Me2135e Lecture Notes - Turbomachinery and Potential Flow 2014

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    NATIONAL UNIVERSITY OF SINGAPORE

    DEPARTMENT OF MECHANICAL ENGINEERING

    ME2135E Fluid Mechanics II

    TURBOMACHINERY AND POTENTIAL FLOW

    (PART I)

    Dr Lua Kim [email protected]

    2013-14

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    mailto:[email protected]:[email protected]:[email protected]
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    Chapter 1

    TURBOMACHINERY

    Definition:A turbomachine is a device which adds energy to or extracts energyfrom the fluid passing through it.

    Add Energy : Pumps Extract Energy : Turbines

    Compressors

    Fans

    PUMPS: 1. Introduction and pump classification

    2. Basic energy consideration

    3. Elementary pump rotordynamics

    4. Pump characteristics and similarity

    5. Matching pump and system requirements

    6. Cavitation

    7. Further topics

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    REFERENCES:

    1. White, F. M. Fluid Mechanics,McGraw-Hill.

    2. Potter, C. P., Wiggert, D. C., & Ramandan, B. H. Mechanics of Fluids,

    Cengage Learning Engineering.

    3. Douglas, J. F., Gasiorek, J. M. and Swaffield, J. A. Mechanics of Fluid,

    Taylor & Francis.

    4. Sayers, A. T. Hydraulics and Compressible Flow Turbo machines,

    McGraw-Hill.

    5. Cengel, Y.A. and Cimbala, J. M. Fluid Mechanics, Fundamentals and

    Applications,McGraw Hill.

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    1. Introduction and Pump Classification

    The Pump is a common engineering device used to add energy to a fluid. Itis employed in all kinds of industries which involve the transport and processing

    of fluids.

    1.1 Terminology

    Pumping of liquids (essentially incompressible): PUMPS.

    Pumping of gases/vapours (compressible):

    FANS BLOWERS COMPRESSORS

    We will concentrate on the pumping of liquids in this course.

    Pumps for liquids may be divided into two categories:

    Dynamic Pumps Positive-displacement Pumps.

    Basic types:

    Dynamic Pump Positive-displacement Pumps

    Centrifugal

    Axial

    Mixed flow

    Reciprocating

    Rotary

    increasing pressure requirements

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    1.2 Basic construction- Positive-displacement Pumps

    Schematic design of positive-displacement pumps: (a) plunger or reciprocating

    piston, (b) gear pump, (c) double-screw pump, (d) sliding vane, (e) three-lobe pump,(f) double-circumferential piston, (g) flexible-tube squeegee.

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    The heart is a two-chamber displacement pump.

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    Basic construction- dynamic Pumps

    The basic components of a centrifugal pump are:

    - the impeller- the volute casing- the diffuser ring. (optional)

    Cut-away schematic of a typical centrifugal pump.

    A centrifugal pump with a stationary diffuser ring.

    Stationary

    diffuser

    vanes

    Diffuser

    Impeller

    Volute

    Impeller Diffuser

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    A centrifugal pump impeller (unshrouded).

    A centrifugal pump impeller.

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    Schematic of a typical axial pump.

    Axial flow impellers.

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    General characteristics ofDynamic andPositive-displacement pumps

    Dynamic Pumps Positive-displacement Pumps

    add energy by fast-moving blades orvane; no closed changes

    steady discharge of fluid

    high flow rate

    low viscosity fluid

    low to moderately high pressure rise

    need priming when filled with air/gas

    force fluid along by volume changes;fluid cavity opens to admit which isthen squeezed through an outlet

    discharge may be pulsatile or periodic

    low flow rate

    may be used for very viscous fluid

    high to very high pressure rise(sturdy construction required)

    no priming needed for mostapplications

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    An electrical powered centrifugal pump

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    2. Basic Energy Consideration

    TheBernoulli Head, H, at a point is given by

    = + + (2-1)The quantity (gH) is a measure of the energy per unit mass of the fluid.

    The Steady-State Energy Equation for flow through the pump is given by

    gH0= gHi+ ws- wf (2-2)

    where

    ws: shaft work per unit mass (energy input),

    wf: energy lost in the pump between inlet i and outlet o,

    which is a statement thatthe energy at outlet is equal to the energy at inlet plus

    net gain in energy (ws-wf) (per unit mass).

    Equation (2-2) can be written in terms of heads as

    H0=Hi+ hs- hf (2-3)

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    where

    =

    , gain in head due to added energy,

    = , loss in head due to frictional losses.Let Q denotes the volume flowrate through the pump.

    Useful Power = Power transmitted to the fluid = (Q) (g), (2-4)mass- flowratewhere =Hi- Hois the head transmitted to the fluid. Power input to pump:

    = = (2-5)whereT : Torque at the shaft of the pump,

    w: Angular velocity of the shaft (radians per second).

    TheEfficiency of the pump,

    = =() (2-6)

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    3. Elementary Pump Rotordynamics

    3.1 Centrifugal impeller

    We shall consider the case of an idealised flow through a centrifugal impeller:

    Assumptions: - No viscosity effects

    - flow enters the impeller tangentially to the blades (no-shockcondition).

    - uniform conditions along the circumferential inlet and outletof the impeller (as if there are infinitely many blades of zerothickness to guide the flow).

    - flow leaves the impeller tangentially to the blades.

