• Title/Summary/Keyword: 지형해석

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Prediction of Long-Term River Bed Changes in Saemangeum Area (새만금지구 장기 하상변동 예측)

  • Jung, Jae-Sang;Song, Hyun Ku;Lee, Jong Sup;Kim, Gweon Su
    • Proceedings of the Korea Water Resources Association Conference
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    • 2016.05a
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    • pp.394-398
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    • 2016
  • Numerical analysis was conducted using Delft3D developed by Deltares in Netherlands to predict long-term river bed changes in Saemangeum Area. Tidal flow, discharge through the drainage gates and river bed changes in numerical model was verified by comparing to the results of field observation and hydraulic experiments. We calculated long-term river bed changes in Saemangeum area for 10 years from 2031 to 2040 after completion of development in Saemangeum. It is shown that 70 cm and 139 cm of accumulation occur in estuaries of Dongjin River and Mankyong River, respectively. Variation of flood level was also investigated considering long-term river bed changes. There was no change in estuary of Dongjin River but maximum flood level in estuary of Mankyong River increased 81 cm.

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Research on Cultural Scenic Landscape in Jingyeong Sansuhwa - Centering around Gyeomjae Jeongseon's Works - (진경산수화에 표현된 풍토경관에 관한 기초연구 - 겸재 정선의 작품을 중심으로 -)

  • Yoo, Kahyun*;Sung, Jong-Sang
    • Journal of the Korean Institute of Landscape Architecture
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    • v.37 no.1
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    • pp.87-99
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    • 2009
  • This research is an introductory study that hopes to interpret the cultural scenic landscape by analyzing Korea's mountains, streams, topography, color, light, human behavior, and more based on real landscape paintings. It places its purpose on understanding our intrinsic cultural scenic landscape by investigating the changed topography and the differing life patterns caused bythe active national land development after the modern era. With Seoul, which is now difficult to find images of its past, and the surrounding areas of the Han riverbed, the interpretation related to its original topography, landscape, climate, weather, and human behaviors was observed while the main focus was placed on the climate of the perception held by people regarding Mt. Geumgang and other ranges which are not fully opened to the public yet. In order to comprehensively analyze the figures of features and appearing landscapes including color, light, and more, it was described through the concept called climate. Hereupon, the real landscape paintings by Gyunjae(Jeong-Seon), mainly bearing features of existing Korean mountains, wereutilized as visual historical material. However, not having all his works, other pieces with representative characteristics were utilized such as "Gyeong-Gyo-Myeong-Seung-Chup(a painting with picturesque sceneries around old Seoul)" and "Hae-Ak-Jeon-Shin-Chup(a landscape painting including even the spirits of the seas and mountains)" which contain the regions' distinct scenery. As a result, the old cultural scenic landscapes of Korea are regarded as containing diverse mountains and where the conceptions of the treatment of mountains were reflected.

The Landscape Interpretation of Joseon Era Gardens in Old West Village, Seoul through the Locational Investigation (서울 서촌지역 조선조 원림의 위치추적을 통한 경관 해석)

  • Kim, Han-Bai;Lee, Seung-Hee
    • Journal of the Korean Institute of Traditional Landscape Architecture
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    • v.32 no.3
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    • pp.168-182
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    • 2014
  • Several Sungsi Gardens were built up in Old West Village during the period of the Joseon Dynasty. Most of them were painted as True-View landscape painting. This study aims at examining original locations of representative gardens of the Old West Village by empirical investigation of related True-View landscape paintings. It seeks to demonstrate the garden landscape in True-View landscape painting by utilizing ArcGIS, 3D topographic modeling to observe geographical locations and landscape more realistically. After forming 3D topographic modeling of estimated locations of the gardens, location of objects at composition of 3D modeling similar to True-View landscape painting was found by shifting viewpoints. And by overlapping the cadastral map on the modeling, we could verify the current lot number of the garden sites. The interpretation of processes and results are as follows. In the early stage, Chungpunggye garden was built at the very end of Mt. InWang valley. The site is hidden from the outside, and appeared as 'Enclosed Landscape'. In the middle stage, Chunghuigak garden was built between Okryu-dong valley and the surrounding ridge. It appeared as 'Semi-Opened Landscape'. In the late stage, Seowon garden was built at the highest level of the ridge among the research areas. It appeared as 'Prospective Landscape'. In the last period, Songsukwon garden, was built at a point of contact of the ridge end and surrounding residential area. So it appeared as 'Opened Landscape' to the town. In other words, the location, landscape and social function of the gardens in Old West Village had been gradually opened in Joseon Dynasty.

