• KSCE Journal of Civil and Environmental Engineering Research
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• v.26 no.6B
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• pp.597-603
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• 2006

The purpose of this study is to improve the short term rainfall forecast skill using neural network model that can deal with the non-linear behavior between satellite data and ground observation, and minimize the flood damage. To overcome the geographical limitation of Korean peninsula and get the long forecast lead time of 3 to 6 hour, the developed rainfall forecast model took satellite imageries and wide range AWS data. The architecture of neural network model is a multi-layer neural network which consists of one input layer, one hidden layer, and one output layer. Neural network is trained using a momentum back propagation algorithm. Flood was estimated using rainfall forecasts. We developed a dynamic flood inundation model which is associated with 1-dimensional flood routing model. Therefore the model can forecast flood aspect in a protected lowland by levee failure of river. In the case of multiple levee breaks at main stream and tributaries, the developed flood inundation model can estimate flood level in a river and inundation level and area in a protected lowland simultaneously.

• Journal of Korea Water Resources Association
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• v.45 no.5
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• pp.445-454
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• 2012

The present study aims to investigate the long-term channel morphological changes derived from channelization, embankment and levee construction works in unregulated fluvial channel of the Jiseock River. Analyses of aerial photographs taken past (Year 1966) and recent (Year 2002) showed the temporally remarkable changes in channel planform such as channel shape, bar migration, vegetation encroachment in bar. During the period, the natural single threading changed into braided types together with decreasing sinuosity by 9.2%, increasing vegetation occupied bar ranged 97% of total bars area. Because such channel morphological changes are closely similar to those in dam downstream channels, we assume that both/either flow regime alteration and/or sediment transport discontinuity may be critical for the fixed channel and spread of vegetated bars even in unregulated river without dam reservoir upstream. We found more reduced frequency and magnitude of flooding water level comparing with past, but no significant alteration of inter annual water level variation. Bed material has been coarsened by 4~5 times and the riverbed has been degraded in overall channel but aggraded locally in conjunction reach of tributaries. The results indicates that reduced sediment dynamics in fluvial channel which derived by bed material coarsening, river bed degradation and unbalanced sediment transport capacity between tributary and mainstem can be a causal factor to trigger channel morphological changes even in unregulated rivers.

• 한국방재학회:학술대회논문집
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• 2008.02a
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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.

• Ecology and Resilient Infrastructure
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• v.5 no.4
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• pp.199-209
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• 2018

In river design, consideration of bed shear stresses is necessary to secure stability of levee and floodplain. In this study distributions of bed shear stresses in compound open channels are analyzed through numerical simulation for various width and depth. LES solver in OpenFOAM is applied to 12 cases of compound channel shapes considering secondary flow which effects distributions of bed shear stresses. By the results time averaged velocity distributions, secondary currents, and distributions of bed shear stresses are analyzed. Overall distributions of bed shears in floodplain show that higher shear stresses are seen in left of floodplain and the shears decrease toward right of floodplain. However, high local variations in shear stresses are shown due to the secondary flow effects. In shallow floodplain, bed shear stresses show low value below 0.8 times of averaged bed shear. In deep floodplain, bed shear stresses show high value over 1.2 - 1.4 times of averaged bed shear.

• Journal of the Korean association of regional geographers
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• v.3 no.2
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• pp.37-87
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• 1997

