|
1
|
- Refraction of q
- Equivalent K for fractured media
|
|
2
|
|
|
3
|
- Downward seepage occurs from a
shallow pond to a water table. A conservative traces is introduced at
point A. Calculate the location of tracer appearance at the water table
and the time it takes. Neglect dispersion, diffusion and assume
subsurface fully saturated.
|
|
4
|
|
|
5
|
- Storage in unconfined aquifers
- & 1-D flow equation
|
|
6
|
|
|
7
|
- Assume horizontal flow h does not
depend on z
- Horizontal aquifer base
- Mass balance
- ROMA= net mass flux in
|
|
8
|
|
|
9
|
|
|
10
|
- Flow through embankment (example 2.3.1)
- Agricultural drains (example 2.3.2)
|
|
11
|
|
|
12
|
|
|
13
|
|
|
14
|
|
|
15
|
- Consider a pumping well in an unconfined aquifer receiving a recharge
at a rate W. The saturated thickness beyond the radius of influence of
the well (R) is H0 examine drawdown distribution and value of R.
|
Notes
