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Dimensionless transient water flux response from aquifer to unit step change in net pay pressure:


(1) W_{eD}(t) = \int_0^{t} \frac{\partial p_1( t_D, r_D)}{\partial r_D} \Bigg|_{r_D=1} dt_D

where

\chi_a

aquifer pressure diffusivity

r_e

net pay area

p_1(t_D, r_D)

solution of unit-pressure radial composite reservoir transient flow (2)(5)


(2) \frac{\partial p_1}{\partial t_D} = \frac{\partial^2 p_1}{\partial r_D^2} + \frac{1}{r_D}\cdot \frac{\partial p_1}{\partial r_D}
(3) p_1(t_D = 0, r_D)= 0
(4) p_1(t_D, r_D=1) = 1
(5) \frac{\partial p_1}{\partial r_D} \bigg|_{(t_D, r_D=r_a/r_e)} = 0


The Dimensionless Water Influx  W_{eD}(t) is a unique function of time  t for each dimensionless value of  r_a/r_e.

This function is well tabulated for a wide range of  r_a/r_e variations.

There are also polynomial approximations.


See Also


Petroleum Industry / Upstream / Subsurface E&P Disciplines / Field Study & Modelling 

Depletion ]   [ Aquifer ] [ Aquifer Drive @model ]

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