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poster - International Conference of Agricultural Engineering

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Table 1 - Reference evapotranspiration (ETo), total precipitation, usable precipitation<br />

and irrigation levels applied at different replacement rates evaluated.<br />

Treatment ETo * Total<br />

precipitation<br />

mm<br />

Usable<br />

precipitation<br />

mm<br />

Irrigation<br />

water depth<br />

50% <strong>of</strong> ETo 986,7 655,8<br />

75% <strong>of</strong> ETo 1480<br />

441,2 330,9<br />

1149,1<br />

100% <strong>of</strong> ETo 1973,4 1642,5<br />

125% <strong>of</strong> ETo 2466,7 2135,8<br />

a) b)<br />

Figure 1 - Operation <strong>of</strong> the emitter (a) and partial view <strong>of</strong> the hybrid UENF / Caliman 01<br />

papaya experiment (b).<br />

2.2 Fertilization and irrigation management<br />

Fertilization was made as indicated by Sobral et al, (2007), weekly using urea (44%<br />

N), potassium chloride (56%K 2 O) and phosphoric acid (50% P 2 O 5 ).<br />

The irrigation water depth, the amount <strong>of</strong> water application, and irrigation time was<br />

determined by equations 2, 3 and 4, respectively, as proposed by Mantovani et al. 2006.<br />

LB =<br />

ETo.<br />

Ks<br />

− Pe<br />

Ef<br />

Equation 2<br />

which:<br />

LB = gross water depth (mm day -1 );<br />

ETo = reference evapotranspiration second Penman-Monteith method (mm<br />

day -1 );<br />

Ks = percentage <strong>of</strong> wetted area by the issuer;<br />

Pe = effective precipitation, in the period (mm);<br />

Ef = irrigation efficiency.

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