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

Chapte

r 2 – T heory

- p14/743

Darcy’s Law states that the pressure drop between two points, close enough to consider all

parameters to be constant, will be:

proportional to the flowrate density (q/A)

proportional to the fluid viscosity (

)

inversely proportional to the reservoir permeability (k)

Darcy’s Law is a fundamental law in dynamic data analysis. It is used to model the flow in

several compartments in the reservoir:

At any point of the reservoir, it is one of the three equations that will be used to define the

diffusion equation (see next section).

When the well is flowing, it determines the pressure gradients at the sandface.

Close to reservoir boundaries it determines that the pressure gradient towards a no-flow

boundary is flat, or it allows the determination of the inflow from the pressure gradient.

Darcy’s law assumes a linear relation between the flow of fluid in one direction and the

pressure gradient, corrected for gravity, in the same direction. This assumes that the density

of flow is small enough to avoid turbulent behaviour.

When there is turbulence, a quadratic term is added and Darcy’s law is replaced by the

Forchheimer’s equation. We then speak about non-Darcy flow. In most cases, non-Darcy

problems will be solved with a numerical model.

2.A.2

The diffusivity equation

The diffusivity equation describes how, in an elementary piece of rock, the pressure will react

in time as a function of the local pressure gradient around this piece of rock.

There may be as many diffusivity equations as there are assumptions on what is happening

downhole. The basic theory in Dynamic Data Analysis uses the simplest possible diffusivity

equation, assuming the following:

The reservoir is homogeneous and isotropic.

The fluid is single-phase and only slightly compressible.

Gravity effects are ignored. If they were not the diffusivity equation would be written in

terms of potential and not pressure.

Darcy’s law applies.

Reservoir and fluid properties are independent of the pressure.

Under these conditions, the diffusivity equation is derived from the combination of:

(1)

The principle of conservation of mass

(2) Darcy’s law

(3)

Slightly compressible fluid equation

Some more complex versions of the diffusivity equation will have different components:

Darcy’s law may be replaced by the Forchheimer’s equation, and more complex PVT models

may be used: real gas diffusion, multiphase black oil correlations or an Equation of state.