Ground water movement due to arbitrary changes in water level
The non self-similar boundary value problem of ground water movement due to arbitrary changes in water level is solved. The non self-similar solutions are generated from known similarity solutions using numerical methods.
permeability of the aquifer
height of water level above the impermeable surface
- x t h
dependent variable, defined in equation (5)
flow through a unit width, defined in equation (23a)
time coordinate in non self-similar description
refers to the value of the function at time τ
is the number of the iteration
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