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SPE DISTINGUISHED LECTURER SERIES
is funded principally
through a grant of the
SPE FOUNDATION
The Society gratefully acknowledges
those companies that support the program
by allowing their professionals
to participate as Lecturers.
And special thanks to The American Institute of Mining, Metallurgical,
and Petroleum Engineers (AIME) for their contribution to the program.
Oilfield Scale:
A New Integrated Approach
to Tackle an Old Foe
Dr Eric J. Mackay
Society of Petroleum Engineers
Distinguished Lecturer 2006-07 Lecture Season
Flow Assurance and Scale Team (FAST)
Institute of Petroleum Engineering
Heriot-Watt University
Edinburgh, Scotland
Eric.Mackay@pet.hw.ac.uk
Slide 3 of 100
Outline
1) The Old Foe
a) Definition of scale
b) Problems caused
c) Common oilfield scales
d) Mechanisms of scale formation
e) Location of scale deposition
2) The New Approach
a) The new challenges
b) Proactive rather than reactive scale management
c) Effect of reservoir processes
3) Conclusions
Formation
Water (Ba)
• ••
•
•
•
•••••
Sea Water
(SO4)
Ba2+ + SO4
2-  BaSO4(s)
Slide 4 of 100
Outline
1) The Old Foe
a) Definition of scale
b) Problems caused
c) Common oilfield scales
d) Mechanisms of scale formation
e) Location of scale deposition
2) The New Approach
a) The new challenges
b) Proactive rather than reactive scale management
c) Effect of reservoir processes
3) Conclusions
Formation
Water (Ba)
• ••
•
•
•
•••••
Sea Water
(SO4)
Ba2+ + SO4
2-  BaSO4(s)
Slide 5 of 100
1a) Definition of Scale
 Scale is any crystalline
deposit (salt) resulting from
the precipitation of mineral
compounds present in water
 Oilfield scales typically
consist of one or more types
of inorganic deposit along
with other debris (organic
precipitates, sand, corrosion
products, etc.)
Slide 6 of 100
1b) Problems Caused
 Scale deposits
 formation damage (near wellbore)
 blockages in perforations or gravel pack
 restrict/block flow lines
 safety valve & choke failure
 pump wear
 corrosion underneath deposits
 some scales are radioactive (NORM)
 Suspended particles
 plug formation & filtration equipment
 reduce oil/water separator efficiency
Slide 7 of 100
Examples - Formation Damage
quartz grains
scale crystals block
pore throats
Slide 9 of 100
Examples - Flow Restrictions
Slide 10 of 100
Examples - Facilities
separator
scaled up
and after
cleaning
Slide 11 of 100
1c) Common Oilfield Scales
Name Formula Specific Solubility
Gravity cold water other
(mg/l)
Common Scales
barium sulphate BaSO4 4.50 2.2 60 mg/l in 3% HCl
calcium carbonate CaCO3 2.71 14 acid soluble
strontium sulphate SrSO4 3.96 113 slightly acid soluble
calcium sulphate CaSO4 2.96 2,090 acid soluble
calcium sulphate CaSO4.2H2O 2.32 2,410 acid soluble
sodium chloride NaCl 2.16 357,000 (insoluble in HCl)
Sand Grains
silicon dioxide SiO2 2.65 insoluble HF soluble
Some Other Scales
Iron Scales: Fe2O3, FeS, FeCO3
Exotic Scales: ZnS, PbS
SPE 87459
Slide 12 of 100
1d) Mechanisms of Scale Formation
 Carbonate scales precipitate due to DP
 wellbore & production facilities
 Sulphate scales form due to mixing of incompatible brines
 injected (SO4) & formation (Ba, Sr and/or Ca)
 near wellbore area, wellbore & production facilities
 Concentration of salts due to dehydration
