Abstract
합류수로에서의 하상변동에 대하여 90<TEX>$^{\circ}$</TEX> 합류부가 있는 수로를 이용하여 유량비 및 교각 위치를 변화시키면서 하상변동을 조사하였다. 유량비가 증가함에 따라 침식 깊이 및 침식 폭이 증가하는 경향이 나타났다. 유량비가 1：0.5에서 전체수로폭의 63%까지 침식되는 것으로 나타났으며, 최대 세굴심은 지류의 영향으로 인하여 가속유로에서는 합류점으로부터 수로 폭의 0.5배 되는 지점에서 직선 수로에서의 세굴심보다 2.5배 이상 큰 것으로 나타났다. 이것은 가속유로에서 나타난 최대 세굴심이 기존의 세굴공식에 의한 결과보다 2배 정도 크게 나타났다. 따라서, 합류부에 교각을 설치 할 경우 위치선정에 상당한 주의가 필요하다고 판단된다. The variation of channel bed which shows the complex hydraulic characteristics at channel junction was investigated by variation of discharge ratio and location of pier. As discharge ratio increase, the depth and width of erosion region become bigger to point of 63% of channel width in case of 1:0.5 discharge ratio. It was observed that the maximum scour depth at the point of 0.5 times of the channel width in the channel junction as 2.5 times bigger than straight channel. It means that the maximum scour depth at the channel junction is 2 times greater than by experimental formulas which are widely used in practical engineering, location of pier should be determined when it is installed in channel junction.
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