Definición:
Proceso consistente en suministrar agua adicional para estabilizar o incrementar el rendimiento en condiciones in situ en las que un cultivo se puede cultivar normalmente con el agua directa de la lluvia por ser el agua adicional insuficiente para la producción del cultivo. La técnica consiste en compensar los déficits de agua de lluvia en etapas críticas del cultivo para aumentar el rendimiento
Fuente:
Food and Agriculture Organization of the United Nations, AQUASTAT Web Site
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