part 8- type curve analysis
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U on com letion of this section, the student should be able to:
1. Identify wellbore storage and middle time regions on type
curve.
2. Identify pressure response for a well with high, zero, or
negative skin.
.
buildup tests using drawdown type curves.
4. Calculate wellbore storage coefficient, permeability, and skin
factor from type curve match.
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If we rearran e terms in the Ei-function solution, we can rewrite
the equation in terms of dimensionless variables.
For the line-source solution, we define the dimensionless
pressure, pD, the dimensionless time, tD, and the dimensionless
radius, r .
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Althou h we did not realize the im ortance at the time, we defined
skin factor to be dimensionless.
To account for wellbore storage, we define an additional
dimensionless variable - the dimensionless wellbore storage
coefficient, CD.
It is important to notice the similarity between Pd and S..
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The Grin arten t e curve describes the ressure res onse under
the following assumptions:
1. Constant rate production from a
2. Vertical wellbore in an
3. Infinite-acting homogeneous reservoir that is
. e w s ng e p ase qu o sma an cons an
compressibility
5. Infinitesimal skin that may be modeled with an apparent
wellbore radius
6. Constant wellbore storage coefficient
The Gringarten type curve was specifically developed for
drawdown tests in oil wells. We will see that we may use it (withsome limitations) to analyze pressure buildup tests in addition to
drawdown tests, and to analyze gas well tests as well as oil well
tests.
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In the Grin arten t e curve, the time is lotted as t /C , and the
dimensionless wellbore storage coefficient and the skin factor are
combined into a parameter CDe2s.
Each value of the parameter CDe2s describes a pressure response
having a different shape.
We call the set of curves with different values of CDe2s a type
curve, and the individual curves for different values of CDe2s are
called stems.
Note the similarity between any adjacent pair of curvescorresponding to different values of CDe2s. This similarity causes
a lot of uncertainty when doing type curve analysis using pressure
curves only.
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If we calculate the lo arithmic derivative of the semilo
approximation to the line source solution, we find that the result is
a constant that depends on flow rate, fluid properties, and rock
properties.
The logarithmic derivative of the dimensionless form of the same
equation is a constant with the value 0.5.
Note that the logarithmic derivative of pressure has the same
units as pressure.
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Just as we constructed a dimensionless t e curve with different
stems corresponding to different values of CDe2s, we can
construct a derivative type curve from the logarithmic derivative of
the pressure type curve.
The shapes of these stems are much more distinctive than those
for the pressure type curve.
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Each of the stems on the Grin arten t e curve exhibits
characteristic behavior.
At early times, the pressure and pressure derivative fall on a unit-
slope line. During this period, the pressure response is
completely determined by the wellbore properties. Permeabilitycannot be estimated if the only data available lies within this
WBS-dominated period.
After WBS effects have ceased, the derivative follows a horizontal
line. This is referred to as the middle time region. Permeability
may be estimated whenever there is 1/2 log cycle or more of data
in the middle time region.
ere s a rans on per o e ween e un s ope ne an e
middle time region. During this transition, both WBS andreservoir properties influence the pressure response. It is
sometimes possible to estimate permeability using data during
WBS and the transition, but the results are not as reliable as
when there is data l in in the middle time re ion.
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Skin factor may be estimated qualitatively by the shape of the
.
High skin factor
The pressure derivative rises to a maximum and then falls
sharply before flattening out for the MTR. The pressure curve rises along a unit slope then flattens out
.
The pressure and pressure derivative are separated by ~2 log
cycles after the end of WBS.
Little or no skin factor
The pressure derivative rises to a maximum, then falls only
sli htl before flattenin out for the MTR.
The pressure and pressure derivative are separated by ~1 log
cycle after the end of WBS.
Negative skin factor
The pressure derivative approaches a horizontal line from
below.
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The pressure and pressure derivative both leave the unit slope
line early, but take a long time to reach the MTR.
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