The change of the flow dynamic axis brings to the intro year variation of Hanyang side bar which presents as scours in flood period and deposits in ft falling stage and dry period.

 
  • 而枯水期水流動(dòng)力軸線(xiàn)彎曲,水流動(dòng)力軸線(xiàn)在潛洲尾部以下由左側過(guò)渡到右側的特點(diǎn)決定了漢陽(yáng)邊灘汛期沖刷,汛后以及枯水期淤積外展的規律;
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