• Proceedings of the Korea Water Resources Association Conference
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• 2006.05a
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• pp.1621-1625
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• 2006

하천은 여러 하천의 연결망으로 구성되어 있으며, 연결부는 절점으로 이루어져 있고, 이 절점은 하천이 합류하는 곳으로서 하천의 시스템을 구성하는 가장 중요한 요소이다. 최근에 친자연 하천 복원 등의 많은 사업을 하고 있음에도 불구하고 이에 대한 검토가 거의 이루어지지 않고 있으며, 이를 검토하고 이해하는 것이 하천을 복원하고 관리하는데 매우 중요하다. 본 연구는 본류와 지류의 하상경사 및 하상고가 다르고, 유사 유입조건이 다른 비평형 유입조건을 갖고 있으며, 하폭이 넓고 수심이 상대적으로 얕은 합류부에서 흐름 및 하상변동에 관하여 수치모의를 수행하여 그 특성을 파악하는데 그 목적이 있다. 적용 대상지역은 금강과 미호천의 합류부로서, 흐름 특성 및 하상변동을 모의하기 위하여 RMA-2와 SED2D를 이용하였다. 유량의 증가에 따라 흐름에 대한 유속이 증가하며, 전단층의 길이가 증가하고, 합류부의 우안의 정체수역에서 발생하는 와(vortex)의 크기도 증가하였다. 부유사의 농도는 실제 상황에 맞도록 비평형 유입조건을 사용하였으며, 미호천에서 유입되는 유사의 농도에 영향을 받아, 합류직후에도 유사의 농도가 높으며, 전단층을 경계로 하여 농도 띠가 하류로 유지되었으며, 합류 후에는 우안에서는 하상이 상승되었다.

• Proceedings of the Korea Water Resources Association Conference
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• 2015.05a
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• pp.110-110
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• 2015

하천 복원을 위해서는 자연 상태에서의 복원 대상 하천의 거동에 대한 지형학적 정보가 필요하다. 하지만, 국내 하천은 대부분 개수되어 있고, 참조하천으로 활용할만한 하천 역시 찾기가 어려운 실정이다. 이에 대상 하천의 과거 자연 상태에서의 자료와 현재 자료를 병용함으로써 지형학적 분석에 필요한 정보를 얻는 방법을 제시하였으며, 미호천과 내성천을 대상으로 분석을 실시하였다. 분석은 강턱하폭, 강턱유량과 하도 패턴(channel pattern), 그리고 하천의 유형과 관계된 지배적인 프로세스에 초점을 맞추었다. 분석 결과 강턱하폭은 강턱유량에 비례하여 증가하였으며, 그 경향성은 기존의 연구 결과와 대체로 일치하였다. 강턱유량과 하도경사간의 관계를 분석한 결과 미호천은 사행하천과 망상하천의 특성을 나타내는 반면, 내성천은 대부분의 구간에서 망상하천 특성을 보이는 것으로 나타났다. 하도경사와 하폭수심비 관계를 이용하여 지배적인 프로세스를 분석한 결과 미호천은 사구-연흔의 특성을 나타내고 있으나 내성천은 하류에서는 망상하천 특성이 지배적인 반면, 상류에서는 여울-소 내지는 평하상 특성이 지배적인 것으로 나타났다. 현재와 자연상태로 판단되는 과거 시점의 자료를 병용하여 분석한 결과들은 정비된 하천의 자료를 이용한 분석 결과에 비해 합리적인 것으로 나타났다.

• Journal of the Korean GEO-environmental Society
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• v.9 no.7
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• pp.5-11
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• 2008

The paper presents the results of qualitative analysis of phthalate esteres in Miho stream in of Cheongju city. Phthalate esters (Di-2-ethylhexylphthalate, Di-n-butylphthalate) are widely used as plasticizers to increase the flexibility and workability of high-molecular-weight polymer. For water phase, DEHP concentration in upper stream and down stream were $12-18{\mu}g/{\ell}$ and $11-21{\mu}g/{\ell}$, respectively. For sediment phase, DEHP concentration in upper stream and down stream were $0.07-0.82{\mu}g/g$ (dry) and $0.06-0.92{\mu}g/g$ (dry), respectively. Also, DnBP concentration of sediment in same site were $0.04-0.25{\mu}g/g$ (dry) and $0.08-0.34{\mu}g/g$ (dry), respectively. DEHP and DnBP concentration of water phase in the small stream of industrial area were $13-28{\mu}g/{\ell}$ and $2-8{\mu}g/{\ell}$, respectively. DEHP and DnBP concentration of sediment phase in the small stream of industrial area were $0.12-0.7{\mu}g/g$ (dry) and $0.17-2.16{\mu}g/g$ (dry), respectively. Phthatlate esteres in water and sediments phase of Miho stream were lower than water bodies around the world.

