tom wilson department of geology and geography west virginia university morgantown, wv

33
TOM WILSON DEPARTMENT OF GEOLOGY AND GEOGRAPHY WEST VIRGINIA UNIVERSITY MORGANTOWN, WV Developing a strategy for CO 2 EOR in an unconventional reservoir using 3D seismic attribute workflows and fracture image logs Tom Wilson, Department of Geology and Geography ACTIVITY & ELEMENT 2.651.070.001.511 FAULT AND FRACTURE ZONE DETECTION AND REDUCED ORDER FRACTURE MODEL DEVELOPMENT FOR RISK ASSESSMENT

Upload: holden

Post on 27-Jan-2016

34 views

Category:

Documents


1 download

DESCRIPTION

Developing a strategy for CO 2 EOR in an unconventional reservoir using 3D seismic attribute workflows and fracture image logs. ACTIVITY & ELEMENT 2.651.070.001.511 FAULT AND FRACTURE ZONE DETECTION AND REDUCED ORDER FRACTURE MODEL DEVELOPMENT FOR RISK ASSESSMENT. Tom Wilson - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

TOM WILSONDEPARTMENT OF GEOLOGY AND

GEOGRAPHYWEST VIRGINIA UNIVERSITY

MORGANTOWN, WV

Developing a strategy for CO2 EOR in an unconventional reservoir using 3D seismic attribute

workflows and fracture image logs

Tom Wilson, Department of Geology and Geography

ACTIVITY & ELEMENT 2.651.070.001.511

FAULT AND FRACTURE ZONE DETECTION AND REDUCED ORDER FRACTURE MODEL

DEVELOPMENT FOR RISK ASSESSMENT

Page 2: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Overview

Tom Wilson, Department of Geology and Geography

1) Reservoir characterization is developed using analysis of 3D seismic and fracture image logs and seismic attribute workflows for fracture driver development to distribute fracture intensity throughout the reservoir.

2) Analysis of fracture image logs reveals that the dominant open fracture trend within the reservoir is coincident with present-day SHmax.

3) Outcrop analogs and satellite observations are used to develop model distributions of fracture length, height and spacing

4) Fracture intensity driver is developed using a combination of seismic discontinuities and directional curvature (orthogonal to SHmax).

5) Reservoir compartmentalization is interpreted.

6) A strategy for CO2 EOR is proposed that incorporates placement of injection and production laterals along compartment boundaries and roughly orthogonal to SHmax.

Page 3: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Location of study area and reservoir structure

Tom Wilson, Department of Geology and Geography

Page 4: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Dip line views of structure

Tom Wilson, Department of Geology and Geography

Basement

MadisonTensleep

Goose Egg

AlcovaMorrison

Wall Creeks

Page 5: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Tom Wilson, Department of Geology and Geography

Fracture characterization using image logs. Open fractures in seal, reservoir and in total

SHmax

Page 6: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Open fracture trends in the reservoir by well and for all wells

Tom Wilson, Department of Geology and Geography

SHmax

Page 7: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

280’Fracture ZoneFracture Zone

Field analogs of seismic discontinuities

Page 8: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Defining fracture parameters-Fracture height distribution

Tom Wilson, Department of Geology and Geography

Length (m)

1 10 100

Num

ber

1

10

100

Fracture Height (m) High Intensity Zone (right)

power = -1.62

R2=0.96

Heights >2m

Length (m)1 10

Num

ber

1

10

100

Fracture Height (m) High Intensity Zone (left)

power = -1.61

R2=0.96

Heights >2m

Length (m)

1 10

Num

ber

1

10

100

Fracture Height (m) Middle Low Intensity Zone

power = -2.18

R2=0.86

Heights >2m

Page 9: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Higher power implies lower probability of higher fractures

Tom Wilson, Department of Geology and Geography

-1.61 -2.18 -1.62

Page 10: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Spacing distributions estimated in Freemont Canyon

Tom Wilson, Department of Geology and Geography

Spacing (meters)10

Num

ber

1

10

100HI Fracture Zone 3

power = -1.28

R2=0.98

power = -2.8

R2=0.97

power = -0.47

R2=0.95

Spacings (meters)10 100

Num

ber

1

10

100

1000Entire Exposure

power = -0.43

R2=0.95

power = -1.55

R2=0.99

Page 11: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Variations of fracture intensity in the reservoir

