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This work deals with subsurface flow between a small Reservoir (named “Açude Cajueiro”, in Tuparetama PE) and its porous boundaries or seepage zones, considering two transects. Based on daily water level readings in piezometers and at the reservoir, and on the hydraulic characteristics of the porous media, the subsurface flow pattern can be investigated. A finite difference numerical model has been applied to assess recharge events and groundwater evaporation. Upward flow from the water table is an important moisture control process, especially when the water table is shallow. This component enables crop development near seepage zones without irrigation, in particular for crops with a short growth cycle.

Evolução da Zona Saturada em Agricultura de Vazante: Açude Cajueiro, Pernambuco