    Idealised flow through a centrifugal impeller. (a) Impeller control

    volume; (b) velocity diagrams at control surfaces.

    (a) ub1

    ub2

    ur2

    ur1

    Vn2

    Vn1

    Vt1

    Vt2

    V2

    V1

    (b)

    Axis of rotation

    V1= Vn11

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    ub: Absolute blade velocity (= rw) ;

    ur : Flow velocity relative to blade;

    V : Absolute flow velocity;

    Vt: Tangential component of V;

    Vn: Normal component of V.

    Using a control-volume analysis:

    Rate of gain of angular momentum by volume = Torque (T) applied to the fluidby the impeller = rateof outflux angular momentum - rate of influx of angularmomentum

    T = (Q) (r2Vt2) - Qr1Vt1mass- flowrate ang. mom/ unit-mass

    or T =Q(r2Vt2 - r1Vt1) (3-1)

    Power input, P= Tw=Q(r2wVt2 - r1wVt1)

    or P =Q(ub2Vt2 - ub1Vt1) (3-2)

    Since Power P = (Q)(gH) , we have :

    = = (3-3)

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    The headHegiven by (3-3) is commonly termed theEuler Head.

    For the ideal or design case, the angle 1= 90 ; the inflow has zero whirl, Vt1=0, Vn1= V1. This is also known as thezero pre-whirl condition. For the design

    case :

    P =Qub2Vt2 (3-4)

    =

    (3-5)

    We note from geometry that

    =(cot) = (cot) (3-6)From volume conservation: (211)1 = (2), so that

    1 = 211 ,

    = 2

    where b1and b2are the blade widths at the inlet and outlet respectively.

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    Applying these to equation (3-5) (the design case) yields

    = (cot) , = (cot) (3-7)

    Equation (3-7) gives theHead versus Flowrate relation for the case of an idealimpeller operating at the design case. It can be seen that the relation is determined

    by thephysical characteristics (quantities) of the impeller:

    =, 2, r2 and b2These quantities may be explicitly controlled by impeller design.

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    The figure on the left shows the effects of

    outlet blade angle 2 on the Head (H)

    versus Flowrate (Q) relationship for an

    ideal impeller. See figure below.

    Backward-curved bladed pumps have a maximum point in their Power versus

    Flowrate curve. The power requirement (P QH) of Radial- and forward- curved

    bladed pumps on the other hand rises continuously with the flowrate Q. An

    electric motor driving a radial- or forward-curved runs the risk of being

    overloaded. Forward-curved pumps may also suffer from unstable operation, an

    oscillatory condition in which a pump 'hunts' for its equilibrium point. Backward-

    curved blade is therefore the generally preferred design.

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    3.2 Real flow in a centrifugal pump

    Fluid viscosity causes boundary layers to form on the blades or vanes.

    The boundary layers may separate due to adverse pressure gradient. Flowmay separate due to 'shock' (non-tangential) condition at entry.

    The formation of boundary layers and separations reduces flow through theimpeller.

    The flow is non-uniform circumferentially at the outlet.

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    3.3 Axial Impeller

    Idealized axial-flow impeller

    We will consider the design case for which the flow has no pre-whirl:1 = 90 1 = 0, 1 = 1 = = (3-8)Let us examine the contribution from one elemental ring of thickness (r) at

    radius r. The mass flowrate through the elemental ring is

    (

    )=(Q) =2r(r )Vf (3-9)

    Elemental ring

    V2

    ub2

    ur2

    ub1

    ur1

    Vn1

    Vn2

    Vt2

    V1Vt1

    Section A-A at radius r

    V1= Vn1

    1

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    The torque contribution from the elemental ring, (T), is

    (T) =(Q) rVt2 (3-10)

    We note from geometry that = (cot) and =1 =(why?).

    From these, we have

    (T) = 2

    (r)Vf[rw Vf (cot2)] (3-11)

    The total torque, T, summing the contributions from all the elemental rings, is

    = () = ,= 2

    (cot

    )

    (3-12)

    The torque Ton the impeller as given by (3-12) may be evaluated when the outlet

    blade angle is given as a function of radius: =(). A changing withradius r corresponds to a 'twist' in the blades.

    The theoretical power transmitted to the fluid is then

    P = Tw (3-13)

    A cruder approximation to the torque Tand power P for an axial impeller may

    be obtained by considering only the flow condition at the mean radius =+ as an average of the condition over the whole blade:T = (T)=

    (Q)(rVt2),

    T (rVt2)Rm(Q) = Q() (3-14)21

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    Thepower and theEuler Head are given respectively by:

    P = Tw = Q(), (3-15)He= =. (3-16)

    Note the close similarity of (3-16) with equation (3-5) for centrifugal pumps.

    Simplifying Assumptions have been made in the above derivations for axialpumps:

    as for centrifugal pumps.

    flow remains essentially parallel as it moves from inlet to outlet

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    4. Pump Characteristics and Similarity

    4.1 Performance Characteristics of centrifugal pumps

    The Fluid Dynamics of pumps is very complex. Until more recent times, pumpdesign is very much an art, derived from experience and trial-and-error. Mostmanufacturers still determine the performance characteristics of their pumps

    through extensive experimental testing.

    Quantities of interest to someone using a pump are:

    Q - theflowrate through the pump,

    H - the head the pump develops,

    Ps - thepower to drive the pump, and

    - the efficiency at which the pump is operating.

