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A LABORATORY STUDY OF FOAM FOR EOR IN NATURALLY FRACTURED RESERVOIRS
William R. RossenBander. I. AlQuaimi
2
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Backround
• Gas‐injection EOR can displace nearly all oil contacted, but sweep efficiency is very poor, because of reservoir heterogeneity, gravity segregation and viscous instability
• Foam can help fight all three causes of poor gas sweep• In reservoir rock, foam shows two flow regimes:• High‐Quality regime: result of foam collapse at limiting Pc
• Low‐Quality regime: thought to reflect invariant bubble size, roughly size of pores
• Fractured reservoirs have especially poor sweep efficiency
• Foam generation in fractures is uncertain
3
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Goals and Strategy
• Develop rules for foam generation and properties in fractures that would apply broadly to fractures of different apertures, different geometries.
• Conduct studies in a medium where foam can be directly observed. • Conduct experiments on samples as large as possible (avoid entrance effects).
• Obtain a variety of samples with very different fracture apertures, permeabilities, and scales of roughness
Implementation• Conduct experiments in model fractures between glass plates, one
roughened, one smooth • large size, cost effective, and available in different geometries
4
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Model Fracture aperture size
5
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Model Fracture Correlation Length
6
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Experimental Setup
7
Initial Study: Trapping and Mobilization in Fractures
• Trapping and mobilization of bubbles is a key to foam mobility.
• Trapping and mobilization of non‐wetting phase in rock is represented as function of capillary number, [kp/]
• In fractures, permeability k is primarily a function of average aperture, but trapping depends on roughness
• What is best definition of capillary number for trapping in fractures?
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CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Desaturation‐experiment example (16x10 cm image)
Trapping and Mobilization of gas (no foam)
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CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Trapping and Mobilization
𝑁𝑘 𝛻𝑃𝛾𝑐𝑜𝑠𝜃
Conventional Nca
New Nca
𝑁𝛻𝑃𝑘𝛾
122
𝑑𝑑
𝐿𝑔𝑑
1
1 𝑑𝑑
0,00
0,20
0,40
0,60
0,80
1,00
1,20
1,E‐05 1,E‐04 1,E‐03 1,E‐02
Normalized
air saturatio
n
Nca
Sample 1
Sample 2
Sample 3
Sample 4
Sample 5
0,00
0,20
0,40
0,60
0,80
1,00
1,20
1,0E‐03 1,0E‐02 1,0E‐01 1,0E+00
Normalized
air saturatio
n
Nca
Sample 1
Sample 2
Sample 3
Sample 4
Sample 5
Force balance on trapped ganglion leads to new Nca for fractures
10
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Generation and Propagation
1. In-situ Foam Generation
2. Pre-generated Foam
11
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
0,0
2,0
4,0
6,0
8,0
10,0
12,0
0,0 20,0 40,0 60,0 80,0
Q, m
l/min
ΔP, mbar
P2
P3
• First model : narrow aperture, regular pattern• Single‐phase water injection to determine
hydraulic aperture• Two inner ports used for pressure gradient• The hydraulic aperture estimated to be 66 µm
40 cm
9 cm9 cm
12
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
1. In‐situ Foam Generation• Can we generate foam, in-situ, in a
fracture?
• How effective is it in reducing gas mobility in the fracture?
13
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
1. In‐situ Foam Generation• Can we generate foam, in-situ, in a
fracture?Foam generated in our model fracture by mechanisms similar to “3D” porous media
14
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
2.2X1.5 cm image, fg = 0.25, and ut = 0.0021 m/s0.65X0.40 cm image, fg = 0.37, and ut = 0.0021 m/s
Snap‐off Leave‐Behind
15
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
1
2 3 4
0.150 s0.117 s0.083 s
0.0 s
1
0.84X0.64 cm image, fg = 0.88 ut = 0.0021 m/s, and t = 0.15s
Lamella Division
16
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
1. In‐situ Foam Generation• Can we generate foam, in-situ, in a
fracture?
• How effective is it in reducing gas mobility in the fracture?