Tom Wilson, Department of Geology and Geography

Zone

FZ1 IntZ FZ2 IntZ

Inte

nsit

y

0.00

0.01

0.02

0.03

0.04

0.05

0.06

0.07Fracture intensity by vertical zone

Selected layers (top-to-bottom)

L1 L2 L3 L4 L5 L6 L7 L8 L9 L10

Inte

nsit

y

0.00

0.01

0.02

0.03

0.04

0.05

0.06

0.07

0.08Variations of fracture intensity through the Tensleep

average = 0.042with 95% confidence limits from 0.031 to 0.054

Page 12: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Fracture length distributions from World view ½ meter resolution imagery

Tom Wilson, Department of Geology and Geography

Outcrop viewed from opposite side of canyon

Page 13: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Local fractures mapped using WorldView imagery

Tom Wilson, Department of Geology and Geography

Page 14: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Fracture length distributions(from WorldView imagery)

Tom Wilson, Department of Geology and Geography

Length(m)

10

Num

ber

1

10

100

1000Fracture Length Distribution (L>4m)

power = -1.85

R2=0.98

Page 15: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Seismic discontinuity length distribution

Tom Wilson, Department of Geology and Geography

Length (meters)100 1000

Num

ber

1

10

100

1000Discontinuity Lengths

Length (meters)100 1000

Num

ber

10

100

Discontinuity Lengths

power = -2.29

250 < length <650

Page 16: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Aperture distributions – log normal with some power law behavior for apertures above ~0.05 mm

Tom Wilson, Department of Geology and Geography

log10 Electrical Aperture-4.0 -3.5 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5 0.0

Freq

uenc

y

0

5

10

15

20

25

30

log10 Hydraulic Aperture-3.5 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5 0.0

Freq

uenc

y

0

5

10

15

20

25

30

35

A B

log10 hydraulic aperture-3.0 -2.5 -2.0 -1.5 -1.0 -0.5

log

cum

ulat

ive

num

ber

0.0

0.5

1.0

1.5

2.0

2.5

log10 electrical aperture-3.5 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5

log

cum

ulat

ive

num

ber

0.0

0.5

1.0

1.5

2.0

2.5

Slope = -1.72

R2=0.98

-1.3

Slope = -1.73

R2=0.97

-1.25

A. B.

Page 17: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Seismic discontinuity detection workflow

Tom Wilson, Department of Geology and Geography

A variety of post-stack processing workflows have been developed as part of this research. Multiple workflows are usually tested and compared. Some example discontinuity detection workflows are shown at left.

Often, discontinuities can be significantly enhanced simply by taking the absolute value of the seismic trace or taking a trace derivative followed by taking it’s absolute value.

Low pass filtering is sometimes required to reduce high-frequency noise.

Discontinuity detection workflow components

Page 18: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Comparison of amplitude and enhanced seismic data

Tom Wilson, Department of Geology and Geography

In general, data prep is an iterative process

Page 19: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

The derivative enhances high frequency content and introduces a 90o phase shift

Tom Wilson, Department of Geology and Geography

Frequency

0 20 40 60 80 100

Am

plitu

de

0.000

0.004

0.008

0.012

0.016

Signal Spectrum

Frequency

0 20 40 60 80 100

Am

plit

ude

0

500

1000

1500

Spectrum of the Derivative

Page 20: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Absolute value doubles apparent spectral content

Tom Wilson, Department of Geology and Geography

Frequency

0 50 100 150 200 250

Am

plitu

de0.000

0.001

0.002

0.003

0.004

0.005

0.006

0.007Spectrum of Absolute Value of the Derivative

Frequency

0 50 100 150 200 250

Am

plitu

de

0.0000

0.0005

0.0010

0.0015

0.0020

0.0025Spectrum of Absolute value of Signal Amplitude

Page 21: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Extracted discontinuities

Tom Wilson, Department of Geology and Geography

Page 22: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

NE oriented discontinuities are interpreted to arise from right lateral transpressional shear

Tom Wilson, Department of Geology and Geography

S1 Fault

Page 23: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Incorporating possible influence of curvature on dominant fracture aperture

Tom Wilson, Department of Geology and Geography

Maximum directional curvature orthogonal to the dominant open fracture set & SHmax.

