• Journal of Korea Water Resources Association
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• v.31 no.2
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• pp.199-208
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• 1998

This study is on the application of TOPMDEL(Topographic based hydrologic model) Which is a distributed rainfall-runoff model to the flood runoff analysis. The test area was Wichun experimental catchment site which is mountainous mid-area (Dongok, 33.63$\textrm{km}^2$ and Goro, 109,725 $\textrm{km}^2$) and being operated by the Ministry of Construction and ransporation. A three-dimensional digital elevation model(DEM) map was constructed using a physiographic map(1/25,000) and GIS software, Arc/Info, was used to the analysis of geofraphic factors. The topographic index of Dongok and Goro subcatchment was similar. As a results of the analysis, the model was validated that the simulated peak flow of a flood runoff was fit to the observed data. For the analysis of the effects of grid size, Dongok subcatchment was divided into 100,120-,240 m grid and Goro subcatchment was divided into grid and 120,200,350 m grid. It was shown that the peak flow increased in proportion to the increases of the grid size, but peak times were constant regardless of the grid size in both of the watershed.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.15 no.2
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• pp.221-230
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• 1997

In hydrology analysis, the result of a slope analysis for terrain have an very important effect on water quality and water quantity Recently, a slope analysis tend to use the digital elevation model rater than the traditional map sheet. But a terrain slope analysis by the digital elevation model depends on grid size of the digital elevation model. Hence the effect of a slope analysis by the digital elevation model is a important factor. In this study, therefor, in order to determine a hydrological parameter and a terrain parameter for simulation of the water quality and the hydrological property, we adapted two sample area that are the Nerin stream of the basin of the Soyang lake and a Osip stream of Samchuk, and its individual coverages are $640\;km^2$ and $33\;km^2$. Also to analyze the effect of grid size in the slope of a basin, we apply DEM changing a grid size respectively at intervals of 100 m from 100 m to 1.000m for the Nerin stream basin and at intervals of 10 m from 20 m to 300 m for the Osip stream basin.

• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.1787-1791
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• 2006

수공 구조물 설계를 위한 설계홍수량의 산정은 실측홍수량의 빈도해석을 통해 빈도별 설계 홍수량을 결정하는 것이 가장 바람직하나, 관측 홍수량 자료의 부족으로 인해 대상 유역의 강우량을 강우-유출 모형에 입력하여 설계 홍수량을 구하는 것이 일반적이다. 이러한 목적을 위해 이용되는 강우-유출 모형의 효과적인 적용을 위해서는 적절한 모형 매개변수의 결정이 매우 중요하며, 이를 위해 주로 이용되는 GIS 프로그램의 경우에는 적절한 격자 크기의 결정이 매개 변수 및 홍수량의 산정에 큰 영향을 미치게 된다. 본 연구에서는 분포형 강우-유출 모형인 TOPMODEL을 이용한 분석을 실시하였으며, 격자 크기의 변화에 따른 홍수량의 변화를 실측 홍수량과 비교 분석하였다. 분석 결과 괴산댐 유역 의 경우 격자 크기 $100{\times}100m$일 때 추출된 지형학적 매개변수를 이용해서 모의한 유출량이 실측 유량과 가장 근접한 것으로 분석 되었으며, 격자 크기에 따른 홍수량의 변화를 파악할 수 있었다. 추후 대상 유역을 확대한 연구를 통해 유역특성에 따른 격자 크기 결정 기준이 수립된 다면 분포형 강우-유출 모형의 신뢰성 향상에 기여할 수 있을 것으로 기대된다.

• Journal of Korea Water Resources Association
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• v.36 no.2
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• pp.251-261
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• 2003

The resolution issue of various soil moisture prediction parameters such as wetness index and curvatures is addressed. The sensitivities of various index are discussed on the base of the statistical aspects. The statistical analysis of three flow determination algorithms on the DEM is performed. The upslope area associated with SFD algorithm appear to more sensitive than the parameters of the other algorithms(MFD, DEMON). The wetness index shows relatively less variation both in resolution and the calculation Procedures.

