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Pipeflow
In hydrology, pipeflow is the name given to a type of subterranean water flow where water travels along the old root systems of the above vegetation or cracks in the soil. In such soils which have a high vegetation content water is able to travel along the 'pipes', allowing water to travel faster than throughflow. Here, water can move at speeds between 50 and 500 m/h.
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Pipeflow」の詳細全文を読む
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