analysis of pressure falloff tests following cold water injection
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Analysis of Pressure-Falloff TestsFollowing Cold-Water InjectionReldar B. Bratvold, * SPE, and Roland N. Home, SPE, Stanford U.
~umma~. This p~per presen~s generaliz~~ procedures. t~ interpret pressure i~jection and falloff data following cold-water injection
Into a hot~OlIrese': '?lr. Th~ relative permeability ch~ractensl:lcs of the porous medium are accounted for, as is the temperature dependence
of t~e.flu~d mobilities. It IS .shown that the saturation and temperature gradients have significant effects on the pressure data for both
the Injection and falloff penods. The matching of field data to type curves generated from analytical solutions provides estimates ofthe t~mperature.-dependent mobilities of the flooded and uninvaded regions. The solutions also may be used to provide estimates of
the size of the Invaded region, the distance to the temperature discontinuity, heat capacities, and wellbore-storage and skin effects.
Introduction
Numerous full-field waterflooding projects are currently under way
throughout the world to improve recovery. In many large oilfields,
water injection is initiated during the early stages of reservoir de-
velopment. Exploratory wells are tested for injectivity, and injectors
are tested during field operation. If properly interpreted, these tests
can give information about the progress of the flood (i.e., frontal
advance), residual oil saturation, the flow characteristics of the virgin
formation, and near-wellbore damage.
In a water-injection well test , the injected fluid usually has a tem-
perature different from the initial reservoir temperature. During
injection, both a saturation and a temperature front propagate intothe reservoir, Furthermore, because of differences in oil and water
properties, a saturation gradient is established in the reservoir. The
water saturation is highest close to the well and continuously
decreases with distance from the well. Ahead of this invaded region
is the unflooded oil bank at initial water saturation.
For the interpretation of well-test data, the most important temper-
ature-dependent fluid property is the viscosity. The viscosity of both
oil and water may change by an order of magnitude between 50
and 572°F, with the major change occuring between 50 and
212 of. 1 This temperature effect strongly influences the fluid mo-
bilities, and hence, the saturation gradient and the transient pressure
response. The total fluid mobili ty changes continuously in the in-
vaded region and has to be accounted for in reservoir modeling
and data interpretation.
Many different models have been introduced for the analysis ofwater-injection and falloff tests. Typically, these models neglect
the temperature effects, the saturation gradient, or both. Refs. 2
and 3 provide reasonably complete reviews of previous works.
For this paper, the most important reference is Fayers'f exten-
sion of the fractional flow theory of Buckley and Leverett> to ac-
count for a radial temperature gradient in the reservoir. Fayers'
work was put into a mathematical framework by Karakas et al.>
and Hovdan.? Hovdan also used this incompressible-fluids solu-
tion to derive a pressure-transient solution for the late stages of a
cold-water-injection test.
Recently, Abbaszadeh and Kamal? presented procedures to ana-
lyze falloff data from water-injection wells. Their procedures are
based on analytical solutions not presented in their original paper
and include the effect of the saturation gradient inthe invaded region.
Nonisothermal effects were not considered.
In summary, a number of studies pertaining to well-test analysisof injection and falloff tests have been presented. However, none of
these account for both of the two most important effects in a typical
waterflood: the saturation gradient and the temperature effect.
The principal objectives of this paper are (I) to derive analytical
solutions that include the most important effects in a nonisothermal
water-injection/fal loff test, (2) to examine the parameters that in-
fluence the well injectivity, and (3) to present procedures to obtain
detailed and accurate information about the important reservoir and
fluid properties in a waterflood. Specifically, we consider the pres-
sure behavior at the well resulting from the simultaneous flow of
'Now a t IBM European Pet roleum App li cat ion Center .
Copyr igh t 1990 Society of Pe troleum Enginee rs
SPE Formation Evaluation, September 1990
oil and water in a reservoir with a radial temperature gradient. Ana-
lytical solutions that account for the effects of temperature and satu-
ration gradients are derived and discussed. Consequences of
neglecting the temperature and saturation effects are illustrated.
Solutions for linear systems, including the effects of linear bound-
aries in cylindrical reservoirs, were presented by Bratvold and
Larsen. 8
Mathematical Model
Fig. 1 presents a schematic of the reservoir configuration consid-
ered. The reservoir is assumed to be cylindrical with the well atthe center. The well penetrates the entire formation thickness, and
fluid is injected at a constant rate. The reservoir is assumed to be
a uniform, homogeneous porous medium, completely saturated with
oil and water, Liquid compressibilities are assumed to be constant,
while the viscosities are assumed to be functions of temperature
only. Neglecting effects of gravity, as well as heat transfer to the
surrounding formation, permits the use of a ID radial model.
Injection Period. The transient, nonisothermal two-phase flow of oil
and water requires that saturations, pressures, and temperatures be
determined simultaneously at any time. Furthermore, because cold-
water injection into a hot-oil reservoir is a moving-boundary prob-
lem, it cannot be solved with standard linear techniques, such as
eigenfunction expansion, integral transforms, or Green's function
methods.
To circumvent the problem of simultaneously solving the coupled
second-order conservation equations, we derive an alternative
approximate solution to the injection problem using a two-step
procedure.
Step 1. Assume incompressible fluids. Then use fractional flow
theory to solve the resulting first-order coupled energy- and mass-
conservation equations.4,6,7 This essentially amounts to decoupling
the equations for saturation and temperature from the pressure equa-
t ion. The saturation profile obtained is a Buckley-Leverett> pro-
file including (convective) temperature effects.