SHmax

Page 24: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Potential compartmentalization within the reservoir suggested by production distribution

Tom Wilson, Department of Geology and Geography

Log 10 yr cumulative production5 yr cumulative production

(Smith, 2008)

Page 25: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Volume probe through combined discontinuity and directional curvature volume

Tom Wilson, Department of Geology and Geography

Page 26: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Composite driver development

Tom Wilson, Department of Geology and Geography

• Discontinuities and directional curvature were extracted from 3D seismic.

• Conditional statements were used to zero-out high-scoring discontinuities and isolate positive curvature.

• Only regions with positive curvature were incorporated in the intensity driver.

• Discontinuity and curvature parameters were upscaled into a model grid and combined to produce an intensity driver that could be used to control the distribution of fractures in the reservoir.

Page 27: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Intensity distribution

Tom Wilson, Department of Geology and Geography

Page 28: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Drilling strategy

Tom Wilson, Department of Geology and Geography

CO2 injection

lateral

Production lateral

SHmax

SHmax

Dominant open

fracture trend

injector

producer

Page 29: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Workflow integration

Tom Wilson, Department of Geology and Geography

Determine Orientation of Shmax

from Drilling Induced fractures

or Breakouts

Analyze Distributions of Dominant Open Fracture Trends

Examine directional Curvature at Scale

of Seismic Discontinuities

Derived 3D Discontinuity

Volume

Identify potential for compartmentalization

Manipulate Attribute Values to Highlight Low and High Permeability regions in Reservoir

Upscale and Combine to Provide Fracture Intensity

Driver

Incorporate Analysis of Field Data to Help

Constrain Length, Height and Spacing

Distributions

Estimate Aperture Distribution

Develop DFN

Field analogImage log3D seismic

Continued from Discontinuity

Detection Workflow

Page 30: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Novel aspects of the approach

Tom Wilson, Department of Geology and Geography

1) The new driver addresses the possibility that NE oriented higher-score discontinuities may represent low permeability zones that could compartmentalize the reservoir; and,

2) use of maximum directional curvature orthogonal to the more prevalent N76oW hinge-oblique open fracture set in the reservoir focuses on that curvature component that could enhance apertures of the dominant fractures set. Curvature in this direction acts in tandem with the orientation of SHmax inferred from induced fractures observed in the fracture image logs to enhance permeability in the N76W trend.

Page 31: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Recent paper and meeting preparations

Tom Wilson, Department of Geology and Geography

Developing a strategy for CO2 EOR in an unconventional reservoir using 3D seismic attribute workflows and fracture image logs: Paper submitted for presentation at the Annual SEG meeting, Sept., 2013, Thomas H. Wilson, National Energy Technology Laboratory and West Virginia University; Valerie Smith, Schlumberger Carbon Services, and Alan Brown, Schlumberger NExT, 5p.

Characterization of Tensleep reservoir fracture systems using outcrop analog, fracture image logs and 3D seismic: Abstract submitted for presentation at the Annual AAPG Rocky Mountain Section meeting, Thomas H. Wilson, National Energy Technology Laboratory and West Virginia University; Valerie Smith, Schlumberger Carbon Services, and Alan Brown, Schlumberger NExT

Page 32: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Future work1. carry through to simulation, or

Tom Wilson, Department of Geology and Geography

Develop DFN in FRACGEN

Field analog

Image log analysis

Seismic analysis

Devise methods for incorporating results from

seismic analysis into FRACGEN model

Bring in production data

Bring in reservoir parameters (Smith, 2008)

Incorporate in ROM

Simulation and history matching

Reservoir Engineering

Bring in additional field observations: Alcova and Granite Mountain Anticlines

Page 33: Tom Wilson Department of Geology and Geography West Virginia University Morgantown, WV

Future work2. carry through to simulation in alternative unconventional reservoir

Tom Wilson, Department of Geology and Geography

The reservoir characterization workflows presented here can be extended to other reservoirs as needed to

support NETL priorities.

DFN’s, although not presented as part of today’s discussions, have been developed for numerous

reservoirs. The methodologies are adaptable and can be readily applied to new settings given sufficient data.