part 3 kicks and gas migration

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    Contents

    • Density of real gases

    • Equivalent Mud Weight (EMW)

    • Wellbore pressure before and after kick

    • Gas migration rate - first order approx.

    • Gas migration rate – with temperature,mud compressibility and Z-factor

    considerations

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    Density of Real Gases

    M = molecular

    weight

    m = mass

    n = no. of moles

    gg = S.G. of gas

    ZRT

    pVn

    V

    nM

    V

    mg

     

    29

    M

    M

    M

    ZRT

    pM

    V

    M

    ZRT

    pV

    air

    g

    g

     

    ZRT

    pgg

    g

     

    29

    (Real Gas Law)

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    Density of Real Gases

    • What is the density of a 0.6 gravity gas at

    10,000 psig and 200oF?

    • From Lesson 2, following figure

    •  ppr = p/ppc = 10,015/671 = 14.93

    •  Tpr = (200+460)/358 = 1.84

    •  Z = 1.413

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    1.413

    14.93

    1.84

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    Density of Real Gases

    g = 2.33 ppg

    TRZ

    p29 gg

    g

    p = 10,000 psig

    T = 200oF

    gg = 0.6

    {660)28.80(413.1

    015,10)6.0(29g 

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    Equivalent Mud Weight, EMW

    • The pressure, p (psig) in a wellbore, at a

    depth of x (ft) can always be expressed interms of an equivalent mud density or

    weight.

    • EMW = p / (0.052 * x) in ppg

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    EMW

    • EMW is the density of the mudthat, in a column of height, x (ft)will generate the pressure, p

    (psig) at the bottom, if thepressure at top = 0 psig

    or, at TD:

    •  p = 0.052 * EMW * TVD

    0po=0

    TVDp

    x

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    0

    2,000

    4,000

    6,000

    8,000

    10,000

    12,000

    0.0 10.0 20.0 30.0 40.0 50.0

    EMW, ppg

       D  e  p

       t   h ,

       f   t

    Depth

    pEMW

    *052.0 

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    10 

    0

    2,000

    4,000

    6,000

    8,000

    10,000

    12,000

    0 1,000 2,000 3,000 4,000 5,000 6,000 7,000 8,000

    Annulus Pressure, psig

       D  e  p

       t   h ,

       f   t After Kick

    Before Kick

    SICP = 500 psig

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    Gas Migration

    • Gas generally has a much lower density than the

    drilling mud in the well, causing the gas to rise

    when the well is shut in.

    • Since the gas, cannot expand in a closed wellbore,

    it will maintain its pressure as it rises (ignoring

    temp, fluid loss to formation, compressibility of

    gas, mud, and formation)• This causes pressures everywhere in the wellbore

    to increase.

    11 

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    12 

    P1

    P2

    P3

    P1 = P2 = P3  ???

    12 3

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    Gas Migration

    Example 1:  A 0.7 gravity gas bubble enters the bottom of a

    9,000 ft vertical well when the drill collars are being pulled

    through the rotary table.

    Flow is noted and the well is shut in with an initial recordedcasing pressure of 50 psig. Influx height is 350 ft. Mud weight

    = 9.6 ppg. Assume surface temperature of 70oF. Temp

    gradient = 1.1oF/100 ft. Surface pressure = 14 psia

    • Determine the final casing pressure if the gas bubble isallowed to reach the surface without expanding

    • Determine the pressure and equivalent density at total

    depth under these final conditions

    13 

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    Gas Properties at Bottom

    • First assumption: BHP is brought to the surface

    • Pressure at the top of the bubble

    • P8,650  = 14 + 50 + 0.052 * 9.6 * (9,000-350)= 4,378 psia

    • T9,000 = 70 + (1.1/100) * 9,000 + 460

    = 629oR

    14 

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    Gas Properties at Bottom

    • ppc = 666 psia

    • Tpc = 389 deg R

    • ppr = 4,378/666 = 6.57

    • Tpr = 629/389 = 1.62

    • Z = 0.925

    15 pseudocritical - pseudoreduced

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    Bottomhole Pressure

    • g = 29*0.7*4,378 / (0.925 * 80.28 * 629)

    = 1.90 ppg

    • DpKICK = 0.052 * 1.9 * 350 = 35 psi

    • BHP = 4,378 + 35

    BHP = 4,413 psia (~surface press.? 

    ZRTpg

    gg

     29

    16 

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    Pressure at Surface

    • Assume, at first, that Zf  = 1.0 (at the surface)

    • Then,

    46070*nR*0.1Vp

    629*nR*925.0V378,4

    ZnRTpV o

    17 

    so, po = 3,988 psia (with Temp. corr.)

    46070*0.1

    p

    629*925.0

    378,4 o

    BOTTOM SURFACE

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    Solution with Z-factor Corr.

