Soil Management Handbook - Ministry of Agriculture and Lands
Soil Management Handbook - Ministry of Agriculture and Lands
Soil Management Handbook - Ministry of Agriculture and Lands
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Table 14<br />
Peak Evapotranspiration Rates For the Okanagan <strong>and</strong> Similkameen Valleys (cm/day)<br />
Maximum <strong>Soil</strong> Water Deficits (cm <strong>of</strong> water)<br />
Location 2.5 5.0 7.5 10.0 12.5<br />
Armstrong .66 .56 .53 .51 .48<br />
Ellison .69 .61 .58 .53 .53<br />
Joe Rich .53 .46 .41 .38 .38<br />
Kelowna .71 .64 .61 .58 .56<br />
Keremeos .79 .76 .74 .71 .71<br />
Oliver .74 .66 .61 .58 .58<br />
Osoyoos .84 .76 .71 .69 .66<br />
Summerl<strong>and</strong> .76 .71 .66 .61 .61<br />
Vernon .66 .58 .56 .53 .53<br />
Example Calculation <strong>of</strong> Maximum <strong>Soil</strong> Water Deficit <strong>and</strong> Maximum Irrigation Interval for Apples Grown on<br />
a Silt Loam in Summerl<strong>and</strong><br />
Effective rooting depth <strong>of</strong> apple crop<br />
Available water storage capacity for a silt loam<br />
Availability coefficient for apples<br />
1.2 m (Table 10)<br />
21.0 cm/m (Table 11)<br />
0.40 (Table 12)<br />
Maximum soil water deficit for apples on a silt loam = 1.2 m x 21.0 cm/m x 0.40<br />
= 10.1 cm<br />
Peak evapotranspiration for maximum soil water deficit <strong>of</strong> 10.1 cm at Summerl<strong>and</strong> is 0.61 cm/day (Table 14).<br />
Maximum irrigation intervals is 10.1/0.61 = 16.5 days.<br />
Recommended irrigation intervals is 16.5 x 0.5 = 8 days (see Section 3.1.1.6)<br />
average ET during an irrigation interval. The ET<br />
values are given in cm per day for maximum soil<br />
water deficits <strong>of</strong> 2.5 to 12.7 cm <strong>of</strong> water.<br />
3.1.2 Application Systems<br />
There are a number <strong>of</strong> systems available for applying<br />
irrigation water. These include solid set, h<strong>and</strong> move,<br />
wheel move, giant reel or big gun <strong>and</strong> trickle or drip<br />
systems. Each system has advantages for use for<br />
specific crops. Sprinkler systems are described in the<br />
publication, B.C. Sprinkler Irrigation Manual.<br />
Careless application <strong>of</strong> water can lead to erosion on<br />
sloping l<strong>and</strong>. Excess applications <strong>of</strong> water on<br />
glaciolacustrine cliffs in the Okanagan can cause<br />
slumping. Alkaline (saline) salts are also present in<br />
some soils <strong>of</strong> the Okanagan <strong>and</strong> Similkameen Valleys<br />
<strong>and</strong> excessive water application may lead to the<br />
development <strong>of</strong> saline seeps. Application rates<br />
should be sufficiently low not to exceed the<br />
infiltration capacity <strong>of</strong> the soil. Furthermore, care<br />
should be taken not to exceed the water-holding<br />
capacity <strong>of</strong> the soil, since further additions <strong>of</strong> water<br />
will cause saturation <strong>and</strong> eventually run<strong>of</strong>f <strong>and</strong><br />
erosion.<br />
<strong>Soil</strong> <strong>Management</strong> <strong>H<strong>and</strong>book</strong> – Okanagan-Similkameen Valleys 51