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LaTeX Math Block
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q(t)=q_{i} \cdot \left( 1+b \cdot D \cdot t \right)^{-1/b}

where

LaTeX Math Inline
bodyq_i = q(t=0)

Initial production rate of a well (or groups of wells)

LaTeX Math Inline
bodyD=-\frac{1}{q}\frac{dq}{dt}

decline decrement (the higher the

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bodyD
the

stringer

stronger is decline)

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body0 \leq b \leq 1

defines the type of decline (see below)


The cumulative production is then:

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Arp's model splits into three types based on the value of 

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bodyb
 coefficient:

ExponentialHyperbolicHarmonic

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bodyb=0

LaTeX Math Inline
body0<b<1

LaTeX Math Inline
bodyb=1


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q(t)=q_{i} \exp \left( -D \, t \right)



LaTeX Math Block
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q(t)=q_{i} \cdot \left( 1+b \cdot D \cdot t \right)^{-1/b}



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q(t)=\frac{q_{i}}{1+D \, t} 



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Q(t)=\frac{q_{i}-q(t)}{D}



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Q(t)=\frac{q_{i}}{D \, (1-b)} \, \left[ q_{i}^{1-b}-q(t)^{1-b} \right]



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Q(t)=\frac{q_{i}}{D} \, \ln \left[ \frac{q_{i}}{q(t)} \right]


Arps decline only work for Boundary Dominated Flow.

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