Step 2. With the saturation and temperature proftles and the mobil-
i ties and diffusivities known from Step I, solve the diffusion equa-
tion for pressure by assuming that the fluid compressibilities are
small and constant . Hence, the pressure distribution in the system
is obtained by superimposing pressure-transient effects on a satu-
ration profile known a p r io r i.Fig, 2 shows an example of a saturation and temperature distri-
butions as functions of the similarity transform t=7rcphr2/qt, as
calculated from the Buckley-Leverett model and including temper-
ature effects. 4,6,7 Note that the profile exhibits two saturation dis-
continuities. In addition to the discontinuity depicted by the standard
Buckley-Leverett theory, the saturation distribution shows a sec-
ond discontinuity caused by the step-change in temperature. The
magnitude of the saturation change at the temperature discontinuity
is related to the ratio between the mobility ratios in the hot and
cold zones. The saturation distribution obtained from a numerical
simulator is superimposed on the analytical saturation profile. The
simulations were performed with a two-phase, 2D, black-oil simula-
tor developed by Nyhus? that is described later in the paper.
293
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Region 1
Region 2
Region 1
Fig. 1- Two-region, radial moving-boundary problem.
As Fig. 2 shows, the saturation distribution obtained numerically
isvery close to the analytical solution for this data set, which isgiven
in Table 1and which is typical for water-injection tests. On the basis
of Fig. 2 and other examples.I it is reasonable to conclude that
the nonisothermal Buckley-Leverett solution is a good approximation
to the actual saturation distribution (neglecting gravity) for typical
water-injection tests where the compressibilities Co and Cw are of
the order 10 - 5 to 10 - 6 psi - l and the mobility ratio M < ! 1 : 100.
Step 2 consists of solving the diffusion equation for pressure in the
composite system schematically illustrated in Fig. 1. With the satura-
tion distribution known as a function of time and space from Step 1,
the total fluid mobility and total system compressibility become func-
tions of time and space. The locations of the saturation and tempera-
ture fronts are time-dependent, and hence this is a moving-boundary
problem. In general, moving-boundary problems are nonlinear and
cannot be solved by standard techniques based on superposit ion.
The moving-boundary problem can be linearized by introducing
the Boltzmann variable (similarity transform) y=rl)4tD' As
shown in Appendix A, the Boltzmann variable is constant at the
moving boundary by virtue of the integrated frontal-advance equa-
tion (Eq. A-lO). Hence, the problem can be transformed to a com-
posite problem with a fixed interface where the independent variable
is y. The mathematical formulation and solution to the injection
problem is presented in Appendix A. To obtain the wellbore pres-
sure in an infinite system we evaluate Eqs. A-22 and A-23 at
rD=1.
PwD =(MI2)E, (1I4tD)' to s, 1I4YBL (1)
294
1.0I
I- - Temperature
I-- Buckley-Leverett00000 Numencal simulator
I
I~I
f-O .S I.
0
0
~ I
(f) I Set 2 0
I
I M = 5
I fj = 21.6
-I
0.00.0 1.0 2.0 3.0
~
Fig. 2-Comparison of simulated and analytical saturat ion and
temperature distributions.
TABLE 1-SIMULATOR INPUT DATA
USED IN VERIFICATION
Reservoir Properties Fluid Properties
TR , OF 180 SWj , fraction 0.2
Tj , OF 60.7 SO" fraction 0.14 > , fraction 0.2 co, psi " ' 1 x 10-5
h, ft 25 cw, psi-1 1 x 10-6
r w , ft 0.25 (pC)o' Btu/(ft3_0F) 23.00
r e' ft 1,000 (pC)w, Btu/(ft3_OF) 62.35
k, md 20 (pC) s' Btu/(ft3_OF) 42.45
P R , psi 1,000 krw(Sw) Sw3
q, BID 250 kro(Sw) (1-Sw) 3
Viscosity, cp
Data Set 1
2.00
8.00
0.25
0.40
Data Set 2
2.40
7.20
0.401.20
flon
floc
flwh
flwc
and PwD='/2E, (l/41)tD) - V2E1 (YBL/1)+ (MI2)E1 (YBL)
+ '/2IBL (f"/f')[(lIF).) -1]dSw, to ~ 1/4YBL' ..... (2)
sw /
Note that YBL is constant and that the saturation at the wellbore
sandface, Swf' is a function of time because of the line-source
inner-boundary condition. Pressure is scaled with respect to the
water propert ies at injection conditions, while time is scaled with
respect to the oil properties in the uninvaded oil zone.
For late times, the above solution approaches
pwD='h(ln tD+O.80907)+sa' (3)
where the apparent skin factor, sa' is given by
..................................... (4)
The late-time solution is equivalent to the solutions derived by Hov-
dan," Benson et al., 10 and Barkve. * These authors assumed the
inner region to be incompressible, not only in describing the satu-
ration profile." but also in solving for the pressure distribution.
This implies that the fluids in the invaded region essentially be-
have as incompressible at late times in the injection period.
'Pers~nal communication with T. Barkve, U. of Bergen. Norway (March 1987).
SPE Formation Evaluation, September 1990
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1.0 -,--------------------,
-_ Injection doto
00000 Folloff doto
"f) 0.5
Set 1
M 5f 7 = 21.6
0.0 +---r----,----.---..,.---,.----,---~o 200 400 600
Fig. 3-Saturatlon distribution during falloff.
Following the approach used by Verigin 1 1 and Ramey, 1 2 we can
derive approximate solutions to the finite outer-boundary problems
by solving a three-region problem with moving boundaries. The
wellbore pressure for the closed system is
..................................... (6)
The constant-pressure outer-boundary solution is given by Eqs. 5
and 6 without the exponential (last) term.
Finally, note that the above solutions apply equally well to thecase where temperature effects are neglected, provided that the ap-
propriate fractional-flow curve is used. As demonstrated in Appen-
dix A, these solutions reduce to the two-region solutions derived
by Woodward and Thambynayagam 13 and Barkve, 14 if the flow
is piston-like.
