Formation Damage Examples

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    Formation Damage

    Examples

    Scale

    Emulsions

    Paraffin

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    Damage What is it?

    Divide the well into three parts:

    Inflow: area from reservoir to the wellbore

    Completion potential: flow to surface

    Surface restrictions: chokes, lines, separators.

    Basically, anything that causes a restriction in

    the flow path decreases the rate and acts asdamage.

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    The first step..

    For the purposes of this work, consider the

    flow connection between the reservoir and

    the wellbore as the primary but not the only

    area of damage.

    Now, is it formation damage or something

    else that causes the restriction?

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    Some sources of the damage in the reservoir-

    wellbore connection

    Wetting phases (from injected or lost fluids)

    Debris plugging the pores of the rock

    Polymer waste from frac and drilling fluids

    Compacted particles from perforating

    Limited entry (too few perforations)

    Converging radial flow wellbore too small

    Reservoir clay interactions with injected fluids

    Precipitation deposits (scale, paraffins, asphaltenes, salt,etc)

    Note that not all are really formation damage How do youidentify the difference?

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    Identification of Damage.

    How good are you at deductive reasoning?

    Identifying the cause and source of damage isdetective work.

    Look at the well performance before the problem Look at the flow path for potential restrictions

    Look to the players:

    Flow path ways

    Fluids

    Pressures

    Flow rate

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    Completion Efficiency

    What is it? a measure of the effectiveness of

    a completion as measured against an ideal

    completion with no pressure drops.

    Pressure drops? these are the restrictions,

    damage, heads, back-pressures, etc. that

    restrict the wells production.

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    The Effect of Damage on Production

    Rate = (P x k x h) / (141.2 o o s)

    Where:

    P = differential pressure (drawdown due to skin)k = reservoir permeability, md

    h = height of zone, ft

    o = viscosity, cpo = reservoir vol factors = skin factor

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    What changeable factors control

    production rate?

    Pressure drop need maximum drawdownand minimum backpressures.

    Permeability - enhance or restore k? - yes

    Viscosity can it be changed? yes

    Skin can it be made negative?

    These factors are where we start ourstimulation design.

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    Formation Damage

    Impact

    Causes

    Diagnosis

    Removal/Prevention?

    Basically, the severity of damage on productiondepends on the location, extent and type of the

    damage. A well can have significant deposits, filland other problems that do not affect production.

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    Impact of Damage on Production

    Look at Effect of Damage

    Type of Damage

    Severity of Plugging

    Depth of Damage

    Ability to Prevent/Remove/By-Pass

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    Observations on Damage

    Shallow damage is the most common and

    makes the biggest impact on production.

    It takes a lot of damage to create large drops

    in production

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    Effect of Depth and Extent of Damage on

    Production

    0

    10

    20

    30

    40

    50

    60

    70

    80

    90

    100

    0 1 2 3

    Radial Extent o f Damage, m

    %o

    foriginalFlow

    80% Damage

    90% Damage

    95% Damage

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    Productivity and Skin Factor

    Q1/Qo = 7/(7+s)

    Where:Q1 = productivity of zone w/ skin, bpd

    Qo = initial productivity of zone, bpd

    s = skin factor, dimensionless

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    Example

    Productivity for skins of -1, 5, 10 and 50 in a

    well with a undamaged (s=0) production

    capacity of 1000 bpd

    s = -1, Q1 = 1166 bpd

    s = 5, Q1 = 583 bpd

    s = 10, Q1 = 412 bpd

    s = 50, Q1 = 123 bpd

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    Improvements

    For s = -1 (1166), -2 (1400), -3 (1750), and -4

    (2333) ..

    Why have we seen better results in field?

    Fracturing past damage!

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    Damage By-Pass

    For 1 well producing 1500 bpd with a skin of

    50, what would frac with s=-2 yield?

