2013 lect2 basic fluid flow

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  • 8/13/2019 2013 Lect2 Basic Fluid Flow

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    is flow within the boundary walls.

    TYPES OF FLOW

    Internal flow

    Types of internal flow include pipe flow, channel flow, airflow in ducts. Thistype of flow is controlled using valves, fans, pumps.

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    is flow outside of a boundary or body.

    External flow

    Examples of this type of flow include :

    flow around immersed bodiesflow over aircraft wings,airflow around buildings/cars

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    in general all fluids flow three-dimensionally, with pressures and velocitiesand other flow properties varying in all directions.

    In many cases the greatest changes only occur in two directions or evenonly in one.

    other direction can be effectively ignored, making analysis much moresimple.

    Flow is one dimensional if the flow parameters (such as V, P, d) at a given instant intimeonly vary in the direction of flow and not across the cross-section

    An example of one-dimensional flow is the flow in a pipe.

    ONE DIMENSION FLOW

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    Possibly - but it is onlynecessary if very high accuracy

    is required.

    A correction factor is thenusually applied.

    ONE DIMENSION FLOW

    FOR real fluid, flow must be zero at the pipe wall - yet non-zero in the centrethere is a difference of parameters across the cross-section.

    Should this be treated as two-dimensional flow?

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    LAMINAR AND TURBULENT FLOW.

    Fluid flow at low velocities is smooth with the fluid particles movingin straight lines along the direction of flow (LAMINER).

    The majority of flows in practice are TURBULENTwith no uniformmotion at the local level but an average velocity in the direction of

    flow.

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    A typical velocity profile across a pipe

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    FLUID FLOW BASIC

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    It is a known fact said thatthe fluid continuously and permanently deformed

    under shear stress

    while solid exhibits a finite deformation which does notchange with time.

    It is also said that liquid cannot return to their originalstate after the deformation.

    Differences between solids and fluids:

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    States of Matter

    FluidSolid

    Shear Stress t

    a fluid, such as water or air, deformscontinuously when acted on by shearing

    stresses of any magnitude.- Munson, Young, Okiishi

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    The fluids like water or oil, flow on the surface in the form of layerswith the top layer moving at the fastest speed and the bottom layermoving at slowest speed.

    Why the speed of the flow of fluid reduces.

    Because there is RESISTANCE to the flow of the fluid, which iscause by FRICTION of the adjoining layers.

    This property of the fluids is called as viscosity.

    FLUID FLOW & VISCOSITY

    Viscosity describes a fluid's internal resistance to flowand may be thought of as a measure of fluid friction.

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    Viscosity of water

    Water at 20 C has a viscosity of 1.0020 cP (centipoise)

    1 P = 0.1 Pas,1 cP = 1 mPas = 0.001 Pas.

    Dynamic viscosity

    Kinematic viscosity

    1 St = 1 cm2s1= 104m2s1.1 cSt = 1 mm2s1= 106m2s1.

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    Fluid Deformation between Parallel Plates

    Side view

    Force F causes the top plate to have velocity U.

    What other parameters control how much force is

    required to get a desired velocity?

    Distance between plates (b)

    Area of plates (A)

    F

    b

    U

    Viscosity!

    the velocity of the upper layer of the fluid is faster than the velocity of the lower layers of the fluid.

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    Shear Stress

    change in velocity with

    repect to distance

    AFt

    2m

    N

    b

    Ut

    b

    U

    dy

    dut

    b

    AUF

    AU

    Fb

    2m

    sN

    s

    1

    Tangential stress

    Rate of deformation

    rate of shear

    F

    b

    U

    dy

    du

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    Shear Stress

    b

    AUF

    bUA

    F

    AU

    Fb

    2m

    sN

    F

    b

    U

    Absolute Viscosity

    Shear stess

    (dyne/cm2 )

    Shear strain rate

    (s-1)

    Dyne-s/cm2=P (poise)

    1000mPa.S1000cPP10Pa.s

    Dyne-s/cm2=g-s/cm=P=103 cP

    P1010g.s.cm100cm

    1000g.s

    m

    kg.s

    m

    skg.m.sPa.s

    m

    sN 11

    2

    -2

    2

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    Shear Stress

    b

    AUF

    F

    b

    U

    sm

    kg

    m

    s

    s

    mkg

    ..

