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(1)

Basic Concepts in Well Testing

for Reservoir Description

Patrick Corbett

Hamidreza Hamdi

Alireza Kazemi

1

The Ball Room, Station Hotel, Guild Street, Aberdeen

Wednesday 6

th

April 2011

(2)
(3)

Description of a well test

DD i BU

P

P P t

P

P t

P

t

=

=

∆ =

- ( )

( ) - (

0)

1

. During a well test, a transient pressure response is created by

a temporary change in production rate.

2

. For well evaluation less than two days.

reservoir limit testing several months of pressure data

Flow rate @ Surface

Pressure @ Down-hole

3

(4)

Well test objectives

• Exploration well

– On initial well, confirm HC existence, predict a first

production forecast (DST: fluid nature, Pi, reservoir

properties

• Appraisal well

– Refine previous interpretation, PVT sampling, (longer

test: production testing)

• Development well

– On production well, satisfy need for well treatment,

interference testing, P

(5)

Well test Types

• Draw down

– Open the well with constant rate decreasing bottom hole pressure

Build Up test

– Shut-in the well  increasing bottom hole pressure

• Injection/ fall-off test ( different fluid type)

– The fluid is injected  increasing Bottom hole pressure

– Shut-in the well  decreasing the bottom hole pressure

• Interference test / pulse test

– Producing well  measure pressure in another shut-in well away from

the producer communication test

• Gas well test

– Back pressure , Isochronal test , modified isochronal test  well

productivity, AOFP, Non-Darcian skin.

(6)

Information obtained from well

testing

• Well Description

– For completion interval (s),

– Production potential (PI), and skin

• Reservoir Description

– “Average” permeability (horizontal and vertical)

– Heterogeneities(fractures, layering, change of Prop.)

– Boundaries (distance and “shape”)

– Pressure (initial and average)

• Note: Well Description and Reservoir Description

(7)

Methodology

• The inverse problem

• Model recognition (S)

– Well test models are different from the geomodels

in the sense that they are dynamic models and

also it’s an average model.

Q vs t

Reservoir

P vs t

(8)

Example: Interference test

1. Create signal at producing well

2. Measure the signal at both wells

Observation well

:

1. The signal will be received with a delay

2. The response is smaller

(9)

Fluid Flow Equation

(10)

concepts

• Permeability and porosity

• Storativity and Transmissibility

• Skin

• Wellbore storage

• Radius of investigation

• Superposition theory

• Flow regimes

(11)

Concepts-Definitions

• Permeability:

– The absolute permeability is a measure of the capacity of

the medium to transmit fluids. Unit: md (10

-12

m

2

)

• Transmissibility

• Storativity

• Diffusivity (Hydraulic diffusivity)

• AOF

• PI

Kh

T

µ

=

t

S

=

ϕ

c h

T

S

η

=

11

(12)

Fluid flow equation: ingredients

• Conservation of mass ( continuity equation)

• EOS, defining the density and changes in density with

pressure

• Transport equation ( Darcy’s law: experimental, or

Navier-Stoke)

v

t

ρ

ρφ

∇ • = −

(

)

(

)

c

t

ρ

ρ

=

1

v

= −

1

K

•∇

P

(13)

Fluid flow equation: radial case

• Continuity + Darcy: in radial coordinate (isotropic)

• Assumptions:

Radial flow into a well opened over entire thickness , single

phase, slightly compressible fluid, constant viscosity ,

ignoring the gravity, constant permeability and porosity

( )

r

r k

P

r r

r

t

ρ

ϕρ

µ

=

1

P

c P

r

r r

r

k

t

ϕµ

 =

1

13

(14)

Solution to radial diffusivity equation

• Inner/outer Boundary conditions:

| 2 w r w p q B r khr µ π ∂ =

1. Constant Pressure

boundary, p=pi @re

2. Infinite reservoir

p=pi @ ∞

3. No flow boundary

∂p/∂r =0 @ re

(15)

Unsteady- Infinit acting reservoirs(radial

flow regime): DD

• Finite diameter well without WBS- infinite acting reservoir

USS,PSS,SS?

