Agriculture Reference
In-Depth Information
E a =
(irrigation water available to the crop)
×
100
/
(water delivered to the field)
(4.1)
where
Irrigation water available to the crop
root zone soil moisture after irrigation
- root zone soil moisture prior to irrigation
Water delivered to the field
=
=
flow meter reading or nozzle flow rate
Kruse ( 1978 ) defined application efficiency as
E a =
(average depth of water stored in the root zone)
×
100
/
(average depth applied)
(4.2)
For in-field evaluations where the depth of water applied is less than the root zone
moisture deficit prior to irrigation and runoff is not evident, the irrigation water
available to the crop can be assumed to be equal to the average depth of water
applied as measured at the soil surface (e.g., with catch cans in sprinkler system). In
these cases,
E a = [average depth applied (mm)
×
area (ha)
/
10]
(4.3)
[water delivered to the field(m 3 )]
×
100
/
1m 3
Application efficiency is primarily affected by the management of the irrigation
and may vary significantly between irrigation events.
Attainable water application efficiencies of different irrigation systems under
normal condition are given in Table 4.1 .
Note :(1mm
×
1 ha)/10
=
Table 4.1 Attainable application efficiencies under different irrigation systems (adapted from
Solomon, 1988 )
Type of irrigation system
Attainable efficiency range
Surface irrigation
Border
75-85%
Basin
80-90%
Furrow
65-80
Sprinkler
Solid set or permanent
75-85%
Hand move or portable
75-85%
Center pivot & linear move
75-90%
Traveling gun
65-75%
Trickle irrigation
Point source emitters
80-90%
Line source
75-85%
 
 
 
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