    .

    m

    sN222

    Kinematic Viscosity

    densityviscosityabsolute

    2s

    mkgN 12

    3

    m

    kg

    sm

    k

    sm

    g

    Stokes

    cm

    /cms-dyne

    s/cmdyne 2

    42

    2

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    ssds

    Fluid classification by response to shear stress

    Newtonian fluida fluid whose stress versus strain rate curve is

    linear and passes through the origin

    The constant of proportionality is known as the viscosity.

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    FLUID CLASSIFICATION BASED ON VISCOSITY

    2) Real fluid:In practice all the fluids are real fluids because all of them have viscosity, smallor high.For the real fluids which are liquids the viscosity reduces as the temperatureincreases and for the gases, the viscosity increases as the temperatureincreases.

    1) Ideal FluidThe fluid which is incompressible and has no viscosity is known as the ideal fluid.However, the ideal fluid is only an imaginary fluid, because all the fluids have

    viscosity and there is no fluid that doesnt have viscosity (see the fig below)

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    3) Newtonian fluid:Is a real fluid that obeys Newtons law of viscosity : the shear stress betweenvarious layers of the fluid is proportional to the rate of shear strain or the

    velocity gradient. Fluids, such as water and most gases which have a constantviscosity.

    4) Non-Newtonian fluid:Is a real fluids that do not obey the Newtons law of viscosity.In such fluids the shear stress between the various layers of fluid is notproportional to the rate of shear strain or the velocity gradient.

    5)Ideal plastic fluid:The fluid in which the shear stress is more than the yield value and shear stressis proportional to the rate of shear strain or velocity gradient is known as idealplastic fluid.

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    Bingham plastic fluidsThe viscosity curve does not go through the origin.It behaves as a solid at low stresses but

    It flows as a viscous fluid at high stresses.

    at a small shear rate (beginning of move), the shear stress can be substantialBut once the fluid is moving, the shear stress is directly proportional to shearrate in exactly the same manner as for Newtonian fluids.

    Fluid behave in this manner are :Water suspensions of rock particlesMore familiarly,, a suspension of potatoes in a liquid,flow in the bowl when you stir, flow harder when you stir harder,and assume a mountain peak shape if undisturbed.

    Non- Newtonian Fluids:

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    Shear thickening:viscosity increaseswith the rate of shear.

    Non- Newtonian Fluids:

    Pseudoplastic fluids(soo doe plastic)

    Shear thinning:

    The viscosity of this pseudoplastic fluids decreases with increased shearing.Shear thinning liquids are very commonly, but misleadingly, described asthixotropic.

    Molten polymers have this characteristic, which is used to advantage ininjection molding when the material flows through small cross section

    gates. Paper pulp suspensions also display pseudoplastic viscosity behavior.

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    for these fluids, the shear stress changes with time of shearing.

    Thixotropic Fluidsthe viscosity decreases at higher shearing rates and become lessviscousover time when shaken, agitated, or otherwise stressed.

    Mayonnaise has this characteristic. its viscosity decreases with higher rates of shearing, but onlyafter a minimum amount of shear is reached. This behavior is related to breaking bonds betweenparticles or molecules or to changes from the at-rest shape to moving shape of long molecules

    Rheopectic:

    materials which become moreviscous over time when shaken, agitated, or otherwise stressed.

    A magnetorheological fluidis a type of "smart fluid" which, when subjected to a magnetic field,greatly increases its apparent viscosity, to the point of becoming aviscoelastic solid.

    Shear Time Dependent Fluids

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    1) Liquids: As the temperature of the liquid fluid increases itsviscosity decreases.

    In the liquids the cohesive forces between the moleculespredominates the molecular momentum transfer between themolecules, mainly because the molecules are closely packed(liquids have lesser volume than gases. The cohesive forces are maximum insolids so the molecules are even more closely packed in them)

    When the liquid is heated the cohesive forces between themolecules reduce thus the forces of attraction betweenmolecules reduce, which eventually reduces the viscosity ofthe liquids.

    Effect of Temperature on Liquid and Gas Fluids

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    Where: - Viscosity of the liquid at t degree Celsius n poiseoViscosity of the fluid at 0

    oCelsius in poise, are the constants

    For liquids: = o/ (1 + t + t2)

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    Effect of Temperature on Liquid and Gas Fluids

    Fundamental mechanisms

    Liquids - cohesion and momentum transfer

    Viscosity decreases as temperature increases. Relatively independent of pressure

    (incompressible)

    Gases - transfer of molecular momentum

    Viscosity __________ as temperature increases.

