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                INTRODUCTION


           Irrigation is necessary for crop production for many reasons: water transports minerals through

           the soil and to roots, is a principal medium for chemical and biochemical processes that sup-
           port plant metabolism, provides physical support, acts as a solvent for dissolved sugars and

           minerals, and evaporation provides plants with the ability to cool so that temperatures are fa-

           vorable for metabolic processes. The primary economic consequence of insufficient water for

           crops is a reduction in yield. There are also economic consequences of over irrigation, such as

           yield reduction, leaching of agrochemicals, and increased costs associated with irrigating.

                A successful irrigation system is defined as a system that functions with minimal water los-

           ses, supplies the correct amount of water to the designated location at appropriate times, and
           is economically viable.  Appropriate allocation of the needed quantity of irrigation waters may

           be achieved through use of the water balance method and/or soil water moisture sensors.




                Water balance

           The water balance for a field is the simplest method for determining irrigation volumes. The
           water balance consists of water flux in and out of a plant system boundary (Fig. 1). The water

           balance may be defined mathematically as:

                           ΔS = R + I - ET - (D + RO)           (1)










                                                                Universidad Autónoma de Chiapas
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