 wellbore & production facilities
Ca2+
(aq) + 2HCO-
3(aq) = CaCO3(s) + CO2(aq) + H2O(l)
Ba2+
(aq) (Sr2+or Ca2+) + SO4
2-
(aq) = BaSO4(s) (SrSO4 or CaSO4)
Slide 13 of 100
seawater
formation brine
1e) Location of Scale Deposition
b c d e
f g
i
h
b
a
SPE 94052
Slide 39 of 100
Outline
1) The Old Foe
a) Definition of scale
b) Problems caused
c) Common oilfield scales
d) Mechanisms of scale formation
e) Location of scale deposition
2) The New Approach
a) The new challenges
b) Proactive rather than reactive scale management
c) Effect of reservoir processes
3) Conclusions
Formation
Water (Ba)
• ••
•
•
•
•••••
Sea Water
(SO4)
Ba2+ + SO4
2-  BaSO4(s)
Slide 40 of 100
2a) The New Challenges
 Deepwater and other harsh environments
 Temperature and pressure
 Residence times
 Access to well
 Production chemicals compatibility
 Inhibitor placement
 Complex wells (eg deviated, multilateral)
 Well value & scale management costs
 Deepwater
 Downhole instrumentation
 Rig hire vs Sulphate Reduction Plant
Slide 43 of 100
Access to Well
 Subsea wells
 difficult to monitor
brine chemistry
 deferred oil during
squeezes
 well interventions
expensive (rig hire)
bullhead (placement)
 squeeze campaigns
and/or pre-emptive
squeezes
Slide 45 of 100
Inhibitor Placement in Complex Wells
 Where is scaling brine
being produced?
 Can we get inhibitor
where needed?
 wellbore friction
 pressure zones (layers /
fault blocks)
 damaged zones
 Options:
 bullhead (from platform /
FPS via subsea chemical
injection or test line)
 bullhead + divertor
 Coiled Tubing (CT) from rig
 Combined stimulation /
inhibitor treatments
Ptubing head
Fault
Shale
Pcomp 1
Pcomp N
Presv 1
Presv N
Slide 46 of 100
Well Value & Scale Management Costs
 Deepwater wells costing US$10-100 million (eg GOM)
 Interval Control Valves (ICVs) costing US$0.5–1 million
each to install
 good for inhibitor placement control
 susceptible to scale damage
 Rig hire for treatments US$100-400 thousand / day
 necessary if using CT
 deepwater may require 1-2 weeks / treatment
 cf. other typical treatment costs of US$50-150 thousand /
treatment
 Sulphate Reduction Plant (SRP), installation and
operation may cost US$20-100 million
Slide 47 of 100
2b) Proactive Rather Than Reactive
Scale Management
 Scale management considered during CAPEX
 Absolute must:
good quality brine samples and analysis
 Predict
 water production history and profiles well by well
 brine chemistry evolution during well life cycle
 impact of reservoir interactions on brine chemistry
 ability to perform bullhead squeezes:
• flow lines from surface facilities
• correct placement
 Monitor and review strategy during OPEX
Slide 48 of 100
2c) Effect of Reservoir Processes
EXAMPLE 1 Management of waterflood leading
to extended brine mixing at producers
(increased scale risk for producers)
EXAMPLE 2 In situ mixing and BaSO4
precipitation leading to barium stripping
(reduced scale risk for producers)
EXAMPLE 3 Ion exchange and CaSO4
precipitation leading to sulphate stripping
(reduced scale risk for producers)
EXAMPLE 4 Impact of reservoir pressures
(correct / incorrect placement profiles)
Slide 49 of 100
SPE 80252
Extended Brine Mixing at Producers
EXAMPLE 1
Slide 50 of 100
SPE 80252
Field M (streamline model)
This well has been
treated > 220 times!