    As an engineer, you will in general be interested in how the headH, the power Ps

    and the efficiency change with the flowrate Q delivered by the pump. Typical

    plots of these relationships for centrifugal pumps are shown below. Theserelationships are termed collectively as the performance characteristics of the

    pump. They are dependent upon the speed of the pump N, which is the rotationalspeed of the impeller.

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    4.2 Geometrically-Similar Pumps and Dimensional Parameters

    Physical Parameters relevant to the performance Geometrically-Similar pumpsare:

    D - Diameter of impeller (a measure of pump size),

    Q - Flowrate,

    H - Head (or gH, the energy per unit mass),

    Ps - Power input to pump (shaft power),

    N - Rotational speed of impeller or shaft,

    - Density of the fluid being pumped,

    - Viscosity of the pumped fluid,

    - Average surface roughness of pump components.

    Dimensional Analysis reduces these dimensional parameters to a smaller number

    of non-dimensional parameters (the - groups). The use of non-dimensionalparameters results in more compact representation for the performance data.

    Dimensional Analysis carried out on the above set of dimensional parametersyield the relations:

    (4-1)

    (4-2)

    Try to establish these non-dimensional parameters for yourself.

    =

    3

    ,

    ,

    35 = 3 , ,

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    For brevity, we abbreviate these non-dimensional groupings as follows:

    =

    :Head Coefficient

    = : Power Coefficient

    =

    : Flow Coefficient

    = :Reynolds numberso that relationships (4-1) and (4-2) become

    =

    ,

    ,

    (4-3)

    = ,, (4-4)Most commercially available pumps operate in thefully-turbulent flow regime;

    the Reynolds number Re being of the order of 107. At such large Reynolds

    numbers, the viscous action of the fluid is small. The effects of Re in (4-3) and

    (4-4) are then fairly weak. If we further assume that the pumps are well made

    with small relative roughness factor/D (so that the effect of /D is also small),then we can simply write (4-3) and (4-4) as (4-5)

    (4-6)

    which are simple two-variable relations.

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    We may also note that = =

    so that () (4-7)Thus efficiency is a function of CQtoo.

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    A geometrically-similar series of pumps is also called a homologous series. The

    diameter of a pump in a series is therefore a good measure of its size. The

    performance of a homologous series of pumps is governed (and fully specified)

    by relations of the form

    and (4-8a,b)when the effects of/D andReare small. The specification of CPmay be replaced

    by that of ().

    REMARKS:

    When using dimensionless performance parameters supplied by others, the units

    of the physical quantities involved must be known.

    For example: =Q: m3/s, cu.ft./min, gal./min etc.

    N : rad./s, rpm, rps etc.

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    EXAMPLE: Given the performance curves for a family of homologous pumps,

    you know that the BEP occurs at CQ* 0.1, CP* 0.6, CH 2.0.

    Calculate Q, H, (static pressure across the pump), Psand for a pump ofimpeller diameterD = 0.6 m operating at 1500 rpm at BEP. You may assume Qin m3/s,Nin rps,Din m and in kg/m3

    SOLUTION: From definitions

    * is the head rise across the pump (inlet to outlet). Assuming that ViVoandzi

    zo , the rise in pressure (static) is

    The power requirement is

    The efficiency is

    =3 = 0.1 1500

    60 (0.6)3 = 0.543/

    = = 2.0 (0.6) 150060 = 45.87

    =0 = 103 9.81 45.87 = 450kPa =35 = 0.6 3 1500603 (0.6)5 = 729

    = = 103 0.54 9.81 45.87729 103 = 0.333

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    The efficiency versus Q and power Psversus Q curves for the pump may also

    be estimated from the series' performance curves (graphs) =fh(CQ)andCP=

    fp(CQ)respectively following the above procedures.

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    4.4 Similarity Rules for Pumps in a Homologous Series

    Pump characteristics for a homologous series:

    Consider the characteristics of two pumpsA andB from the same homologous

    series. The above figure shows that for every point on the pump characteristics

    of pumpA, there is a corresponding point on the characteristics of pumpB with

    the same CQ .

    The two corresponding points will also have the same CH, Cpand because these

    are functions of CQ. In particular, for corresponding points we have:

    =

    =

    =

    3 (4-10)

    () = () = = (4-11)() = () ()35 = ()35

    ()() = 3 5 (4-12)

    Q

    H

    DA, NA

    CQ

    CH

    Seris

    Q

    H

    DB, NB

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    = (4-13)

    Using equations (4-10) to (4-13), we can predict (estimate) the performance of

    one pump, sayB, from the known performance curves (data) of another pump,

    sayA, from the same homologous series.

    Since a pump is always homologous to itself, the performance of the pump at one

    speed, sayN2, may be predicted (estimated) from its performance data at another

    speed, sayN1.

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    Another empirical relation obtained by Anderson from thousands of tests:

    0.94

    0.94 110.3

    These formulae assume equal value of surface roughness for both pumps. 0.94

    instead of l.0 was assumed by Anderson to be the maximum efficiency a pump

    can attain regardless of size.

    Centrifugal pumps have often been used to pump oils and some rather viscous

    liquids. Typical centrifugal pump performance curves are:

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    The maximum efficiency tend to decline with the viscosity . Typical values are:

    / Water : 1 10 100 1000

    max; 0.85 0.76 0.52 0.11

    Beyond

    300

    Water

    , the loss of efficiency is so great that positive

    displacement pumps are to be preferred.

