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Improved oil recovery and environmental aspects by using carbon - - PowerPoint PPT Presentation

Improved oil recovery and environmental aspects by using carbon dioxide as EOR fluid in carbonates Eli J. Hgnesen Outline Introduction Carbon dioxide in general CO 2 flooding History CO 2 flooding in general


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SLIDE 1

Improved oil recovery and environmental aspects by using carbon dioxide as EOR fluid in carbonates

Eli J. Høgnesen

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SLIDE 2

Outline

  • Introduction

– Carbon dioxide in general

  • CO2 flooding

– History – CO2 flooding in general

  • Carbonates
  • CO2 flooding in carbonates

– Sources – Example from the Permian Basin in Texas

  • Environmental aspect
  • CO2-EOR and CO2 storage

– Example from the Weyburn field in Saskatchewan – North Sea

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SLIDE 3

Introduction

  • CO2

– Greenhouse gas (CO2, CFC, CH4, N2O and O3) – Photosynthesis – An everyday gas (soft drinks, beers, fire extinguishers)

  • Released by burning fossil fuels

– Coal, oil and natural gas – The main source of CO2 greenhouse gas from human activities

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SLIDE 4

Physical properties of CO2

  • MW= 44.011 g/ mole
  • Sp. gravity= 1.529
  • Tc= 31 oC
  • Pc= 72.83 bar
  • Soluble in water

– Forms carbonic acid

  • Soluble in oil
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SLIDE 5

Phase diagram for CO2

  • Triple point
  • Critical point
  • Supercritical

state

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SLIDE 6

CO2 flooding - A historical perspective

  • Early EOR research in 1940’s and 1950’s

– Water flood leaves residual oil – Re-mobilize oil by miscible flooding

  • CO2 research in 1950’s and 1960’s

– Oil and CO2 immiscible – Dynamic miscibility

  • Permian Basin, West Texas, 1970’s

– Field testing and commercial CO2 flooding

  • Commercially in 1980’s in US

– CO2 pipeline network – Only EOR motivated

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SLIDE 7

CO2 solubility in crude oil

  • CO2 more soluble in lighter oils

– C5-C12 fraction

  • CO2 dissolution leads to

– Oil swelling and reduction in oil density – Reduction in oil viscosity

  • Oil swelling leads to lower residual oil saturation
  • The viscosity reduction leads more mobile oil
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SLIDE 8

CO2 solubility in water

  • CO2 soluble in water

– Waterflooding – WAG

  • Solubility affected by

– Pressure (increases with increasing pressure) – Temperature (decreases with increasing temp.) – Brine salinity (decreases with increasing salinity)

  • Viscosity of water increases slightly
  • Carbonic acid

– Reacts with wellbore hardware and reservoir minerals

− + +

⇔ +

3 2 2

HCO H O H CO

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SLIDE 9

Miscibility

  • Miscibility

– CO2 not directly miscible with most crude oils – Extracts hydrocarbons from the residual oil – CO2 dissolves into the

  • il

– Dynamic miscibility

Simon et al., SPEJ 18(1), 1978

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SLIDE 10

Minimum Miscibility Pressure (MMP)

  • MMP= f(T, P and composition of oil)
  • The pressure needs to be above the MMP
  • This is corresponds to about 800 m depth
  • If flooding pressure is below MMP, only swelling

and viscosity reduction will occur

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Determination of MMP

  • Slimtube experiments

– Real fluids – Expensive and time consuming

  • Mathematical models

– Phase equilibria data – Equation of State

  • Thermodynamic MMP

Correlations

– MMP increases with increasing sp. grav. – MMP increases with increasing temperature MMP 90 %

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SLIDE 12

Carbonates

  • Sedimentary rocks composed of carbonate

minerals

  • Chalk (CaCO3)

– Skeletons of planktonic algae

  • Limestone (CaCO3)

– Re-crystallization of the skeletons

  • Dolomite CaMg(CO3) 2

– Alternating CaCO3 and MgCO3

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SLIDE 13

EOR in Carbonates

  • Carbonates

– 60% of oil reserves in carbonates – Fractured reservoirs – 90% Neutral- or Oil-wet

  • Wettability

– Acid Number of the oil – Potential determining ions (Ca2+ , CO3

  • and SO4

2-)

– Recovery less than 30% – Big EOR potential

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SLIDE 14

Rock-fluid interaction

  • Dissolution of carbonate due to carbonic acid in

the carbonated water may take place:

  • Carbonates

– Improve injectivity – Compaction – Precipitation of CaCO3 leads to reduced matrix permeability

− + +

+ ⇔ +

3 2 3

HCO Ca CaCO H

− + +

+ ⇔ +

3 2 3

HCO Mg MgCO H

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SLIDE 15

Techniques for CO2 flooding

  • Gas injection

– Continuous Gas Injection (CGI) – Water Alternating Gas (WAG)

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SLIDE 16

Continuous Gas Injection

  • Used for gravity drainage
  • Often used in combination with WAG

– CGI until gas breakthrough – Change to WAG

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Water Alternating Gas (WAG)

  • Alternate injection of CO2 and water

Keewatin publicatons

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CO2 flooding in carbonates

  • Most important EOR process in US carbonate

reservoirs since early 1980’s

  • 48 of 71 CO2 floods were in carbonates
  • Majority located in Texas
  • Cheaper than thermal and hydrocarbon flooding
  • CO2 flooding is expected to expand
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SLIDE 19

CO2 sources

Jarrel et al., 2002

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Manufactured CO2

  • Refineries

– CO2 separated from the natural gas

  • Ammonia plant
  • Fertilizer plants
  • Power plants

– Coal – Gas

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SLIDE 21

Naturally occurring CO2 sources

  • Trapped in dome-like structures
  • Lithology: sandstone and dolomite
  • Natural commercial reservoirs:

– McElmo Dome (Dolomite) – Sheep Mountain Fields – Bravo Dome (Conglomeratic sandstone) – La Barge Field (Dolomite)

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SLIDE 22

The Permian Basin

SPE monograph 22

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Example from the Permian Basin

  • Kelly-Snyder field

– Limestone

  • Discovered in 1948
  • Developed 1951

– Initially pressure depletion

  • Water injection in 1954

– 1 billion bbl un-recovered after flooding

  • CO2 flood planned in 1968
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The CO2 project

  • CO2 injection 1971
  • CO2 from processed natural gas

– Pipeline

  • CO2 followed by water
  • Later WAG
  • CO2 removal facilities installed
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The CO2 WAG recovery

  • Problems

– Needed additional CO2 extraction facilities – Re-complete injection wells – CO2 delivery inconsistent – Re-injected CO2 containing methane

  • Production peaked in the mid 1970’s at 210,000

bbl/ d

  • Followed by a decline of 20% per year
  • In 1995 the oil production was 9000 bbl/ d
  • The economic limit was 7000 bbl/ d
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New work-over

  • New operator in 1995

– Increased production well pressures – Water injection curtain around CO2 project areas to maintain miscibility pressure – Methane separated from the re-injected CO2

  • The recovery rate leveled
  • In 2002 the recovery had increased 50%
  • The lifetime of the field has been extended by at

least 25 years

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SLIDE 27

The recovery history

  • Recovery in the different recovery stages

Kinder Morgan, 2001

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SLIDE 28

The recovery turnaround

Kinder Morgan

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Summary of the Kelly-Snyder project

  • CO2 is a good EOR fluid

– But the process needs to be monitored and maintained

  • This flooding has only been minded on EOR, not

for storing of CO2

  • Environmental aspects?
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SLIDE 30

Environmental Aspects of CO2

  • Largest contribution of

greenhouse gases from human activities

  • Global Warming

– Change in mean temperature and CO2 concentration in atmosphere

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SLIDE 31

Effects of global warming

  • Mean sea level rises
  • Extreme weather (droughts, hurricanes, etc.)
  • Increased damage on life, health and material values
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SLIDE 32

What to do about global warming?

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SLIDE 33

How to reduce CO2 emission

  • Use energy more efficiently

– Buildings, transportation – Power generation

  • Switching to low-carbon fuels

– Coal to gas in electricity generation

  • Substituting fossil fuels for non-carbon renewable

sources

– Wind, solar, biomass, geothermal and tidal power

  • Trapping and storing of CO2

– Geological storage

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SLIDE 34

Combined CO2 EOR and storage

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The Weyburn EOR project

  • Saskatchewan
  • Discovered in 1954
  • Medium oil (850 – 930 kg/ m 3)
  • Fractured carbonate reservoir, mostly limestone
  • Waterflooding since 1964
  • CO2 injection in 2000

– Extend life of Weyburn 25 years

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Why CO2 flooding in Weyburn field?

  • Continuous reservoir
  • Geology promotes gravity segregation
  • Crude oil

– Swells – Large viscosity reduction

  • MMP can be achieved
  • Successful waterflood
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SLIDE 37

CO2 source

  • CO2 piped from a synthetic fuel plant in USA
  • This is the eighth by-product of this plant
  • The CO2 pipeline is 325 km long
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SLIDE 38

Recovery prediction

  • 24 %

recovery

  • At least 15%

extra with the CO2 (19.4 million Sm 3)

Historical production and predicted CO2 response

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SLIDE 39

IEA Monitoring and Storage Project

  • International Energy Agency (IEA)

– Research program

  • Project objectives

– Develop expertise in CO2 EOR and storage – Prove the ability of oil reservoirs to store CO2 – Identify risks associated with geological storage – Develop CO2 mobility control methods – Develop technology to monitor CO2 movement – Develop an economic model

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SLIDE 40

CO2 injection in Norway

  • Only sandstone
  • Sleipner West

– Gas contains 9% CO2 – Piped untreated to Sleipner East

  • Sleipner East

– CO2 separated by liquid amine – CO2 free gas piped – Amine separated from the CO2 and reused – CO2 injected into the Utsira sand

  • Gullfaks

– Not profitable

  • Volve

– CO2 flooding planned Sintef

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SLIDE 41

CO2 storage in the North Sea

  • The oil and gas fields of the southern part of the

North Sea are chalk reservoirs

  • In Ekofisk there has been a significant

compaction due to pressure depletion and water weakening

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The impact of CO2 on chalk

Madland et al., JPSE (2006), in press.

  • Laboratory work has shown that:

– Chalk exposed to carbonated water is weakened – Pure CO2 gas had minor effect on chalk compression – Preferentially oil-wet chalk cores at Sor were weakened more than completely water-wet cores

10 20 30 40 50 60 2000 4000 6000 8000 10000

Time (min) Axial strain (mS) CO2 gas Water CO2 + water

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SLIDE 43

Summary of the presentation

  • As long as CO2 is available it is a logical EOR choice for

Dolomite and Limestone reservoirs

  • Dolomite and Limestone reservoirs can probably be used for

safe storing of CO2

  • CO2 flooding in chalk reservoir may be used as an EOR

technique, but significant compaction can be expected.

– The compaction can be a drive mechanism but it can also result in production problems like pipe buckling and formation instability.

  • Using a chalk reservoir for CO2 storage can be questionable,

since the rock layers above might fracture if the reservoir is compacted.

– Then the CO2 can escape through the fracture system.