N. Michelakis et al., WATER-USE, WETTED SOIL VOLUME, ROOT DISTRIBUTION AND YIELD OF AVOCADOUNDER DRIP IRRIGATION, Agricultural water management, 24(2), 1993, pp. 119-131
The effect of three water use (WU) levels corresponding to 0.3, 0.6 an
d 0.9 Ep (Ep=Evaporation ''A'' pan) on wetted soil volume, root distri
bution and yield of avocado cv. Fuerte was investigated over a 5-year
period at Chania, Greece. The average amounts of irrigation water appl
ied annually (in addition to rain) for the three WU levels were 238, 5
53 and 868 mm, respectively. Soil volumes, with a volumetric soil wate
r content percentage (theta) corresponding to a soil water potential (
psi(s)) higher than -0.1 MPa, increased markedly from 0.3 to 0.6 Ep, a
nd slightly from 0.6 to 0.9 Ep WU levels, being 26.3, 41.7 and 52%, re
spectively. Deep percolation did not occur at 0.3 Ep, was moderate but
acceptable at 0.6 Ep, and high at 0.9 Ep. Root distribution was simil
ar in all treatments. Some 72% of the root system was concentrated in
the upper 0.5 m soil layer and within 2 m on either side of the drip l
ine. Root density (RD) increased greatly from 0.3 to 0.6 Ep, and sligh
tly from 0.6 to 0.9 Ep level. RD in relation to theta did not show any
notable difference between WU levels. Root growth rate, estimated by
the lateral to main root ratio (r), was higher in a 0 range of 20 to 3
0%, corresponding to a psi(s) range of -0.05 to -0.3 MPa for the soil
in the experiment. Yield at 0.3 Ep was lower than at 0.6 and 0.9 Ep WU
levels among which no significant differences were seen. Size of indi
vidual fruits and oil content were not significantly different between
treatments. When water saving, deep percolation, wetted soil volume,
root development, and yield quantity and quality are taken into accoun
t, then a WU level of 0.6 Ep can be considered optimal under the condi
tions of this experiment.