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    Specific speed

    A design parameter which is used by engineers in the selection of pumps is a

    quantity known as the specific speed Ns.

    For a given series of homologous pumps

    the specific speed Ns is obtained by

    eliminating the size factorDbetween CQand

    CHto give :

    =/()/ =//

    (4-14)

    Moreover, the specific speed Nsis defined at thepoint of best efficiency (BEP).

    Nscharacterizes the homologous pump series independent of the pump sizes.

    For another homologous series of pumps (a different geometrical design), CQ*

    and CH* are most probably different so that the specific speed Nswill be different.

    Specific speed Nsversus Optimal pump design

    CQ

    CH*

    CH

    CQ*

    B. E. P

    = =(

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    The figure below shows the relationship between specific speed Ns (rad.) and

    optimal pump design.

    Dimensionless specific speed,Ns(rad)

    Variation of hydraulic pump impeller design

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    Thus if an application has an estimatedNsof 1.0 and a flowrate of 0.8 m3s-1, a

    suitable pump would be of the mixed-flow design. Such a pump is likely to have

    a maximum efficiency (at its BEP) in excess of 90%.

    As Ns increases, the optimal pump design changes from one of radial-flow

    (centrifugal-pump) design to mixed-flow design and to axial-flow design

    (propeller pump).

    When using specific speed Nsdata supplied by others, it is important to know

    what are the units involved in its definition. In the following example, Ns is

    defined as

    = 1/3/4 = [rpm] [gal/min]1/[ft]3/4

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    EXAMPLE: We want a pump to deliver a flowrate of Q = 0.2 m3/s with a head

    of 1.83 m of water. We have a motor which runs at 800 rpm. What type of pump

    should we use (for good efficiency)? Estimate the power required.

    SOLUTION:

    = 800 260

    (0.2)1/

    (9.81 1.83)3/4 = 4.29 (0.683 )TheNsversuschart on page 42 indicates that we should use an axial or propeller

    pump. An efficiency of about 80 per cent is expected. The power given to the

    water is

    P =QgH

    = 1000 x 0.2 x 9.81 x 1.83

    = 3.59 kW

    The shaft power is

    =3.59

    0.8= 4.49

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    5. Matching of Pump and System Requirements

    5.1 System Head Curve

    The System refers to that part of the set-up without the Pump.

    To transport water from reservoir A to reservoir B, we need to supply energy

    (1) to meet the static head rise due to increase in elevation:

    = (5-1)(2) to overcomefrictional losses along the conveying pipes:

    =2 +2 (5-2)

    Pump

    Suction

    side

    Delivery

    side

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    where fi: friction factor for the flow in pipe i ,

    Li: length of pipe i ,

    di: diameter of pipe i ,

    kj: loss coefficient of thej-th valve, bend, joint etc.

    Since flow velocities Vi , Vj Q (velocity = Q / X-sectional area), the total

    frictional head losses hfQ2 or

    (5-3)

    The head (energy) requirement of the system delivering a flowrate of Q is

    therefore given by :

    (5-4)

    which is a quadratic curve in theH versus Qplot.

    hf= KQ2

    Hsys= z+KQ2

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    5.2 Equilibrium Operating Point

    In delivering water at the flowrate of Q , the pump must supply this amount of

    head. At an equilibrium (steady-state) operating point, the head (energy)

    supplied by the pump must exactly match what the system requires. Thus

    The equilibrium operating point is determined by the intersection of the pump

    and system characteristics curves.

    The system characteristics curve can be altered by changing the setting of the

    valve if one is available. The flowrate Q is changed by the adjustment to the valve.

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    5.3 Pumps in parallel

    If one pump gives sufficient head but too little discharge, two or more of the same

    or different pumps may be used in parallel.

    To determine the Head versus Flowrate curve (H vs Q) forpumps in parallel, we

    add their flowrates for given head.

    Two identical pumps in parallel

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    Check valves (which allows flow in only one direction) are usually employed for

    pumps operating in parallel to prevent backflow through the other pump when

    one pump is operating.

    Two non-identical pumps in parallel

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    Power requirement forpumps in parallel:

    =

    (

    ) +

    (

    ) =

    ()

    (

    )

    +

    ()

    (

    )

    (5-5)

    = (5-6)

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    5.4 Pumps in Series

    When the discharge rate of one pump is adequate but the head is too low, pumps

    can be arranged in series to increase the head. In series arrangement, the deliveryside of one pump is connected to the suction (inlet) side of the pump that follows.

    For pumps arranged in series, we add the heads delivered by the pumps for given

    flowrate.

    Pumps in Series

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    Power requirement forpumps in series:

    =

    (

    ) +

    (

    ) =

    ()

    (

    )

    +

    ()

    (

    )

    (5-5)

    = (5-6)

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    6. Cavitation

    6.1 The Physical Phenomenon of Cavitation

    Cavitation is the name given to the physical phenomenon which consists of the

    formation of tiny bubbles in a liquid as a result of a fall in the absolute pressure

    within the liquid.

    At least twophysical processes are known to be responsible:

    1. reduction in absolute pressure causes air and gases initially dissolved inthe liquid to come out of solution.

