US2014288836A1PendingUtilityA1
Method for determining the inflow profile of fluids of multilayer deposits
Assignee: SCHLUMBERGER TECHNOLOGY CORPPriority: Oct 23, 2011Filed: Oct 25, 2012Published: Sep 25, 2014
Est. expiryOct 23, 2031(~5.3 yrs left)· nominal 20-yr term from priority
E21B 47/103E21B 49/08E21B 43/14E21B 49/0875E21B 2049/085
39
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Claims
Abstract
A method for determining the profile of fluids inflowing into multi-zone reservoirs provides for a temperature measurement in a wellbore during the return of the wellbore to thermal equilibrium after drilling and determining a temperature of the fluids inflowing into the wellbore from each pay zone after perforation at an initial stage of production. Specific flow rate for each pay zone is determined by a rate of change of the measured temperatures.
Claims
exact text as granted — not AI-modified1 . A method for determining profile of fluid inflow from multi-zone reservoirs into a wellbore comprising:
measuring a temperature in the wellbore during a wellbore-return-to-thermal-equilibrium time after drilling, perforating the wellbore, determining a temperature of the fluids inflowing into the wellbore from each pay zone at an initial stage of production, and determining a specific flow rate for each pay zone by a rate of change of the measured temperatures.
2 . The method of claim 1 , wherein the temperature of the fluids inflowing into the wellbore from the pay zones is determined by a direct measurement of temperature of the fluids inflowing into the wellbore from each pay zone, and a specific flow rate of each pay zone is determined by the formula
Q
i
=
4
π
χ
·
a
·
h
1
·
(
T
.
in
,
i
T
.
s
-
1
)
,
where Q i is a flow rate of the ith pay zone,
{dot over (T)} s is a rate of temperature recovery in the wellbore before perforation,
{dot over (T)} in,i is a rate of temperature variation of the fluid inflowing into the wellbore from the ith pay zone at the initial stage of production,
h i is a thickness of the ith pay zone,
a is a thermal diffusivity of the reservoir,
χ
=
c
f
·
ρ
f
ρ
r
·
c
r
,
ρ f c f is a volumetric heat capacity of the fluid,
ρ r c r =φ·ρ f c f +(1−φ)·ρ m c m is a volumetric heat capacity of the rock saturated with the fluid,
ρ m c m is a volumetric heat capacity of a rock matrix,
φ is a porosity of the reservoir.
3 . The method of claim 1 , wherein the wellbore-return-to-thermal-equilibrium time is 5-10 days.
4 . The method of claim 1 , wherein the temperature of the fluids inflowing into the wellbore from each pay zone at the initial stage of production is measured within 3-5 hours after start of production.
5 . The method of claim 1 , wherein the temperature of the fluids is determined by sensors installed on a tubing string above each perforated interval, a specific flow rate of a lower pay zone is determined by the formula
Q
1
=
4
π
χ
·
a
·
h
1
·
(
T
.
1
T
.
s
-
1
)
,
where Q 1 is a flow rate of the lower zone,
{dot over (T)} s is a rate of temperature recovery in the wellbore before perforation,
{dot over (T)} 1 is a rate of temperature change of the fluid inflowing into the wellbore from the pay zone at the initial stage of production as measured above the lower perforated interval,
h 1 is a thickness of the lower pay zone,
a is a thermal diffusivity of the reservoir,
χ
=
c
f
·
ρ
f
ρ
r
·
c
r
,
ρ f c f is a volumetric heat capacity of the fluid,
ρ r c r =φ·ρ f c f +(1−φ) ρ m c m is a volumetric heat capacity of the rock saturated by the fluid,
ρ m c m is a volumetric heat capacity of the rock matrix,
φ is a porosity of the reservoir, and a specific flow rate of overlying pay zones is determined by temperatures measured by the sensors installed on the tubing string, using the flow rates determined for the underlying pay zones.
6 . The method of claim 5 , wherein the wellbore-return-to-thermal-equilibrium time is 5-10 days.
7 . The method of claim 5 , wherein the temperature of the fluids inflowing into the wellbore from each pay zone at the initial stage of production is measured within 3-5 hours after start of production.Cited by (0)
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