Extended Brine Mixing at Producers
EXAMPLE 1
Slide 51 of 100
Barium Stripping (Field A)
% seawater
Barium(mg/l)
Dilution line
SPE 60193
EXAMPLE 2
Slide 52 of 100
Barium Stripping (Theory)
 Seawater (containing SO4) mixes with
formation water (containing Ba)
leading to BaSO4 precipitation in the
reservoir
 Minimal impact on permeability in the
reservoir
 Reduces BaSO4 scaling tendency at
production wells
SPE 94052
EXAMPLE 2
Slide 53 of 100
Barium Stripping (Theory)
Ba2+
Rock
SO4
2-
1) Formation water (FW): [Ba2+] but negligible [SO4
2-]
FW
(hot)
EXAMPLE 2
Slide 54 of 100
Barium Stripping (Theory)
Ba2+
SO4
2-
2) Waterflood: SO4
2- rich seawater displaces Ba2+ rich FW
Rock
FWSW
(cold) (hot)
EXAMPLE 2
Slide 55 of 100
Barium Stripping (Theory)
Ba2+
SO4
2-
Rock
3) Reaction: In mixing zone Ba2+ + SO4
2- → BaSO4
FWSW
(cold) (hot)
BaSO4
EXAMPLE 2
Slide 56 of 100
Barium Stripping (Theory)
0
100
200
300
400
500
600
700
800
900
0 20 40 60 80 100
seawater fraction (%)
[Ba](mg/l)
0
500
1000
1500
2000
2500
3000
[SO4](mg/l)
Ba
Ba (mixing)
SO4
SO4 (mixing)
•Large reduction in
[Ba]
•Small reduction in
[SO4]
(SO4 in excess)
•Typical behaviour
observed in many
fields
EXAMPLE 2
Slide 57 of 100
Barium Stripping (Model)
0
10
20
30
40
50
60
70
80
90
0 20 40 60 80 100
% seawater
bariumconcentration(ppm)
Field A - actual
Field A - dilution line
Field A - modelled
EXAMPLE 2
Slide 63 of 100
Barium Stripping (Field G)
a) water saturation b) mixing zone
c) BaSO4
deposition (lb/ft3)
SPE 80252
Field G (model)
EXAMPLE 2b
Slide 64 of 100
Barium Stripping (Field G)
0
50
100
150
200
250
0 500 1000 1500 2000 2500
time (days)
bariumconcentration(ppm)
0
500
1000
1500
2000
2500
3000
sulphateconcentration(ppm)
Ba
Ba (no precip)
SO4
SO4 (no precip)
[Ba] at well when no
reactions in reservoir
[Ba] at well when
reactions in reservoir
Field G (model)
EXAMPLE 2b
Slide 65 of 100
Barium Stripping (Field G)
0
50
100
150
200
250
0 20 40 60 80 100
% seawater
bariumconcentration(ppm)
Field B - observed
Filed B - dilution line
Field B - modelled
deep reservoir + well/near
well mixing
deep reservoir mixing
0
50
100
150
200
250
0 20 40 60 80 100
% seawater
bariumconcentration(ppm)
Field B - observed
Filed B - dilution line
Field B - modelled
deep reservoir + well/near
well mixing
deep reservoir + well/near
well mixing
deep reservoir mixingdeep reservoir mixing
Field G (model & field data)
EXAMPLE 2b
Slide 71 of 100
Sulphate Stripping (Theory)
 Seawater (with high Mg/Ca ratio) mixes with
formation water (with high Mg/Ca ratio)
leading to Mg and Ca exchange with rock to
re-equilibrate
 Increase in Ca in seawater leads to CaSO4
precipitation in hotter zones in reservoir
 Minimal impact on permeability in the
reservoir
 Reduces BaSO4 scaling tendency at
production wells
SPE 100516
EXAMPLE 3
Slide 72 of 100
Ion Exchange
Ca
Mg
Ca
Mg
C
C
0.50
Cˆ
Cˆ

FW: 0.077
SW: 3.2