    • At surface:

     –ppr = 3,988 / 666 = 6.00

     –Tpr = 530 / 389 = 1.36

     – Zf  = 0.817

    p0 = 3,258 psia

    18 

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    Solution with Z-factor

    • A few more iterative steps result in

     –Z0 = 0.705 and p0 = 2,812 psia

    • At the surface

    • f  = 29*0.7*2,812 / (0.705*80.28*530)

    = 1.9 ppg

    ZRT

    pgg

    g

     

    29

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    New BHP & EMW

    • New BHP = 2,812 + 0.052 * 1.9 * 350+ 0.052 * 9.6 * 8,650

    • New BHP = 7,165 psia

    • EMW = (7,165 - 14)/(0.052 * 9,000)

    • EMW = 15.3 ppg

    20 

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    21 

    1. 4,413 psia2. 4,378

    3. 3,988 (T)

    4. 3,258 (Z)

    5. 2,812 (Z)

    6. 2,024 (mud)Mud9.6 ppg

    Gas

    0.1 bbl/ft

    7,004 psia

    7,179 psia

    7,378 psia

    4,413 psia

    629 R

    8,650’ 

    9,000’ 

    64 psia

    530 R2,812 psia

    ΔPmud=2,626 psi

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    Compression of Mud in Annulus vA = 0.1

    bbl/ft)

    • DV = compressibility * volume * Dp

    • = -6 * 10-6 (1/psi) * 0.1(9,000-350)*2,626

    • DV = -13.63 bbls

    • Initial kick volume = 0.1 * 350 = 35 bbls

    • New kick volume = 35 + 13.63

    = 48.63 bbl

    22 

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    Compression of Mud in Annulus

    • From Boyle’s Law, pV = const 

     – p2 * 48.63 = 2,812 * 35

     – p2 = 2,024 psia

    p8650  poA  poB  poC

    Consider: V,p,Z const. p,Z change mud comp.

    2nd iteration ? ……………. 3rd

    or, Is there a better way? 

    23 

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    Gas Migration Rate

    • A well is shut in after taking a 30 bbl kick.

    The SIDPP appears to stabilize at 1,000 psig.

    One hour later the pressure is 2,000 psig.

    Hole Cap = 0.1 bbl/ft

    MW = 14 ppg

    TVD = 10,000 ft

    24 

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    Gas Migration Rate

    • How fast is the kick migrating?

    •  What assumptions do we need to make

    to analyze this question?

    25 

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    26 

    P1

    P2

    P3

    12 3

    1 Hr

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    Gas Migration Rate

    • Field rule of thumb ~ 1,000 ft/hr

    •  Laboratory studies ~ 2,000 – 6,000 ft/hr

    •  Who is right?

    •  Field results?

    •  Is the previous calculation correct?

    28 

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    Second Attempt

    • Consider mud compressibility

    • Hole capacity = 0.1 bbl/ft * 10,000 ft

    = 1,000 bbl of mud

    • Volume change due to compressibility and

    increase in pressure of 1,000 psi,

    • DV = 6*10-6 (1/psi) * 1,000 psi * 1,000 bbl

    = 6 bbl

    29 

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    Second Attempt

    • i.e. gas could expand by 6 bbl, to 36 bbl

    •  Initial kick pressure

    =1,000 + 0.052 * 14 * 10,000 (approx.)

    = 8,280 psig

    = 8,295 psia

    30 

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    Second Attempt

    • A 20% expansion would reduce the

    pressure in the kick to ~ 0.8*8,295

    = 6,636 psia

    = 6,621 psig

    •So, the kick must have migrated more than1,374 ft!

    31 

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    Second Attempt

    • How far did it migrate in 1 hour?

    • The pressure reduction in kick fluid

    = 8,260 - 6,621=1,659 psi

    • The kick must therefore have risen an

    additional x2 ft, given by:

    1,659 = 0.052 * 14 * x2 x2 = 2,279 ft

    32 

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    Second Attempt

    • 2nd estimate = 1,374 + 2,279

    = 3,653 ft/hr

    • What if the kick size is only 12 bbl?

    • What about balooning of the wellbore?

    • What about fluid loss to permeable

    formations? T? Z?...

    33 

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    Bore Hole Ballooning

    34 

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    Example

    • Kick occurs. After shut-in, initial csg.

    Press = 500 psig. 30 minutes later,

    p = 800 psig

    • What is the slip velocity if the kick volume

    remains constant?

    • MW = 10.0 ppg

    35 

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    Simple Solution

    36 

    hr ttftpsi

    g

    psippv

    12

    12slip

     

     

     

     

    Ignoring

    temperature,

    compressibility and

    other effects.

    5.00.10052.0

    500800vslip

    hr /ft154,1vslip  

    What factors affect

    gas slip velocity, or

    migration rate?

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    Gas slip velocity

    • The bubble size, and the size of the gas void fraction,

    will influence bubble slip velocity.

    • The “void fraction” is defined as the ratio (or

    percentage) of the gas cross-sectional area to the

    total flow area.

    37 

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    Gas Slip Velocity

    Bubbles with a voidfraction > 25% assume a

    bullet nose shape and

    migrate upwards along

    the high side of the

    wellbore concurrent

    with liquid backflow, on

    the opposite side of the

    wellbore

    38 

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    Gas slip velocity

    •Large bubbles rise faster than smallbubbles

    •  Other factors:

     –  Density differences

     –  Hole geometry

     –  Mud viscosity

     –  Circulation rate

     –  Hole inclination

    •  One lab study showed max. rate at 45o.

    39 

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    End

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