. No further severe degradation of this reach is expected, however, because the river-bed of this reach has been well armored since then with gravels and cobbles. Some places in the study reach were degraded locally by 2 m, due mainly to the large-scale gravel mining activities in that reach. On the other hand, a 20 km long reach in downstream study reach is aggraded more or less by 0.5~1 m. Calculation by the computer program HEC-6 is close to measurement for the study river reach. According to the results by HEC-6, the study river reach would remain generally stable in the future, except a few places in the mid-upstream where further river-bed degradation of 1~2 m would occur and a few places in the far downstream where local river-bed aggradations of about 0.5 m would occur.

• Journal of Industrial Technology
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• v.25 no.A
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• pp.3-14
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• 2005

In order to accurately analyze the detailed hydraulic characteristics of the curved channel in the downstream of dam with the hydraulic structures such as bridge piers, RMA2 model which is one of two-dimensional models is applied to ChunCheon dam downstream curved channel. A series of hydraulic model tests are carried out for comparison studies. HEC-RAS model is also applied to the same site. There are no errors when velocities and water levels resulted from HEC-RAS model RMA2 model are compared with those of hydraulic model test on the straight channel. But, it is found that results of RMA2 model have a better agreement with those of hydraulic model test than those of HEC-RAS model on the curved channel with bridge piers. Additionally, RMA2 model can be predicted the eddy phenomena around bridge piers of the curved channel.

• Journal of the Korean Society of Industry Convergence
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• v.7 no.3
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• pp.281-288
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• 2004

The objective of this study is to propose a methodology of the flood runoff analysis in steep mountainous basins and the analysis basin is the Jasa valley basin in Chungju city Analyzing the spatial pattern of the rainfall in 1994. 6 30~7.1, the seasonal rainy front was tied up in the whole central district, and the rainfall center was moving from the northern Chungbuk province to the northern Kyongbuk province and caused heavy storm. Analyzing the temporal pattern with the Huff method, the 52.5% of the rainfall was concentrated on the 3rd quartile. Rainfall frequency analysis is accomplished by five distribution types; 2-parameter Lognomal, 3-parameter Lognomal, Pearson Type III, Log-Pearson Type III and Extremal Type I distribution Rainfall-runoff analysis in Jasa valley basin was made using HEC-HMS model. Jasa valley basin was divided into 3 sub-basins and the analysis point was 3 points{A, B and C point) With the rainfall data measured by the 10 minutes, the flood runoff also was calculated by as many minutes. SCS CN model, Clark UH model and Muskingum routing model in HEC-HMS model were used to simulate the runoff volume using selected rainfall event.

• Journal of Environmental Science International
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• v.26 no.4
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• pp.411-420
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• 2017

This research aims at comparing the accuracy of flood discharge estimation. For this, we focused on the Oedo watershed of Jeju Island and compared flood discharge by analyzing the values as follows: (1) the concentration of the lumped model (HEC-HMS) and distributed model (Vflo), and (2) the in-situ data using Fixed Surface Image Velocimetry (FSIV). The flood discharge estimation from the HEC-HMS model is slightly larger than the Vflo model results. This result shows that the estimations of the HEC-HMS are larger than the flood discharge data by 4.43 to 36.24% and that of the Vflo are larger by 8.49 to 11%. In terms of the error analysis at the peak discharge occurrence time of each mapping, HEC-HMS is one hour later than the measured data, but Vflo is almost the same as the measured data.