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Presented at the 19 th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen, SPE, Edward N. Steadman, John Hamling, John A. Harju Energy & Environmental Research Center Grand Forks, North Dakota Steven Melzer, Melzer Consulting

Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

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Page 1: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Presented at the 19th Annual CO2 Flooding Conference

December 11-13, 2013, Midland, Texas

Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen, SPE,

Edward N. Steadman, John Hamling, John A. Harju

Energy & Environmental Research Center

Grand Forks, North Dakota

Steven Melzer, Melzer Consulting

Page 2: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

How meaningful is MMP?

Does “miscibility” really occur?

Does anything interesting happen below and

above MMP?

What happens as pressure drops below injection

pressure?

Full disclosure: I am an

analytical chemist.

Page 3: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Basic Properties of Three Fluids

O H Not linear

H Permanent dipole moment

Wets minerals well

Solvates polars, but not nonpolars (sort of)

O=C=O Linear

No permanent dipole moment

Polarizable

“Wets” minerals a little

Solvates nonpolars and moderately polar compounds,

(but not very well)

H3C-CH3 (hydrocarbons)

No dipole moment

Not polarizable

Poor at wetting minerals

Solvate nonpolars

Page 4: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

• CO2’s critical T and P are close to “normal” values. Therefore, we operate

with liquid, gaseous, and supercritical states.

• CO2 is “polarizable.” That is, it tries to mimic the polarity of it’s

surroundings (but doesn’t do it very well).

• CO2 is highly compressible, even as a liquid. Accurately controlling mass

flows (etc.) is VERY difficult.

• CO2 shows VERY large J-T cooling and heating. Temperature changes

every time you move CO2, and depressurization can cause freezing.

Significant cooling/heating occurs even without a phase transition (and is

huge with phase change).

Why is CO2 “special?”

Page 5: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Definitions of “Miscibility”

To a chemist: miscible fluids mix in any ratio without

forming two phases (e.g., alcohol and water).

To a PVT lab: 90% of the oil in a 50 foot “slim tube”

of sand came out in 1.2 pore volumes.

To a petroleum engineer: “I don’t care as long as I

get more oil.”

EERC approach (via Rao, et al.): vanishing

interfacial tension.

Page 6: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

MMP by capillary rise.

Patent pending

Sequeira thesis, LSU, 2006 MMP is when there is no interfacial tension between CO2 and oil phases. Based on measuring interfacial tension at various pressures. Requires measured density of

both phases at each P. ($$$) Requires accurate capillary i.d. Must extrapolate MMP from a

curved plot.

EERC modification greatly simplifies the apparatus (<<<$$), and is much faster.

Simply measure capillary height vs. pressure.

Yields linear plots with many data points per plot.

Allows multiple conditions to be evaluated.

Page 7: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

© Energy and

Environmental

Research

Center, 2013

Page 8: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

MMP by capillary rise.

y = -0.0022x + 8.1397R² = 0.9982

y = -0.0015x + 5.4982R² = 0.9967

y = -0.0011x + 3.9581R² = 0.9912

0

1

2

3

4

5

6

7

500 1000 1500 2000 2500 3000 3500

Cap

iill

ary

He

igh

t, m

m

Pressure (psi)

Bakken Crude Oil X, Capillary MMP

RSQ = 0.998 0.997 0.991

MMP = 3738 3632 3628

MEAN SD RSD

3666 62 2%

Page 9: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Method is now rapid (cheap) enough to

ask interesting questions (to me, at least !).

For example:

“How reproducible are the MMP values the lab gives me?”

“How might reservoir oil MMP change during CO2 EOR?”

“How do methane and NGLs affect the performance of recycle

CO2?”

“How important is reservoir temperature in determining MMP?”

“What is the effect of different gases on MMP?”

Page 10: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

MMP values by capillary rise method.

Bakken Crude (110 C)

Reproducibility?

Well 2, trial 1 3564 ± 43

Well 2, trial 2 3674 ± 64

Well 2, trial 3 3429 ± 158

Mean 3556 ± 123

Effect of reservoir T on MMP?

Well 3, 110 C 2685 ± 27

Well 3, 42 C 1316 ± 24

Pure CO2 density ca. 0.4 at both conditions.

Effect of CO2 exposure on MMP?

Well 2, before CO2 exposure 3556 ± 123

Well 2, after 3000 psi CO2 3270 ± 17

Page 11: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

0

2

4

6

8

10

0 500 1000 1500 2000 2500

Cap

illar

y H

eig

ht,

mm

Pressure (psi)

Conventional Reservoir Crude Oil, Capillary Rise MMP with 700 psi Methane

Page 12: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

What is the effect of various gases on MMP?.

