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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 \quad {\rm or} \quad  p_1(t_D, r_D = \infty) = 0

which represents a specific unique function of dimensionless time

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and distance
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.

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

is universal a unique dimensionless function of dimensionless time time

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which can be tabulated via numerical solution or approximated by polynomspolynom.


See Also

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Petroleum Industry / Upstream / Subsurface E&P Disciplines / Field Study & Modelling / Aquifer Drive / Aquifer Drive Models / Radial VEH Aquifer Drive @model

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