As a results of researches on the cultivation processes and settlement developments on the Mangyoung river valley as a whole could be have four 'Space-Time Continuity' through a [Origin-Destination] theory model. On a initial phases of cultivation, the cultivation process has been begun at mountain slopes and tributory plains in upper part of river-basin from Koryo Dynasty to early Chosun Dynasty. At first, indigenous peasants burned forests on the mountain slopes for making 'dryfield' for a cereal crops. Following population increase more stable food supply is necessary facets of life inducing a change production method into a 'wetfield' in tributory plains matching the population increase. First sedentary agriculture maybe initiated at this mountain slopes and tributory plains on upper part of river basin through a burning cultivation methods. Mountain slopes and tributory plains are become a Origin area in cultivation processes. It expanded from up to down through the valleys with 'a bits of land' fashion in a steady pace like a terraced fields expanded with bit by bit of land to downward. They expanded their land to the middle part of river basin in mid period of Chosun Dynasty with dike construction techniques on the river bank. Lower part of river cultivated with embankment building techniques in 1920s and then naturally expanded to the tidal marshes on the estuaries and river inlets of coastal areas. 'Pioneer fringes' are consolidated at there in modern times. Changes in landscapes are appeared it's own characters with each periods of time. Followings are results of study through the Mangyoung river valley as a whole. (1) Mountain slopes and tributory plains on the upper part of river are cultivated 'dryfields' by indigenous peasants with Burning cultivation methods at first and developed sedentary settlements at the edges of mountain slopes and on the river terrace near the fields. They formed a kind of 'periphery-located cluster type' of settlement. This type of settlement are become a prominant type in upper part of river basin. 'Dryfields' has been changed into a 'wetfields' at the narrow tributory plains by increasing population pressure in later time. These wetfields are supplied water by Weir and Ponds Irrigation System(제언수리방법). Streams on the tributory plains has been attracted wetfields besides of it and formed a [water+land] complex on it. 'Wetfields' are expanded from up to downward with a terraced land pattern(adder like pattern, 붕전) according to the gradient of valley. These periphery located settlements are formed a intimate ecological linkage with several sets of surroundings. Inner villages are expanded to Outer villages according to the expansion of arable lands into downward. (2) Mountain slopes and tributory plains expanded its territory to the alluvial deposited plains on the middle part of river valley with a urgent need of new land by population increase. This part of alluvial plains are cultivated mainly in mid period of Chosun Dynasty. Irrigation methods are changed into a Dike Construction Irrigation method(천방수리방법) for the control of floods. It has a trend to change the subjectives of cultivation from community-oriented one who constructed Bochang along tributories making rice paddies to local government authorities who could be gather large sums of capitals, techniques and labours for the big dike construction affairs. Settlements are advanced in the midst of plains avoiding friction of distances and formed a 'Centrallocated cluster type' of settlements. There occured a hierarchical structures of settlements in ranks and sizes according merits of water supply and transportation convenience at the broad plains. Big towns are developed at there. It strengthened a more prominant [water+land] complex along the canals. Ecological linkages between settlements and surroundings are shaded out into a tiny one in this area. (3) It is very necessary to get a modern technology of flood control at the rivers that have a large volume of water and broad width. The alluvial plains are remained in a wilderness phase until a technical level reached a large artificial levee construction ability that could protect the arable land from flood. Until that time on most of alluvial land at the lower part of river are remained a wilderness of overgrown with reeds in lacks of techniques to build a large-scale artificial levee along the riverbank. Cultivation processes are progressed in a large scale one by Japanese agricultural companies with [River Rennovation Project] of central government in 1920s. Large scale artificial levees are constructed along the riverbank. Subjectives of cultivation are changed from Korean peasants to Japanese agricultural companies and Korean peasants fell down as a tenant in a colonial situation of that time in Korea. They could not have any voices in planning of spatial structure and decreased their role in planning. Newly cultivated lands are reflected company's intensions, objectives and perspectives for achieving their goals for the sake of colonial power. Newly cultivated lands are planned into a regular Rectangular Block settings of rice paddies and implanted a large scale Bureaucratic-oriented Irrigation System on the cultivated plains. Every settlements are located in the midst of rice paddies with a Central located Cluster type of settlements. [water+land] complex along the canal system are more strengthened. Cultivated space has a characters of [I-IT] landscapes. (4) Artificial levees are connected into a coastal emnankment for a reclamation of broad tidal marshes on the estuaries and inlets of rivers in the colonial times. Subjectives of reclamation are enlarged into a big agricultural companies that could be acted a role as a big cultivator. After that time on most of reclamation project of tidal marshes are controlled by these agricultural companies formed by mostly Japanese capitalists. Reclaimed lands on the estuaries and river inlets are under hands of agricultural companies and all the spatial structures are formed by their intensions, objectives and perspectives. They constructed a Unit Farming Area for the sake of companies. Spatial structures are planned in a regular one with broad arable land for the rice production of rectangular blocks, regular canal systems and tank reservoir for the irrigation water supply into reclaimed lands. There developed a 'Central-located linear type' of settlements in midst of reclaimed land. These settlements are settled in a detail program upon this newly reclaimed land at once with a master plan and they have planned patterns in their distribution, building materials, location, and form. Ecological linkage between Newly settled settlemrnts and its surroundings are lost its colours and became a more artificial one by human-centred environment. [I-IT] landscapes are become more prominant. This region is a destination area of [Origin-Destination] theory model and formed a 'Pioneer Fringe'. It is a kind of pioneer front that could advance or retreat discontinously by physical conditions and socio-cultural conditions of that region.

• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.1246-1250
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• 2006

국내에 있어 하천피해지역 등의 피해조사를 위하여 주로 인적자원을 동원하여 조사자들이 개략적인 측량을 통해 피해규모를 산정하는 방식이 활용되고 있다. 그러나 하천피해지역 등과 같이 수적으로 대부분을 차지하는 국지피해지역을 주로 인적자원을 동원하여 피해규모를 산정하는 것은 한계가 있는 것으로 여겨진다. 따라서 실용적 측면에서 하천제방을 중심으로 한 디지털 스테레오 영상을 이용하여 피해범위를 산정하고, 피해액 산정 프로그램을 개발하여 적용하므로써 피해하천제방의 피해액 산정의 적용성을 검토하였다. 디지털 영상취득을 위하여 피해영상 촬영장비를 개발하였으며 피해영상을 통하여 얻어진 피해정보와 실제 측량을 통한 성과의 차이가 $0.12{\sim}0.34m$로 나타나 평균 0.24m의 차이를 나타내었다. 따라서 피해영상 촬영시스템을 통하여 얻어진 성과는 실무적 측면에서 상당히 유효한 결과로 여겨진다. 또한, 피해정보를 입력하여 피해액을 자동으로 산정하는 프로그램을 개발하였다. 본 연구 결과는 실제 피해현장에서 활용도가 매우 높을 것으로 판단되며 차후 지속적인 연구를 통하여 통합처리시스템이 구축될 경우 재해예방에 있어 보다 효율적이고 능동적인 시스템으로 자리 잡게 될 것으로 여겨진다.

• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.1835-1839
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• 2006

최근 빈번히 발생하는 국지성 집중호우 등의 기상이변과 도시화로 인한 불투수 면적의 증가는 급격한 유출량의 변화를 가져와 홍수로 인한 피해를 가중시킬 수 있다. 따라서 홍수방어시설인 제방의 경우 발생가능성은 낮지만 확률홍수량에 따른 제방 여유고의 평가도 필요하다. 본 연구에서는 대표적 도시하천인 탄천을 대상으로 하천정비기본계획(2000)에 수립된 계획홍수량과 최근 7년간 실측한 관측 결과로 계산한 확률홍수량을 조건으로 각각의 경우에 따른 한강 합류부(하류단)부터 상류 9 Km까지의 제방 여유고를 국내와 국외의 설계기준으로 비교, 검토하였다. 검토조건으로는 계획홍수량에 대해서는 3가지 경우의 하류단 수위를 경계조건으로 설정하였고 확률홍수량(80년, 100년, 200년 빈도)에 대해서는 각각의 경우에 발생 가능한 하류단 수위를 경계조건으로 설정하였다. 검토결과 탄천의 경우 계획홍수량에 대해서는 대체로 안전측으로 나타났지만 계획빈도 이상의 확률홍수량에 대해서는 국내, 일본의 설계기준에 제시된 여유고보다 상류 일부구간에서 여유고가 부족한 경향을 보이는 것으로 나타났다. 제방 여유고를 미국(도시하천의 경우 최소 0.91 m)의 경우와 비교하여도 안전측에 속한다고 평가할 수 있다. 하지만 본 검토의 대상인 제방이외의 일부 수공구조물(교량등)에서 여유고가 일부 부족한 것도 확인할 수 있었다. 이에 새로이 하천정비를 실시할 탄천(2006년 예정)의 경우 이러한 부분에 대한 검토 및 보완이 필요할 것으로 사료된다.