Falloff Period. The solid line in Fig. 3 shows the saturation distri-
bution obtained from the numerical model after 100 days of injection
with the data in Table 1. The saturation profile obtained from the
same simulator after the well is shut in for 100 days after the 100
days of injection is also shown. The saturation profiles are virtually
identical, implying that the saturation distribution during falloff re-
mains stationary. This is consistent with use of th e Buckley-Leverett
theory for the injection solution because the assumption of incom-
pressible fluids will result in the immediate stoppage of the mov-ing saturation distribution and temperature discontinuity. The falloff
problem can then be approximated by a linear problem (fixed in-
terface) where the mobilities and diffusivities are given by their
value at the end of the injection period. The solution to this variable-
coefficient problem can be obtained by dividing the invaded region
into several regions where the saturation is approximated by its aver-
age value within each region. The pressure distribution at the end
of the injection period is the appropriate initial value for the falloff
problem. The formulation and solution to the problem are given
in Appendix B. Because we do not rely on the use of a similarity
transform in solving the falloff problem, we can implement a finite
wellbore radius with storage, skin, and a finite outer boundary. The
SPE Formation Evaluation, September 1990
30~-------------------,-- Similarity solut ion00000 Numerical solution
- - Piston-like displacement
20
10
Set 2
10'
t o10 • 10 •
Fig.4-Comparison of analytical andnumerical solutions for
the Injection period in an infinite reservoir.
wellbore-pressure solution for the SD =0 case is obtained by in-
verting Eq. B-14 and evaluating the pressure at rD =I:
+ £-I[X llK O (-.j~ )]+ £ -1[X I2 Io(~ )], (7)
while the solution including wellbore storage is obtained from the
inner-boundary condition (Eq. B-6).
As demonstrated by Bratvold ' and Bratvold and Horne, 15 the
falloff solution can also be obtained by superposing the solutions
to the stationary saturation-distribution problem.
Solution Verification
In this section, the analytical solutions for the injection and falloff
periods are compared with numerically simulated results. The simu-
lator is a single-well thermal model, which numerically solves a
more-detailed model of the physical situation." The appropriate
partial-differential equations are solved with a finite-difference tech-
nique, and the solution procedure is fully implicit with respect topressure, saturation, and temperature. Effects of gravity, capillary
pressure, and variations in relative permeabilities are accounted for
in the simulator. The simulator can include heat convection and
conduction in two dimensions in the reservoir, as well as conduction
between the reservoir and the cap- and bedrock. The heat capacities
and conductivit ies are assumed to be independent of temperature
and pressure. The densities are assumed to be linear functions of
pressure and temperature, while the viscosities are entered in table
form as functions of pressure and temperature.
Gravity was neglected in all the simulations conducted. A total
of 1,000 gridblocks was used in the simulator to permit an accurate
determination of the saturation, temperature, and pressure through-
out the reservoir.
Injection Period. Fig. 4 presents data from two injection tests in
an infinite reservoir. Table I gives the data used in the numerical
reservoir simulator. The dimensionless pressures are plotted vs.
injection time. The two cases shown differ in the values of the vis-
cosities at injection and reservoir temperature, and hence, differ
in mobility ratios. The numerical results compare very well with
the analytical solution for both cases.
Fig. 4 also shows the results from a three-bank analytical solution,
where the displacement is assumed to be piston-l ike and the fluid
discontinuities move according to mass and energy balance. 13,14
Obviously, significant errors are introduced by neglecting the vari-
able saturation profile. In particular, application of the three-region
solution results in a large underestimation of the apparent skin fac-
tor, and hence, an overestimation of the formation damage.
295
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2 5 ~ - - - - - - - - - - - - - - - - - - - - - - - - - - ~ - - - - - - - ,
15
Set 2
20
-- Similarity solution00000 Numerical solution
08
o
•.10
Fig. 5-Comperlson of analytical and numerical solutions for
the Injection period In a finite reservoir.
Fig. S shows injection results for closed and constant-pressure
outer boundaries. Again, we get a very good match between the
numerical and analytical solutions for the closed outer-boundary
case. The numerical simulator used lacked the capability of im-
plementing a constant-pressure outer boundary. Unlike the constant-
pressure case, however, the closed outer-boundary solution actu-
ally violates a boundary condition.? and hence we expect the
constant-pressure outer-boundary solution to give a better approx-
imation to the actual pressure behavior.
Falloff Period. Fig. , presents falloff results for the two injection
cases shown in Fig. 4. Fig. 7 shows falloff results following injec-
tion into a finite reservoir. The injection time was 100days in both
figures.
As discussed previously, the falloff problem is a variable-
coefficient problem that is solved by dividing the -invaded region
into several regions where the saturations and the coefficients in
the governing equation are approximated by their average values.
The accuracy of this approach increases with the number of regions
and is also a function of the saturation gradient in the flooded region.
For the examples presented in Figs. 6 and 7, we found eight regions
to be sufficient. As with the injection results, the analytical solu-
t ions compare excellently with the results obtained numerically.
In addition to the examples presented here, numerous other cases
were investigated. 3 In all cases where typical water-injection data
were used, the agreement between the numerical and analytical so-
lutions was excellent. Hence, the validity of the mathematical model
2 5 , - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ,Set 2
-- Analytical solution00000 Numerical solution
20
15
o•.10
5
10'
6t O
Fig. 7-Comparl80n o f .... ytlc.l.nd numerical solutions for
the f.lloff period In a finite reaervolr.
296
10 •
3 0 ~ - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ,-- Analytical solution00000 Numerical solution- - Piston-like displacement
20
o
•.10
10 •10 •
llto10 • 10 •
Fig. 6-Comparison of analytical and numerical solutions for
the falloff period in an infinite reservoir.
is established and the use of the analytical solutions for well-test
interpretation is justified.
Results
Inthis section we illustrate the general behavior and the applicability
of the solutions derived in the previous sections. All examples use
the data in Table 1.
Injection Period. For both cases shown in Fig. 4, two well-defined
straight lines are evident. From the solution (Eqs. 1 and 2), we
see that the first straight line corresponds to the mobility of the virgin
reservoir fluid and has slope M12. The second line has slope 1/2
and corresponds to the mobility in the completely flooded region
where Sw = I-Sor·
Fig. 8 is a plot of the solution in real variables with Data Set
2. The calculated wellbore pressures for isothermal injection tests
are also shown. The uppermost curve is generated with the cold
viscosities, 1 - ' 0 = 7.2 cp and I-'w = 1.2 cp, while the lowermost curve
depicts the result when only hot viscosities are used, 1 - ' 0 =2.4 cp
and I - 'w= 0.4 cp. It is obvious that any estimate of the permeability-
thickness product, kr1kh, 1=0, w , will be greatly in error if the vis-
cosities are not adjusted for temperature. Furthermore, the appar-
ent skin factor caused by the injected fluid bank will be significantly
overestimated, resulting in an equally large underestimate of the
formation damage at the wellbore.