(conventional reservoir oil)

0

500

1000

1500

2000

2500

3000

3500

0 200 400 600 800 1000 1200 1400 1600

Cap

illa

ry r

ise

MM

P w

ith

CO

2

CH4 head pressure, psi

Effect of CH4 exposure on CO2 MMP

MEAN SD RSD

3793 111 3%

MMP with pure CH4

pure CO2 MMP = 1450 psi

Page 13: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Bakken crude/CO2

behavior, 110 oC

CO2 pressure

increased from

ambient to 5000 psi,

then reduced back to

ambient.

Does anything interesting happen

above and below MMP?

Page 14: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

© Energy and

Environmental

Research

Center, 2013

Bakken Crude Oil

110 oC (230 F)

MMP = 2800 psi

Page 15: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Conventional crude/CO2 behavior, 42 oC

CO2 pressure increased from ambient to 2300

psi, then reduced back to ambient.

Does anything interesting happen

above and below MMP?

Page 16: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

© Energy and

Environmental

Research

Center, 2013

Page 17: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Where do these “extra”

phases come from?

Page 18: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Dissolved Hydrocarbons Affect the Critical Temperature (a lot)

NIST Standard Reference Database, 23. Version 9.0, “Reference Fluid

Thermodynamic and Transport Properties”

Page 19: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Dissolved Hydrocarbons Affect the Critical Pressure (a lot)

NIST Standard Reference Database, 23. Version 9.0, “Reference Fluid

Thermodynamic and Transport Properties”

Page 20: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Is there MW selectivity in

CO2-mobilized

hydrocarbons—both as

the pressure is rising, and

then falling below

injection pressure?

15 mL oil pressurized for

ca. 1 h between each

sample collection (ca. 5X

at each condition).

Each pressure was tested

with new oil.

Page 21: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

FID

Res

po

nse

Retention Time (Minutes)

CO2-mobilized oil

remaining oil

after CO2 C7

C35

Page 22: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

1500 psi up

2300 psi

2000 psi down

1750 psi down

1500 psi down

1250 psi down

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

% o

f C

7 t

o C

12 H

C v

s

tota

l H

C

CO2 selectively mobilizes lighter hydrocarbons,

especially at lower pressures. (Heavier hydrocarbons will be left in the reservoir.)

Page 23: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

1500 psi up

2300 psi 2000 psi down 1750 psi

down 1500 psi down

1250 psi down

0

20

40

60

80

100

120

mg

to

tal h

yd

rocarb

on

per

g C

O2

Mobilized oil almost doubles from MMP (1450 psi) to

injection pressure.

Some oil is lost as pressure is reduced to MMP, then

much is lost below MMP.

Page 24: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Observations and Preliminary

Conclusions

1. Capillary rise method allows rapid determinations of MMP under

varying conditions, and with various fluids.

2. Slim tube is a powerful tool to design EOR in conventional

reservoirs, but it does not measure “miscibility.” (And may not apply

to unconventional plays?)

3. “MMP” is not a magic number. Lots of oil mobilization occurs below

MMP. Lots of oil deposition occurs above MMP.

4. True miscibility does not happen. However, formation of an extra

CO2/oil mobile phase does occur. (A functional definition of multiple

contact miscibility.)

Page 25: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Future Experiments (near term)

1. Comparison with slim rube results using live oil.

2. Effects of hydrocarbons (and nitrogen) in recycle CO2.

3. Changes in produced oil MMP during EOR.

4. Determining the effect on MMPs of different flare gas

compositions.

5. Try to better understand the multi-phase behavior of oil

and CO2 below, at, and above MMP.

6. Apply these insights to unconventional plays like the

Bakken.

Page 26: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Acknowledgments

This material is based upon work supported by the U.S. Department of

Energy, National Energy Technology Laboratory under Award Nos. DE-

FC26-08NT43291 and DE-FC26-05NT42592.

The support of Marathon Oil Company; TAQA North, Ltd.; Continental

Resources, Inc.; and the North Dakota Industrial Commission (Oil and Gas

Research Council) is also gratefully acknowledged as is the support of the members of the PCOR Partnership Program.

Page 27: Steven B. Hawthorne, Charles D. Gorecki, James A. Sorensen ......Dec 07, 2013  · Presented at the 19th Annual CO 2 Flooding Conference December 11-13, 2013, Midland, Texas Steven

Disclaimer

This presentation was prepared as an account of work sponsored by an agency of the

United States Government. Neither the United States Government, nor any agency

thereof, nor any of their employees, makes any warranty, express or implied, or assumes

any legal liability or responsibility for the accuracy, completeness, or usefulness of any

information, apparatus, product, or process disclosed or represents that its use would not

infringe privately owned rights. Reference herein to any specific commercial product,

process, or service by trade name, trademark, manufacturer, or otherwise does not

necessarily constitute or imply its endorsement, recommendation, or favoring by the

United States Government or any agency thereof. The views and opinions of authors

expressed herein do not necessarily state or reflect those of the United States

Government or any agency thereof.