• Journal of The Korean Society of Agricultural Engineers
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• v.47 no.2
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• pp.15-21
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• 2005

This study is to trace the change of stream shape using the past series of aerial photographs, and to compare the land use changes of riparian area along the stream. For the Gyeongan national stream, aerial photographs of 1966, 1981 and 2000 were selected and ortho-photographs were made with interior orientation and exterior orientation, respectively. Apparent changes of the stream were found that the consolidated reaches of stream by levee construction became straight together with widening of their stream widths. Especially the stream width of inlet part of Paldang lake widened almost twice because of the rise of water level by dam construction in 1974. The land use of riparian areas of three selected years were classified into six categories (water, forest, agricultural land, urban area, road, sandbar) by digitizing method. The forest and agricultural lands decreased and urban area increased as the stream maintenance had been performed.

• 한국방재학회:학술대회논문집
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• 2011.02a
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• pp.43-43
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• 2011

본 연구에서는 한강제방 취약구간인 성산대교와 잠실철교 부근 지역에 대한 홍수범람을 수치모의 하였다. 사용된 수치모형은 스위스의 Beffa에 의해 개발된 FLUMEN(FLUvial Modeling ENgine)으로서 스위스, 독일, 오스트리아 등에서 홍수범람해석에 사용된 바 있는 모형이다. 제방 취약지역은 한강 하천정비기본계획(2002)과 대학과 연계한 하천관리에 관한 연구용역(2단계 4차년)에 제시된 HEC-RAS 부등류 해석에 의해 계산된 홍수위와 기존 제방의 높이를 비교하여 산정하였다. 범람모의를 위해 HEC-RAS 부정류 해석을 통해 경계조건을 산정하고, FLUMEN을 이용하여 한강제방의 취약지역에 대한 범람모의와 파제 시나리오를 작성하여 파제에 따른 범람모의를 실시하고 적용성을 검토하였다. 제방 취약지역에서 월류로 인한 범람이 발생하였고, 이로 인해 일부 주거지역이 침수되었다. 가상 파제시나리오를 통한 수치모의 결과에서 여의도에서 $2.179km^2$의 넓은 지역에 침수현상이 계산되었으며, 최대 침수심은 5.054m로 성산대교 남단의 가상 파제 시나리오에서 계산되었다. 수치모의 결과 FLUMEN은 한강유역의 범람모의에 적합하다고 판단되며, 본 연구는 홍수 방어대책을 수립함에 있어 홍수 취약지역의 선정과 수공구조물의 설치 방향을 결정하는데 기초자료로 활용이 기대 된다. 정확도를 높이려면 보다 정밀한 제내지, 제외지의 측량자료의 적용, 내수 침수모형과의 연계, 조밀한 불규칙 삼각망의 작성이 필요하며, 국내실정에 맞는 정확한 적용기준마련과 유역의 수리학적 특성이 고려된 홍수해석 모형의 개발이 필요하고 보다 정확한 조도계수의 산정을 위한 지속적인 연구가 필요하다.

• Journal of Korean Society on Water Environment
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• v.22 no.4
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• pp.605-613
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• 2006

Discharge characteristics of non-point source pollutant and load amount of the discharge in the urban area were investigated in the Pungyeongjeong-stream basin and the Yongbong-stream basin in this present study. The land use of the studied basins were divided into paddy field, industrial complex area, combined sewage system, separate sewer system and point sources discharge. The descriptive statistics on the event mean concentrations (EMCs) of non-point pollutants by the the land use showed in the range of 4.43-32.28 mg/L for BOD and 8.27~56.17 mg/L for COD. The highest concentration was shown from the combined sewage system. The EMC of SS at the paddy field in the Pungyeongjeong-stream basin showed the highest range with the values ~ from 35.76 to 358.86 mg/L, which might have been influenced by a levee construction in the adjacent of the area. The relatively high concentration values of 4.43~32.28 mg/L and 1.617.13 mg/L emerged from TN and TP,respectively, at the discharge points of the both stream basins.