∂P/∂t=f(x,t) USS (Well test)

∂P/∂t=cte PSS (boundary)

∂P/∂t=0  SS( aquifer)

(

u tD

)

J u Y ur

(

Y u J ur

)

q

P r t

e

du

T

u

J u

Y u

π π

∞ −

=

+

2 1 0 1 0 2 2 2 0 1 1

( ) (

)

( )

(

)

2

( , )

1

2

( )

( )

2

1

( , )

2

2

4

i

q B

cr

P r t

P

Ei

kh

kt

µ

ϕµ

π

= −

2

162.6

( )

log

3.23 0.87

i wf t w

q B

kt

P

P

t

S

Kh

c r

µ

ϕµ

=

+

15

(16)

Radius of investigation

The radius of investigation

ri tentatively

describes the distance that the pressure

transient has moved into the formation.

Or it’s the radius beyond which the flux

should not exceed a specified fraction

or percentage of the well bore flow rate

0.032

i t

k t

r

c

ϕµ

=

Can we

use the radius of investigation to

calculate the pore volume and reserve?

1. Based on radial homogeneous if

fracture ?

2. Is it a radius or volume?

3. How about gauge resolution?

4. Which time we are talking about?

5. How about a close system?

(17)

Radius of investigation

Rate time Q=0, T-dt -Q, t Rate time Q, T-dt -Q, dt

Injection

Observation

Pressure drop , at “r” time

17

(18)

Skin Pressure Drop

Skin Pressure drop: higher pressure drop

near the well bore due to mud filtrate,

reduced K , improved K, change of flow

streamlines, fluid composition change,….

It is one of the most important parameter

used in production engineering as it could

refer to a sick or excited well and leads to

additional work-over operations.

(19)

Q(surface)

Q(Sand face)

Q(wellbore)

q

t

log

∆P

,

log

∆P

Pure

WBS

Transition

Radial FR

In surface production or shut in the surface rate is controlled

However due to compressibility of oil inside the well bore we have difference

between sandface production and surface production

(

)

24

qB

P

t

t

C

∆ ∆ =

Pure WBS

It can affect the inner boundary condition and make the solution more

complicated

0 wb

V

C

c V

P

= −

=

Wellbore Storage

(20)

Superposition

• Effect of multiple well

– ∆P

tot@well1

=∑∆P

wells @well1

• Effect of rate change

• Effect of boundary

• Effect of pressure change

1 ( 1 0) ( 2 1)

...

( 2 1)@ i tot q q q q q tn t

P

P

P

P

− − − − −

= ∆

+ ∆

+ + ∆

tot

act

image

P

P

P

(21)

Radius of investigation:superposition

Rate time Q=0, T-dt -Q, t Rate time Q, T-dt -Q, dt

Injection

Observation

Pressure drop , at “r” time

(

)

2 , , 1 , 2 2 , 1 2 , 2 948 , 2 max

948

70.6(

)

948

70.6(

)

1694.4

948

t r t r t r t t r t t r t c r kt r t t

P

P

P

c r

q B

P

Ei

kh

kt

c r

q B

P

Ei

kh

k t

t

P

e

kht

c r

t

k

ϕµ

ϕµ

µ

ϕµ

µ

µ

ϕµ

= ∆

+ ∆

=

=

− ∆

=

=

21

(22)

Fluid flow equation : complexity

• Linear , bilinear , radial, spherical

• Depends on the well geometry, and reservoir

heterogeneities

• Change the fluid flow equation and the solution

• The fluid heterogeneities affect the diffusivity

(23)

Derivative Plots

(24)

Derivative plot

Reservoir Pore

volume

Transient

PSS

SS

Transient

PSS

SS

Tr

ans

iti

on

Tr

ans

iti

on

(25)