Rock: 0.038
CCa Ca in solution
CMg Mg in solution
ĈCa Ca on rock
ĈMg Mg on rock
Gyda FW (mg/l)
30,185
2,325
SW (mg/l)
426
1,368
EXAMPLE 3
Slide 73 of 100
Sulphate Stripping (Theory)
Ba2+
Rock
SO4
2- Ca2+ Mg2+
1) Formation water: [Ca2+] and [Mg2+] in equilibrium with rock
FW
(hot)
EXAMPLE 3
Slide 74 of 100
Sulphate Stripping (Theory)
Ba2+
SO4
2- Ca2+ Mg2+
2) Waterflood: [Ca2+] and [Mg2+] no longer in equilibrium
Rock
CWSW
(cold) (hot)
EXAMPLE 3
Slide 75 of 100
Sulphate Stripping (Theory)
Ba2+
SO4
2- Ca2+ Mg2+
3) Reaction 1: Ca2+ and Mg2+ ion exchange with rock
Rock
CWSW
(cold) (hot)
EXAMPLE 3
Slide 76 of 100
Sulphate Stripping (Theory)
Ba2+
SO4
2- Ca2+ Mg2+
4) Reaction 2: In hotter zones Ca2+ + SO4
2- → CaSO4
Rock
CWSW
(cold) (hot)
CaSO4
EXAMPLE 3
Slide 77 of 100
Modelling: Ion Exchange
0
5,000
10,000
15,000
20,000
25,000
30,000
35,000
0 20 40 60 80 100
seawater fraction (%)
[Ca](mg/l)
0
500
1,000
1,500
2,000
2,500
3,000
3,500
[Mg](mg/l)
Ca
Ca (mixing)
Mg
Mg (mixing)
As for field data:
•Large reduction
in [Mg]
•No apparent
change in [Ca]
EXAMPLE 3
Slide 78 of 100
Modelling: Sulphate Stripping
0
100
200
300
400
500
600
700
800
900
0 20 40 60 80 100
seawater fraction (%)
[Ba](mg/l)
0
500
1000
1500
2000
2500
3000
[SO4](mg/l)
Ba
Ba (mixing)
SO4
SO4 (mixing)
As for field data:
•Small reduction
in [Ba]
•Large reduction
in [SO4]
(No SO4 at
< 40% SW)
EXAMPLE 3
Slide 84 of 100
Impact of Reservoir Pressures on
Placement
 Question for new subsea field under
development:
Can adequate placement be achieved
without using expensive rig
operations?
EXAMPLE 4
Slide 85 of 100
Placement (Field D)
-200
-100
0
100
200
300
400
500
0 200 400 600 800
well length (m)
flowrate(m3/d)
prior to squeeze
shut-in
INJ 1 bbl/m
INJ 5 bbl/m
INJ 10 bbl/m
1 year after squeeze
production
injection
(squeeze)
• Good placement along length of well during treatment (> 5 bbls/min)
• Can squeeze this well
SPE 87459
EXAMPLE 4
Slide 86 of 100
Placement (Field D)
production
injection
(squeeze)
• Cannot place into toe of well by bullhead treatment, even at 10 bbl/min
• Must use coiled tubing (from rig - cost), or sulphate removal
-600
-500
-400
-300
-200
-100
0
100
0 200 400 600 800
well length (m)
flowrate(m3/d)
prior to squeeze
shut-in
INJ 1 bbl/m
INJ 5 bbl/m
INJ 10 bbl/m
1 year after squeeze
SPE 87459
EXAMPLE 4
Slide 99 of 100
3) Conclusions
 Modelling tools may assist with understanding of where
scale is forming and what is best scale management option…
 identify location and impact of mixing
 evaluate feasibility of squeeze option (placement)
 calculate chemical requirements
… thus providing input for economic model.
 Particularly important in deepwater environments, where
intervention may be difficult & expensive
 But – must be aware of uncertainties…..
 reservoir description
 numerical errors
 changes to production schedule, etc.
… so monitoring essential.
