• Journal of Environmental Science International
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• v.17 no.11
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• pp.1211-1220
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• 2008

In this study, we estimated, the equivalent roughness using an estimation model, which considered grain distribution on the bed and the protrusion height of the grains. We also reviewed the appropriateness of the estimated equivalent roughness at the Goksung and Gurey station in the Seomjin River. To review the appropriateness of this model, we presented the water level-discharge relation curve applying the equivalent roughness to the flow model and compared and reviewed it to observed data. Also, we compared and reviewed the observed data by estimating the Manning coefficient n, the Chezy coefficient C, and the Darcy-Weisbach friction coefficient f by the equivalent roughness. The calculation results of the RMSE showed within 5% error range in comparison with observed value. Therefore the estimated equivalent roughness values by the model could be proved appropriate.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.43 no.6
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• pp.749-762
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• 2023

A depth-integrated model with an approximate Riemann solver for flux computation of the shallow water equations was applied to hydraulic jump experiments. Due to the hydraulic jump, different flow regimes occur simultaneously in a single channel. Therefore, the Weisbach resistance coefficient, which reflects flow conditions rather than the Manning roughness coefficient that is independent of depth or flow, has been employed for flow resistance. Simulation results were in good agreement with experimental results, and it was confirmed that Manning coefficients converted from Weisbach coefficients were appropriately set in the supercritical and subcritical flow reaches, respectively. Limitations of the shallow water equations that rely on hydrostatic assumptions have been revealed in comparison with hydraulic jump experiments, highlighting the need for the introduction of a non-hydrostatic shallow-water flow model.

• Journal of Korean Society of Disaster and Security
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• v.14 no.4
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• pp.37-45
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• 2021

Flooding damage may occur due to an unexpected increase in rainfall in summer. Previously, the roughness coefficient, which is a major factor of conveyance, was calculated through on-site measurement, but in case of on-site measurement, there are many limits in accurately grasping changes in vegetation. In this study, the vegetation index (NDVI) was calculated using the Sentinel-2 optical images, and the modified roughness coefficient was calculated through the density and distribution area of the vegetation. Then the calculated roughness coefficient was applied to HEC-RAS 1D model and verified by comparing the results with the water level at the water level station directly downstream of the Soyang River dam. As a result, the error rate of the water level decreased about 14% compared to applying the previous roughness coefficient. Through this, it is expected that it will be possible to refine the flood level of rivers in consideration of seasonal flood characteristics and to efficiently maintain rivers in specific sections.

• Journal of the Korean Society of Safety
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• v.33 no.2
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• pp.132-137
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• 2018

Compared with general rivers, fluctuations of the water level and the river bed are severe in the tidal river. In hydro-dynamic aspect, such fluctuation gives different river-bed data to us according to observing period. The time-dependent river-bed data and pre-estimation of the Manning's roughness coefficient which is the key factor of numerical modelling induces uncertainty of evaluating the design flood level. Thus it is necessary to pay more attention to calculate the flood level at tidal rivers than at general rivers. In this study, downstream of the Imjin River where is affected by tide of the West Sea selected as a study site. From the numerical modelling, it was shown that the unsteady simulation gave considerable mitigation of the water level from the starting point to 15 km upstream compared to the steady simulation. Either making a detention pond or optional dredging was not effective to mitigate the flood level at Gugok - Majung region where is located in the downstream of the Imjin River. Therefore, a more sophisticated approach is required to evaluate the design flood level estimation before constructive measures adopted in general rivers when establishing the flood control plan in a tidal river.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.32 no.6B
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• pp.345-354
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• 2012

The main objective of this study is evaluating experimentally roughness coefficients of the Korean riparian vegetations based on the n-VR analysis to suggest the practical guideline for Manning's roughness coefficients for the channel design. Hydraulic experiments were conducted for Phragmites japonica Steud., Miscanthus sacchariflorus (Maxim.) Benth., and Phragmites communis Trin. under both submerged and un-submerged conditions, and the n-VR relationships are developed for each grass. Three vegetations tested in this study can be considered as same group showing similar roughness characteristics, though these grasses are strongly affected by vegetation stiffness. Vegetation roughness are also affected by the growth state of plants according to experimental results of Phragmites communis Trin.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.1654-1658
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• 2008