The solid lines in Fig. 9 show the injection profiles including
temperature effects for Data Sets I and 2. The isothermal solution
3500~----------------------------------__,
-- - Nonisothermol solut ion- - Isothermal, cold v iscosities------ Isothermal. hot viscosit ies
3000
/
Set 2
/
/
/
0:,2000
/
1500 /
l0001-~mr~~_n~rT~~~mr~~-n~rT~10" 10--' 10-. 10 10•
t, hours
Fig. 8-Ef fects of assuming temperature-independent viscosi-
t ies during inject ion.
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3 0 , - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ,--- Nonisothermal
25 00000 Isothermal, p.." I J . o > ,
20
o~15
Q.
oo~
oo~Set 2
10
5
10•
to10• 10•0•
Fig. 9-Comparlson of nonlsothermal and Isothermal solu-tions with temperature-adjusted viscosities during Injection.
where the water viscosities are taken at their cold values (l'w=OA
and 1.2 cp) while the hot values of the oil viscosities are used
(1'0=2.0 and 2.4 cp) is also included. From this graph, we see that
the isothermal solution-the solution where the temperature dis-
continuity in saturation is neglected but the temperature-dependent
values of the viscosities are used-will yield both the correct krlkhand a good estimate of the formation damage.
Ifwe take a closer look at Fig. 9, which compares the noniso-
thermal and isothermal solutions, we see that the nonisothermal solu-
tion has a discontinuous time derivative. This discontinuity does
not occur at the point where the solution switches from Eq. 1 to
Eq. 2 but at some later time corresponding to the location of the
step-change in temperature. For Data Sets 1 and 2, this occurs at
the dimensionless t imes 1,535 and 1,280 (about 4 minutes). At this
time, the viscosities used in the solution switch from hot to cold
values, and we get a discontinuous time derivative. This abrupt
change in the mobilities has the same immediate effect as a perme-
ability boundary (increasing permeability in this example). Short-
ly thereafter, the invaded region starts behaving like a positive skin
zone, and the pressure starts to increase more rapidly. This sud-
den change in the mobilities is also apparent in the solution ob-
tained numerically (Fig. 4). The temperature change, however, is
gradual in the simulator because of the finite grid, and the slope
iscontinuous although different from the isothermal case. The major
effect of this peculiarity for the injection case is the shortening of
the two semilog straight lines as seen in Fig. 9. Because nonlinear
regression techniques typically rely on accurate calculations of the
pressure derivatives with respect to the parameters being investigat-
3 0 , - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - ,o 0
00
o 0
00
-- Nonisothermol solution
- - lsotherrnol, / L w o . Jl.ot,
0000 0 lsotberrnot, Ji..-h. / J . o n
. A6 6.6 Isothermal. J . l . w c . J . ' o c
25
.. .20
..o~15
0...
oo
10
oo
Set 2
• 0
• 0
o5
10• 10•
6tO10•
Fig. 11-Comparison of nonlsothermal and Isothermal solu-tions during falloff.
SPE Formation Evaluation, September 1990
25
15
o(f)
Corey rei. perm.
n = 3 - 8
5
o 6 8 104
M
Fig. 10-Apparent skin factor.
ed, this difference in the rate of change may lead to errors if the
isothermal solution is used. This obviously is also a concern if type-
curve-matching techniques are used to estimate reservoir and fluid
parameters.
A closer inspection of the equation for the apparent skin factor
(Eq. 4) shows that it is a function of the saturation-dependent pa-rameters. In particular, i t will be a function of the relative permea-
bility data, which usually are not known in advance. In Fig. 10
we have plotted the apparent skin factor as calculated from Eq. 4 vs.
the mobility ratio, M. The graphs correspond to different values
of the exponent in Corey's 1 6 relative permeability equations. Note
that the functional form of the relative permeability data will de-
pend on the exponent, while the endpoint values are independent
of the exponent. The mobility ratio, M, on the abscissa, however,
is a function of the endpoint values and not of the functional form
of the relative permeability data. From Fig. 10, we see that the
data for the various exponents are very close, in particular for the
lower range of mobility ratios. The interpretation is that if the mo-
bil ity ratio is known, the apparent skin factor can be estimated from
the graph in Fig. 10. Similar graphs can be generated from the
analytical solution for any chosen set of relative permeability equa-tions. Furthermore, because the apparent skin factor does not de-
pend strongly on the functional form of the relative permeability
data, but rather on the endpoint values that can be obtained from
the analysis of the injection and falloff data, we can estimate saand obtain the formation damage (or stimulation), s, as s=St -sa'where SI is the total skin factor obtained by standard analysis. 1 7
10,------------------------------------,
(l)
0...o(f)
--- Nonisothermol solution00000 Numerical solution- - Isothermal solution. JJ-. J .loo,
~(l)
C~oI
Set 2
10' 10• 10•0 •
M o
Fig. 12- Temperature and saturation effects on pressure-de-rivative type curves.
2 9 7
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The injection solution for the constant-pressure, outer-boundary
case (Fig. 5) has a sign change in the slope as the outer boundary
is "felt" in the wellbore pressure. This slope change is described
mathematically by the late-time solution to the constant-pressure
outer-boundary case and the late-time slope- is
1/2(I-M). . (8)
Hence, the slope will change sign at approximately tD =teD' where
teD is given by Eq. A-28, if M> 1. Physically, this can be ex-
plained by comparing the mobility of the reservoir oil with the mo-
bili ty of the injected water. If the cold water is more mobile than
the hot oil, the overall resistance to flow (or injection) will decreaseas water occupies a larger fraction of the reservoir. Eventually,
the pressure must be given by the steady-state solution
PwD= lilreD , (9)
which requires a drop in the wellbore pressure if M> 1.
