Borehole (Downhole or THP) pressure survey based on the pressure response to the periodic flow rate variations (also called "cycles" or "pulses" ).

The usual practise is to create 3 - 5 pulses.

The pressure response is recorded in

or


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


q=q_0 \cdot \cos \left(\frac{2 \pi \, t}{T} \right)


p=p_0 \cdot \cos \left(\frac{2 \pi \, t}{T}  + \delta \right)

where


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



phase shift related to the pressure response delay to the flowrate variation


p_0 = \frac{q_0}{\sigma} ...



pressure response to the flowrate variation


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



transmissbility


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



pressure diffusivity