    2. when the absolute pressure is near or below the vapour pressure (pvap) ofthe liquid at the prevailing temperature, vaporization of the liquid occurs

    rapidly leading to the formation of vapour bubbles-Boiling.

    Process (1) normally precedes process (2) as the pressure is reduced. The bubbles

    produced are generally very tiny.

    Cavitation usually begins at the point of lowest absolute pressure in a system.

    In a pumping situation, the point of lowest absolute pressure is normally at theinlet to the pump.

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    When the cavitation bubbles move with the liquid to a region of higher absolute

    pressure, such as inside an impeller, they collapse. The collapse of a vapour

    bubble (an implosion):

    1. may produce locally very high pressure (up to 1000 atmosphere).

    2. may produce locally very high temperature (up to 800 K).

    3. sound is produced.

    4. light may be emitted (sono-luminescence).

    It is interesting to note that the collapsing bubbles have a tendency to be attracted

    to solid surfaces (Bjerknes effect). Near the end of the collapse, the bubbles may

    actually develop a tiny liquid jet that impacts the solid surface with great local

    pressure. The en-mass collapse of cavitation bubbles is accompanied by a

    distinctive crackling noise.

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    Beauty of cavitation: spiral bubble sheets form from the surface of a marinepropeller

    Ugliness of cavitation: Collapsing bubbles erode a propeller surface

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    6.3 Nett Positive Suction Head (NPSH)

    Applying the steady-state energy equation between the pump inlet and a point on

    the surface of the reservoir: () =or

    + () = + + 2which leads to

    = (

    )

    2 where hsuc=zi-zr, is termed the static suction lift.

    We require the pump inlet pressure pi>Pvap to avoid cavitation.

    (6-1)

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    The following quantity, which has the dimension of head,

    =

    ()

    2

    may be used a measure of the tendency for cavitation to set in at the pump inlet.

    The following quantity is termed theNett Positive Suction Head (NPSH) :

    = + 2 = () Pump manufacturers frequently supply data on the required NPSH necessary to

    prevent cavitation in their pumps.

    To avoid cavitation, the engineer must design his system so that the NPSH at

    pump inlet is greater than the required NPSH at all times during operation.

    (6-2)

    (6-3)

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    From (6.3), we can overcome the problem of cavitation by making the suction

    lift hsucsufficiently negative (i.e. pump placed below the level of the reservoir).

    We can also apply Dimensional Analysis to obtain a new dimensional parameter

    (6-4)

    (6-5)

    The scaling law forNPSH is

    ()()1 =1 1

    as for pump head.

    (6-6)

    = ()

    = ,,

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    6.4 Other Cavitation Parameters

    Other cavitation parameters used in the literature are :

    1. The cavitation index

    = 12

    2. The Thoma cavitation coefficient

    = 3. The Suction Specific Speed

    = 1/[()]3/4

    We note that =3/4

    (6-7)

    (6-8)

    (6-9)

    (6-10)

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    Chapter 2

    Potential Flow

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    References

    Karamcheti, K.Principles of ideal-fluid Aerodynamics, John Wiley, New York

    Fox, R.W. & McDonald, A.T. Introduction to Fluid Mechanics, John Wiley,New York)

    Green, S. I.Fluid Vortices, Kluwer Academic Publisher

    Massey, B. S. Mechanics of Fluids, Van Nostrand Reinhold Co.

    Schlichting, H.Boundary Layer Theory,

    Shames, I. H.Mechanics of Fluids, McGraw Hill International

    Valentine, H. R.Applied Hydrodynamics, Butterworths, London

    White, F. M.Fluid Mechanics, McGraw Hill International

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    surprising close to the actual ones. In any event, they give valuable insight to

    the actual behaviour of the fluid.

    Patching viscous and inviscid flow regions. Potential theory that we are

    going to study does not apply to the boundary layer regions.

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    For Example:

    (a) Consider flow over a flat plate

    Assuming potential flow, the flow pattern would look as shown below

    Flow

    Wall

    Flow

    Wall

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    (b) Flow around a circular cylinder.

    Assuming potential flow, the flow pattern would look as shown below

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    Hele-Shaw flow past a circle. Dye shows the streamlines in water flowing at

    1mm per second between glass-plates spaced 1 mm apart. It is at first sight

    paradoxical that the best way of producing the unseparated pattern of

    plane potential flow past a bluff object, which would be spoiled by

    separation in a real fluid of even the slightest viscosity, is to go to the opposite

    extreme of creeping flow in a narrow gap, which is dominated by viscous

    forces.

    Circular cylinder atR = 10,000. The drag coefficient consequently remains

    almost constant and drops later when the boundary layer becomes turbulent

    at separation.

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    If we have a more streamlined looking body (aerofoil), the wake would be muchsmaller

    Assuming potential flow, the flow pattern would look as shown below

    Hence in many cases, classical hydrodynamics gives GOOD

    APPROXIMATION to flow in REAL FLUIDS.

    We will now develop a number of concepts which will be used in

    potential flow. Attention will be confined almost entirely to STEADY

    TWO DIMENSIONAL FLOW.

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    Hele-Shaw flow past an inclined airfoil. Dye in oil shows the streamlines of

    plane potential flow past an NACA 64AOI5 airfoil at 13 angle of attack.However, because the Hele-Shaw flow cannot show circulation, the Kutta

    condition is not enforced at the trailing edge. Hence infinite velocities are

    represented there. The model is between glass plates 1 mm apart.