    Viscosity __________ as pressure increases.increases

    increases

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    In gases there is opposite phenomenon. The viscosity of thegases increases as the temperature of the gas increases. Thereason behind this is again the movement of the molecules andthe forces between them.In the gases the cohesive forces between the molecules is lesser,

    while molecular momentum transfer is high. As the temperatureof the gas is increased the molecular momentum transfer rateincreases further which increases the viscosity of the gas.

    For gases: = o+ t + t2

    Effect temp on Gases:

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    Ostwald viscometers measure the viscosity of afluid with a known density.

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    GL SS C PILL RY VISCOMETERS

    P = Pressure difference across capiller

    R = Radius of capiller

    L = Length od capiller

    V = Volume fluida

    = ViscosityLV

    t

    8

    Pr4

    ASTM D445

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    SIMPLE VISCOMETER :A CALIBRATED HOLE IN THE BOTTOM.

    2

    1

    txV

    Dzg o

    128

    4

    )(

    xz

    xQ

    Dzg o

    128

    4

    )(

    V

    tk

    (Poiseuille Eq.)

    tk

    cP = fluid density X cSt

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    0.02m

    0.1m D=1mm

    =1050kg/m3

    2

    1

    FV

    zzg 2

    2

    2

    12 )(

    Fzzg )(12

    xQ

    Dzg o

    128

    4

    )(

    PENGUKURAN VISKOSITAS

    Fdm

    dWVgzP o )2

    (2

    4

    0

    128..

    DxQ

    PF

    x V2 diabaikan untuk laminer

    z

    4( )

    128. .

    og z D waktu

    Vol x

    2 1 4

    0

    128( ) . .g z z Q x

    D

    H.Newton

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    Fd is the frictional force (acting on the interface between the fluid and the particle(in N), is the dynamic viscosity (N s/m2),R is the radius of the spherical object (in m), andvs is the particle's settling velocity (in m/s).

    Stokes' law

    vs is the particles' settling velocity (m/s)(vertically downwards ifp>f, upwards ifp

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    b

    AU

    F

    Co-axial cylinder viscometer

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    Example: Measure the viscosity of water

    The inner cylinder is 10 cm in diameter and rotates at 10 rpm.The fluid layer is 2 mm thick and 10 cm high. The powerrequired to turn the inner cylinder is 50x10-6watts. What is thedynamic viscosity of the fluid?

    Outer

    cylinder

    Thin layer of water

    Inner

    cylinder

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    Solution Scheme

    Restate the goal Identify the given parameters and represent

    the parameters using symbols

    Outline your solution including the equationsdescribing the physical constraints and anysimplifying assumptions

    Solve for the unknown symbolically

    Substitute numerical values with units and dothe arithmetic Check your units!

    Check the reasonableness of your answer

    Solution

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    Viscosity Measurement: Solution

    hr

    Pt32

    2

    23-

    32

    6-

    s/mN1.16x10

    m)(0.1m)(0.05(1.047/s)2

    m)(0.002W)10(50

    x

    t

    AUF

    UA

    t

    hrF22

    P

    t

    hr

    P

    322

    Outercylinder

    Thin layer of water

    Inner

    cylinder

    r= 5 cm

    t= 2 mmh= 10 cmP= 50 x 10-6W10 rpm

    r

    2rh

    Fr

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    A rotating disk viscometer has a radius, R = 50 mm, and a clearance,h = 1 mm, as shown in the figure.

    a. If the torque (T) required to rotate the disk at n= 900 rpm is 0.537 N

    m,

    determine the dynamic viscosity of the fluid. You may neglect the viscous forces

    acting on the rim of the disk and on the vertical shaft.b. If the uncertainty in each parameter is 1%, determine the uncertainty in the

    viscosity.

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    PERS. KONTINUITAS

    HUKUM KEKEKALAN MASSA

    PERSAMAAN NERACA

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    Input + Generation Output Consumption = Accumulation.

