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


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W_{eD}(t, r_{aD}) =  \int_0^{t}  

\frac{\partial p_1( t_D, r_D)}{\partial r_D}  \Bigg|_{r_D=1} dt_D

where

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body\chi_a

aquifer pressure diffusivity

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bodyr_e

net pay area

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bodyp_1(t_D, r_D)

solution of unit-pressure radial composite reservoir transient flow

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\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}



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p_1(t_D = 0, r_D)= 0



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p_1(t_D, r_D=1) = 1



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\frac{\partial p_1(t_D, r_D)}{\partial r_D} 
\Bigg|_{r_D=r_{aD}} = 0

or

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 p_1(t_D, r_D = \infty) = 0



The Dimensionless Water Influx 

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bodyW_{eD}(t)
 is a unique function of time 
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bodyt
 for each dimensionless value of 
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bodyr_{aD}
 which represents the ratio of external aquifer size 
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bodyr_a
 to net pay size
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bodyr_e
:

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r_{aD} = \frac{r_a}{r_e}


This function is readily tabulated for a wide range of 

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bodyr_{aD}
 variations.

There are also polynomial approximations.


See Also


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

Depletion ]   [ Aquifer ] [ Aquifer Drive @model ]