Derivative plot : Example1

Structure effect on well testing

25

(26)

Derivative plot

Example2 : Radial Composite

K

2

<K

1

2 2 1 1

m

k

m

=

k

m

2

m

1

Equivalent

Homogeneous

Composite

ΔP

Log(t)

ΔP &

ΔP’

(27)

Example:

Derivative plot : Example3 :

Horizontal Well Testing

1 Vertical radial S

w

2 Linear flowS

pp

, S

w

3 Later radial flow 

S

T

=f(S

w

,S

pp

,S

w

,S

G

,…)

Linear flow:

(28)
(29)

Practical Issues

• Inaccurate rate history

• Shut-in times

• Gauge resolution

• Gauge drift

• Changing wellbore storage

• Phase segregation

• Neighbouring well effect

• Interference

• Tidal effects

• Mechanical noise

• Perforation misties

(30)

Uncertain parameters

Complex permeability / porosity (higher order of heterogeneities)

Complex thickness

Complex fluid

Wellbore effect?

Any deviation from assumption

New phenomena ?

Gauge resolution

Measurements? Correct rate history

Numerical- Analytical

Core-Log values ? Seismic?

Averaging process?

Layering response?

Test design? Sensitivities? Multiple models ?

(31)

Rock Description

(32)

Core data evaluation

• Summary numbers

(statistics) for comparison

with well tests

• Variability measures

• How do the numbers

relate to the geology

• How good are the

summary numbers

• How representative are

the numbers

(33)

33

Measures of Central Tendency

• Mean - population parameter

• Average - the estimator of the population mean

• Arithmetic average

• Geometric average

• Harmonic average

k

N

k

ar

i

i

N

=

=

1

1

( )

k

N

k

geom e i i N

=

=

exp

1

log

1

k

N

k

har

i

i

N

=

=

1

1

1

k

geom

k

i

i

N

N

=

=

1

1

(34)

Differences between averages

Measures of heterogeneity

Each permeability average has a

different application

in

reservoir engineering

(35)

35

• Used to estimate effective property for

certain arrangements of permeability

• Horizontal (

bed parallel flow)

• Vertical and Horizontal

(random)

• Vertical

(bed series flow)

Remember these assumptions….

not the application!!

k

ar

k

geom

k

har

k

ar

k

har

(36)

Comparing the well test and core perms.

• Need to

consider the

nature and

scale of the

layering in the

volume of

investigation of

a well test

-k

ar

-k

geom

-k

har 1-5ft 5-10ft 10-50ft

(37)

37

Well test comparison example

• Well A: Kar =400md ktest = 43md kgeom = 44md

• Well B: Kar =600md ktest = 1000md

Well A

Well B

Core plug data

(38)

Permeability distributions in well

Well A

Well B

Major

channels

Minor

channels

(39)

39

10k

55m

XX10

WELL A

XX20

XX55

35m

.01

0 2000 4000

WELL B

Minor

Channel

Major

Channels

LogK

LinK

LogK

LinK

Triassic

Sherwood Sandstone

Braided fluvial system

(Toro Rivera, 1994,SPE 28828, Dialog article)

Well test comparison example

WELL A

(40)

Core plug petrophysics

Coun

t

0 10 20 30 40 50 60 70 -4 -6 -2 0 2 4 6 8 10 12 0 10 20 30 40 50 60 -4 -6 -2 0 2 4 6 8 10

WELL A

WELL B

Arith. av.: 400mD

Geom. av: 43mD

Arith. av.: 625mD

Geom. av: 19.8mD

Permeability distributions similar

Permeability averages similar

(41)

41

WT log-log plot

P

WELL A

ETR MTR LTR

r

Time

WELL B

ETR MTR LTR

P

r

ETR: Linear flow

MTR: Radial flow (44mD)

Negative skin

LTR: OWC effect

ETR: Radial flow?

MTR: Radial flow (1024 mD)

Small positive skin

LTR: Fault?

