In hydrology, pipeflow is a type of subterranean water flow ^[1] where water travels along cracks in the soil or old root systems found in above ground vegetation.^{[ citation needed ]}

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.^{[ citation needed ]}

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