Forchheimer 포화항력모델을 이용한 투수성 호안의 해수교환량 모의

In this study, FLOW-3D''s Forchheimer''s saturation drag model was used to physically reproduce the flow of infiltrating water in the body of the permeable seawall. This study confirmed that Forchheimer''s saturation drag model could be applied to the permeability evaluation of the sea wall. The flow patterns in the body were compared between the temporary seawall constructed using only rubble stones and the back reinforced seawall in which the back part of the seawall was reinforced with filter rocks and mats. The flow patterns in the temporary seawall body were well-reproduced, in which the infiltration water moves from the open sea to the inside, and the flow accelerates as the stream tube shrinks. In the back-reinforced seawall, the flow pattern in which the seepage line of the body rises compared to the temporary seawall is well-reproduced due to the low permeability of the filter mat. When the simulated results of the inland tide surrounded by the seawall were compared with the observation data, the simulated and observed values showed a slight difference within 0.3m. At the T5 point, seawater exchange through the seawall was relatively as large as the temporary seawall installed. The simulation results reproduced the phenomenon that the tidal wave occurred smaller than the T5 point because the seawater exchange rate through the seawall was relatively low at the T6 point. After all, the back-reinforced seawall was smaller. In addition, it reproduced the observation data in which the tide was delayed, and the duration of the ebb tide was superior to that of the flood tide.