하천에서는 최적 하도계획의 수립과 하천관리를 위하여 유량관측소가 설치 운영되고 있으며, 통상 자기기록계에 의해 수위를 계속적으로 기록하고 있다. 또한 하천의 흐름 해석시 부등류 및 부정류 해석을 통하여 수위를 계산하게 되는데 이때 조도계수는 매우 중요한 매개변수이다. 이러한 조도계수는 대상하도의 복합적 요소에 의하여 결정되어지며 특히 유량에 대한 가변성이 크다. 본 연구에서는 도시하천인 우이천 유역을 대상으로 과거 수위 및 유량관측 자료를 토대로 유속 및 경심을 산정한 후 Manning의 평균유속 공식에 의해 역산하여 조도계수를 산정하였다. 또한 고정조도계수모형과 멱함수형태의 역산조도 계수모형의 결과를 실측 홍수위와 비교 분석하였다. 실제로 관측 수위에 대한 검증결과 유량에 따른 조도계수의 가변적 특징을 확인할 수 있었으며, 역산 조도계수 방법에 의한 흐름해석의 결과가 관측홍수위에 민감하게 반응함을 확인하였다.

• Proceedings of the Korea Water Resources Association Conference
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• 2011.05a
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• pp.83-87
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• 2011

산지하천은 지형 및 지질적인 요인으로 경사가 급하고 만곡수충부가 많이 발달되어 있기 때문에 홍수시 수충부에서 호안파괴의 문제가 많이 발생한다. 본 연구에서는 급경사 만곡수로의 외측 벽면에 돌출줄눈을 설치할 때 조도계수에 미치는 영향을 조사하였다. 실험유량은 $100{\ell}/s$, $120{\ell}/s$, $140{\ell}/s$이고, 수로경사는 1/50으로 고정하였다. 모든 구간에서 돌출줄눈의 영향으로 약 5-63%의 조도계수 변화가 발생하였다. 상대적으로 유량이 많을 때 외측벽면조도에 의한 조도계수의 증가는 더 크다. 이는 급경사 만곡수충부의 조도계수가 돌출줄눈에 의하여 제어될 수 있음을 나타내는 것이다.

• The Journal of the Korea Contents Association
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• v.12 no.7
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• pp.445-452
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• 2012

This study is used to analyze the distribution of resistance factors and the relationships of flow resistance with the field measurements which consist of the total 2,604 rivers for 1,865 bed material in natural channels and 739 vegetation in vegetated channels. Resistance factor relationships and distribution range of Manning roughness coefficients and Darcy-Weisbach friction coefficients by the regression analysis are derived from the power law form as a function of flow discharge and friction slope with bed materials and vegetations in natural and vegetated rivers, respectively.

• 한국방재학회:학술대회논문집
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• 2010.02a
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• pp.96.1-96.1
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• 2010

하천의 설계홍수위를 결정할 때 가장 중요한 변수중의 하나는 우리가 흔히 부르는 Manning의 조도계수 n으로 과거 수십 년 동안 국내 외에서 많은 연구가 진행되어 왔고 현재에도 끊임없이 여러 연구자들의 관심의 대상이 되고 있다. 이러한 조도계수는 보통 부등류 모형에 의한 방법, NCALC 모형에 의한 방법, 하상재료 또는 사진 index를 통한 방법을 사용하고 있지만 일관성이 떨어질 뿐만 아니라 산정된 조도계수가 유량 또는 수위에 관계없이 일정한 조도계수 만을 제시하고 있다는 문제점을 가지고 있다. 이러한 문제점 등을 해결하고자 부정류 수치모형을 이용하여 하천 구간에서의 조도계수를 유량의 함수로 산정하는 연구가 활발히 진행되어 왔다. 본 연구에서는 이러한 조도계수의 여러 특성을 파악하고자 국내 주요 하천인 한강, 낙동강, 금강의 본류 및 지류에 대해서 수위관측소를 기준으로 구간을 구분하고 과거 주요 홍수 수문곡선을 선정하고 부정류 해석을 통하여 다양한 유량에 대한 하천 구간별 조도계수를 산정하였다.

• Proceedings of the Korea Water Resources Association Conference
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• 2009.05a
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• pp.1306-1310
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• 2009

The roughness coefficients were estimated by the Manning's equation for the measured stage and flow velocity of Bocheong stream basin in Kum river. The relationships between the estimated roughness coefficients and the geomorphologic factors were formulated by the linear, logarithmic, exponential and power type function, thereafter correlation equations were presented. The correlation analysis was performed between the measured stream length and the basin area of Bocheong stream basin by the linear, logarithmic, exponential and power type function, and correlation equation for the stream length was given. The roughness coefficient has strong correlationship with stream slope, but low correlation coefficients with stream length and basin area. For the correlationship with the roughness coefficients and the stream slope, the logarithmic type function has the smallest correlation coefficient, on the other hand, the exponential type function has the largest correlation coefficient. For the relationship between the stream length and the basin area, the correlation coefficient of the logarithmic type function shows the smallest value, linear type function shows the largest value.