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Petrochemical Engineering - Petroleum Entrapment

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    By the end of chapter 1, you will be able to:

    Explain different steps involved in the generation of the petroleum.

    Describe the effect of pressure and temperature in the migration

    and conversion of petroleum.

    Explain different entrapments which can hold the petroleum in

    place underground.

    Name some of the duties of reservoir, production, formation and

    drilling engineers.

    1

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    Petroleum and reservoirs

    Main elements of a reservoir

    Origin of petroleum

    o Organic material deposition

    o Migration and conversion

    o Entrapment

    Quality of reservoir rock

    o Porosity

    o Permeability

    Petroleum Engineering

    Formation Evaluation

    Drilling Engineering

    Reservoir Engineering

    Production Engineering

    Chapter_1_Introduction

    2

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    Introduction/Main elements of a reservoir

    Source rock (source of hydrocarbons)

    Reservoir trap (structural or stratigraphic)

    Reservoir seal (to contain hydrocarbons within reservoir trap)

    Quality of reservoir rock (reasonable porosity and permeability)

    3

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    Introduction/Origin of petroleum/Organic deposition

    Petroleum reservoirs are created through three sequential steps:

    deposition, migration/conversion and entrapment.

    A. Organic material deposition:

    Petroleum originates mainly from algae and plankton (fatty

    molecules called lipids).

    This organic material must be buried under a sediment or silt.

    The silt guards the organic material from aerobic consumption.

    Deposition process normally takes place in the river deltas or

    between shores and reefs (stagnant flow zone).

    The organic material and sediment form a source bed which is

    required for the remaining steps in the process.

    This is often called black shale or sedimentary rock. Black

    shale contains an organic feature called Kerogen enriched in

    high molecular weight organic chemicals.

    4

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    Introduction/Origin of petroleum/Organic deposition

    B. Migration/Conversion:

    Pressure: Responsible for the primary migration

    Buoyancy: Responsible for the secondary migration

    Temperature: Responsible for petroleum generation

    5

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    Introduction/Origin of petroleum/migration

    Primary migration: The release of petroleum compounds after they are

    generated from Kerogen in source beds. The cause of expulsion of

    petroleum is due to the overburden pressure on the source rock, pushing

    out water and hydrocarbons.

    Secondary migration: The expelled oil from the source bed passes through

    wider pores of more permeable porous rocks. Small droplets of petroleum

    coalesce to form larger volumes. Surrounding water pushes the oil and gas,which have a lower density, upward through the reservoir rock layer until

    they are accumulated in traps. This is caused by buoyancy forces.

    Petroleum Formation and Occurance2ndedition, Tissot, B.P. and Welte, D.H., Springer-Verlag, Berlin, 1984, 294.6

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    7

    Introduction/Origin of petroleum/conversion

    For a reservoir to be formed, a porous rock (such as sandstone,

    dolomite and so on) must form above the source bed rock.

    Petroleum Formation and Occurance2ndedition, Tissot, B.P. and Welte, D.H., Springer-Verlag, Berlin, 1984, 294.

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    Conversion (Effect of temperature):

    The series of events involved in the transformation of organics intopetroleum is not well known. This conversion takes place duringboth the primary and secondary migrations.

    Temperature plays a major role in the conversion.

    Temperature in the porous rock is determined by the averagesurface T and the geothermal gradient. An average value is 30C/km. In western Canada these values are: 0 C and 38 C/km.

    Some Types of Kerogen release crude oil and natural gas above 50

    C.

    Although the overburden pressure is the driving force for theprimary migration, it does not appearto be an important parameterin the chemistry of converting organic material to petroleum since asimilar crude oil is obtained at a wide range of well depths at

    different locations in the world.

    Introduction/Origin of petroleum/conversion

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    Conversion (Effect of temperature):

    Introduction/Origin of petroleum/conversion

    Generation of crude oil is promoted at temperature between

    50 C (1.3 km) and 160 C ( 4.2 km) considering an average

    geothermal gradient of 38 C/km.

    At temperatures higher than 160 C, the petroleumundergoes thermal degradation to form gas. At temperatures

    over 225-250 C, organic matter loses all its hydrogen and

    transforms into graphite.

    At temperatures lower than 50 C, Kerogen tends to be

    selectively degraded by bacteria where the lower density

    components are consumed and the higher density fluids remain

    (e.g. Bitumen within the Oilsands)

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    Hydrocarbon Exploration and Production,Jahn, F., Cook, M., Graham, M., Elsevier, 2008, 2ndEdition 22.

    Conversion (Effect of temperature):

    Introduction/Origin of petroleum/conversion

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    Introduction/Origin of petroleum/Summary

    Earth, portrait of a Planet, 4th edition, Stephen Marshak, W.W. Norton & company, 201211

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    C. Entrapment:

    Entrapment occurs when the petroleum reaches an impermeable layerwhere no further migration can occur. This rock layer is known as a trap.

