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Dynamic Data Analysis – v5.12.01 - © KAPPA 1988-2017

Chapter

3 – P ressure Transient Analysis (PTA)

- p88/743

How does this work?

We had 400 hours of production and 100 hours of shut-in. Deconvolution is attempting to

provide 500 (theoretical) hours of constant production. The first 100 hours of the spline

representation are rigid, because they have to match the build-up. We have a loose tail

between 100 and 500 hours. The regression moves the tail up or down in order to match the

initial pressure pi after superposition, i.e. to match the depletion during the producing phase.

If the initial pressure is higher than the infinite case, the depletion is greater, and the reservoir

has to be bounded. If the initial pressure is lower, the depletion is less and the derivative of

the deconvolution will tail down and exhibit pressure support.

Now, there are hundreds of tail responses that could produce a specific depletion. Which one is

picked? The simplest one, because the regression selects the solution with the lowest

curvature, i.e. the one that will go smoothly from the part of the response that is fixed to

whatever PSS level. The first part of the data is rigid, the last part is more or less set by the

depletion and the transition is as smooth as possible.

Naturally, if we had more intermediate data, like some reliable flowing pressures, this would

‘firm up’ the deconvolution algorithm. The optimization first focuses on matching the data

before trying to get a smooth response.

3.D.5.a

Implementation in Saphir 5

The implementation in Saphir gives access to two of the above mentioned methods, through a

very logical workflow.

The periods to analyze must be first selected for extraction, they may be picked interactively:

Fig. 3.D.24 – Selecting the periods

Having selected one or more build-up, when the deconvolution process is called its dialog

offers possible methods:

-

Deconvolution on one period as reference, and the end of the other periods (Houze et

al.)

-

Separate solutions with a common Pi (Levitan et al.)