• Journal of the Korean Geographical Society
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• v.44 no.2
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• pp.122-145
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• 2009

Terrain parameters calculated from digital elevation models (DEM) have become increasingly important in current spatially distributed models of earth surface processes. This paper investigated how the ability of upslope area for predicting the spatial distribution of soil properties varies depending on the selection of spatial resolutions of DEM and algorithms. Four soil attributes from eight soil-terrain data sets collected from different environments were used. Five different methods of calculating upslope area were first compared for their dependency on different grid sizes of DEM. Multiple flow algorithms produced the highest correlation coefficients for most soil attributes and the lowest variations amongst different DEM resolutions and soil attributes. The high correlation coefficient remained unchanged at resolutions from 15 m to 50 m. Considering decreasing topographical details with increasing grid size, we suggest that the size of 15-30 m may be most suitable for soil-landscape analysis purposes in our study areas.

• Journal of Environmental Science International
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• v.16 no.4
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• pp.523-532
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• 2007

This study utilized the 1/25,000 topographic map of the upper area from the Geum-ho watermark located at the middle of Geum-ho river from the National Geographic Information Institute. For the analysis, first, the influence of the size of critical area to the hydro topographic factors was examined changing grid size to $10m{\times}10m,\;30m{\times}30m\;and\;50m{\times}50m$, and the critical area for the formation of a river to $0.01km^2{\sim}0.50km^2$. It is known from the examination result of watershed morphology according to the grid size that the smaller grid size, the better resolution and accuracy. And it is found, from the analysis result of the degree of the river according to the minimum critical area for each grid size, that the grid size does not affect on the degree of the river, and the number of rivers with 2nd and higher degree does not show remarkable difference while there is big difference in the number of 1st degree rivers. From the results above, it is thought that the critical area of $0.15km^2{\sim}0.20km^2$ is appropriate for formation of a river being irrelevant to the grid size in extraction of hydro topographic parameters that are used in the runoff analysis model using topographic maps. Therefore, the GIUH model applied analysis results by use of the river level difference law proposed in this study for the explanation on the outflow response-changing characters according to the decision of a critical value of a minimum level difference river, showed that, since an ogival occurrence time and an ogival flow volume are very significant in a flood occurrence in case of not undertow facilities, the researcher could obtain a good result for the forecast of river outflow when considering a convenient application of the model and an easy acquisition of data, so it's judged that this model is proper as an algorism for the decision of a critical value of a river basin.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.1717-1721
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• 2008

집중호우로 인한 도시 내수배제 능력의 부족으로 월류가 발생하거나 하천의 제방붕괴, 통수능의 부족 등으로 인하여 범람이 발생하는 경우, 재해 예방차원에서 가장 근본적인 것은 침수의 양상을 파악할 수 있어야 한다. 즉, 어느 지역까지 침수지역이 확장될 것인가, 얼마나 빠르게 범람된 흐름이 흘러갈 것인가, 그리고 언제 홍수위가 감소할 것인가를 파악하는 것이 매우 중요하다. 그러므로 국내 도시지역 지형특성에 적합한 침수예측 모형의 개발이 필요하며, 이를 이용하여 다양한 범람 조건을 좀 더 합리적으로 모의할 수 있게 된다. 또한 물리적인 모형과의 비교를 통해 매우 복잡한 지형을 가진 도시침수계산 등이 이루어질 수 있으며, 침수구역에 대한 적절한 예 경보 및 피난대책의 수립이 가능하게 된다. 본 연구에서는 기존의 DEM 기반 침수해석 모형에서 계산시간이 오래 걸린다는 단점을 보완하기 위해 Sub-Grid를 적용한 침수해석 모형을 개발하였다. 하나의 격자는 $e_1$, $e_2$, $e_3$, $e_4$의 표고를 가지는 4개의 보조격자로 구성하였다. $25m{\times}25m$의 Sub-Grid를 갖는 $50m{\times}50m$의 격자에 대한 침수해석 결과와 Sub-Grid가 없이 $25m{\times}25m$ 및 $50m{\times}50m$ 격자로 구성된 대상유역에 대한 침수해석 결과를 비교하였다.