17
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
~0 72278
2389
0
500
1000
1500
2000
2500
3000
Gas Injection (Nowater)
Water Injection(No gas)
Water + Gas (fg =0.37)
Foam (fg = 0.37)
Pressure gradien
t, mbar/m
ut = 0.0021 m/s
Foam Injection Benchmark
18
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Quality Scan
1
23
4
567
8
0
500
1000
1500
2000
2500
3000
0,00 0,20 0,40 0,60 0,80 1,00
Pressure gradien
t ,mba
r/m
fg
(Fixed ut = 0.0021 m/s)
19
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Bubble Size Analaysis (fixed ut = 0.0021 m/s)
fg = 0.25
0.37
0.52
0.75
0.88
0.96
Images captured during stabilized pressure drop 27 cm from injection port
Gaswater
Effect of Gas Fraction (Foam Quality)
20
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Bubble Size Analaysis (fixed ut = 0.0021 m/s)
Foam Bubble Size Analaysis (fixed ut = 0.0021 m/s)
71 2
3
4
5 6
0
8
0,00
0,05
0,10
0,15
0,20
0,25
0,30
0,35
0,000
0,005
0,010
0,015
0,020
0,025
0,030
0,035
0,040
0,045
0,00 0,20 0,40 0,60 0,80 1,00
AverageBu
bbleSize, m
m2
µ app, p
a s
fg
Foam mobility inversely related to bubble size
21
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Bubble Size Analaysis (fixed ut = 0.0021 m/s)Foam Bubble Size Analaysis
fg = 0.37 vt = 0.0021 m/s Surfactant Concentration 1% wt
0.8 X 0.77 cm Images
321
Inlet Outlet
Distance from in let, mm 20 120 270
Average bubble size, mm2 0.250 0.138 0.081
Bubble size, std. dev. , mm2 0.205 0.125 0.056
Number of bubbles 165 217 303
Bubble sizes evolve along fracture: “entrance effect”
22
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
2. Pre‐generated Foam
1. Fine‐textured foam
2. Coarse‐textured foam
23
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
0,000
0,005
0,010
0,015
0,020
0,025
0,030
0,035
0,040
0,045
0,00 0,20 0,40 0,60 0,80 1,00
µ app, p
a s
fg
In‐situ Generated Pre‐generated 400 Micron Pre‐generated 7 Micron
vt = 0.0021 m/s
{might local‐equilibrium value lie between pre‐generated and in‐situ‐generated?
24
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
y = 0,0001x‐0,899y = 0,0003x‐0,806
y = 0,0002x‐0,815
y = 0,0002x‐0,765
0,01
0,1
0,001 0,01
µ app, p
a s
Total Superficial Velocity Ut, m/s
fg = 0.24fg = 0.51fg = 0.88fg = 0.96
shear‐thinning rheology
25
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Low Quality
High QualityOsterloh & Jante,(1992)
two flow regimes
26
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
1.0X0.86 cm image, fg = 0.37and ut = 0.0021 m/s
9.1X8.9 cm image, fg = 0.92and ut = 0.0021 m/s
Flow
dire
ction
high‐quality regime: caused by intermittent generation
27
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Foam Generation and Propertiesin Five Different Model Fractures
28
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Model Fracture aperture size
29
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Model Fracture Correlation Length
30
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Section 1 2 3 4
Distance from inlet, mm 60 150 230 360
Average bubble size, mm2 2.48 0.66 0.60 0.53
Bubble size, std. dev. , mm2 7.84 0.57 0.48 0.36
Number of bubbles 37 160 176 194
1 3 42
Sample 5: fg = 0.46, ut = 0.0007 m/s; black is gas and white is water. Image size 1.6X1.6 cm.
31
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Sample 4 fg = 0.70, ut = 0.0016 m/s; black is gas and white is water. Image size 1.4X1.0 cm.