Well test response very different

Geological interpretation?

(42)

Well Test Informed Geological Interpretation

WELL B

LogK

LinK

WELL A

LogK

LinK

Many small channels

Limited extent

Few large channels

More extensive

“Channel effective flow”

(43)

43

‘Well A’

‘Well B’

(44)

Coefficient of variation

• Normalised

measure of

variability

Homogeneous core plugs

Aeolian wind ripple (1)

Aeolian grainflow (1)

Shallow mar. low contrast lam.

Fluvial trough-cross beds (2)

Fluvial trough-cross beds (5)

M ix'd aeol. wind rip/grainf.(1)

Lrge scale x-bed dist chan (5)

Shallow marine SCS

Aeolian interdune (1)

Shallow marine Rannoch Fm

Shallow mar. Lochaline Sst (3)

Shall. mar. high contrast lam.

Shallow marine HCS

Heterolithic channel fill

Beach/stacked tidal Etive Fm.

Dist/tidal channel Etive ssts

Fluv lateral accretion sst (5)

Sh. mar.rippled micaceous sst

Crevasse splay sst (5)

S.North Sea Rotliegendes Fm (6)

Carbonate (mix pore type) (4)

Homogeneous

Heterogeneous

Very heterogeneous

0 < Cv < 0.5 Homogeneous

0.5 < Cv < 1 Heterogeneous

1 < Cv Very Heterogeneous

Cv

SD

k

ar

=

(45)

45

Sample sufficiency

• Representivity of sample sets

for a tolerance (P) of 20%

and 95% confidence level

• N

zero

or N

o

= optimum no. of data points

• Where N

s

= actual no. of data points

• P

s

gives the tolerance

(

)

N

0

=

10

Cv

2

(

)

P

Cv

N

s

s

=

200

(46)

Sample sufficiency

• Representivity of sample sets

for a tolerance (P) of 20%

and 95% confidence level

• N

zero

or N

o

= optimum no. of data points

• Where N

s

= actual no. of data points

• P

s

gives the tolerance

(

)

N

0

=

10

Cv

2

(

)

P

Cv

N

s

s

=

200

(47)

47

Zheng et al., 2000

(48)

Lorenz plot

• Order data in

decreasing k/φ and

calculate partial

sums

0

Fj

k h

k h

j

j

j

j

i i

i

i

=

=

=

1

1

j

φ

h

0

0

1

1

Fj

Transmissivity

Φj

Storativity

I

J

J

(49)

49

Lorenz plot

• Order data in

decreasing k/φ and

calculate partial

sums

0

Fj

k h

k h

j

j

j

j

i i

i

i

=

=

=

1

1

Cj

h

j

j

j

j

i i

i

i

=

=

=

φ

φ

h

1

1

0

0

1

1

Fj

Transmissivity

Φj

Storativity

Lc = 0

Homogeneity

J

J

I

I

(50)

Lorenz plot >> Lorenz Coefficient

• Order data in

decreasing k/φ and

calculate partial

sums

0

Fj

k h

k h

j

j

j

j

i i

i

i

=

=

=

1

1

j

φ

h

0

0

1

1

Fj

Transmissivity

Φj

Storativity

Lc = 0.6

Heterogeneity

(51)

51

Unordered Lorenz Plot

(52)

Example Lorenz Plots

Lorenz Plot 0.10 0.20 0.30 0.40 0.50 0.60 0.70 0.80 0.90 1.00 kh Series1

Modified Lorenz Plot

0.10 0.20 0.30 0.40 0.50 0.60 0.70 0.80 0.90 1.00 kh Series1 SPEED ZONES

(53)

53

Hydraulic Units and Heterogeneity

( Ellabed et al., 2001)

Rotated Modified

Lorenz Plot

(54)
(55)

55

104 102 100 10 -2 10 -4 10 -6 .001 .01 .1 1

Rannoch anisotropy

Sample volume (m3)

kv/ kh

Probe

Plug

Plug averages

WB Formation SCS HCS

Probe average

Lamina

Bed

Parasequence

Grain

Scale dependant anisotropy

Estimate of kv/kh anisotropy depends on the

scale of application

(56)

Ebadi et al., 2008

(57)

Putting it all together

(58)

Conclusions

• Well testing

– Model driven

– Simple Models

– Averaging process

• Reservoir Description

– Heterogeneous

– Scale dependant

– Upscaling challenge

K x h = 600mDft Where h = 60ft Which K = 10mD???