    Symmetric plane flow past an airfoil. An NACA 64A015 profile is at zero

    incidence in a water tunnel. The Reynolds number is 7000 based on the

    chord length. Streamlines are shown by colored fluid introduced upstream.

    The flow is evidently laminar and appears to be unseparated, though one

    might anticipate a small separated region near the trailing edge.

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    CONTINUITY EQUATION:

    Consider a small rectangular element, x y in size, through which the fluid

    flows. The average velocities across each face of the element are as shown. For

    an incompressible fluid, volume flow rate into the element equals volume flow

    rate out; thus for unit thickness perpendicular to the diagram

    Vol. flow rate into the element = uyl + vxl

    Vol. flow rate out of the element =

    Continuity states that:

    Vol. flow rate into the element = Vol. flow rate out of the element

    u + u

    x x y 1 + v + v

    y y x 1

    uyl + vxl =

    u +

    u

    x x

    y 1 +

    v +

    v

    y y

    x 1

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    Continuity Equation for 2-D

    For three-dimensional flow, it can be shown that continuity equation is given by

    (1)

    (2)

    u

    x+v

    y= 0

    u

    x

    +v

    y

    +w

    z

    = 0

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    Line Integral of Velocity

    From your earlier lecture, you have learned that work done is by a force F going

    from A to B is given by

    = sindBA Similarly, if we integrate velocity along line AB, line integral of velocity is given

    by

    =

    sin

    d

    BA

    (3)

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    Now, in terms of the velocity components (u, v) in the Cartesian coordinates, it

    can be shown that

    udx + vdy = (Vcos )(dscos) + (V sin)(dssin )

    = Vds(cos cos + sin sin )

    = Vdscos ( - )= Vdscos (90- )

    = Vdssin ()

    Therefore

    sindBA = d + dBA (4)

    V sinds = udx + vdy

    -

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    Circulation

    The circulation denoted by (Greek capital letter 'gamma') is defined as a line

    integral of velocity taken around a closed loop, i.e.

    =

    sin

    d

    =d + dFor example, circulation around an elemental area is

    =d + + dd + dd d= dd=dd

    (5)

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    Where

    (Greek letter xi) = = VORTICITY

    In other words,

    Circulation = Vorticity area (for an elemental area)

    What is the circulation around a finite area?

    Consider a closed curve ABCD within the fluid medium. The circulation around

    such a curve is defined as the summation of the circulations round component

    small circuit.

    Circulation around a Closed Contour

    In other words

    Total circulation =circulation around small area

    or mathematically,

    =d + d = dd

    (6)

    For finite area (7)

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    IMPORTANT NOTES:

    (a)The concept of vorticity may be utilised for distinguishing a flow as eitherIRROTATIONAL or ROTATIONAL. If the vorticity is zero at all points

    in a flow region (except at certain special points known as 'singular points'

    where the velocity or acceleration is zero or infinite), the flow in that region

    is known as IRROTATIONAL.

    (b)If the vorticity is non-zero, the flow is known is ROTATIONAL FLOW(c)Vorticity is a vector quantity whose direction is perpendicular to the plane

    of the small circuit round which circulation is measured.

    (d)In vector form, vorticity is defined as

    =

    V (curl of velocity)

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    As you go once around the in the carousel, you rotate once about your axis

    Or solid body rotation

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    Example: The steady plane flow in

    the figure has the polar velocity

    components v = r and vr = 0.

    Determine the circulation around

    the path shown.

    Solution:Start at the inside right corner, point A, and go around the complete

    path:

    = d = 0( 1) + () + 0(1 ) + 1(1)=( 1)

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    The Concept of Stream Function ()

    The concept of stream function (Greek letter psi) is based on the principle ofcontinuity and properties of a streamline. It is applicable to two dimensional flow

    cases. For incompressible two-dimensional flow, continuity equation gives

    + = 0This equation is satisfied if a function (x,y) is defined such that the above

    equation is defined as + = 0

    Comparing the above two equations show that this new function must be

    defined such that

    = = Note: Stream function is a scalar quantity and is considered positive according to

    sign convention.

    1. Convention

    (a) anticlockwise is positive

    (b) clockwise is negative

    2. The direction of normal goes from left to right when facing the positive

    direction

    or

    +

    = 0

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    Geometric Interpretation of

    It can be shown that lines of constant are streamlines. Consider a streamline as

    shown below.

    or udy vdx = 0 streamline

    Introducing the stream function from above, we have

    + = 0 =Thus the change of is zero along a streamline, or

    There is also a physical interpretation which relates to volume flow. From the

    figure below, we can compute the volume dQ through an element ds of the

    control surface of unit depth.

    =

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    Volume flow rate through an element ds of unit thickness is given by

    dQ = Vds

    = (udy - vdx)

    but

    =

    =

    therefore dQ =y dy +x dx

    = d

    In other words the change in across the element is numerically equal to the

    volume flow through the element. Conversely, the volume flow between any two

    points in the flow is equal to the change in stream function between those points.

    Q1 =1

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    The difference inbetween two points = volume flux cross any line joiningthe two points.

    Further, the direction of the flow can be ascertained by noting whether increases or decreases.

    i.e.

