Equations of Change ChE 131

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    Equations of Change

    ChE 131

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    Shell Balance Approach. . .

    Is a tool to train the student invisualizing transport problems.Introduces the Equations of Change sothat the student understands thephysical significance of each term.

    Can be a tedious exercise if done forevery problem we encounter.

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    Equations of Change

    General Balance Equations (PDEs) that canbe applied to any problem

    Steady- or unsteady-stateSimple or complexCartesian, cylindrical, spherical coordinatesystems

    It is important to understand the physicalsignificance of each term (from shellbalance exercises) in order to write theappropriate equation for a system

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    Equations of Change forIsothermal Systems

    Equation of ContinuityEquation of Motion

    Equation of Mechanical Energy(Kinetic Energy)

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    Equation of Continuity

    Total mass balance:

    t

    z y xt z y x

    Note that if density were constant,

    0

    0

    t

    Divergence of ordiv

    For incompressible fluids

    Or,

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    Equation of Motion

    x-, y-, z-component momentum balances:

    z zz yz xz

    y zy yy xy

    x zx yx xx

    g z y x

    g z y x

    g z y xt

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    Equation of Motion in vectornotation

    Per component of velocity:

    z y xi g t iii

    ,,,

    Add all 3 components:

    g t

    recall:

    p

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    Equation of Motion

    g pt

    Rate ofmomentum

    accumulation/volume

    Rate of momentumaddition by

    convection/ volume

    Rate of momentumaddition bymolecular

    transport/ volume

    Externalforces/volume

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    Equation of MechanicalEnergy

    Dot product of equation of motion

    g pt

    Equation of change for kinetic energy

    g

    p pt

    :

    2212

    21

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    Different Time Derivatives

    Consider that there are different ways of measuring theconcentration change with time in a tubular reactor

    t c

    1. Fix the sensor at one point in the reactor will give us the partialtime derivative

    2. Install the sensor on a mount that can be moved up and downthe reactor independent of the fluid motion will give us the totaltime derivative dc/dt.

    3. Let the sensor drift with the fluid as it flows down the reactor,

    i.e., the sensor and the fluid move at the same velocity. Thisgives us the substantial time derivative

    ct c

    z c

    yc

    xc

    t c

    Dt Dc

    z y x

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    Special Cases

    Navier-Stokes equation (constant , )

    g p Dt

    D 2

    Stokes or Creeping flow equation (substantialderivative ~ 0 )

    g p

    20Euler or inviscid flow equation ( ~0)

    g p Dt D

    Flow throughporous media,particle motion

    in fluids

    Flow around bluffobjects (airplane

    wings, piers, tanks)

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    Equations of Change for Single-Component Non-IsothermalSystems

    Equation of EnergyEquation of Change for Internal EnergyEquation of Change for EnthalpyEquation of Change for Temperature

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    Forms of Energy Accountedfor in the Equation of Energy

    Kinetic energy, K.E. = 2

    Internal energy, U = U( , T)

    Potential energy will be accounted forby the work done by gravityHeat by conduction

    Work done by molecular mechanismsand by external forces (e.g. gravity,centrifugal, electromagnetic, etc.)

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    Equation of Energy

    g eU t

    221

    Recall that

    q H qU e )

    ()

    ( 2

    212

    21

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    Equation of Energy

    g p

    qU U t

    2212

    21

    g

    q H U t

    2212

    21

    or

    Note: nuclear, radiative, electromagnetic and chemicalsources of energy are not included. These are added assource terms or as boundary conditions as the case maybe.