    Qo = 12,214 bpd to get to s = 0

    Qimproved = 17,100 bpd at s = -2

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    Causes

    Pseudo damage - very real effect, but no

    visible obstructions

    Structural damage

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    Pseudo Damage

    Turbulence

    high rate wells

    gas zones most affected

    Affected areas: perfs (too few, too small)

    fracture (conductivity too low)

    tubing (tubing too small, too rough) surface (debottle necking needed)

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    Structural Damage

    Tubular Deposits

    scale

    paraffin

    asphaltenes

    salt

    solids (fill)

    corrosion products

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    Perforation Damage

    debris from perforating

    sand in perf tunnel - mixing?

    mud particles

    particles in injected fluids

    pressure drop induced deposits

    scales

    asphaltenes

    paraffins

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    Near Well Damage

    in-depth plugging by injected particles

    migrating fines

    water swellable clays

    water blocks, water sat. re-establishment

    polymer damage

    wetting by surfactants

    relative permeability problems

    matrix structure collapse

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    Deeper Damage

    water blocks

    formation matrix structure collapse

    natural fracture closing

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    l ll

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    Horizontal Well Formation Damage

    TheoriesZone of Invasion - Homogeneous Case

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    i l ll i

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    Horizontal Well Formation Damage

    TheoriesZone of Invasion - Heterogeneous Case

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    Clay like smectite may have a major effect on damage in some cases none in others

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    Clay like smectite may have a major effect on damage in some cases, none in others.

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    Narrow (

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    Wide, often cavernous fractures are present in some rocks,

    particularly limestones. These types of fractures can take

    whole mud, making cleanout and effective restoration of

    permeability nearly impossible. Air drilling is often the onlypractical approach to prevent excessive damage.

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    Mud Damage

    Common problems

    fines in the mud - physical plugging

    wetting of formation by mud surfactants

    Emulsions from formation fluids and both oil

    based mud (OBM) and water based mud (WBM)

    reactions with the formation fluids

    reaction with the formation clays

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    One common and severe problem is the creation of a

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    One common and severe problem is the creation of a

    rigid sludge (extremely viscous emulsion) from mixing

    the heavier ranges of oil based muds (typically over 12

    lb/gal) with some brines and most acids and/or spent

    acids. The emulsion is stabilized and its viscosity

    significantly increased by the cuttings in the oil based

    mud. The result is a nearly solid sludge when the oilbased mud emulsifiers react with the low pH acid or

    high chloride brines.

    Testing with laboratory samples of OBM and acid will

    not predict this problem it usually only occurs with

    field samples of the OBM (containing the cuttings) and

    the field samples of acid and spent acid, which contain

    iron.

    To prevent the problem, overflush OBM in the well

    with xylene or a suitable safe substitute and backflow

    before acidizing. Jetting the solvent assists in OBM

    removal. Apply the solvent before acidizing and use amutual solvent in the acid

    To clean up a sludge, a strong OBM solvent (xylene is

    usually the best) is soaked for several hours before

    flowing back and then acidizing with acid and a

    suitable mutual solvent. Test on field samples.

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    50/50 mixtures of a field sample of

    14.5 lb/gal OBM and acid produced

    this solid sludge. The sample was

    stable for months.

    The well it was from was expected to

    come in a 12 mmscf/d but the flow

    was too small to measure after the

    well was perforated and acidized with

    straight 12%/3% HCl/HF.

    The well was treated with high quality

    xylene (soaked for 12 hours), before

    circulating the solvent and mud out of

    the well. After acidizing with HCL and

    a mutual solvent, the rate increased to12 mmscf/d within 24 hours.

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    Another sample of OBM that was

    treated with acid.

    In the sample on the left, a field

    sample of OBM was mixed directlywith acid. The sample was stable for

    three months until discarded.

    In the sample in the left, the OBM was

    mixed with xylene and allowed to

    soak. The water in the OBM is thedarker brown and the cuttings that

    have dropped out are at the bottom of

    the cylinder.

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    Deposits

    Paraffin - precipitated by:

    loss of temperature in the tubing

    loss of light ends of the liquids such as ethanes,

    propanees and butanes by venting (pressurereduction)

    mixing with cool fluids (acids, frac, kill, etc) thatreduce the oil temperature below the cloud point.

    flood front breakthrough that cool the oil (wateror CO2 expansion) or by dry gas stripping thatremoves the light ends.