Analysis of GIUH Model by Using GIS in River Basin (하천유역에서 GIS를 이용한 GIUH 모형의 해석)

  • Heo, Chang-Hwan;Lee, Sun-Tak
    • Journal of Korea Water Resources Association
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    • v.35 no.3
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    • pp.321-330
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    • 2002
  • This study aims at the analysis of the geomorphological instantaneous unit hydrograph model (GIS-GIUH) with geographic information system for the rainfall-runoff analysis of watershed which is ungaged or doesn't have sufficient hydrologic data. The rainfall-runoff analysis was performed in Wi stream(Dongkok, Koro, Miseung, Byeungchun, Hyoreung, Museung) which is a representative experimental river basin of IHP. In the process of analysis of the GIUH model, developed GIS-GIUH model and Rosso-GIUH model were applied the study basin and computed hydrographs by these models were compared with observed hydrograph. The GiS-GIUH model shows more closely to the observed hydrograph than Rosso-GIUH model in the peak discharge of the hydrograph. For the development of the GIS-GIUH model, Gamma function factor N was given by N=3.25( $R_{B}$/ $R_{A}$)$^{0.126}$ $R_{L}$$^{-0.055}$, which is the relation of the watershed geomorphological factor, K was also obtained as K=1.50( $R_{A}$/( $R_{B}$. $R_{L}$))/$^{0.10}$.(( $L_{{\Omega}}$+ $L_{{\Omega}-1}$)/V)$^{0.37}$. As the results of analysis, it was found that GIS-GIUH model can be applied to an ungaged watersheds.eds.

2-D Numerical Simulation Considering Channel Topographical Features (하도의 지형특성을 고려한 2차원 수치모의)

  • Song, Seung-Won;Lyu, Si-Wan;Kim, Young-Do;Seo, Il-Won
    • Proceedings of the Korea Water Resources Association Conference
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    • 2009.05a
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    • pp.853-857
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    • 2009
  • 2차원 흐름해석 모형인 SMS(Surface-Water Modeling System)와 RAMS(River Analysis Modeling System)를 이용한 유속장 모의를 통해 Manning 조도계수와 와점성계수에 대한 민감도 분석을 수행하여 흐름특성은 Manning 조도계수에 큰 영향을 받음을 알 수 있었다. 본 연구에서는 Manning 조도계수의 변화를 통하여 실측치에 근사한 유속 분포의 모의결과를 도출하고자 현장실측을 통해 취득한 자료를 이용하여 2차원 수치모형의 모의결과와 비교하였다. 국가하천 형산강 본류 중 안강수위관측소에서 부조수위관측소 사이 약 4.3 km 의 구간을 모의구간으로 선정하였으며, $2006{\sim}2007$년에 걸쳐 취득된 현장실측자료를 바탕으로 매개변수 추정 및 모의결과와 비교하였다. 대상구간에 대한 모의결과의 정확도를 개선하기 위하여 하도의 지형특성 등을 고려하여 모의구간을 다수의 구획으로 구분한 후 수심 및 하도 평면선형을 고려한 Manning 조도계수를 차등적으로 할당하여 모의하였다. 이상의 과정을 통해 모의결과의 정확도 제고가 가능함을 관찰할 수 있었다.

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The Calculation of Reflection Coefficients of Water Waves over Various Shear Currents with a Uniform Depth Topography (다양한 외부흐름에 대한 평탄한 지형을 통과하는 파랑의 반사율 산정)

  • Lee, Jun-Whan;Cho, Yong-Sik
    • Journal of Korea Water Resources Association
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    • v.46 no.3
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    • pp.245-252
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    • 2013
  • The reflection coefficients of monochromatic water waves over various shear currents flowing on a constant topography are estimated analytically in this study. The region of varying shear currents is represented by a finite number of tiny steps with a uniform depth topography. The proper numbers of steps and evanescent modes needed for the analysis are proposed by a series of convergence tests. The characteristics of reflection coefficients for various shear currents conditions are also examined.

