• Korean Journal of Ecology and Environment
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• 제49권2호
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• pp.124-129
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• 2016

This study was conducted to suggest the cause analysis and mitigation measures of foaming generated in the effluent of wastewater treatment plant. The foam generated in the outlet connected with the tidal river system was identified as structural problems. And the main cause of foaming was air entrainment by an impinging jet and the internal accumulation by the diffusion barrier. In consideration of these conditions, it present the effective ways such as micro-screen and submerged outlet, to mitigate the foaming generated in the water channel and outlet end.

• Proceedings of the Korea Water Resources Association Conference
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• 한국수자원학회 2012년도 학술발표회
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• pp.686-686
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• 2012

일반적으로 첨두 홍수량 경감을 위하여 유역종합치수계획 등에서 많이 계획되고 있는 방수로는 방수로 종단에서의 방류 방식에 따라 크게 자기 완결 방식과 타 하천 또는 해양 방류 방식으로 구분할 수 있다. 일반적으로 타 하천 또는 해양 방류 방식을 방수로라 부르며, 홍수 방어의 대상이 되는 지역을 우회하여 다시 본천으로 합류하는 자기 완결 방식으로 계획되는 방수로 즉 홍수 방어용 수로를 분수로라 부른다. 방수로를 계획하는 경우 가장 중요한 것은 본류에서의 첨두 홍수량 분담이기 때문에 방수로로 유입되는 분류량을 정확히 예측하는 것이 매우 중요하다. 하지만 분수로의 경우 다시 본천으로 재합류하기 때문에 재합류되는 지역에서 본류의 유량이 다시 크게 증가하고, 합류점 상류에서 예상치 못한 홍수위의 상승이 발생할 가능성이 있다. 따라서 만약 합류부에서 유황에 대한 적절한 검토 없이 합류 지역을 설계하는 경우 예상치 못한 수위 상승 및 국부 유속 증가에 의한 홍수 피해가 발생할 가능성이 있다. 따라서 본 연구에서는 분수로 형태의 방수로가 일정한 합류각을 가지고 본류로 합류하는 경우 본류에서의 유황 변화 및 수위 상승이 어떠한 형태로 나타나는지 실험을 통하여 검토하고자 하였다. 합류하는 분수로의 폭은 본수로의 폭이 에 대하여 0.50B, 0.75B, 1.00B가 되도록 하였으며, 합류각은 본류와 분수로 사이의 예각이 75도가 되도록 하였다. 이러한 수로 제원에 대하여 본류 유량 및 유입량을 다양하게 변화시켜 합류부에서의 수위 변화를 검토하였다.

• Journal of Korea Water Resources Association
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• 제35권6호
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• pp.715-727
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• 2002

The travel time of a flood through a river reach can be estimated by dividing the river length by the mean velocity with which the flood passes downstream. It is closely related to storage constant for the watershed routing of a flood. There are so many empirical formulas available for the estimation of travel time but the results computed generally show great different depending on individual formulas. In the present study, the mean velocity data computed in the process of water surface profile computation for a probability flood through more than 100 different river reaches were collected along with the mean river bed slope of each river reach. And then, a regression analysis is made between the mean river bed slope and the mean velocity, which showed a wide scatter along the mean regression curve, which appears to be due to the different in the magnitude of probability rainfall and size of watershed area. Therefore, methods have been developed to remove the effect of these factors and generalized empirical equation is proposed to relate the mean velocity to mean river bed slope of a reach. Hence, if the mean river bed slope of a river reach is estimated from the longitudinal river profile, the mean velocity can be computed by the generalized equation along with the probability rainfall and watershed area of the river reach under consideration, which leads to the estimation of travel time through a river reach.

• Journal of Korea Water Resources Association
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• 제53권1호
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• pp.29-43
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• 2020

The purpose of this study is to propose the design criteria and detailed design model by reviewing the issues related to geometry, formation process, destruction process, hydraulic function, restoration and ecological function of the step-pool from the existing research results, to apply the step-pool sequences to river restoration. Based on the analysis and review results, the design criteria for the structure and size of the step-pool are presented as ratio of the step spacing and the channel width, ratio of the unit step slope and channel slope, and ratio of step height and the particle size. To ensure structural stability of the step, stability analysis method of overturning based on the keystone theory was proposed as a design criterion. As a detailed design concept, a layout model was proposed by applying the imbricating structure of keystones and arch stones to the planar, longitudinal and transverse configurations of the step-pool.

• Journal of Korea Water Resources Association
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• 제42권5호
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• pp.425-432
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• 2009

Gongneung Weir 2 was built in 1970s to supply water for irrigation. For a long time, the weir was left uncared because of the land use change of the nearby area. The weir is 1.5 m high, and the stream in which the weir was installed has bed materials of fine sands to fine gravels. In 2006, the local government and residents agreed on uninstalling the weir, and the weir was removed completely on April 14. This paper reports the results of three field investigations for the study of the stream morphology change after the weir removal. Changes in grain size distribution, bed elevation, and cross section before and after the weir removal are provided and discussed. Net amount of sediment deposits within 1 km reach of the stream is estimated, and the results illustrates that the sediment process, leading to an equilibrium of the bed, progressed very swiftly, namely within 45 days.