Section 1 2 3 4
Distance from inlet, mm 60 150 230 360
Average bubble size, mm2 NA 0.36 0.26 0.14
Bubble size, std. dev. , mm2 NA 0.47 0.40 0.16
Number of bubbles NA 207 216 479
2 3 4
32
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
0
200
400
600
800
1000
1200
1400
0 0,2 0,4 0,6 0,8 1
Pressure gradien
t,mba
r/m
fg
0.0077 m/s
0.0047 m/s
0.0032 m/s
0.0016 m/s
0
100
200
300
400
500
600
700
800
0 0,2 0,4 0,6 0,8 1
Pressure gradien
t, mba
r/m
fg
0.0036 m/s
0.0022 m/s
0.0015 m/s
0.0007 m/s
two foam‐flow regimes
NOT!
33
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Summary of all fractures: Mobility Reduction Factors
Sample 4
Sample 2
Sample 5
Sample 3
Sample 1
0
10
20
30
40
50
60
70
80
0 200 400 600 800
MRF
dH, µmaperture
34
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Summary of all fractures: Mobility Reduction Factors
787
2031
563
34
23
799137
162116
0
1000
2000
3000
4000
5000
6000
0 200 400 600 800
Lp, µ
m
dH, µm
Samples 1, 2 and 3 Sample 4 (increasing dH)Sample 5 (Increasing dH)
MRF
aperture
Correlation Length of R
oughne
ss
35
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
Increase aperture at fixed roughness: two cases
36
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
0
100
200
300
400
500
600
0 0,2 0,4 0,6 0,8 1
Pressure gradien
t ,mba
r/m
fg
dH = 114.9 µm dH = 144.7 µm dH = 170.1 µm
Sample 5
Wide aperture
37
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
• Images are captured in section 4, fixed fg of 0.45, and bubbles at the edges are excluded• Images are identical in size (1.1X0.86 cm)
dH, µm 114.9 144.70 170.10
Average bubble size , mm2 0.468 0.74 0.943
Standard Deviation, mm2 0.343 0.438 1.02
No of bubbles 120 55 54
Larger aperture bigger bubbles
38
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
0
200
400
600
800
1000
1200
0 0,2 0,4 0,6 0,8 1
Pressure gradien
t ,mba
r/m
fg
dH = 51.0 µm dH = 71.9 µm dH = 206.9 µm
Wide aperture
39
CharacterizedFractures
Trapping & Mobilization
Foam Generation
VelocityEffect
RoughnessEffect
Aperture Effect Gravity Effect
• Images are captured in section 4, fixed fg of 0.45, and bubbles at the edges are excluded• Images are identical in size (1.7X1.5 cm)
dH 51.00 71.90 206.9
Average bubble size, mm2 0.097 0.148 1.37
Standard deviation, mm2 0.114 0.133 1.32No. of bubbles 972 750 78
Larger aperture bigger bubbles
40
Summary and Conclusions
• Foam generation was observed in the model fractures, mainly by capillary snap‐off and lamella division.
• Hydraulic aperture alone is not enough to determine foam‐generation and mobility reduction. Roughness scale, both laterally and vertically, plays a significant role. Slit‐shaped throats & wet conditions favor snap‐off.
• Bubble size was inversely related to pressure gradient, as expected• Shear‐thinning behaviour was observed as velocity increases.• Two flow regimes were observed in 2 cases out of 3. However, the
high‐quality regime evidently reflected reduced and fluctuating generation, not collapse of foam at limiting capillary pressure Pc*. Bubbles were smaller than pore size in low‐quality regime.
• With fixed roughness, pressure gradient decreases with increasing hydraulic aperture. Foam bubbles became larger as aperture increases.
41
Reports and Publications
• The dissertation has details on both the Nca and foam experiments and analysis and is available online. Search for AlQuaimi at
https://www.tudelft.nl/en/library/
• Journal and Conference Publications• AlQuaimi, B. I., Rossen, W. R. (2017), New capillary number definition
for displacement of residual nonwetting phase in natural fractures.Geophys. Res. Lett., 44 (11), 5368–5373.
• AlQuaimi, B. I., Rossen,W. R. (2017), Capillary Desaturation Curve for Residual Nonwetting Phase in Natural Fractures. Accepted by SPE Journal.
• AlQuaimi, B. I., and Rossen, W. R., "Characterizing Foam Flow in Fractures for Enhanced Oil Recovery," presented at the EAGE IOR Symposium, Stavanger , April 24‐27, 2017.
Thank YouFor Your Attention
42