• 제목/요약/키워드: Vegetation flow resistance

검색결과 26건 처리시간 0.027초

FLOW-VEGETATION-SEDIMENT INTERACTION

  • Dittrich Andreas;Jarvela Juha
    • Water Engineering Research
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    • 제6권3호
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    • pp.123-130
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    • 2005
  • A good understanding of the interaction between flow, vegetation, and sediment is required for successful river restoration and sustainable flood management. The purpose of this paper is to provide a summary of available methods to determine flow resistance of natural rivers with vegetation, and discuss the influence of vegetation on erosion and sedimentation processes. Recently, significant advances have been made, but the effects of vegetation on flow and sediment dynamics are still not fully understood. Possible solutions to close the gaps in the current knowledge are suggested, with special focus directed to the determination of the interactive width between main channel and vegetated floodplains, the flow resistance of flexible vegetation with and without leaves, and the flow over submerged vegetation with low water depth.

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홍수터 식생의 물리적 특성을 고려한 흐름저항계수 산정 및 흐름특성 변화 모의 (Evaluation of Flow Resistance Coefficient based on Physical Properties of Vegetation in Floodplains and Numerical Simulation of the Changes in Flow Characteristics)

  • 지운;장은경;안명희;배인혁
    • Ecology and Resilient Infrastructure
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    • 제8권4호
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    • pp.212-222
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    • 2021
  • 본 연구에서는 홍수터 식생의 물리적 특성과 분포 특성을 고려하여 흐름저항계수를 산정하고 이를 2차원 수치모의에 반영하여 홍수터 식생분포가 흐름특성에 미치는 영향을 분석하였다. 홍수터 식생의 물리적 특성을 기존의 식생 흐름저항산정 공식에 적용하기 위해 지상라이다를 이용한 식생의 3차원 포인트 클라우드 분석을 수행하였으며, 홍수터 식생분포는 국부적으로 식생이 존재하는 경우와 홍수터 전체에 식생이 분포하는 경우로 구분하여 모의를 수행하였다. 대상구간의 모의결과, 홍수터 식생의 흐름저항계수는 매닝의 조도계수를 기준으로 계획홍수량이 발생할 경우 주하도 하상 조도계수에 비해 약 5배 이상의 값을 갖는 것으로 나타났으며, 이는 주하도와 홍수터의 수리특성 변화에도 영향을 미치는 것으로 나타났다.

개수로 내 식생구간의 흐름저항 및 흐름특성에 관한 실험적 고찰 (Experimental Study of Flow Resistance and Flow Characteristics over Flexible Vegetated Open Channel)

  • 여홍구;박문형;강준구;김태욱
    • 한국환경복원기술학회지
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    • 제7권6호
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    • pp.61-74
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    • 2004
  • Hydraulic engineers and scientists working on river restoration recognize the need for a deeper understanding of natural streams as a complex and dynamic system, which involves not only abiotic elements(flow, sediments) but also biotic components. From this point of view, the role played by riverine vegetation dynamics and flow conditions becomes essential. Hydro-mechanic interaction between flow and flexible plants covering a river bed is studied in this paper and some previous works are discussed. Measurements of turbulence and flow resistance in vegetated open channel were performed using rigid and flexible tube. Measuring detailed turbulent velocity profiles within and above submerged and flexible stems allowed to distinguish different turbulent regimes. Some interesting relationships were obtained between the velocity field and the deflected height of the plants, such as a reduced drag coefficient in the flexible stems. Turbulent intensities and Reynolds stresses were measured showing two different regions : above and inside the vegetation domain. In flexible vegetated open channel, the maximum values of turbulent intensities and Reynolds stresses appear above the top of canopy. Method to predict a flow resistance in flexible vegetated open channel is developed by modifying an analytical model proposed by Klopstra et al. (1997). Calculated velocity profiles and roughness values correspond well with flume experiments. These confirm the applicability of the presented model for open channel with flexible vegetation. The new method will be verified in the real vegetated conditions in the near future. After these verifications, the new method should be applied for nature rehabilitation projects such as river restorations.