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    Paraffin Location

    Deposit first appears at or near the surface

    Location moves downhole as field is produced

    and pressure drops reduce the light end

    concentrations)

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    Paraffin Composition

    C18 to C60+ straight chain hydrocarbons

    C18 82F melting point

    C23 122F melting point

    C32 158F melting point C42 181F melting point

    C60 211F melting point

    Paraffin deposits are never pure (pure paraffin is

    white).

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    Deposition Location

    Top 5 joints of tubing

    Downstream of pressure drop

    Sea floor flow lines, wellheads, risers

    Gas breakout points

    On old paraffin deposits

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    Paraffin Removal Methods Hot Oiling better for surface lines and the very top tubing joints.

    Dont expect to get heat deep in a well by circulating hot fluids itsa shell-and-tube heat exchanger.

    Solvents good but need heat at the reaction site to be about130oF (54oC) and add jetting or agitation to speed the removalprocess.

    Dispersants water based with additives designed to disperseparaffin and hold it in suspension works only where lab and fieldtesting are coordinated to develop the best product and approach.

    Scraping a short term fix - turns loose a lot of debris and leavesparaffin on the tubing, which serves as a growth site for more

    paraffin. Heating cables good but often expensive to install and operate.

    Plastic rod guides can be effective in rod pumped wells, if area ofcontact overlaps other guides.

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    Paraffin Prevention Methods

    Crystal modifiers that prevent wax deposition.

    Need by careful selection and a consistent

    method of application.

    Heating cables expensive?

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    Asphaltene Sources

    Dispersions - kept suspended by micelles

    Soluble in oil (very limited)

    Additives to muds (gilsonites)

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    World Wide Crude Oil Chemical Compositions (SARA)Hydrocarbon Number

    Field As phaltene Re s in Aro matic Saturated Total of

    (Wt %) (Wt %) (Wt %) (Wt %) (Wt %) Samples

    Athabas ca 23.3 28.6 32.1 15.9 48.1 15

    Wabas ca 21.6 30.6 32.1 15.6 47.7 7

    Peace River 48.7 23.2 20.5 7.6 28.1 3

    Cold Lake 20.6 28 30.5 20.9 51.4 7

    E. Vene zue la 12.6 32.4 36.4 18.6 55 5

    Average on 22.9 30.6 30.4 16.1 46.5 4646 Heavy Oils

    PB HOT (EOA) 14.13 13.37 28.1 44.4 72.5

    PB HOT (WOA) 10.38 20.42 28.23 40.97 69.2

    W. Ven. (ne ar 13.2 12.9 38 35.9 73.9

    HOT)

    Co nventio nal 14.2 28.6 57.2 85.8 517Normal Oils

    PBU Normal 16.52 1.9 31.93 49.67 81.6

    Oil 18.42

    Schrader Bluff 4.9 29.0 24.7 41.5 66.2 153/14/2009 41George E. King Engineering

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    Asphaltenes

    precipitated by:

    CO2

    acid

    pH

    turbulence

    chemical shift that upsets micelle

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    Asphaltene Stability

    Maltenes and resins form the micelle

    Asphaltene is the small platelet (35A) held inthe middle of the micelle

    Dispersed platelets are not usually a problemalthough the oil may have a high viscosity

    When micelles are upset and broken, the

    platelets coagulate and form a mass.

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    Scales

    calcium carbonate - upset driven

    calcium sulfate - mixing waters, upset, CO2

    barium sulfate - mixing waters, upset

    iron scales - corrosion, H2S, low pH, O2

    rarer scales - heavy brines

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    Calcium carbonate scale, note the layers.

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    An unusual form of calcite scale in the

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    form of 1 to 2 mm diameter pellets

    where the calcite layers formed

    around a grain of silt and grew until

    the were too heavy to be suspended

    in a well with very strong water drive

    (E. Texas circa 1975).

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    Scale Location

    at pressure drops - perfs, profiles

    water mixing points - leaks, flood breakthru

    outgassing points - hydrostatic sensitive

    shear points - pumps, perfs, chokes,

    gravel pack - formation interface

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    In one case, scale was forming at

    the interface of a gravel pack and

    formation sand in an extremely fine

    and poorly sorted sand. The

    formation water was high inbicarbonate ion and calcium.