    There are four types of traps: structural, stratigraphic, combination

    and differential.

    C.1. Structural traps:

    Structural traps are formed by folding (Anticline) or faulting (normal or

    thrust) or salt dome.

    Folding occurs from compression and tension in the earths crust

    including uplifts caused by salt or shale. The inverted U-shape of

    the fold (the anticline) results in a trap where the upper layer (the

    cap rock) is impermeable to the oil.

    Fault traps result from shifting and displacement along a fault line,

    which places a reservoir layer adjacent to an impermeable layer.

    Introduction/Origin of petroleum/Entrapment

    12

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    Structural trap (Anticline)

    Introduction/Origin of petroleum/Entrapment

    Where rock layers are folded into anticlines and synclines, the oil and

    gas migrates to the crests of the anticlines within the reservoir rock,

    and are trapped if overlain by an impermeable layer. If fractures occur,

    oil and gas may seep to the surface. Examples include the Bubbles

    and Jedney gas fields in northeastern British Columbia.http://www.drillingfunds.com/common_traps.html

    Surface gravel

    Shale

    Salt

    Sandstone

    Limestone

    Gas

    OilGas

    Oil

    Anticline

    13

    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    Structural trap (Normal fault)

    Faults drop one side down and push the other side up to place the

    reservoir rock against impermeable sealing rocks, forming a structural

    fault trap. An example is the Dunvegan gas field in northwestern

    Alberta.

    Introduction/Origin of petroleum/Entrapment

    http://www.drillingfunds.com/common_traps.html

    Surface gravel

    LimestoneSandstone

    Salt

    Shale

    Oil

    Gas

    14

    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    Structural trap (Thrust fault)

    Introduction/Origin of petroleum/Entrapment

    In the foothills of Western Canada, east of the Rockies, the original

    limestone layer was first folded and then thrust-faulted over itself. An

    overlying seal of impermeable rock completes the structural trap.

    Examples include the Turner Valley oil and gas field and Jumping

    Pound gas field, both in south-western Alberta.http://www.drillingfunds.com/common_traps.html

    Shale

    Sandstone

    Limestone

    Gas

    Oil

    15

    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    Structural trap (Salt dome)

    Under the weight of overlying rock layers, layers of salt will push their

    way toward the surface in salt domes and ridges. Oil and gas are

    trapped in folds and along faults above the dome and within upturned

    porous sandstones along the flanks of the dome. Examples are found

    off Canada's East Coast.

    Introduction/Origin of petroleum/Entrapment

    http://www.drillingfunds.com/common_traps.html

    Sandstone Shale

    Salt dome

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    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    C.2. Strarigraphical Traps:

    Stratigraphic traps are formed by a change in the character of

    the reservoir rock (less permeable) or a change in the deposition

    environment where an impermeable layer is deposited around

    the reservoir rock. The layering must have both a vertical and

    lateral aspect to act as a trap. Three common stratigraphictraps: Pinch out, Reef, and Unconformity.

    Examples:Reservoir Rock Impermeable

    Layer

    Sandstone Shale

    Deolomite Limestone

    Reef limestone Limestone

    Introduction/Origin of petroleum/Entrapment

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    Stratigraphic trap (pinch out)

    Introduction/Origin of petroleum/Entrapment

    This occurs where the porous limestone reservoir loses its porosity

    and becomes impermeable limestone, or the porous sandstone

    reservoir simply thins and pinches out. Overlying impermeable rocks

    act as seals. Examples include the D-1 Crossfield sour gas field and

    many oil and gas fields in Saskatchewan.http://www.drillingfunds.com/common_traps.html

    Sandstone

    Limestone Shale

    Gas

    Oil

    18

    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    Stratigraphic trap (reef)

    Introduction/Origin of petroleum/Entrapment

    Porous ancient coral reefs grew in the warm seas that once covered

    much of Western Canada. They now provide prolific oil and gas

    reservoirs. Often overlying porous rock layers are "draped," or folded

    over the reefs and form separate traps. Overlying impermeable shales

    act as seals to the reservoirs. An example is the Leduc oil and gas

    field in Alberta.http://www.drillingfunds.com/common_traps.html

    Limestone

    Limestone

    Shale

    Shale

    19

    http://www.drillingfunds.com/common_traps.htmlhttp://www.drillingfunds.com/common_traps.html
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    Stratigraphic trap (unconformity)

    An unconformity is a break in the depositional sequence of rocks. If the

    underlying beds were tilted, eroded and then covered with flat laying

    impermeable rocks, then oil and gas may be trapped at the

    unconformity. The reservoirs are commonly covered by shale.http://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swf

    Introduction/Origin of petroleum/Entrapment

    Introduction to Oil and Gas Production, API, Dalla, Texas, 1983, 4.

