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An Analysis on the Characteristics of Separation Zone Due to a Bed Discordance at Confluence

합류부 하상고 불일치에 의한 분리구역 특성분석

  • Received : 2015.01.21
  • Accepted : 2015.06.11
  • Published : 2015.08.31

Abstract

The diverse patterns of separation zone according to the marked bed discordance by dredging at confluence in addition to the confluence angle of tributary and discharge ratio between tributary and main channels have been analyzed by CCHE2D model simulation. The separation zone is defined by inside of zero velocity boundary at down-stream of confluence. The separation zone dose not formed at the $30^{\circ}$ of confluence angle of tributary. The size of separation zone increases as the discharge ratio and confluence angle increase in general. The separation zone decreases as the dredging depth increases which shows the relative momentum reduction compared by the flow volume increasing by dredging at confluence. The contraction factor with the variation of confluence angle and discharge ratio has been investigated and confirmed the corresponding conveyance decreasing results in backwater effect. The regression equation of shape factor with confluence angle and discharge and dredging depth ratios has been suggested.

합류부에서의 지류의 합류각, 지류와 본류의 유량비에 추가하여, 본류 준설에 의한 하상고 불일치에 따른 다양한 양상의 분리구역의 특성을 CCHE2D 모형을 사용하여 분석하였다. 분리구역은 지류가 합류되어진 직후 단면에서의 유속이 0(영)인 경계로 정의하였다. 합류각 $30^{\circ}$ 이하에서는 분리구역이 형성되지 않았다. 유량비와 합류각 증가에 따른 분리구역의 크기는 일반적으로 증가하는 양상으로 나타났다. 준설 깊이비 증가에 따른 분리구역의 크기는 합류부 수용체의 증가에 기인한 지류에서의 상대적인 운동량의 감소로 인하여 감소되었다. 유량비와 합류각의 변화에 따른 분리구역의 수축지수를 규명하였고, 통수기능의 저하에 따른 배수영향을 확인하였다. 합류각, 유량비, 준설 깊이비에 따른 분리구역의 형상지수의 관계식을 제안하였다.

Keywords

References

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