    PERSAMAAN NERACA

    = Deposits Account-penalties- withdrawal+ Interest

    ratesavings

    imigration + born - emigration -death = City population

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    THE CONSERVATION OF MASS

    Matter cannot be created or destroyed - (it is simply changed in to adifferent form of matter

    Mass entering per unit time = Mass leaving per unit time +Increase of mass in the control volume per unit time

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    air

    Natural gas

    Exhaust Gas

    System boundary

    No accumulation

    gas stove

    Mass entering per unit time = Mass leaving per unit time

    MASS CONSERVATION LAW ONA STEADY FLOW PROCESS

    inflow equals outflow

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    222111 vAvAm

    CONTINUITY EQUATION(STEADY STATE, one dimension)

    Accumulation = 0

    Rate of mass entering = Rate of mass leaving

    1

    2

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    Example

    Water flows through a 4.0 cm diameter pipe at 5 cm/s.The pipe then narrows downstream and has a diameter of of 2.0 cm.What is the velocity of the water through the smaller pipe?

    112

    2

    2

    12

    2211

    4vvr

    rv

    vAvA

    = 20 cm/s

    Flow through a pipe of changing diameter

    Example

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    If pipe 1 diameter = 50mm, mean velocity 2m/s, pipe 2 diameter40mm takes 30% of total discharge and pipe 3 diameter 60mm. What

    are the values of discharge and mean velocity in each pipe?

    Exampleto determine the velocities in pipes coming from a junction.

    F t

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    Faucet :

    Explain this phenomenonusing the equation ofcontinuityA1

    A2

    V1

    V2 A1V1=A2V2.

    as it falls down, A will bedecreased.

    on the other hand V will beincreased because of gravity.therefore, this phenomenon is

    appropriate for the equation forcontinuity.

    22

    A stream of water gets narrower as it falls from a faucet (try it & see)

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    steady flow

    is the type of flow in which the various parameters at any point donot change with time.

    0,,

    zyxdt

    d

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    unsteady or non-steady

    is a flow which changes with time.Real flows are generally the latter type

    but in completing flow assessmentsit is often more practical

    to assume steady flow conditions.

    0,,

    zyxdt

    d

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    outinsys mmdt

    dM

    UNSTEADY FLOWSATU DIMENSI,

    Example :

    A tank is filled with water flow rate qf and flowing out q. Find height

    of the level of the surface .

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    dtMdmm oi )(

    dt

    Ahdqq ooii

    )(

    dt

    Ahdqq ofi

    )(

    qqdt

    Ahdf

    )(

    )(1)(

    qqAdt

    hdf

    Solution

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    BERNOULLI EQUATION

    F

    dm

    dWVgz

    P other

    )(2

    2

    What is Bernoulli equation

    Bernoulli's principle can be derived from the principle of conservation of energy.

    This states that, in a steady flow, the sum of all forms of mechanical energy (kinetic energy and potentialenergy, pressure energy) in a fluid along a streamline is the same (remain constant) at all points

    on that streamline.

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    It can be expanded to include these simply, by adding the appropriateenergy terms:

    Loss

    Work done

    Heatsupply

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    Energy form

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    Energy form

    Kinetic energy is the energy in moving objects or mass.

    Potential energy is any form of stored energy of position

    The gravitational potential energy

    Objects have mechanical energy if they are in motionand/or if they are at some position relative to a zero

    potential

    The internal energy the sum of the kinetic and potential energies of theparticles that form the system

    the internal energy of the system is still proportional to itstemperature.

    ENERGY BALANCE (TERMODYNAMICS)

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    Heating cooling jacket

    Volume-changing

    piston

    ENERGY BALANCE (TERMODYNAMICS)

    Work

    Propeler

    Fluida

    Internal Energy

    Potential Energy

    Kinetics EnergyHeat

    Volume work

    )

    2(

    2V

    gzu

    dt

    dQ

    dtdWother

    dt

    dWinjection

    dt

    dmm in

    outdm

    mdt

    Mechanical work

    Internal Energy

    Potential Energy

    Kinetics Energy

    Energy is conserved;

    Energy can be transferred from the system to its surroundings, or vice versa,but it can't be created or destroyed

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    Accumulation = Flow in - Flow out

    dQ

    sys

    Vgzumd )

    2(

    2

    outoutdmV

    gzu )2

    (2

    Heating cooling jacket Volume-changing

    piston

    otherdW

    inindmV

    gzu )2

    (2

    inin dmPv )(

    outout dmPv )(

    outin dQdQdQ

    inoutother dWdWdW

    The sign convention for w is

    decreases when the system doeswork on its surroundings.