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    SUMMARY:

    Therefore, we get inCartesian coordinates,

    Inpolar coordinates,

    It can be shown that

    =

    1 =

    u

    v

    y

    x

    (8)

    (9)

    (10)

    y

    x

    u'v'

    = =

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    Example:

    In a two-dimensional incompressible flow, the fluid velocity components aregiven by u = x - 4y and v = -y - 4x. Determine the stream function of the flow as

    well as vorticity.

    We know that

    Integrating the above gives

    or

    Similarly

    u =

    v =x

    y = 4

    =( 4) = xy 2y + f(x)

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    The above two equations are compatible only if

    The vorticity is given by

    Therefore

    x=( 4)

    =( 4) = xy + 2x + g(y)

    = xy + 2x

    2y

    =vx uy

    v

    x

    =4 and u

    y

    =4 =4 (4) = 0 (irrotational flow)

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    Example:

    A two-dimensional flow field is described by = x - y2. Calculate the horizontal

    and vertical components of velocity and an expression for velocity of flow at any

    point in flow field. State whether the flow is rotational or irrotational, and

    determine the volume flow rate between (x1, y1) = (1, 2) and (x2, y2) = (1, 3).

    Sketch the streamlines for = 0, l and 2.

    The horizontal and vertical components of velocity are given by

    But = x y2, and hence

    u = -2y v = -l

    The resultant velocity is

    The vorticity is given by

    Since the vorticity is not zero, the flow is rotational. Volume flow rate (Q) is

    given by

    Q = 2- 1

    = (1 - 32) - (1 - 22) = -5 units

    u = y v =x

    V =u + v =(2y) + (1) =1 + 4 y

    = v

    x u

    = 0 (2) = 2

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    From the earlier part of the lecture, the VORTICITY EQUATIONwas shown to

    be

    Substituting equations (8) and (9) intothe above equation.

    we get

    If the flow is IRROTATIONAL, Vorticity () = 0

    Or :.

    2= 0 (which is a Laplace's Equation)

    The above equation shows that for an irrotational flow, the stream function must

    also satisfied the Laplace Equation. Conversely, fluid-flow problems which do

    not satisfy Laplace equation in are ROTATIONAL.

    (6) =

    v

    x u

    v

    x=

    x

    x

    =

    x

    uy = y y = y =

    vx uy =x + y

    x + y = 0

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    IMPORTANT NOTE:

    One very important property of Laplace's equation is that it is LINEAR. This

    means that if we have a series of simple solutions, 1, 2, 3, .. etc, then the

    more complex solution can be obtained by

    (x, y) = 1(x, y) + 2(x, y) + 3(x, y) + .

    Let us now study some simple solutions. More complex solutions can be obtained

    from sum of simple solutions.

    PARALLEL FLOW

    From equation

    y = u

    x =

    v

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    Hence

    where 1 and 2are functions of integration. These equations are compatible

    only if

    2(x) = k (constant)

    Therefore, = Uy + k

    The value of k is arbitrary and is usually set to 0 for y = 0. Hence

    = Uy for flow parallel to the x-axis

    y = u

    x = v = 0 =1(y) = U y +(x)

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    SOURCE

    Consider point source

    For steady flow,

    u'(2r)l = Q = volumetric flow/unit length

    assume unit length

    From equations (10)

    (11a)

    (11b)

    u = 2

    v = 0

    r =1 =

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    Substituting 11(a) and 11(b) into above equations, we get

    These equations are compatible only if

    Usual to put k = 0 when = 0

    in Polar Coordinates (12)

    or

    in cartesian coordinates (12a)

    Note: Artan is the same as tan inverse.

    r= 0

    1 = 2 =1() =

    2

    +(r)

    (r) = k =

    2

    +

    = 2

    = 2 Artan

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    SINK

    Similarly it can be shown that the stream function for a sink is given by

    in Polar Coordinates (13)

    in Cartesian Coordinates (13a)

    =2

    =2 Artan

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    POINT VORTEX (or POTENTIAL VORTEX)

    Also known as irrotational vortex orfree vortex.

    From equation (5), circulation is defined as

    =sindFor a potential vortex:

    Integration of the above equations gives

    (14)

    v =r = 2

    =2rvor v =

    2

    u = 0 = 1 = 0

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    IMPORTANT NOTE:

    The reason why a potential vortex is also called an irrotational vortex is because

    the circulation around any contour not surrounding the origin is zero

    Proof:

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    Circulation around a potential vortex (excluding the origin)

    The velocity (v') at A and D =r

    The velocity (v') at Band C =

    (r+dr)

    Note: there is no u' component

    Segment AD = rd

    Segment BC = (r + dr)d

    Therefore circulation around ABCDA =

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    Circulation around a forced vortex:

    The velocity (v') at A and D = Kr

    The velocity (v') at B and C = K(r+dr)

    Note: There is no u' component

    Segment AD = rd

    Segment BC = (r + dr)d

    Therefore circulation around ABCDA =

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    (d) A vortex

    Tornado Waterspout

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    Helmholtz Theorem: The circulation around a vortex filament is constant.

    (for proof of the theorem, see Fluid Vortices, edited by S.L Green)

    In other words, if a vortex filament comes to a waist, where the filament cross-

    sectional area is minimal, the average vorticity over that cross-section must be

    maximal, and conversely for a broadening of the tube. A related observation is that

    vortex tube cannot terminatein a fluidbecause constancy of circulation would not

    be achieved. Vortex tubes are thus constrained to forming loopsentirely within a

    fluid, or terminating at a solid boundary.