Slide 100 of 100
Acknowledgements
 Sponsors of Flow Assurance and Scale
Team (FAST) at Heriot-Watt University:
Baker Petrolite, BG Group, BWA Water
Additives, BP, Champion Technologies,
Chevron, Clariant, ConocoPhillips,
Halliburton, M I Production Chemicals,
Nalco, Hydro Oil & Energy, Petrobras,
REP, Rhodia, Shell, Solutia, Statoil, Total

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SPE-DL slides EricMackayALL

  • 1. SPE DISTINGUISHED LECTURER SERIES is funded principally through a grant of the SPE FOUNDATION The Society gratefully acknowledges those companies that support the program by allowing their professionals to participate as Lecturers. And special thanks to The American Institute of Mining, Metallurgical, and Petroleum Engineers (AIME) for their contribution to the program.
  • 2. Oilfield Scale: A New Integrated Approach to Tackle an Old Foe Dr Eric J. Mackay Society of Petroleum Engineers Distinguished Lecturer 2006-07 Lecture Season Flow Assurance and Scale Team (FAST) Institute of Petroleum Engineering Heriot-Watt University Edinburgh, Scotland Eric.Mackay@pet.hw.ac.uk
  • 3. Slide 3 of 100 Outline 1) The Old Foe a) Definition of scale b) Problems caused c) Common oilfield scales d) Mechanisms of scale formation e) Location of scale deposition 2) The New Approach a) The new challenges b) Proactive rather than reactive scale management c) Effect of reservoir processes 3) Conclusions Formation Water (Ba) • •• • • • ••••• Sea Water (SO4) Ba2+ + SO4 2-  BaSO4(s)
  • 4. Slide 4 of 100 Outline 1) The Old Foe a) Definition of scale b) Problems caused c) Common oilfield scales d) Mechanisms of scale formation e) Location of scale deposition 2) The New Approach a) The new challenges b) Proactive rather than reactive scale management c) Effect of reservoir processes 3) Conclusions Formation Water (Ba) • •• • • • ••••• Sea Water (SO4) Ba2+ + SO4 2-  BaSO4(s)
  • 5. Slide 5 of 100 1a) Definition of Scale  Scale is any crystalline deposit (salt) resulting from the precipitation of mineral compounds present in water  Oilfield scales typically consist of one or more types of inorganic deposit along with other debris (organic precipitates, sand, corrosion products, etc.)
  • 6. Slide 6 of 100 1b) Problems Caused  Scale deposits  formation damage (near wellbore)  blockages in perforations or gravel pack  restrict/block flow lines  safety valve & choke failure  pump wear  corrosion underneath deposits  some scales are radioactive (NORM)  Suspended particles  plug formation & filtration equipment  reduce oil/water separator efficiency
  • 7. Slide 7 of 100 Examples - Formation Damage quartz grains scale crystals block pore throats
  • 8. Slide 9 of 100 Examples - Flow Restrictions
  • 9. Slide 10 of 100 Examples - Facilities separator scaled up and after cleaning
  • 10. Slide 11 of 100 1c) Common Oilfield Scales Name Formula Specific Solubility Gravity cold water other (mg/l) Common Scales barium sulphate BaSO4 4.50 2.2 60 mg/l in 3% HCl calcium carbonate CaCO3 2.71 14 acid soluble strontium sulphate SrSO4 3.96 113 slightly acid soluble calcium sulphate CaSO4 2.96 2,090 acid soluble calcium sulphate CaSO4.2H2O 2.32 2,410 acid soluble sodium chloride NaCl 2.16 357,000 (insoluble in HCl) Sand Grains silicon dioxide SiO2 2.65 insoluble HF soluble Some Other Scales Iron Scales: Fe2O3, FeS, FeCO3 Exotic Scales: ZnS, PbS SPE 87459