    INJECTION WORK

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    inin

    sys

    dmPvV

    gzumd )()2

    (2

    INJECTION WORK

    inin

    sys

    dmV

    gzuV

    gzumd )2

    ()2

    (22

    inin

    sys

    dmV

    gzPvuV

    gzumd )2

    ()2

    (22

    Step 1

    Step 2

    INJECTION WORK

    W=PV

    beginningPiston move

    Constant pressure

    Change of energy in step 1

    Piston move back

    Change of energy in step 2

    Change of energy in step 1 and 2

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    inin

    sys

    dmV

    gzPvuV

    gzumd )2

    ()2

    (22

    otheroutout dWdQdmVgzPvu )2

    (

    2

    inin

    sys

    dmV

    gzhV

    gzumd )2

    ()2

    (22

    ENTALPY

    otheroutout dWdQdmV

    gzh )2

    (2

    ENERGY BALANCE

    ?

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    ADIABATIC THROTTLE TURBIN & COMPRESOR

    SIMPLE HEATERSteady state flow,

    SIMPLE REACTORSteady state flow,

    ENERGY BALANCE IN PROSES SYSTEM?

    inin

    sys

    dmV

    gzhV

    gzumd )

    2

    ()

    2

    (22

    otheroutout dWdQdm

    Vgzh )

    2(

    2

    In many applications of Bernoulli's equation, the change in thegztermalong the streamline is so small compared with the other terms it can be

    ignored, and omitted. T

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    horizontal

    ENERGY BALANCE for THROTTLE PROSES

    inin

    sys

    dmV

    gzhV

    gzumd )2

    ()2

    (22

    otheroutout dWdQdm

    Vgzh )

    2(

    2

    outoutinin dmhdmh

    P1 P2

    ADIABATIC THROTTLE Steady flow

    Adiabatic

    work=0

    V1=V2

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    ENERGY BALANCE for TURBIN/COMPRESSOR

    inin

    sys

    dmV

    gzhV

    gzumd )2

    ()2

    (22

    otheroutout dWdQdmV

    gzh )2

    (2

    TURBIN & COMPRESSOR

    outinoa hh

    dm

    dW.

    Steady flow

    Elevation difference is neglected

    Q is neglected

    Kinetic energy diff is neglected

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    ENERGY BALANCE for Heater

    inin

    sys

    dmVgzhVgzumd )2

    ()2

    (22

    otheroutout dWdQdmV

    gzh )2

    (2

    inout hhdm

    dQ

    SIMPLE HEATERSteady flow

    Flowing horizontally.

    V is neglected

    Work =0

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    inin

    sys

    dmVgzhVgzumd )2

    ()2

    (22

    otheroutout dWdQdmV

    gzh )2

    (2

    SIMPLE REACTOR

    tanreacproduct hhdm

    dQ

    outoutinin dmhdmhdQ

    ENERGY BALANCE for SIMPLE REACTOR

    Steady flow

    Flowing horizontally.

    V is neglected

    Work =0

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    Bottle Filling Problem

    ininsys dmhmud )(

    UNSTEADY STATE SYSTEM

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    UNSTEADY STATE SYSTEM

    inin

    sys

    dmVgzhVgzumd )2

    ()2

    (22

    otheroutout dWdQdmV

    gzh )2

    (2

    ininsys dmhmud )(

    Q=0

    Bottle Filling ProblemSteady flow

    Flowing horizontally.