Determination of Equivalent Roughness for Estimating Flow Resistance in Stabled Gravel-Bed River: I. Theory and Development of the Model

  • Park, Sang-Woo;Lee, Sin-Jae;Jang, Suk-Hwan
    • 한국환경과학회지
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    • 제17권11호
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    • pp.1203-1210
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    • 2008
  • Flow resistance in a natural stream is caused by complex factors, such as the grains on the bed, vegetation, and bed-form, reach profile. Flow resistance in a generally stable gravel bed stream is due to protrudent grains from bed. Therefore, the flow resistance can be calculated by equivalent roughness in gravel bed stream, but estimation of equivalent roughness is difficult because nonuniform size and irregular arrangement of distributed grain on natural stream bed. In previous study, equivalent roughness is empirically estimated using characteristic grain size. However, application of empirical equation have uncertainty in stream that stream bed characteristic differs. In this study, we developed a model using an analytical method considering grain diameter distribution characteristics of grains on the bed and also taking into account flow resistance acting on each grain. Also, the model consider the protrusion height of grain.

하천환경에서의 그라스콘크리트의 적용성 연구 (Hydraulic Application of Grass Concrete In River Environment)

  • 장석환;남용혁;김서영;박성범;박웅서;박상우
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2006년도 학술발표회 논문집
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    • pp.472-477
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    • 2006
  • This study aims at investigating the failure cases of the pre-cast block system in river environments which widely used nowadays and reviewing the effect and flow resistance for grass concrete structure through the physical experiments by hydraulic model test and developing application method in river slope or levee which has rigid flood resistance. Grass concrete structure has been independently tested under high velocity flow under the super critical condition, it survived the 8 m/sec maximum flow velocity. This results shows grass concrete system is also suited to use in aggressive river environments such as repairing a flood damaged embankment that had placed at risk the adjacent drainage channel with vegetation.

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식생수로의 유속분포에 관한 실험적 연구 (An Experimental Study on Velocity Profile in a Vegetated Channel)

  • 권도현;박성식;백경원;송재우
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2004년도 학술발표회
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    • pp.957-960
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    • 2004
  • From a water-environmental point of view, with a change of understanding and concern about vegetation, it changes that vegetation acts as stability of channel and bed, providing habitats and feed for fauna, and means improving those with appreciation of the beautiful but resistant factor to the flow So, it becomes important concern and study subjects that turbulent structure by vegetation, shear stress and transport as well as roughness and average velocity by vegetation. But from a hydraulic point of view, vegetation causes resistance to the flow and can increase the risk of flooding, Therefore, this thesis concern the flow characteristics in vegetated open channels. According to the experimental results, $z_0$ was on an average $0.4h_p$ in a vegetated open channel. So, the elevation corresponding to zero velocity in a vegetated channel was the middle of roughness element. The limit for logarithmically distributed profile over the roughness element was from $z_0$ to $0.80h_{over}$ for a vegetated channel. Among the existing theory, the method of Kouwen et al.(1969), Haber(1982), and El-Hakim and Salama(1992) except Stephan(2001) gave a very good value compared to the measured velocity profile.

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쓰나미 파형이 수중식생의 에너지소산에 미치는 영향 (Effects of Tsunami Waveform on Energy Dissipation of Aquatic Vegetation)

  • 이우동;박종률;전호성;허동수
    • 한국해양공학회지
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    • 제31권2호
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    • pp.121-129
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    • 2017
  • The present study numerically investigated the influence of the waveform distribution on the tsunami-vegetation interaction using a non-reflected wave generation system for various tsunami waveforms in a two-dimensional numerical wave tank. First, it was possible to determine the wave attenuation mechanism due to the tsunami-vegetation interaction from the spatial waveform, flow field, vorticity field, and wave height distribution. The combination of fluid resistance in the vegetation and a large gap and creates a vortex according to the flow velocity difference in and out of the vegetation zone. Thus, the energy of a tsunami was increasingly reduced, resulting in a gradual reduction in wave height. Compared to existing approximation theories, the double volumetric ratio of the waveform increased the reflection coefficient of the tsunami-vegetation interaction by 34%, while decreasing the transfer coefficient and energy attenuation coefficient by 25% and 13%, respectively. Therefore, the hydraulic characteristics of a tsunami is highly likely to be underestimated if the solitary wave of the approximation theory is applied for the tsunami.