  • 11. Slide 12 of 100 1d) Mechanisms of Scale Formation  Carbonate scales precipitate due to DP  wellbore & production facilities  Sulphate scales form due to mixing of incompatible brines  injected (SO4) & formation (Ba, Sr and/or Ca)  near wellbore area, wellbore & production facilities  Concentration of salts due to dehydration  wellbore & production facilities Ca2+ (aq) + 2HCO- 3(aq) = CaCO3(s) + CO2(aq) + H2O(l) Ba2+ (aq) (Sr2+or Ca2+) + SO4 2- (aq) = BaSO4(s) (SrSO4 or CaSO4)
  • 12. Slide 13 of 100 seawater formation brine 1e) Location of Scale Deposition b c d e f g i h b a SPE 94052
  • 13. Slide 39 of 100 Outline 1) The Old Foe a) Definition of scale b) Problems caused c) Common oilfield scales d) Mechanisms of scale formation e) Location of scale deposition 2) The New Approach a) The new challenges b) Proactive rather than reactive scale management c) Effect of reservoir processes 3) Conclusions Formation Water (Ba) • •• • • • ••••• Sea Water (SO4) Ba2+ + SO4 2-  BaSO4(s)
  • 14. Slide 40 of 100 2a) The New Challenges  Deepwater and other harsh environments  Temperature and pressure  Residence times  Access to well  Production chemicals compatibility  Inhibitor placement  Complex wells (eg deviated, multilateral)  Well value & scale management costs  Deepwater  Downhole instrumentation  Rig hire vs Sulphate Reduction Plant
  • 15. Slide 43 of 100 Access to Well  Subsea wells  difficult to monitor brine chemistry  deferred oil during squeezes  well interventions expensive (rig hire) bullhead (placement)  squeeze campaigns and/or pre-emptive squeezes
  • 16. Slide 45 of 100 Inhibitor Placement in Complex Wells  Where is scaling brine being produced?  Can we get inhibitor where needed?  wellbore friction  pressure zones (layers / fault blocks)  damaged zones  Options:  bullhead (from platform / FPS via subsea chemical injection or test line)  bullhead + divertor  Coiled Tubing (CT) from rig  Combined stimulation / inhibitor treatments Ptubing head Fault Shale Pcomp 1 Pcomp N Presv 1 Presv N
  • 17. Slide 46 of 100 Well Value & Scale Management Costs  Deepwater wells costing US$10-100 million (eg GOM)  Interval Control Valves (ICVs) costing US$0.5–1 million each to install  good for inhibitor placement control  susceptible to scale damage  Rig hire for treatments US$100-400 thousand / day  necessary if using CT  deepwater may require 1-2 weeks / treatment  cf. other typical treatment costs of US$50-150 thousand / treatment  Sulphate Reduction Plant (SRP), installation and operation may cost US$20-100 million
  • 18. Slide 47 of 100 2b) Proactive Rather Than Reactive Scale Management  Scale management considered during CAPEX  Absolute must: good quality brine samples and analysis  Predict  water production history and profiles well by well  brine chemistry evolution during well life cycle  impact of reservoir interactions on brine chemistry  ability to perform bullhead squeezes: • flow lines from surface facilities • correct placement  Monitor and review strategy during OPEX