The Generation of Accurate Digital Orthophoto by DTM Accuracy Improvement (DTM의 정확도 향상에 의한 정밀 수치정사사진 생성)

  • 박운용;이기부;정성모;이인수
    • Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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    • v.16 no.2
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    • pp.243-250
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    • 1998
  • From early plane-table photogrammetry through the analog and analytical stages, photogrammetry has now reached the digital photogrammetry stage using the image stored at computers. Digital Photogrammetry using aerial photograph generates the DTM and digital orthophoto. Expecially, DTM is important for improving the accuracy of digital ortho photo. so Many experimental are required. In this study, therefore deals with the generation process of digital orthophotos using DTM with breakline and without breakline.

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Numerical Solution of the Mild Slope Equation by Conjugate Gradient Method (CGM을 이용한 완경사방정식의 수치해석)

  • 윤종태
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.5 no.2
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    • pp.84-90
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    • 1993
  • Iterative solution procedure (Conjugate Gradient Method, Panchang et al., 1991) is implemented for solving the complete mild slope equation for the spherical shoal and the coast with detached breakwater. The numerical results agreed well with the experimental data. The disadvantage that mild slope eguation could be solved only for small domains is now overcome by using this solution procedure. Moreover it can be easily applied to the coastal regions with complex geometry and structures, and needs not so much computer time as the conventional models.

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Bragg Reflection of Obliquely Incident Waves (비스듬히 입사하는 파랑의 Bragg반사)

  • Jo, Yong-Sik;An, Yeong-Chang
    • Journal of Korea Water Resources Association
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    • v.35 no.1
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    • pp.91-96
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    • 2002
  • The present research describes the Bragg reflection of obliquely incident waves propagating over sinusoidally varying topographies. A numerical model based on the boundary element method is employed. Wave numbers providing Bragg reflection are calculated and compared to theoretical predictions. The reflection coefficients obtained from this model are also compared with those of the eigenfunction expansion method. A very good agreement is observed.

Numerical Simulation for Shallow-water Flow with Wetting and Drying over Paraboloidal Topography (천수 흐름에 의한 포물면 지형의 잠김과 드러남에 대한 수치모의)

  • Hwang, Seung-Yong
    • Proceedings of the Korea Water Resources Association Conference
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    • 2017.05a
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    • pp.322-322
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    • 2017
  • 천수 흐름에 대한 수치해석에서 매우 작은 수심의 발생은 해가 불안정해지는 주요 원인 중 하나이며, 경사면이 잠기고 드러나는 그 전선에서 그 현상은 더욱 두드러질 수 있다. 특히, 지배 방정식이 보존형으로 기술되는 경우, 흐름률이나 생성항의 계산에서 수심에 의한 나눗셈이 불가피하므로 보존변수를 정확하게 계산하는 것이 해의 안정성을 도모하기 위한 관건이 된다. 이러한 기대에 부응할 수 있는 수치해법으로 흐름률을 정확한 계산할 수 있는 Riemann 해법을 들 수 있다. 또한, 생성항을 정확하게 계산할 수 있도록 계산 격자를 적절하게 구성하고 그 격자가 완전히 잠기지 않을 경우에 대해 물리적으로 타당하게 처리할 필요가 있다. 이 연구에서는 흐름률의 계산에 근사 Riemann 해법을 적용하여 포물면 지형을 지나는 천수 흐름에 대해 모의하였다. 1981년에 W. C. Thacker는 회전 포물면 위의 천수 문제에 대해 천수방정식의 정확해를 처음으로 유도하였다. 이 문제는 지형의 잠김과 드러남이 다수의 계산 격자에서 지속적으로 이루어지기 때문에 천수흐름의 수치 모의에서 극도로 혹독한 조건의 시험으로 알려져 있다. 회전 포물면 위의 천수 문제에 대해 근사 Riemann 해법에 따른 자료의 재구축 방법, 잠김과 드러남의 처리 등에 대해 검토하였다.

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