Finally, to apply the above results to field data, note that the well-
bore storage effect may mask the first straight line. Furthermore,
in a relatively small reservoir, the outer-boundary effects may mask
the second straight line; i.e., the line corresponding to the com-
pletely flooded region at the residual oil saturation. As shown in
Ref. 3, however, the injection data will eventually plot as a straight
l ine with slope 2M7r on a dimensionless Cartesian graph for the
closed-outer-boundary case. If the outer boundary is a constant-
pressure type, the dimensionless late-time data will plot as a semi-
log straight line with slope 'h(l-M). Hence, if the test is longenough, the injection data will give an estimate ofthe water mobil-
ity for the completely flooded region if the system is infinite-acting,
or it will give M if outer-boundary effects mask the infinite-acting
semilog straight line.
Falloff Period. Let us now return to Fig. 6 to investigate the char-
acteristics of the pressure/time curve during the falloff period. Fig.
11presents the analytical solution from Data Set 2. The graph also
includes the solutions with cold and hot viscosity values. As in the
injection case, we see that neglecting the temperature effects on
the viscosity results in gross errors in the calculation of both krlkh
and s. The dashed line in Fig. 11 represents an isothermal analyti-
cal solution of the cold-water and hot-oil viscosit ies. The isother-
mal solution is shifted above the nonisothermal at early times but
will give .the correct values at late times.
A cursory inspection of the falloff data in Fig. 6 suggests that
the pressure/time data will yield two straight lines separated by a
transition period. Intuitively, and from other work, 13,14, 18·21 we
would expect the slope of these straight lines to correspond to the
completely flooded and uninvaded regions, respectively. Fig. 12is a log-log plot of the pressure derivative, d pwD /[ d I n( tD . + atD) /
atD], vs. time. The analytical solution (the solid line) indi~ates that
the falloff data will not plot as a semilog straight line correspond-
ing to Sw =I-So" This is explained by Fig. 3, the saturation pro-
fi le in the reservoir during the falloff period, which shows that the
only place where S w =I-So, is at the sandface. From the Buckley-
Leverett theory, we know that
ro drD I o c r I s (10)
dtD Sw w
or rD21s ocrls to. (11)w w
When the analytical relative permeabili ty curves are used, /'(1-
So,) =0 and hence rDl1-sor =0; i.e ., the only location where the
saturation can be at its endpoint value, I-Sop is at the line source.
This may be an artifact of the analytical solution, but even if the
injected fluid was slightly mobile at the sandface, the fully flooded
region would be very small, and the corresponding straight line
would be too short to be identifiable. If this is the case, why do
the injection data yield the properties of the completely flooded
region? The difference in the wellbore-pressure behavior between
the injection and falloff cases can be explained with the qualitative
concept of a radius of investigation. 22 Remember that the injection
29 8
problem is a moving-boundary problem where the saturation front
propagates into the reservoir with time. Inthe falloff problem, how-
ever, the saturation distribution is approximately stationary for all
times. The wellbore-pressure response reflects the average reser-
voir and fluid properties within the radius of investigation. In the
injection case, the location of the saturation front is proportional
to the radius of investigation and, after a short time, the wellbore
pressure will be dominated by the mobility near the sandface. In
the falloff case, however, the saturation reflected by the wellbore
pressure will be I-So, at atD =0, and then will continuously
decrease to SW ; , as the saturation distribution in Fig. 3 and the
pressure derivative in Fig. 12 show. Hence, if the well is shut inlong enough, the falloff data will plot as a straight line representing
the mobility of the uninvaded region with saturation S w =Sw; '
A second interesting feature of the analytical falloff solution is
the decreasing slope about halfway through the time period investi-
gated in Fig. 12. The solid line corresponds to the nonisothermal
analytical solution, the dashed line is the isothermal solution with
temperature-corrected viscosities, and the circles reflect the numer-
ical solution. The oscillating slope, which is caused by the same
phenomenon, is related to the discontinuous slope in the injection
solution. At early times (small atD) , the radius of investigation en-
compasses the cold region and the mobilities are low. Later, the
average fluid properties reflected by the wellbore pressure will shift
gradually toward their hot or high values in the invaded region,
resulting in a decreasing slope. As the radius of investigation in-
creases further, the propert ies within the radius of investigationeventually will be dominated by the properties in the uninvaded
region-i.e., the hot oil properties. This is also reflected by the
nonisothermal solution obtained numerically. The oscillatory slope
effect, however, is more diffuse in the numerical solution because
of the finite grid system. The resolution in the slope obtained nu-
merically is also sensitive to the timestep size used. Fig. 12 also
shows the isothermal solution for cold-water and hot-oil viscosities.
Although the isothermal solution will represent the init ial and the
straight-line portions of the falloff data correctly, its slope character-
istics are significantly different from the nonisothermal solution.
Hence, in analysis of the falloff data by type-curve methods or non-
linear regression techniques, the temperature effects will be im-
portant and must be accounted for to obtain a good representation
of the solutions. This is particularly true if the falloff test is not
long enough to obtain the semilog straight line.
For the examples presented here, the straight-line portion repre-
senting the uninvaded region will be reached almost one full log
cycle earl ier in the nonisothermal case than in the isothermal case
because the mobili ties used in generating the isothermal solution
give a larger invaded region-i.e., a larger rDBL than the noniso-
thermal solution used in the match.
Finally, the shut-in time required to reach the semilog straight
line of the uninvaded region may be too long to be practically attain-
able. In the example discussed here, the well must be shut in for
about 30 days or about one-third ofthe injection time to get within
5% of the correct slope. This suggests that type-curve-matching
techniques, preferably automated, will be essential for the analysis
of the falloff data.
Conclusions
1. Both temperature and saturation effects must be accounted for
to analyze injection-falloff tests associated with cold-water injection
into hot-oil reservoirs accurately.
