Diffusivity Equation

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    FUNDAMENTALS OFFUNDAMENTALS OF

    -

    -

    Diffusivity EquationDiffusivity Equation

    Ali F. M. Altaee

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    To Derive Diffusivity Equation.

    (CTP)

    To apply constant terminal rate solution(CTR)

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    -Pi Pi

    r3 r2 r1 r1 r2 r3

    re

    Const.

    Flow rate

    Pi

    Pit1 t2

    t3

    r3

    r2

    r1

    r1

    r2

    r3

    re

    Const.

    Pwf

    i Pit1 t2t3

    Pressure disturbance as a function of time

    re

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    Pressure disturbance moves away fromwellbore at a rate determined by

    Permeability

    Viscosity

    Transient flow is defined as the time period

    boundary has no effectduring which theon the pressure behavior in the reservoir

    its infiniteand the reservoir will behave as

    .in size

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    Basic Transient Flow E uation

    porous media may not be the same as the flow

    The fluid content of the porous medium changes

    The variables in unsteady-state flow:

    me, t

    Porosity, Total compressibility, ct

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    Basic Transient Flow Equation

    Q

    1

    Q

    2

    The flow rate into & out of an element of volume Q = Q The variables in unsteady-state flow:

    Time, t Porosity,

    Total compressibility, ct

    Transient Flow equation

    must have these

    independent variables +

    limits

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    on nu y qua on MBE

    Transport EquationDarcy

    Compressibility Equation Isotherm coeff

    u y

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    on nu y qua on A material balance equation that accounts for

    every pound mass of fluid produced, injected,

    or remaining in the reservoir.

    Transport Equation

    The transport equation is Darcys equation in

    its eneralized differential form

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    Compressibility Equation

    Is used in formulating the unsteady-state

    changes in the fluid volume as a function of

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    Boundary Conditions:

    e orma on pro uces a a cons an ra e n o e

    wellbore

    the reservoir behaves as if it were infinite in size,

    i.e. re =

    The reservoir is at a uniform pressure when

    =, . .,

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    where k = permeability, md

    r = radial position, ft

    =

    ct = total compressibility, psi1

    t = time, hrs

    = porosity, fraction

    = v scos y, cp

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    CONTINUITY EQUATION

    According to the concept of the material-balance equation

    Mass entering

    volume element

    Mass leaving

    volume elementur ng nterva t ur ng nterva t

    rate of mass

    accumulation

    durin interval t

    ---------------- ((5656))

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    Illustration of radial flow

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    Mass entering the volume element during

    ---------------- 5757where = velocity of flowing fluid, ft/day

    = fluid density at (r + dr), lb/ft3A = Area at r + dr

    t = time interval, days

    The area of element at the entering side is:

    ---------------- ((5858))

    Combining Equation (58) with (57) gives:

    ---------------- ((5959))

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    Mass leaving the volume element

    ---------------- 6060

    o a ccumu a on o assThe volume of

    some element

    with a radius

    of r

    Differentiating

    with respect to r

    ----------------

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    Total mass accumulation during t = dV [()t + t()t]

    Substituting for dV

    Total mass accumulation = (2rh) dr [()t + t()t ] ----------------

    Replacing terms of material balance Equation with calculated relationships

    Dividing by (2rh) drt

    OR---------------- ((6363)) where = porosity

    = densit lb/ft3

    = fluid velocity, ft/daycontinuity equation

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    The transport equation

    arcy s aw s essen a y e as c mo onequation

    ------------ ((6464))

    where k = permeability, md

    = velocit ft/da

    ---------------- ((6565))

    Expanding the right-hand side by taking the indicated derivatives eliminates the porosity

    from the partial derivative term on the right-hand side:

    ---------------- ((6666))

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    porosity is related to the formation compressibilityCOMPRESSIBILITY EQUATION

    ---------------- ((6767))

    Applying the chain rule of differentiation to /t,

    Substituting Equation (67) into this equation

    substituting the above relation into Equation (66)and the result into Equation (65), gives:

    ---------------- ((6868))

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    Radial Flow of Slightly

    Compressible Fluids the permeability and viscosity are constant over

    pressure, time, and distance ranges

    ---------------- ((6969))

    Expanding

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    Using the chain rule in the above relationship yields:

    Recalling that the compressibility of any fluid is related to its density by:

    Combining the two equations

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    very small and may be ignored

    ---------------- ((7070))

    Define total compressibility, ct, as:

    ---------------- ((7171))

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    petroleum engineering

    where the time t is commonly recorded in hours

    ---------------- ((7373))

    where k = permeability, mdr = radial position, ft

    p = pressure, psia

    ct = total compressibility, psi1

    =

    e us v y ons an

    = porosity, fraction

    = viscosity, cp

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    When the reservoir contains more than one fluid, total

    ---------------- 7474

    Co,w,g= compressibility of oil, water and gas

    So,w,g = fractional saturation of oil, water and gas

    ---------------- ((7575))

    The diffusivity equation can then be written in a more convenientorm as:

    ---------------- ((7676))

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    Laplaces Equation

    for a steady-state flow condition, the pressure at any

    with time

    Substitute in diffusivity equation

    ---------------- ((7777))

    Laplaces equation