• Journal of Korea Water Resources Association
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• v.33 no.3
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• pp.279-288
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• 2000

The impact of land slope to the degree of flow divergence was considered employing distributional applications of slope exponents in the now directlOn algoriUnns. Lmear, exponential and ]X)wer law of distributional functIons were employed to address the variation of slope exponents m a terrain analysis. Dongok subwatershed at Wichun test watershed was selected as a study area. Digital Elevation Models of 20m, 30m, 40m and 50m grid size were made to perfonn the analysis. Various calcualtion methodologies of topographic index and the impact of grid sizes were investigated in terms of statistical and spatial aspects. DIstributional applications of slope e.xponents made it possible to represent the flow divergence and convergence about the ten-ain characteristics. The Monte~Carlo method was used to simulate six runoff events to check the impact of topographic factor in the runoff simulation.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.36 no.1
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• pp.143-149
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• 2016

This study evaluated the shear behavior of geogrid reinforced ballast material using a large scale direct shear test and discrete element method (DEM) based on PFC 3D program. The direct shear test was conducted on ballast materials that have different particle size distributions. Whereas the test results revealed that the shear strength generally increased with the larger particle size of ballast material without geogrid reinforcement, the shear behavior of ballast material was found to change pertaining to the relationship between particle size distribution and geogrid rib size. Generally, it is deemed the effectiveness of reinforcement can be achieved when the rib size is two times greater than average particle size. A numerical analysis based on DEM was conducted to verify the test results. The geogrid modeling was successfully completed by calibration process along with sensitivity analysis to have actual tensile strength provided by manufacturer. With a given geogrid model, the parametric evaluation was further carried out to examine the interactive behavior between geogrid and ballast material. Consequently, it was found that the effectiveness zone of geogrid reinforcement generated within a specific depth.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.933-933
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• 2012

최근 들어 우리나라를 포함한 전 세계적으로 극심한 기후변화와 기상이변으로 집중호우에 의한 피해가 급증하고 있으며, 기상재해에 따른 강우-유출 현상에 관한 정확한 해석이 필요하게 되었다. 국내의 경우에도 1990년 중반부터 매년 국지적 집중호우나 이상호우로 인해 재산 및 인명피해가 속출하고 있다. 대상유역으로 선정한 우이천 유역 또한 강북구의 대표적인 상습침수지역으로 피해 받고 있는 상황이며, 이를 예방하기 위해 홍수범람도 작성, 재해지도 작성 등의 지리정보시스템 기법 및 각종 수해대책이 활발하게 진행되고 있지만 아직은 미비한 실정이다. 본 연구에서는 우이천 유역에 대한 강우-유출 해석을 위한 분포형 모형인 Vflo$^{TM}$의 적용성을 검토 분석하는 데에 의의를 두었다. 또한 각 격자크기별로 유출량의 변화를 타 모형과의 비교를 통하여 적정성을 검토하였다. 이를 위해 대상유역의 1:1000 수치지형도를 이용하여 50m, 100m, 150m, 200m의 DEM을 생성하였고 ArcGIS 프로그램의 Hydro툴을 이용하였다. DEM을 보간하기 전 총 세 곳의 Sink를 발견하여 조정한 후 Filling하였으며 수치지형도와 정밀토양도로부터 초기 입력자료를 생성한 후 ASCII 파일로 변환하여 분포형 모형에 적용하였다. 또한 VfloTM 를 통해 구성한 격자망을 실제 흐름 방향을 고려하여 최종 유출구로 흐를 수 있도록 격자망을 재구성하였으며, 강우의 공간적 분포 방법으로 Cokriging 기법을 사용하였다. 분석 결과 격자 크기가 작은 경우 오히려 첨두유량이 작게 산정되었는데 이는 배수계통의 변화 및 수치지형도와는 다른 지표면 특성으로 인한 것으로 사료된다. 또한 배수구역의 최적화 결과 전반적으로 실측치와 유사한 값을 나타내었으며, 타 모형과 비교한 결과 비슷하거나 조금 나은 결과를 보였다.