  • 19. Slide 48 of 100 2c) Effect of Reservoir Processes EXAMPLE 1 Management of waterflood leading to extended brine mixing at producers (increased scale risk for producers) EXAMPLE 2 In situ mixing and BaSO4 precipitation leading to barium stripping (reduced scale risk for producers) EXAMPLE 3 Ion exchange and CaSO4 precipitation leading to sulphate stripping (reduced scale risk for producers) EXAMPLE 4 Impact of reservoir pressures (correct / incorrect placement profiles)
  • 20. Slide 49 of 100 SPE 80252 Extended Brine Mixing at Producers EXAMPLE 1
  • 21. Slide 50 of 100 SPE 80252 Field M (streamline model) This well has been treated > 220 times! Extended Brine Mixing at Producers EXAMPLE 1
  • 22. Slide 51 of 100 Barium Stripping (Field A) % seawater Barium(mg/l) Dilution line SPE 60193 EXAMPLE 2
  • 23. Slide 52 of 100 Barium Stripping (Theory)  Seawater (containing SO4) mixes with formation water (containing Ba) leading to BaSO4 precipitation in the reservoir  Minimal impact on permeability in the reservoir  Reduces BaSO4 scaling tendency at production wells SPE 94052 EXAMPLE 2
  • 24. Slide 53 of 100 Barium Stripping (Theory) Ba2+ Rock SO4 2- 1) Formation water (FW): [Ba2+] but negligible [SO4 2-] FW (hot) EXAMPLE 2
  • 25. Slide 54 of 100 Barium Stripping (Theory) Ba2+ SO4 2- 2) Waterflood: SO4 2- rich seawater displaces Ba2+ rich FW Rock FWSW (cold) (hot) EXAMPLE 2
  • 26. Slide 55 of 100 Barium Stripping (Theory) Ba2+ SO4 2- Rock 3) Reaction: In mixing zone Ba2+ + SO4 2- → BaSO4 FWSW (cold) (hot) BaSO4 EXAMPLE 2
  • 27. Slide 56 of 100 Barium Stripping (Theory) 0 100 200 300 400 500 600 700 800 900 0 20 40 60 80 100 seawater fraction (%) [Ba](mg/l) 0 500 1000 1500 2000 2500 3000 [SO4](mg/l) Ba Ba (mixing) SO4 SO4 (mixing) •Large reduction in [Ba] •Small reduction in [SO4] (SO4 in excess) •Typical behaviour observed in many fields EXAMPLE 2
  • 28. Slide 57 of 100 Barium Stripping (Model) 0 10 20 30 40 50 60 70 80 90 0 20 40 60 80 100 % seawater bariumconcentration(ppm) Field A - actual Field A - dilution line Field A - modelled EXAMPLE 2
  • 29. Slide 63 of 100 Barium Stripping (Field G) a) water saturation b) mixing zone c) BaSO4 deposition (lb/ft3) SPE 80252 Field G (model) EXAMPLE 2b
  • 30. Slide 64 of 100 Barium Stripping (Field G) 0 50 100 150 200 250 0 500 1000 1500 2000 2500 time (days) bariumconcentration(ppm) 0 500 1000 1500 2000 2500 3000 sulphateconcentration(ppm) Ba Ba (no precip) SO4 SO4 (no precip) [Ba] at well when no reactions in reservoir [Ba] at well when reactions in reservoir Field G (model) EXAMPLE 2b
  • 31. Slide 65 of 100 Barium Stripping (Field G) 0 50 100 150 200 250 0 20 40 60 80 100 % seawater bariumconcentration(ppm) Field B - observed Filed B - dilution line Field B - modelled deep reservoir + well/near well mixing deep reservoir mixing 0 50 100 150 200 250 0 20 40 60 80 100 % seawater bariumconcentration(ppm) Field B - observed Filed B - dilution line Field B - modelled deep reservoir + well/near well mixing deep reservoir + well/near well mixing deep reservoir mixingdeep reservoir mixing Field G (model & field data) EXAMPLE 2b
  • 32. Slide 71 of 100 Sulphate Stripping (Theory)  Seawater (with high Mg/Ca ratio) mixes with formation water (with high Mg/Ca ratio) leading to Mg and Ca exchange with rock to re-equilibrate  Increase in Ca in seawater leads to CaSO4 precipitation in hotter zones in reservoir  Minimal impact on permeability in the reservoir  Reduces BaSO4 scaling tendency at production wells SPE 100516 EXAMPLE 3