• Journal of the Korean Geophysical Society
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• 제6권4호
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• pp.269-276
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• 2003

Sub-bottom profile were conducted in Chungju Regulation Lake by use of ground penetrating radar(GPR). The survey area covers approximately 1,000,000 $m^2$ and total survey line length is about 5km and more. GPR surveys with GPS system were made across and transverse direction of the lake. From the survey results of GPR, it could be possible to distinguish the gravel and/or sand dominant bed from silt and/or clay material dominant bed.

• Proceedings of the Korea Water Resources Association Conference
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• 한국수자원학회 2017년도 학술발표회
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• pp.294-294
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• 2017

본 연구에서는 입력 매개변수의 변화에 따른 하천의 수리특성의 변화를 분석하기 위하여 2차원 수리해석 모형의 입력변수들에 대하여 초기 입력값의 15%~ +15% 범위로 변화시켜 해석하였다. 하도내 구조물 주변의 2차원 부정류 해석으로 각각의 매개변수의 입력값에 따라 나타나는 해석결과 최댓값들의 영향을 검토하여 하도내 2차원 분석결과에서 각각의 매개변수의 민감도를 파악하였다. 2차원 수리해석 입력자료의 민감도 분석을 위하여 수온, 밀도, 난류교환계수, 조도계수, MP(Marsh Porosity)에 대한 초기치를 기준으로 $0%{\sim}{\pm}15%$ 변화된 값을 각각 입력하여 하도내 합류부와 구조물 주변에 나타나는 2차원 수리특성 변화를 분석하고 하도구간의 종단 및 횡단에 대해서 각각 매개변수들의 결과 값에 따라 변화되는 특성을 분석하였다.

• Journal of Korea Water Resources Association
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• 제44권10호
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• pp.797-807
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• 2011

Phenomenon of vegetation recruitment on the sand bar is drastically rising in the streams and rivers in Korea. In the 1960s prior to industrialization and urbanization, most of the streams were consisted of sands and gravels, what we call, 'White River'. Owing to dam construction, stream maintenance, etc. carried out since the '70s, the characteristic of flow duration and sediment transport have been disturbed resulting in the abundance of vegetation in the waterfront, that is, 'Green River' is under progress. This study purposed to identify the correlation among water level, water temperature, rainfall, soil moisture and soil texture out of the factors which give an effect on the vegetation recruitment on the sand bar of unregulated stream. To this purpose, this study selected the downstream of Naeseong Stream, one of sand rivers in Korea, as the river section for test and conducted the monitoring and analysis for 289 days. In addition, this study analyzed the aerial photos taken from 1970 to 2009 in order to identify the aged change in vegetation from the past to the present. The range of the tested river section was 361 m in transverse length and about 2 km in longitudinal length. According to the survey analysis, the tested river section in Naeseong Stream was a gaining river showing the higher underground-water level by 20~30 m compared to Stream water level. The difference in the underground water temperature was less than $5^{\circ}C$ by day and season and the Stream temperature did not fall to $10^{\circ}C$ and less from May when the vegetation germination begins in earnest. The impact factor on soil moisture was the underground water level in the lower layer and the rainfall in the upper layer and it was found that all the upper and lower layer were influenced by soil particle size. The soil from surface to 1 m-underground out of 6 soil moisture-measured points was sand with the $D_{50}$ size of 0.07~1.37 mm and it's assumed that the capillary height possible in the particle size would reach around 14~43 cm. On the other hand, according to the result of space analysis on the tested river section of unregulated stream for 40 years, it was found that the artificial disturbance and drought promoted the vegetation recruitment and the flooding resulted in the frequency extinction of vegetation communities. Even though the small and large scales of recruitment and extinction in vegetation have been repeated since 1970, the present vegetation area increased clearly compared to the past. It's found that the vegetation area is gradually increasing over time.

• Journal of The Geomorphological Association of Korea
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• 제18권4호
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• pp.203-212
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• 2011

The objective of this paper is to identify the present-day surficial sediment distribution patterns of the tidal river, Gongneungcheon, through the grain size and statistical analysis. Four major findings of this study are as follows; First, the composition of sediments over the study area are mainly silt in texture. Second, the surficial sediment distribution reveals that grain size becomes coarser as they approach seawards not only in summer but also in winter. It can be concluded that tidal flows play a significant role, especially in winter, in the distribution of surficial sediments in Gongneungcheon. However, samples obtained in summer were relatively small in mean size and showed better sorting compared to those obtained in winter. Third, the mean sizes of the samples on the transects decrease as the distance from the channel increases. Finally, the artificial structure such as a floodgate affects the distribution of the sediments.

• Journal of Korean Society of Forest Science
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• 제96권6호
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• pp.611-619
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• 2007

This study was carried out to analyze the landslide characteristics and forest environment factors on the landslide area of 7 national parks in korea. The results obtained from this study were summarized as follows; The total number of landslide occurrence was 44 areas. The average length of the landslides scar was 152 m, average width was 17 m. And the average area was $2,818m^2$. The factors influencing landslides were highly occurred in Metamorphic rock, mixed forest type. And also, $30{\sim}35^{\circ}$ in slope gradient, NE in slope aspect, slope higher than 1,000 m, concave (凹) type in vertical and cross slope, 0 ordered stream. The main factors affecting landslide area in stepwise regression analysis were sheet type in landslided shape, NE in slope aspect, 2 ordered stream, SE in slope aspect, slope gradient and complex slope in cross slope type in order of regression coefficient.