Drainage equation

Hooghoudt's equation

Hooghoudt's equation can be written as:.

Q L² = 8 Kb d (Di - Dd) (Dd - Dw) + 4 Ka (Dd - Dw)²

where:

Q = steady state drainage discharge rate (m/day)

Ka = hydraulic conductivity of the soil above drain level (m/day)

Kb = hydraulic conductivity of the soil below drain level (m/day)

Di = depth of the impermeable layer below drain level (m)

Dd = depth of the drains (m)

Dw = steady state depth of the watertable midway between the drains (m)

L = spacing between the drains (m)

d = equivalent depth, a function of L, (Di-Dd), and r

r = drain radius (m)

Steady (equilibrium) state condition
In steady state, the level of the water table remains constant and the discharge rate (Q) equals the rate of groundwater recharge (R), i.e. the amount of water entering the groundwater through the watertable per unit of time. By considering a long-term (e.g. seasonal) average depth of the water table (Dw) in combination with the long-term average recharge rate (R), the net storage of water in that period of time is negligibly small and the steady state condition is satisfied: one obtains a dynamic equilibrium.

Derivation of the equation
For the derivation of the equation Hooghoudt used the law of Darcy, the summation of circular potential functions and, for the determination of the influence of the impermeable layer, de method of mirror images and superposition.
Hooghoudt published tables for the determination of the equivalent depth (d), because the function (F) in d = F (L,Di-Dd,r) consists of long series of terms.

Determining:

the discharge rate (Q) from the recharge rate (R) in a water balance as detailed in the article: hydrology (agriculture)

the permissible long term average depth of the water table (Dw) on the basis of agricultural drainage criteria

the soil's hydraulic conductivity (Ka and Kb) by measurements

the depth of the bottom of the aquifer (Di)

the design drain spacing (L) can be found from the equation in dependence of the drain depth (Dd) and drain radius (r).

Drainage criteria
One would not want the water table to be too shallow to avoid crop yield depression nor too deep to avoid drought conditions. This is a subject of drainage research. The figure shows that a seasonal average depth of the water table shallower than 70 cm causes a yield depression
The figure was made with the SegReg program for segmented regression.

Equivalent depth

In 1991 a closed-form expression was developed for the equivalent depth (d) that can replace the Hooghoudt tables:

d = πL / 8 { ln(L/πr) + F(x) }

where:

x = 2π (Di − Dd) / L

F(x) = Σ 4e^−2nx / n (1 − e^−2nx), with n = 1, 3, 5, . . .

Extended use

Theoretically, Hooghoudt's equation can also be used for sloping land. The theory on drainage of sloping land is corroborated by the results of sand tank experiments. In addition, the entrance resistance encountered by the water upon entering the drains can be accounted for.

Definitions of drainage of sloping land and entrance resistance

Amplification

The drainage formula can be amplified to account for (see figure on the right):

the additional energy associated with the incoming percolation water (recharge), see groundwater energy balance

multiple soil layers

anisotropric hydraulic conductivity, the vertical conductivity (Kv) being different from the horizontal (Kh)

drains of different dimensions with any width (W)

Computer program

The amplified drainage equation uses an hydraulic equivalent of Joule's law in electricity.

It is in the form of a differential equation that cannot be solved analytically (i.e. in a closed form) but the solution requires a numerical method for which a computer program is indispensable.

The availability of a computer program also helps in quickly assessing various alternatives and performing a sensitivity analysis.

The blue figure shows an example of results of a computer aided calculation with the amplified drainage equation using the EnDrain program. It shows that incorporation of the incoming energy associated with the recharge leads to a somewhat deeper water table.