부자 측정 시 식생을 고려한 유량산정에 관한 연구 (Discharge Computation from Float Measurement in Vegetated Stream)

  • 이태희;정성원
    • 대한토목학회논문집
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    • 제39권2호
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    • pp.307-316
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    • 2019
  • 하도 내 식생발달은 흐름저항을 크게하여 홍수 시 하천 수위를 상승시키고 수위-유량관계의 변화에도 영향을 미치고 있다. 홍수 시 수위가 첨두에 도달하고 하강하여 하도 내 드러난 식생은 대부분 도복(倒伏, prone) 상태에 있다. 이렇게 식생이 도복상태로 되어있는 식생층 구간은 식생된 개수로 흐름의 유속분포를 고려하였을 때 유속이 0인 지점의 높이로 고려된다(Stephan and Guthnecht, 2002). 그러나 부자 측정에 의한 유량산정에 있어서 식생층 구간의 높이를 고려하지 않고 하상높이를 유하면적으로 적용하면 유량이 과대 산정되는 경향이 발생한다. 본 연구에서는 식생된 하천에서 정도 높은 유량을 산정하기 위해 영강의 점촌, 내성천의 향석 지점에서 홍수 후 식생층 높이를 측량하고 통수단면적에서 식생층 투영면적을 제외하여 유량을 산정하였다. 그 결과, 유량의 규모에 따라 차이는 있지만 최소 4.34 %에서 최대 10.82 %의 유량편차를 보였다. 따라서 홍수 시 통수단면적을 적용하여 유량을 산정하는 유속-단면적 방법에 있어서 식생하천에서 식생층 높이의 투영면적을 고려하여 유량을 산정한다면 좀더 적합한 유량산정이 이루어질 것으로 판단된다.

접착성 식생기반재의 침식저항능력 평가 (Evaluation of Erosion Resistance Capability with Adhesive Soil Seeding Media)

  • 성시융;신은철
    • 한국지반신소재학회논문집
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    • 제14권2호
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    • pp.71-79
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    • 2015
  • 기존의 비탈면녹화공법인 식생기반재취부공법은 결합력의 부족이나 건조화, 유기물의 부족 등의 문제점들을 보이고 있다. 특히 비산이 심한 지역의 비탈면은 식생피복율이 현저히 떨어지고 시간이 경과함에 고사율이 증가되어 피복율이 더 저하되고 또다시 침식 및 비산이 증가하는 악순환이 이루어지고 있는 상황이다. 따라서 본 연구에서는 침식이나 비산에 저항하기 위해 친환경 토양안정재를 적용하고, 적정 배합비 결정을 위해 장기침수시험과 유수저항시험을 실시하였다. 친환경토양안정재와 기존의 녹화토기반재를 활용한 장기침수시험결과, 토양안정재의 혼합율 0%는 30시간, 2%는 40일 후 100% 붕괴가 발생되었으며, 4% 이상의 혼합비에서는 실험종료시까지 시료의 원형이 그대로 남아 있어 2% 이상의 토양안정재가 극한 조건에서도 형상을 유지하는데 영향을 줄 수 있는 혼합비임을 확인하였다. 또한, 식생기반재의 구조적 안정성을 평가하기 위해 인공강우시험을 40, 45, $55^{\circ}$ 경사비탈면에 대해 실시하였으며, 토양안정재의 혼합비 0, 4, 8%에 대해 유수저항시험을 실시하고 침식저항능력을 평가하였다. 실험결과, 토양안정재의 혼합에 따라 유실률이 급격히 감소하는 경향을 보이는 등 비산을 방지하거나 우수에 의한 침식에 저항하기 위해 적용한 친환경 토양안정재가 큰 유실감소효과를 거둘 수 있을 것으로 판단된다.