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    Equation of Internal EnergySubtract the Equation of Mechanical Energy from the

    Equation of Energy

    g

    p pt

    :

    2

    212

    21

    g

    q H U t

    2

    212

    21

    : pqU U t

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    Equation of Internal Energy interms of substantial derivative

    : pqU Dt D

    Recall that :

    pU H

    pU H

    or

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    Equation of Enthalpy

    Dt Dp

    q H Dt D

    :

    T k q

    T k q2

    Recall that:

    And if k wereconstant,

    Also,

    :

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    Using derived thermodynamicrelations,

    dP T

    dT C H d

    dP

    T T

    dT C H d

    dP T V

    T V dT C H d

    dP P H

    dT T

    H H d

    T P H H

    P p

    P

    p

    P

    p

    T P

    lnln1

    1

    11

    ,

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    Equation of Change forTemperature

    Dt Dp

    T T k

    Dt DT

    C P

    p

    lnln

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    Special Forms of the Equation ofEnergy

    for systems with constant k at low to moderate fluidvelocities

    For an ideal gas, ( ln/lnT) P=1

    Dt Dp

    T k Dt DT

    C p 2

    For fluid flowing at constant pressure, Dp/Dt=0

    T k Dt DT

    C p2

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    Special Forms of the Equation ofEnergy

    for systems with constant k at low to moderate fluidvelocities

    For a fluid with constant density, ( ln/lnT) P= 0

    T k Dt DT

    C p2

    For stationary solid, = 0

    T k Dt DT

    C p2

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    Boussinesq Equation of Motion forForced and Free Convection

    In a fluid where there are temperature gradients, the fluid density andviscosity will not be uniform resulting in natural or free convection

    The equation of state may be written as a Taylor series expansiontruncated to two terms (a.k.a Boussinesq approximation)

    T T T

    T T g g p Dt D

    Boussinesq Equation

    Neglected inforced

    convection

    Neglected infree

    convection

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    Equations of Change forMulticomponent Mixtures

    Mass and Molar Equations ofChange

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    Equations of Continuity forMulticomponent MixturesOne equation of continuity may be written for each

    specie in a mixture composed of N components

    r nt

    r jt

    convection diffusionreaction

    Note that if we add all the equations of continuity for all the energy definitions,

    we will get the equation of continuity for a mixture.

    Mass balance

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    Equations of Continuity forMulticomponent MixturesOne equation of continuity may be written for each

    specie in a mixture composed of N components

    R N ct

    R J cct **

    convection diffusionreaction

    Note that if we add all the equations of continuity of all the species in the

    mixture, we will get the equation of continuity for a mixture.

    Mole balance

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    Special Cases of BinarySystems

    A A AB A A r w Dwt

    w

    2

    B A A B A AB A A

    R x R x xcD xt

    x

    c

    2

    Mass balance for a binary system

    Mole balance for a binary system

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    Special Cases of BinarySystems

    A A AB A A r w Dwt

    w

    2 Systems with zero flow, and where density and viscosity are constant

    A AB

    A c Dt

    c 2

    Or,

    Ficks second law of diffusion

    Used for diffusion in solids,stationary liquids and equimolar

    counterdiffusion.

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    How to use Equations of Changeto solve Transport Problems

    Isothermal Newtonian Flow ProblemsNon-isothermal steady-state problemsSimultaneous heat and mass transfer

    in a flow reactor

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    Equations that Describe IsothermalNewtonian Flow Problems

    Equation of ContinuityEquation of Motion

    Components of the Shear Stress Tensor An Equation of State [p = p( )]Equation(s) for viscosity

    [ = ( ), = ( )]Boundary and Initial conditionsNavier-Stokes Equation

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    What the solution will give

    Velocity distributionPressure distributionDensity distribution

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    Equations that describe nonisothermalflow of a Newtonian Fluid

    Equation of ContinuityEquation of Motion ( explicit in and )

    Equation of Energy ( explicit in , and k )Thermal Equation of State (p = p( , T))Caloric Equation of State ( CP=C P ( , T) )

    Viscosity Equations [ = ( ), = ( )]Thermal Conductivity Equations (k = k(T))Boundary and Initial Conditions

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    Solution will yield

    Temperature distribution, T(x,y,z,t)Pressure distribution, P(x,y,z,t)Density distribution, (x,y,z,t)Velocity distribution, (x,y,z,t)

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    Equations to describe multicomponent,nonisothermal, Newtonian flow systems andgravity as the only external force

    Equations of ContinuityEquation of MotionEquation of EnergyEquation of StateEquations for Cp, , , kBoundary and Initial conditions