2. A combined semilog and type-curve (nonlinear regression)
analysis of field data can provide estimates of the mobilit ies of the
completely flooded and the uninvaded regions; the apparent skin
factor caused by saturation and temperature gradients, and from
this, the formation damage (or stimulation); the size of the uninvaded
region and the distance to the temperature discontinuity; and the
product of the density and heat capacity of the reservoir rock or
one of the fluid phases.
3. Changes in slope caused by nonisothermal pressure transients
may be incorrectly interpreted as reservoir boundaries.
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4. If saturation gradients are ignored, the formation damage can
be grossly overestimated.
5. The solution technique presented is applicable to a wide range
of injection-falloff problems.
Nomenclature
ai = distance to Interface iin multizone problem
an = distance to oil /water interface in multizone problem
C = compressibility, psi - 1
ct = total compressibility, ct=ct(Sw), psi r !
C
to = total compressibili ty of oil region, psi=!C = specific heat capacity, Btu/(ft3 -OF)
d= right-side vector
E1(x) = exponential integral, 1 00
e-U/udu
f = fractional flow of water
f' = df/dSw
I" = d2f/dS~
FA = total mobility, (A o +Aw)/~w' dimensionless
h = formation thickness, ft
Io(x) = modified Bessel function, first kind, order zero
IIx) = modified Bessel function, first kind, order one
k = permeability, md
t:= kro(Swi)
krw = krw(l-Sor)
Ko = modified Bessel function, second kind, order zero
K, = modified Bessel function, second kind, order one.£ -I(u) = inverse Laplace transform of u
M = mobility ratio, ~wc/~oh
P = pressure
PD = dimensionless pressure, 27r~w(P-PR)/q
P R = ini tial reservoir pressure, psi
PwD = dimensionless wellbore pressure, 27r ~w(Pwf -PR)!q
Pwf = wellbore pressure, psi
q = injection rate, BID
r = radius, ft
fe = exterior reservoir boundary radius, ft
rt = radius to temperature discontinuity, ft
rw = wellbore radius, ft
s = skin factor
SBL=
Buckley-Leverett saturation, fractionSD = dimensionless wellbore storage coefficient based on
injected water properties
Sor = residual oil saturation, fraction
Sw = water saturation, fraction
Swf = water saturation at the wellbore sandface, fraction
Swi = initial water saturation, fraction
t = time, hours
to = dimensionless time, ~ot!</>ctor~
teD = dimensionless time at which outer boundary is felt
in wellbore pressure
ilt = shut-in time, hours
T = temperature, OF
TD = dimensionless temperature, (T-T;)I(TR-T[)
T, = injection temperature, OF
TR = initial reservoir temperature, OFu = Laplace transform parameter
X i = unknown constants in multizone problem
y = Boltzmann variable, rB/4tD
YBL = Boltzmann variable evaluated at rBL, r8SL/4tD
'Y = Euler constant , 0.57722 ...
r = matrix
E = qCto!27r~oh
.I= similarity transform, 7rf2h</>!qt
1] = diffusivity ratio, M(ctolct)
~ = endpoint diffusivity ratio, M(ctolctw)
K = 1 I F A 1 1
A = mobility
SPE Formation Evaluation, September 1990
~o = endpoint oil mobility, kkro(Swi)/ J.loh, md/cp
~w = endpoint water mobility, kkrw(l-Sor)/J.lwc, md/cp
J. I = viscosity, cp
~= variable of integration, dimensionless
p = density, lbm/ft '
< /> = porosity, fraction
if i = pressure distribution at shut-in time, dimensionless
Subscripts
a = apparent
BL = Buckley-Leverett
D = dimensionless
f = reservoir rock
i=Region iin falloff solution or injection
1= 0 or w
n =number of regions used in falloff solution
0= oil
oc = oil at injection temperature (cold)
oh = oil at reservoir temperature (hot)
P = production time
r = relative
t = total
w = water
wc = water at injection temperature (cold)
wh = water at reservoir temperature (hot)
1 = invaded zone2 =uninvaded zone
Superscripts
= average
= vector
r = first derivative
" = second derivative
Acknowledgments
This work was supported financially by SUPRI-D, the Stanford U.
Research Consortium for Innovation in Well Test Analysis. Finan-
cial aid to one of the authors from the Norway-America Assn., The
Royal Norwegian Council for Scientific & Industrial Research
(NTNF), Rogaland Research Inst., and Statoil are gratefully ac-
knowledged. Many thanks also to Svein M. Skjaeveland at RogalandU. Center for suggesting the problem and to Takao Nanba for
providing us with the nonlinear regression program he developed
as a student at Stanford U.
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9. Nyhus, E.: "Modelling of Thermal Injection and Falloff Tests ," techni-
cal report , Rogaland Research Inst., Stavanger, Norway (Oct . 1987)
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10. Benson, S.M. et al.: "Analysis of Thermally Induced Permeability En-
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able from SPE Book Order Dept., Richardson, TX.
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Appendix A-Injection Solution
We wiJI derive the injection solution in an infinite reservoir with
the similarity-transform approach. The disadvantage of this approach
is that, although it is exact for a given saturation distribution, it
is limited to a line-source well, and hence, wellbore-storage effects
cannot be included. To include wellbore-storage effects, the solu-tions obtained by the quasistationary approach3,15 should be used.
We limit our discussion to cold-water injection into a hot-oil reser-
voir. The procedure, however, applies to any system for which the
saturation profile can be described a priori.
Infinite Reservoir. Assuming that the reservoir consists of two
different regions separated by a moving discontinuity in fluid satura-
tion, as outlined in Fig. I, we obtain the following mathematical
model for an infinite system with a line-source well.
