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Sub-irrigation q infil
Drainage q drain
φ gwl
φ drain,1
φ gwl
φ drain,2
φ gwl
φ drain,3
-
-
-
q drain
=
+
+
γ 1
γ 2
γ 3
φ drain,3
Groundwater
height φ gwl
φ gwl γ 1
φ drain,1
φ gwl γ 2
φ drain,2
-
-
q drain
=
+
φ drain,2
φ gwl
φ drain,1
-
q drain
=
γ 1
φ drain,1
φ drain,1
γ inf
φ gwl
-
q infil
=
Figure 9.7 Drainage or sub-irrigation lux as function of groundwater height, drain-
age level ϕ and drainage or sub-irrigation resistance γ .
conductivity in this region (m d -1 ), L is the drain spacing (m) and r d is the hydraulic
radius of the drainage canal (-). The variable d is an 'equivalent thickness', which is
smaller than the thickness of the aquifer D and which expresses the hydraulic head loss
due to convergent streamlines near the drainage canal. If the required drainage lux is
known, Equation ( 9.8 ) can be solved iteratively to ind the drain spacing L .
Question 9.5: Consider a ield where the relation between drainage lux and ground-
water level is similar as depicted in Figure 9.7 . The three drainage resistances are: γ 1 =
1000 d, γ 2 = 500 d and γ 3 = 250 d. The three drainage levels are situated at: φ drain,1 = -3.0
m, φ drain,2 = -2.0 m and φ drain,3 = -1.0 m with respect to soil surface. To solve this ques-
tion, use method the irst method from the above list:
a) How large is the drainage lux (mm d -1 ) at a groundwater level 2.5 m below the soil
surface?
b) How large is the drainage lux (mm d -1 ) at a groundwater level 1.5 m below soil
surface?
c) How large is the drainage lux (mm d -1 ) at a groundwater level 0.5 m below soil surface?
Question 9.6: At an orchard high groundwater tables occur due to an aquitard at
4 m depth. We want to install subsurface drains such that the maximum groundwater
level is 0.80 m below soil surface at a design discharge of 10 mm d -1 . The drains
have a hydraulic radius of 5 cm and will be installed at a 2.0 m depth. The saturated
 
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