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    Scale Prediction

    Chemical models - require water analysis and

    well conditions

    Predictions are usually a worst case - this is

    where the upset factor comes in.

    added shear - increased drawdown, choke

    changes, etc.

    acidizing venting pressure

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    Polymer Damage

    From: muds, pills, frac, carriers

    Stable? - for years

    location - depends on form polymer was in

    dispersed properly - surface to deep in formation

    in pills and mass - right in perfs

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    Using dry polymer

    mixed into cold

    water, a crust of un-

    hydrated polymerformed and

    separated to the

    top of the tank. If

    this layer were

    drawn into the

    pump as the tanklevel dropped, the

    polymer mass could

    be displaced into

    the perfs and would

    be a significant

    barrier toproduction for

    years. Acid has

    little effect on this

    type of deposit.

    Even pre-mixed polymer has un-hydrated gels or fish-eyes after mixing

    ith t Sh i d filt i th l th h i t i ht

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    with water. Shearing and filtering the gel through a six to eight gauge

    screen is the fastest way to remove the plugging debris. Incidentally

    the sales representative said this would never happen with their product.

    BP

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    Particles in the Fluid

    Solids from tanks, lines and fluids

    Severe problem, but often ignored

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    h f h d b

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    Much of the debris

    that is pumped down a

    well comes from debris

    left in the water and

    mix tanks.

    If you think tank

    cleaning is too time

    consuming, you will

    live with the

    production decrease inyour well.

    Will the same

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    truck be used

    to haul mix

    water to yournext job?

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    Cartridge filters before use.

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    Afterwards

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    Downhole camera

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    picture of a perforation

    completely filled with

    debris after displacing a

    few loads of dirty fluids.What is the cost in

    production?

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    Migrating Fines

    Sources

    kaolinite - not really that likely!

    Smectite - very likely, but clay is rare

    zeolites - common in younger sands, GOM area

    weathered feldspar - older sands

    micas, silts, drilling additives

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    Area of Clays

    Sand Grain 0.000015 m2/g

    Kaolinite 22

    Smectite 82

    Illite 113

    Chlorite 60

    The areas for clay are highly variable and depends ondeposit configuration.

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    Many chemical

    reactions are

    surface areadependant. The

    more area, the

    faster the

    reaction.

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    The surface area of clay compared to the volume of reactive fluid in contact drives the reaction.

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    Fibrous or spider web

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    Illite is actually low

    reactivity in most cases

    but serves as a trap for

    migrating fines.

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    Migrating Clay Catalysts

    water salinity changes

    surfactants and mutual solvents

    overburden increases

    wettability changes

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    Other Migrators

    The following are dwarfs compared to the problems

    with smectite.

    Zeolites - (common in young marine sands) - clintoptolite

    Weathered or altered feldspars

    one very rare form of chlorite

    a few loosely attached kaolinite bundles

    broken illites (and mixed layers)

    silt and other grains (

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    Is Clay a Problem?

    Usually not.

    Very few formations are water sensitive to a

    degree that will affect production.

    Clay is a problem when it is in contact with a

    reactive fluid and the effects or the reaction

    significantly lower permeability (30% or

    more?).

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    Microporosity

    Refers to the very small (non flowable?)volume between clay platelets that can trapand hold water.

    May explain non recovery or slow recovery ofload fluids

    May explain errors in log calculations involvinghigh Sw prediction and subsequent dryhydrocarbon flows.

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    In some forms,

    particularly the Chl i i llKaolinite (left) and Chlorite (right) are

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    particularly the

    weathered and loosely

    attached forms,

    kaolinite has been

    known to migrate, butvery little reactivity has

    been seen in most

    instances that have

    been investigated by

    flow.

    Chlorite is usually

    strongly attached and

    most forms of the

    mineral are non

    reactive with water. Itdoes contain ferrous

    iron, but tests have

    shown only slow

    reactivity with the

    concentrations and

    volumes of acid thatare likely to come in

    contact with Chlorite

    in the pores of a rock.

    Rare examples are

    known of free

    standing chlorite rims

    these are unstable

    and can break during

    flow.

    two common clays found in pore

    throats. Reactivity is low, but some

    caution is needed.

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    Migrating???

    Because fines are there means nothing

    What turns the fines loose?

