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Along
the upper course of wadi Saoura (Algeria) the dams stop the underground
flow and produce surface water for the crops planted along both
sides of the riverbed. When floods occur and form water courses
flowing on the ground, the latter are conveyed to the lateral
terraces (A) in order to allow irrigation by gravity at a higher
level than the natural run-off (B). In periods of aridity, humidity
is retained in the subsoil and water is drawn up from an outlet
situated at the foot of the dams (C).
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