    V is neglected

    Work =0

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    inin

    sys

    dmVgzPuVgzumd )()(22

    22

    otheroutout dWdQdmV

    gzP

    u )(2

    2

    1. Electrostatic, magnetic, and surface energy are

    negligible2. The content of the system are uniform

    3. The inflow and outflow streams are uniform

    4. The acceleration of gravity is constant

    ENERGY BALANCE

    FOR A STEADY INCOMPRESSIBLE FLOW

    )(

    Puh

    inin

    sys

    dmV

    gzhV

    gzumd )2

    ()2

    (22

    otheroutout dWdQdmV

    gzh )2

    (2

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    inin

    sys

    dmV

    gzP

    uV

    gzumd )()(22

    22

    BERNOULLI

    dm

    dQu

    dm

    dWVgz

    P other)(

    2

    2

    Steady

    Fdm

    dWVgz

    P other

    )(2

    2

    otheroutout dWdQdmV

    gzP

    u )(2

    2

    ENERGY BALANCE

    dm

    dQu

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    BERNOULLI EQUATION

    Fdm

    dWVgz

    P other

    )(2

    2

    g

    F

    gdm

    dW

    g

    Vz

    g

    P other

    )(2

    2

    HEAD FORM OF BERNOULLI EQUATION

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    SATUAN BERNOULLI

    g

    F

    gdm

    dW

    g

    Vz

    g

    P other

    )(2

    2

    HEAD FORM OF BERNOULLI

    EQUATION

    zgP

    ZERO FLOW =STATIK,

    FdmdWVgzP other )(

    2

    2

    What is the Unit ?Energy/massa

    lengthWhat is the unit?V=0, W=0, F=0

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    BERNOULLI EXAMPLE

    SPEED OF FLUIDFLOW OUT OF THE TANK

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    A large bucket full of water has two drains.

    One is a hole in the side of the bucket at thebottom, and the other is a pipe coming out ofthe bucket near the top, which bent isdownward such that the bottom of this pipeeven with the other hole, like in the picture

    below:Though which drain is the water spraying outwith the highest speed?

    1. The hole

    2. The pipe

    3. Same CORRECT

    40

    Note, the correct height, is where the water reaches theatmosphere, so both are exiting at the same height!

    FLOW OUT OF THE TANK

    SPEED OF FLUIDFLOW OUT OF THE TANK

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    Through which hole will the water come out fastest?

    A

    B

    C

    P1+gz1+ v12

    = P2+gz2+ v22

    Note:

    All three holes have same P=1 Atm

    1gz1+ v12= 1+ gz2+ v2

    2

    gz1+ v12= gz2+ v2

    2

    Smaller y gives larger v. Hole C is fastest

    36

    v22= 2gz1z2)+ v1

    2

    FLOW OUT OF THE TANK

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    1

    we take the datum through the orifice

    Between 1 and 2

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    Between 1 and 3

    If the mouth piece has been removed,

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    Example

    A closed tank has an orifice 0.025m diameter in oneof its vertical sides. The tank contains oil to a depth of0.61m above the centre of the orifice and thepressure in the air space above the oil is maintainedat 13780 N/m2 above atmospheric. Determine thedischarge from the orifice.(Coefficient of discharge of the orifice is 0.61, relativedensity of oil is 0.9).[0.00195 m3/s]

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    Example

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    Example

    In a vertical pipe carrying water,pressure gauges are inserted at points A and Bwhere the pipe diameters are dA=0.15m and dB=0.075m respectively andpoint B is 2.5m below A.

    When the flow rate down the pipe is 0.02 m3/sec, the pressure at B is 14715N/m2 greater than that at A.Assuming the losses in the pipe between A and B can be expressed as

    where vis the velocity at A, find the value of k.

    If the gauges at A and B are replaced by tubes filled with water andconnected to a U-tube containing mercury of relative density 13.6, give asketch showing how the levels in the two limbs of the U-tube differ andcalculate the value of this difference in metres.[k = 0.319, 0.0794m]

    THE SKETCH OF PROBLEM

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    THE SKETCH OF PROBLEM

    Part i

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    By continuity: Q = uAAA= uBAB

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    Part ii

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    Lift a House

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    Calculate the net lift on a 15 m x 15 m house when a 30 m/swind (1.29 kg/m3) blows over the top.

    P1+gy1+ v12= P2+gy2+ v2

    2

    P1P2= (v22v1

    2)

    = (1.29) (302) N / m2

    = 581 N/ m248

    F = P A

    = 581 N/ m2(15 m)(15 m) = 131,000 N

    = 29,000 pounds!

    G

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    lift

    drag

    U

    q

    2

    2UACF LL

    p > p0positive pressure

    DAYA ANGKATSAYAP PESAWAT TERBANG

    Sh d P F

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    Shear and Pressure Forces:Horizontal and Vertical Components

    lift

    drag

    U

    Parallel to the approach velocity

    Normal to the approach velocity

    q

    2

    2U

    ACF dd

    2

    2UACF LL

    Adefined as projected

    area _______ to force!normal

    drag

    lift

    p < p0negative pressure

    p > p0positive pressure

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