    Velocity - unlikely

    salinity change in fluids - very common wetting change

    cleaning agents

    solvents (and mutual solvents)

    shock loads (perforating for example)

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    Damage from clays?

    The potential for clay damage depends on claytype, form, location and presence of reactivefluids.

    In hundreds of sensitivity tests, most corescontaining clays are not highly sensitive (>30%permeability reduction) to changes in fluidsalinity.

    The question is how representative the clays inthe core being tested are to the higherpermeability sections of the reservoir.

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    Preventing Clay Damage

    Unless the clays in the higher permeabilitysections of the rock are sensitive to the fluids thatwill actually contact them, any type of claycontrol treatment will likely be unnecessary and

    potentially damaging.

    When clay damage is possible, test for the bestfluid and monitor performance in the field.

    In practice, fluids with 2% to 3% KCl are common.These may be effective, unnecessary orineffective depending on the clay.

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    Removing Clay Damage

    Shallow (to a depth of about 6 inches or 15

    cm), 1%HF and 9%HF may be effective in some

    cases.

    Deeper damage usually requires fracturing tobypass the damage.

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    Emulsions

    Multiple phases that do not separate quickly. Creating an emulsion generally requires an energy

    source.

    If oil and water do not separate quickly, then look for

    the stabilizing mechanism Surfactant either added or natural

    Silt from the formation or from drilling

    Viscosity high viscosity emulsions often require thinning

    to break. Charge even weak electric charges can be stabilizers but

    are more common in water-in-gas emulsions (clouds).

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    Changes in Fluid Viscosity with Change in Internal Phase of Dispersed or Emulsified

    Flow

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    Increasing internal fraction of the emulsion

    52% 74% 96%

    Viscosity

    WidelyDispersed

    Contact

    Deformation

    Inverted

    Flow

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    Energy Sources

    lift system

    gas breakout

    shear at any point in the well

    choke

    gas expansion

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    Common Stabilizers in Oil Production

    surfactant (film stiffeners)

    solids (silt, rust, wax, scale, cuttings)

    emulsion or component viscosity (prevents

    particle or droplet contact)

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    bl

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    Iron Problems

    Precipitates - usually with acid spending - not

    typically a problem

    Sludges - more of a problem than we realize -

    can be controlled with iron reducer and anti-sludge

    Solid particles - multiple problems

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    B i l P bl

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    Bacterial Problems

    Aerobic - lives only w/ oxygen Anerobic - lives w/o oxygen

    Facultative - w/ or w/o, but better one way

    Problems Caused

    eats polymer

    causes formation damage and corrosion SRBs may sour reservoir

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    B t i l P l ti

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    Bacterial Populations

    Free Floating - easy to kill, not that plentiful

    Sessile (attached colonies)

    100,000 x free floating populations,

    very difficult to kill,

    live in densly matter layers

    protected by slime layer

    highly accelerated corrosion underneath

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    B t i l S

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    Bacterial Sources

    Some small populations dormant in reservoir? Probably.

    drinking water < 1000 cells/ml

    sea water - high populations of SRBs

    brackish waters - very high populations

    river/pond - moderate to high populations

    concentrated brines - very low concentrations

    acids - very low to almost none

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    B t i l C t l

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    Bacterial Control

    Acids - kills free floating, little effect on sessilecolonies

    Bactericides - (same as acid) kills free floating, little

    effect on sessile colonies Bleaches and Chlorine - (3% to 8%) strips slime layer,

    dissolves cell wall, cant remove biomass. Watch

    corrosion!

    Bleach, followed by acid - good removal history.

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    Relative Permeability Damage

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    y g

    Mechanisms

    Wetting surface wetting

    Water blocks trapping water some effects

    of capillary pressure in small pores in wells

    with low differential pressures.

    Condensate banking and retrograde

    condensate a phase drop-out that decreases

    perm to a single fluid.

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    Controlling Relative Permeability

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    g y

    Mechanisms

    Water blocks reduce the interfacial andsurface tension of the intruding fluid and re-establish the connate fluid saturation.

    Wetting can modify by cleaning, but thenatural surfactants ultimately will define thewetting of the rock.

    Condensate drop-out increase the flow area

    by fracturing to negate the effects of lowingthe permeability of the formation.