    20

    http://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swfhttp://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swf
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    C.3. Combination traps:

    Combination traps have characteristics of both structural andstratigraphic traps. A trap is created due to a salt dome or salt

    plug moving upward. As the salt dome pushes upward through

    the sedimentary layers (stratigraphic component), it causes

    folding and faulting (structural component). This results in

    formation of combination traps.

    Introduction/Origin of petroleum/Entrapment

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    Introduction/Origin of petroleum/Entrapment

    http://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swf

    http://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swfhttp://www.carbonet.net/bjarne/Stoupakova%20et%20al%202006.swf
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    23DIFFERENTIAL TRAPPING OF HYDROCARBONS, WM. C. GUSSOW. CONSULTANT.

    Introduction/Origin of petroleum/Entrapment

    C.4. Differential Traps:

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    Introduction/Origin of petroleum/Entrapment

    C.4. Differential Traps:

    Stage 1

    Both oil and gas continues to be trapped while water is displaced. Stage 1ends when oil water interface reaches the spill points.

    24

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    25

    Introduction/Origin of petroleum/Entrapment

    C.4. Differential Traps:

    Stage 2

    Gas continues to be trapped while oil is spilled up dip. Stage 2ends when oil-gas interface reaches spill point and coincides with

    the oil-water interface

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    26

    Introduction/Origin of petroleum/Entrapment

    C.4. Differential Traps:

    Stage 3

    Gas spills up dip as more gas enters trap. Oil by-passes the

    trap and continues up dip.

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    Introduction/Origin of petroleum/Entrapment

    Summary of traps

    1. Structural (89%)

    Folding (Anticline)

    Faulting

    Normal fault

    Thrust fault Salt dome

    2. Stratigraphic (9%)

    Pinch out

    Reef

    Unconformity

    3. Combination (2%)

    4. Differential 27

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    Porosity:

    Connected porosity to store economic volume of hydrocarbons.

    Permeability:

    The ease with which fluids can flow through the porous rock.

    Introduction/Reservoir rock

    Hydrocarbon Exploration and Production,Jahn, F., Cook, M., Graham, M., Elsevier, 2008, 2ndEdition, 96, 165.28

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    Petroleum and reservoirs

    Main elements of a reservoir Origin of petroleum

    o Organic material deposition

    o Migration and conversion

    o

    Entrapment Quality of reservoir rock

    o Porosity

    o Permeability

    Petroleum Engineering

    Formation Evaluation

    Drilling Engineering

    Reservoir Engineering

    Production Engineering

    Introduction

    29

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    1) Formation Evaluation:

    Objective:

    Formation evaluation activities attempt to develop a composite

    description of the reservoir.

    Seismic testing (e.g. sonic waves)

    Well logging (e.g. electrical resistivity of the reservoir)

    Well testing (e.g. determination of the flow behaviour)

    Information from the formation evaluation will determine the extent of thereservoir and provide an estimate of the amount of oil available and the

    difficulty in obtaining the oil. The preliminary feasibility of the reservoir

    can be determined from this information. The results also guide the work

    of the other disciplines in determining the most effective method to

    produce oil from the field.

    Introduction/Petroleum Engineering

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    2) Drilling Engineering

    Objective:

    Determine the optimum approach to create an oil well.

    Plan and execute the drilling process and all related activities

    such as well logging, cementing, completion, stimulation.

    Responsibilities also include the design of networks of horizontal wells.

    A key concern of the drilling engineer is to limit the extent of wellbore

    damage during drilling.

    Introduction/Petroleum Engineering

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    3) Reservoir Engineering

    Objective: Determine the best method to operate all the wells in the

    oil field using:

    Well testing

    Material balance

    Reserve estimation update

    Stimulation

    This work involves modelling the entire oil field. There are a number of

    modeling and simulation software in the market.

    Introduction/Petroleum Engineering

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    4) Production Engineering

    Objective: Determine the best method to operate individual wells

    using:

    Well testing

    Well work-over

    Stimulation

    Artificial lift

    The production engineer must obtain the maximum production from oneor more wells at the minimum cost.

    Introduction/Petroleum Engineering

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    34

    Introduction/Petroleum Engineering

    Identify the type of engineering work in each video.

    http://www.youtube.com/watch?v=vSTLyEC6QqM

    http://www.youtube.com/watch?v=c83CvjQ6nYE

    http://www.youtube.com/watch?v=RX4jHN4Fu-k

    http://www.youtube.com/watch?v=vSTLyEC6QqMhttp://www.youtube.com/watch?v=c83CvjQ6nYEhttp://www.youtube.com/watch?v=RX4jHN4Fu-khttp://www.youtube.com/watch?v=RX4jHN4Fu-khttp://www.youtube.com/watch?v=RX4jHN4Fu-khttp://www.youtube.com/watch?v=c83CvjQ6nYEhttp://www.youtube.com/watch?v=vSTLyEC6QqM

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