  • 33. Slide 72 of 100 Ion Exchange Ca Mg Ca Mg C C 0.50 Cˆ Cˆ  FW: 0.077 SW: 3.2 Rock: 0.038 CCa Ca in solution CMg Mg in solution ĈCa Ca on rock ĈMg Mg on rock Gyda FW (mg/l) 30,185 2,325 SW (mg/l) 426 1,368 EXAMPLE 3
  • 34. Slide 73 of 100 Sulphate Stripping (Theory) Ba2+ Rock SO4 2- Ca2+ Mg2+ 1) Formation water: [Ca2+] and [Mg2+] in equilibrium with rock FW (hot) EXAMPLE 3
  • 35. Slide 74 of 100 Sulphate Stripping (Theory) Ba2+ SO4 2- Ca2+ Mg2+ 2) Waterflood: [Ca2+] and [Mg2+] no longer in equilibrium Rock CWSW (cold) (hot) EXAMPLE 3
  • 36. Slide 75 of 100 Sulphate Stripping (Theory) Ba2+ SO4 2- Ca2+ Mg2+ 3) Reaction 1: Ca2+ and Mg2+ ion exchange with rock Rock CWSW (cold) (hot) EXAMPLE 3
  • 37. Slide 76 of 100 Sulphate Stripping (Theory) Ba2+ SO4 2- Ca2+ Mg2+ 4) Reaction 2: In hotter zones Ca2+ + SO4 2- → CaSO4 Rock CWSW (cold) (hot) CaSO4 EXAMPLE 3
  • 38. Slide 77 of 100 Modelling: Ion Exchange 0 5,000 10,000 15,000 20,000 25,000 30,000 35,000 0 20 40 60 80 100 seawater fraction (%) [Ca](mg/l) 0 500 1,000 1,500 2,000 2,500 3,000 3,500 [Mg](mg/l) Ca Ca (mixing) Mg Mg (mixing) As for field data: •Large reduction in [Mg] •No apparent change in [Ca] EXAMPLE 3
  • 39. Slide 78 of 100 Modelling: Sulphate Stripping 0 100 200 300 400 500 600 700 800 900 0 20 40 60 80 100 seawater fraction (%) [Ba](mg/l) 0 500 1000 1500 2000 2500 3000 [SO4](mg/l) Ba Ba (mixing) SO4 SO4 (mixing) As for field data: •Small reduction in [Ba] •Large reduction in [SO4] (No SO4 at < 40% SW) EXAMPLE 3
  • 40. Slide 84 of 100 Impact of Reservoir Pressures on Placement  Question for new subsea field under development: Can adequate placement be achieved without using expensive rig operations? EXAMPLE 4
  • 41. Slide 85 of 100 Placement (Field D) -200 -100 0 100 200 300 400 500 0 200 400 600 800 well length (m) flowrate(m3/d) prior to squeeze shut-in INJ 1 bbl/m INJ 5 bbl/m INJ 10 bbl/m 1 year after squeeze production injection (squeeze) • Good placement along length of well during treatment (> 5 bbls/min) • Can squeeze this well SPE 87459 EXAMPLE 4
  • 42. Slide 86 of 100 Placement (Field D) production injection (squeeze) • Cannot place into toe of well by bullhead treatment, even at 10 bbl/min • Must use coiled tubing (from rig - cost), or sulphate removal -600 -500 -400 -300 -200 -100 0 100 0 200 400 600 800 well length (m) flowrate(m3/d) prior to squeeze shut-in INJ 1 bbl/m INJ 5 bbl/m INJ 10 bbl/m 1 year after squeeze SPE 87459 EXAMPLE 4
  • 43. Slide 99 of 100 3) Conclusions  Modelling tools may assist with understanding of where scale is forming and what is best scale management option…  identify location and impact of mixing  evaluate feasibility of squeeze option (placement)  calculate chemical requirements … thus providing input for economic model.  Particularly important in deepwater environments, where intervention may be difficult & expensive  But – must be aware of uncertainties…..  reservoir description  numerical errors  changes to production schedule, etc. … so monitoring essential.
  • 44. Slide 100 of 100 Acknowledgements  Sponsors of Flow Assurance and Scale Team (FAST) at Heriot-Watt University: Baker Petrolite, BG Group, BWA Water Additives, BP, Champion Technologies, Chevron, Clariant, ConocoPhillips, Halliburton, M I Production Chemicals, Nalco, Hydro Oil & Energy, Petrobras, REP, Rhodia, Shell, Solutia, Statoil, Total