??

(59)

References

Bourdet 2002, Well-test Analysis: The use of advanced interpretation models, Elsevier

Corbett and Mousa, 2010, Petrotype-based sampling to improved understanding of the variation of Saturation Exponent, Nubian Sandstone Formation, Sirt Basin, Libya, Petrophysics, 51 (4), 264-270

Corbett and Potter, 2004, Petrotyping: A basemap and atlas for navigating through permeability and porosity data for reservoir comparison and permeability prediction, SCA2004-30, Abu Dhabi, October.

Corbett, Ellabad, Egert and Zheng, 2005, The geochoke test response in a catalogue of systematic geotype well test responses, SPE 93992, presented at Europec, Madrid, June

Corbett, Geiger, Borges, Garayev, Gonzalez and Camilo, 2010, Limitations in the Numerical Well Test Modelling of Fractured Carbonate Rocks, SPE 130252, presented at Europec/EAGE, Barcelona, June

Corbett, Hamdi and Gurev, Layered Reservoirs with Internal Crossflow: A Well-Connected Family of Well-Test Pressure Transient Responses, submitted to Petroleum Geoscience, Jan, abstract submitted to EAGE/Europec Vienna, June 2011

Corbett, Pinisetti, Toro-Rivera, and Stewart, 1998, The comparison of plug and well test permeabilities, Advances in Petrophysics: 5 Years of Dialog – London Petrophysical Society Special Publication.

Corbett, Ryseth and Stewart, 2000, Uncertainty in well test and core permeability analysis: A case study in fluvial channel reservoir, Northern North Sea, Norway, AAPG Bulletin, 84(12), 1929-1954.

Cortez and Corbett, 2005, Time-lapse production logging and the concept of flowing units, SPE 94436, presented at Europec, Madrid, June. Ellabad, Corbett and Straub, 2001, Hydraulic Units approach conditioned by well testing for better permeability modelling in a North Africa oil

field, SCA2001-50, Murrayfield, 17-19 September, 2001

Hamdi, Amini, Corbett, MacBeth and Jamiolahmady, Application of compositional simulation in seismic modelling and numerical well testing for gas condensate reservoirs, abstract submitted to EAGE/Europec Vienna, June 2011

Hamdi, Corbett and Curtis, 2010, Joint Interpretation of Rapid 4D Seismic with Pressure Transient Analysis, EAGE P041 Houze, Viturat, and Fjaere, 2007 : Dynamic Flow Analysis, Kappa.

Legrand, Zheng and Corbett, 2007, Validation of geological models for reservoir simulation by modeling well test responses, Journal of

Petroleum Geology, 30(1), 41-58.

Matter, 2004 : Well Test Interpretation, Presentation by FEKETE , 2004

Robertson, Corbett , Hurst, Satur and Cronin, 2002, Synthetic well test modelling in a high net-gross outcrop system for turbidite reservoir description, Petroleum Geoscience, 8, 19-30

Schlumberger , 2006, : Fundamental of Formation testing , Schlumberger Schlumberger ,2002: Well test Interpretation, Schlumberger Toro-Rivera, Corbett and Stewart, 1994, Well test interpretation in a heterogeneous braided fluvial reservoir, SPE 28828, Europec, 25-27

October.

Zheng, Corbett, Pinisetti, Mesmari and Stewart, 1998; The integration of geology and well testing for improved fluvial reservoir

References

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