Governing equations:
10 ( OPD2) OPD2
and -- ro=rr: =--, ro <rD<C:X> ' (A-2)ro orD orD otD BL
where rDBL
=rDBL
(tD)'
1 ) [ Sw(rD ,tD ) ] =1 ) (rD ,tD ) =M(ctol ct),
c t=Swcw+(I-Sw)co +cJ '
and FX[Sw( rD , tD ) ] =F } . .( rD , tD )=(Ao +Aw) /~w'
Initial conditions:
P Dl = PD2=0, tD=O, (A-3)
and rDBL
=0, to =0. . (A-4)
300
Boundary conditions:
lim rD (o PD lo rD ) =-I (A-5)'D-O 1
and lim PD =0. . (A-6)'D -co 2
Moving-boundary conditions:
PD1=PD
2' rD=rD
BL.••.•••.••••••••••••....•••• (A-7)
OPDl 1 OPD2and F x--= ---, rD=rD (A-8)
orD M orDBL
All variables and parameters are dimensionless. PD and PD are
the pressures in the invaded and uninvaded regions,'respecti~ely.
rDBL is the position of the moving interface between the two re-
gions. A second moving discontinuity-the temperature discontinu-
ity-exists in the reservoir. In the above model, this is accounted
for through the time- and space-dependent total mobili ty, F } . . .
From the Buckley-Leverett- theory, we know that the satura-
tion profile is defined by the frontal-advance (mass-conservation)
equation
[rD(drDldtD)]s =ff'ls, (A-9)w w
where f= [(qc to)/(21f ~oh)] , and where f' =dfldSw denotes the
slope of the fractional-flow curve. By integrating Eq. A-9, we obtain
(rD2ItD)S =2ff'ls =constant. (A-IO)
w w
Hence, by transforming the problem from the independent vari-
ables ro and to to the Boltzmann variable y=rl j14tD' we fix the
moving interface and transform the moving-boundary problem into
a composite problem in one variable.
d ( dPD ,) Y dpD l- F xY-- +---=O,O< Y< YBL, (A-II)dy dy 1) dy
d ( dPD2) dpD2- Y-- +Y-- =0, YBL< y <00 ....•...... (A-12)dy dy dy
lim y(dpD,/dy)=-'/z, (A-l3)y-O
lim PD2=0, (A-14)
y-co
PD , = PD2, Y= YBL' (A-IS)
dPDl 1 dpD2and F ) ..--= ---, Y=YBL' (A-16)
dy M dy
where YBL= lh.ffBL=constant. . (A-l7)
The problem now consists of two ordinary linear differential equa-
t ions with variable coefficients. The moving boundary is fixed in
terms of Y, and the solution is obtained by integration.
YB L dy' ( Y' dy" )PD1(y)=V:zj --,exp -j --
Y F xY 0 FX1)
+ M exp(YBL _ j YB L dy )E1(YBL), O ::; Y::; YB L ..... (A-IS)
2 0 FX 1)
M ( J YB L dy )andpD
2(y)=-exp YBL -- E1( y) , YB L: :; Y :: ;C : X> '
2 0 Fx 1)
.................................. (A-19)
Eq. A-IS is singular atthe line source y=O. This singularity is re-
moved by adding and subtracting:
I' f Y BL( - 'liIl ')d ., ( 2012 J e Y Y y. A- )
Y
Furthermore, for a typical water-injection test, the reservoir and
fluid parameters are such that e is small and YBL= ff'12 is of order
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10 - 2 to 10 - 3, while FA 7 J > 1. This makes the exponential terms
in the solution close to one after the first few seconds of injection,
and the fluids in the invaded region essentially behave as if they
were incompressible. Because
y=rj)4tD =c/>cor2/4i..ot= 'hE/', (A-21)
we can change variables to obtain the solution in terms of radius
and time (note that YBL is constant):
PD2 (rD,tD) =(MI2)E I (rji4tD)' to S, rji4YBL (A-22)
and PDI (rD,tD)= '12EIrlJl4~tD) -'12EI(YBL/~)
S r ( 1 ) M+1/2J BL - --I dSw+-EI(YBL)
I-Sor/' FA 2
I-S f"(I) r2+ 'l 2 J or - - -I dSw' tD? __!2_. . (A-23)
Sw(rD.tD) I' FA 4YBL
Evaluating the pressure at the wellbore, we note that for late times
Sw(l,tD)-I-Sor> and the last integral in Eq. A-23 becomes
negligible. At these times, we can also use the approximation
-EI(x)",dnx+" and obtain the wellbore pressure as
pwD=1/2(ln tD+0.80907)+sa+s, (A-24)
where sa is given by
Sa= '12 SBL /': ( _ 1 _ - I )dSw + '12(lnYBL +,,)(l-M). . . (A-25)
I-Sor f FA
Therefore, the wellbore pressure is given by the familiar Theis
solution 1 7 plus an apparent skin factor caused by the saturation
gradient and the propagating temperature and phase discontinuities.
In this expression for the wellbore pressure, we have added a me-
chanical skin factor, s, to account for formation damage or stimu-
lation near the wellbore.
Ifthe relative permeabilities and viscosities of the fluids are such
that the injection results in piston-like displacement, FA =1, 7 J =~,
and removal of the singularity from Eq. A-18 gives the Veriginsolution 1 1,23 :
PDI = '12EIrlJl4~tD) -'12E IYBL/~)
+(MI2)eYBL(l-I/~) EIYBL)' o s ro S, rDBL
(A-26)
and PD2 =(MI2)eYBL(l-I/~) E, (Y), rDBL
S, ro <00 . (A-27)
Finite Outer Boundary. During injection into an infinite reservoir,
only the compressibilit ies in the uninvaded zone are significant. 3
Consequently, it is likely that the outer boundary of a finite cylindri-
cal reservoir will start influencing the wellbore pressure at the time
given by the radius-of-investigation concept->:
t-o = 'Ar~D' (A-28)
The Buckley-Leverett phase-front position at time teD is given by
rbBL =2EfBLteD=(EfBL/2)r~D' (A-29)
Because E is of order 10 -4 to 10 - 5 while filL is of order I, the in-
vaded region is still occupying only a small part of the total reservoir
at the end of the infinite-acting period. Hence, it is expected that
the compressibility in the large uninvaded region also dominates
after the outer boundary is felt in the wellbore pressure.
