Lecture GB - GMS intro (see above besides VB lecture)
3 important questions on Lecture GB - GMS intro (see above besides VB lecture)
What is the principle of drainage theory?
From the top recharge is introduced at the groundwater table
One ditch or drain discharges the precipitation of half of neighbouring fields
What are the basic assumptinos behind the drainage theory (6)?
- Stationary flow
- Recharge from precipitation
- DIscharge = recharge
- Dupuit
- Fully penetrating ditches
- Homogeneous soil
What does dH = 2/3 m0 indicate?
So due to the parabola shape the average head build up is 2/3 of the (max) head build up
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