• Journal of Environmental Impact Assessment
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• v.28 no.4
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• pp.373-386
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• 2019

In The study, is to investigate the spatial characteristics of the Miho stream, which is the main tributary of the Geum River system, and to identify the main factors influencing the water quality using water quality analysis and multivariate analysis. The survey subjects were selected as 7 main sites in the Miho stream water system, From 2012 to 2017, 16 items including weather temperature and weather data were used for multivariate analysis. As a result of the water quality analysis, the average concentration of BOD and COD for 6 years was 3grade (normal) compared with the water quality environmental standard (river) of conditions. The concentrations of nitrogen and phosphorus were highest at th upstream site, then decreased and then increased again by the hydrogeological and geomorphological effect. Cluster analysis of spatial and water quality characteristics, it was evaluated as three clusters and the pollution sources is the greatest impact. As a result of principal component analysis and factor analysis on each cluster and mainstream, three to four major components were extracted. Main stream and the Cluster 1, Cluster 3 first principal factor included nitrogen and seasonal factors,first factor of Cluster 2 included nitrogen and water temperature. Nitrogen is the principal factor which affects water quality in Miho stream.

• Ecology and Resilient Infrastructure
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• v.8 no.1
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• pp.9-21
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• 2021

In this study, fish and flow surveys were conducted at 12 survey points to calculate the fish habitat suitability index of Miho Stream in the Geum River Water System. The field surveys were conducted four times from September 2019 to May 2020. The results show the presence of 8 families, 37 species, and 5,754 individuals. The number of water purification species that preferred waters with a low flow rate was the highest. The habitat suitability index was calculated according to the Washington Department of Fish and Wildlife method based on the populations collected at various water depths and flow rate sections and the flow rate survey results. For the dominant species, Zacco platypus and swimming species, the results were compared by calculating at Gasan Bridge and Palgye Bridge at the upper stream. The single species showed no significant difference between the upstream and downstream at water depths of 0.1 - 0.5 m and flow rates of 0.2 - 0.5 m/s. The species swimming ability was similarly calculated at water depths of 0.2 - 0.5 m and flow rates of 0.2 - 0.5 m/s. The dominant species, Pyramid, had a wide range of physical habitats. The habitat suitability index between the swimming species was similarly calculated. These results can be effectively used as basic data for calculating the environmental ecological flow rate and establishing a river restoration plan of the Miho Stream.

• Journal of Korea Water Resources Association
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• v.55 no.7
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• pp.481-494
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• 2022

This study proposed a evaluation of the monthly vulnerable period for groundwater level management in the Miho stream watershed and a technique for evaluating the vulnerable period for future groundwater level management using LSTM. Observation data from groundwater level and precipitation observation stations in the Miho stream watershed were collected, LSTM was constructed, predicted values for precipitation and groundwater levels from 2020 to 2022 were calculated, and future groundwater management was evaluated when vulnerable. In order to evaluate the vulnerable period of groundwater level management, the correlation between groundwater level and precipitation was considered, and weights were calculated to consider changes caused by climate change. As a result of the evaluation, the Miho stream watershed showed high vulnerability to underground water management in February, March, and June, and especially near the Cheonan Susin observation well, the vulnerability index for groundwater level management is expected to deteriorate in the future. The results of this study are expected to contribute to the evaluation of the vulnerable period of groundwater level management and the derivation of preemptive countermeasures to the problem of groundwater resources in the basin by presenting future prediction techniques using LSTM.

• KCID journal
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• v.3 no.1
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• pp.113-127
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• 1996

• Magazine of the Korean Society of Agricultural Engineers
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• v.60 no.2
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• pp.27-34
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• 2018

• Proceedings of the Korea Water Resources Association Conference
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• 2003.05b
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• pp.863-866
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• 2003

• Proceedings of the Korea Water Resources Association Conference
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• 2000.05a
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• pp.173-178
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• 2000