Verigin II and Ramey 12 discussed approximate solutions for
moving-boundary problems in finite domains. Applying their ideas,
we can add an outer region to obtain an additional moving boundary
in an infinite reservoir. The two outer regions have constant, but
different, mobilities, while the inner region has a saturation gradient
and a temperature discontinuity as before. The interfaces move ac-
cording to mass and energy balances and hence the saturation and
temperature distributions remain constant at any constant value of
the Boltzmann variable. An approximation to a closed outer bound-
ary can be obtained by taking the limit as the mobility in the outer-
SPE Formation Evaluation, September 1990
most region approaches zero while i ts interface is kept at r.o- Theapproximate closed-outer-boundary solution is given by Eqs. 5
and 6.
The constant-pressure outer-boundary approximation is obtained
by taking the limit as the mobility in the outermost region approaches
infinity. The solution to this problem is given by Eqs. 5 and 6
without the exponential terms.
Appendix B-Falloff Solution
Inthe paper we show that the falloff problem can be approximated
by a linear, variable-coefficient problem. This variable-coefficient
problem can be solved by dividing the invaded region into (n+ 1)
regions where the coefficients are evaluated at the average satura-
tion of each region. The governing equations and boundary condi-
tions in dimensionless form for the (n+ lj-region composite
reservoir follow.
Governing equations:
................................... (B-1)
................................... (B-2)
Initial conditions:
PDJj
=v"I(rD)' tD=O (B-3)
and PD2=h(rD), to =0, (B-4)
where 1fi(rD) is the injection solution for the appropriate outer-
boundary condition evaluated at to =i»;
Inner-boundary conditions:
(SDIM)(dPwDldtD)-[rD(iJPD/iJrD)]rD=1 =0 (B-5)
and PwD =[PD1 -srD(iJPD/iJrD)]rD=I' (B-6)
Outer-boundary conditions:
Infinite: lim PD =0. . (B-7)'D-OO 2
Closed: iJPD/iJrD I reD=0. . (B-8)
Constant pressure: PD I r =0. . (B-9)2 eD
Interface conditions:
PDIi
=PD1(i+I)' rD=ai' i=I n-l, (B-IO)
iJPDli iJPDI(i+1) •Mi--= ,rD=ai' 1=1 n-I, (B-ll)
iJrD iJrD
PD1n
=PD2' rD=an, ••••. .. •• .. .. •• •. .. .. •. .. .• . (B-12)
- iJPDln iJPD2andFA i1 M--=--, rD=an, (B-13)
iJrD iJrD
where Mi=F).,iIFAi+I'
We now use the average values for F)"i and 7 J i in each of the n re-
gions. The problem is then a linear, constant-coefficient problem
and can be solved by Laplace transformation. Note that the nonzero
init ial condit ion results in a nonhomogeneous problem in Laplace
space. The two linearly independent, homogeneous solutions in
~place space are KoCJ~ rD) and lo(~ rD), where Ki=(l1
FA illi'The general solution in Laplace space to the nonhomogeneous
problem is then obtained by variation of parameters.
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Authors
Reldar Brumer
Bratvold Is asenior scientistwith IBM EuropeanPetroleum Applica-tion Center InStavanger, wherehe works with com-puter applicationsIn reservoir engi-neering. Heholds a
Bratvold Horne DH. Ing degree Inpetroleum engi-
neering from Rogaland Regional C., an MSdegree In petrole-um engineering from the U. of Tulsa, and an MS degree inmathematics and PhD degree In petroleum engineering fromStanford U. Bratvold currently serves on the Editorial ReviewCommittee. RolandN. Horne Is an associate professor ofpetroleum engineering at Stanford U. He holds BE and PhDdegrees In theoretical and applied mechanics, and a DScdegree in engineering, all from the U. of Auckland, NewZealand. His research Interests are computerized well-test anal-ysis, tracer testing, flow through fractures, geothermal reser-voir engineering, simulation, optimization, and microcomputerapplications. Horne, the 1982 recipient of the SPE Distin-guished Achievement Award for Petroleum EngineeringFaculty, has served on various committees and Is currentlyserving on the Textbook Committee and a Technical Program
Committee for the 1990 Annual Meeting.
P D1i
= K i K o ( ~ r D )I» ~ 1 / t l ( D ! o ( - . r ; ; ; ; ~)d~ai_l
+ K i 1 o ( - . r ; ; ; ; r D )I aj
~ 1 / t 2 m K o ( - . r ; ; ; ; ~)d~r»
30 2
+Ii'ru r D ) I reD ~ 1 / t 2 ( ~ ) K O ( . J ; ~)d~ro
+ X ( n + 1) 1 K O ( . J ; r D ) + X ( n + l ) 2 I O ( . J ; r D ) ' (B-I5)
The constants are determined by applying the boundary and inter-
face conditions. In doing this, we need to solve for the following
(n+ 1) x (n+ 1) block tridiagonal system of equations for the con-
stants Xii and x i 2 , i=1 n+ 1:
rx=d. (B-I6)
The coefficients of matrix r and the right-side vector d depend
on the auxiliary conditions given in Ref. 3.
The well bore pressure in Laplace space now can be obtained by
substituting Eq. B-I4 and its gradient into Eq. B-6 with ro =1. The
inverted wellbore pressure for the case where SD=O is given by
Eq. 7. The last two terms of this solution are inverted numerically
with the Srehfest-" inversion algori thm.
51Metric Conversion Factors
bbl x 1.589873 E-Ol m3
Btu x 1.055056 E+OO kJ
cp x 1.0* E-03 Pa-sft x 3.048* E-Ol m
ft3 x 2.831 685 E-02 m3
OF (OF-32)/1.8 °C
md x 9.869233 E-04 p.m2
psi x 6.894757 E+OO kPa
psi-1 x 1.450377 E-Ol kPa-1
'Conversion factor is exact. SPEFE
Original SPEmanuscript received for reviewOct. 2. 1988. Paper accepted for publication
May 21,1990. Revised manuscript received March 19, 1990. Paper (SPE 18111) first
presented at the 1988 SPEAnnual Technical Conference and Exhibition held in Houston,
Oct. 2-5.
SPE Format ion Evaluat ion, September 1990