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In case of harmonic periodic pulsations and sufficiently long pressure-rate delay and a simple diffusion model (single-bed homogeneous reservoir without boundary) the pressure pulse response can be approximated by analytical model:

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q= \sum_k q_1k \cdot \cos \left(\frac{2 \pi \, k \, t}{T} \right)


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p = \sum_k p_1k \cdot \cos \left(\frac{2 \pi \, k \, t}{T}  + \delta_k \right)

where



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bodyL



distance between the pint of flow variation and point of pressure response, being:

  • well radius
    LaTeX Math Inline
    bodyL=r_w
    for Self-Pulse Test

  • distance between generating and receiving well
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    bodyL= \sqrt{ \left({\bf r}_{\rm Generator} - {\bf r}_{\rm Receiver} \right ) ^2}
    for Pressure Pulse Interference Test

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bodyq_1k

k-th 1st harmonic amplitude of flowrate variation


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p_1k = \frac{q_0k}{\sigma} ...



1st k-th harmonic amplitude of pressure response to the flowrate variation


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\delta_k = \frac{\pi}{8} + \frac{L}{\sqrt{\chi \, T}}



phase shift caused by pressure response delay to the flowrate variation


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\sigma = \left< \frac{k}{\mu} \right> h



formation transmissbility


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\chi = \left< \frac{k}{\mu} \right> \frac{1}{c_t \, \phi}



formation pressure diffusivity

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