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    Kelvin's Theorem: states that the circulation around a material loop is

    time-independent, provided the fluid is inviscid, only subject to potential body

    forces, and its pressure is a function of density alone,

    i.e.

    (for proof of this theorem, see Fluid Vortices, edited by S.I. Green)

    DDt

    = 0

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    COMPLEX FLOWS:

    SOURCE AND UNIFORM FLOW

    For uniform flow 1= -Uy

    For source

    New flow

    =1+ 2

    We now look at the velocity components, this gives

    (keeping in mmd that )

    (15)

    =

    Uy +

    2Artan

    d(Artan q)

    ds=

    1

    1 + q dqds

    = Q2 or Q2Artan yx

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    (16)

    Similarly

    (17)

    Stagnation Point is defined as a place where u = v = 0 and is located at x0, y0.

    From equation (I7)

    y0= 0 since v = 0 at y = 0

    Therefore stagnation point lies on x-axis

    From equation (16)

    x0 = Q2U

    Therefore, Stagnation point is located at

    (this is obtained by putting y = 0 and

    solve for x)

    Q2U , 0

    u =

    y

    =U + Q

    2

    1

    1 +

    y

    x

    1

    x

    u =U + Qx2(x + y)v =

    x

    =Q2 1

    1 + yx

    y

    x=

    Qy

    2(x + y)

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    Let us now locate streamline where = 0

    = 0 =Uy + Q2

    Artan yx

    Here we note that the solution has two branches one is when: y = 0

    The other is when x = ycot2Uy

    Q ()

    This is a curve which looks like

    For

    : x is indeterminate since x =

    0

    0

    we need to use LHospitals rule to find x

    x = lim=0 ytan 2yU

    Q

    x = lim

    =01

    2U

    Q sec 2yU

    Q

    R

    y

    0 P x

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    =Q2U(see x0from before)

    HENCE the curve passes through stagnation point.

    For the coordinates ofR:

    Put x = 0 in equation (17a), we get

    2UyQ

    = 2

    When x ,

    Since no fluid can cross a streamline, now any streamline may be replaced by a

    solid boundary.

    y = Q

    4U

    2UyQ

    y Q

    2

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    Hence, we could say that we have solved for flow about a body whose shape is

    given by

    (18)

    and is in a uniform flow field U.

    x = ycot2Uy

    Q

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    SOURCE - SINK PAIR

    For source:

    For sink:

    Therefore, combine flow

    or (19)

    Therefore if is constant then = constant.

    From geometryPmust lie on a circle passing through A and B

    A = QA2

    B=

    QB2

    =A +B=

    Q2 (A B)

    =

    Q

    2 where

    = (

    A B)

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    In rectangular coordinates

    tanB = yx + s

    tan

    A=

    y

    x s

    tan(A B) = 2syx + y s

    Hence,

    (20)

    =

    Q

    2=

    Q

    2tan

    12sy

    x + y s

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    A SOURCE-SINK PAIR IN UNIFORM FLOW

    Source-sink pair:

    Uniform flow (from right to left):

    Combined flow:

    Express in Cartesian coordinates

    A = Q2 (A B)

    B=

    Uy

    =A +B=

    Q2 (A B) Uy ()Let = (A B)

    tan = tanA tanB1+ tanAtanB = Artan tanA tanB

    1+ tanAtanB

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    = 0 when y = 0

    or if

    (22)

    This is an equation of an OVAL shaped curve whose shape depends on

    parameter (Uy/Q) and it "scales" with s, i.e. if you double s, you double all

    other dimensions.

    = Artan yx yx + 1 +

    yx

    =Uy + Q2Artany

    x yx + 1 +

    yx

    yx yx + s1 +

    yx = tan

    2UyQ

    2yx

    + y = tan2UyQ

    x + y = 2sy cot2UyQ x + y 1 = 2 y cot 2 UsQ

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    In Cartesian coordinates

    =

    2y

    x + y (doublet)

    r

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    A DOUBLET IN UNIFORM FLOW: Flow past a circular cylinder

    For a doublet:

    or

    For uniform flow (right to left):

    Combined flow (24)

    The streamline = 0is given byy = 0

    or (equation of a circle with radius a)

    A =

    2

    y

    x + y= Qs yx + yB =Uy

    =Uy + Q yx + y

    x + y = QU = awhere a =

    Q

    U122

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    Hence we have a circular boundary

    Rewriting equation (24) in term of a and polar coordinates

    (25)

    Stream function of a cylinder placed in a free stream going from right to left

    =1

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    Pressure Distribution on cylinder:

    From equation (25)

    = 1

    =cos 1

    = =sin 1 + on the surface of the body, i.e. r = a

    u = 0

    and v'= 2U sin(which is maximum at = 90and 270)

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    Applying Bernoulli's equation

    + 12 = + 1

    2( + )

    + 1

    =

    +1

    ( 0 + 4

    sin

    )

    i.e.

    = + 12(1 4sin)

    = 12

    = (1 4sin)

    In other words, is a function of only.Note:

    (i) At S, = 0or 180,Therefore sin

    = 0

    free stream static pressure

    static pressure at cylinder

    Pressure coefficient

    CP= 1

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    (ii)

    Therefore,

    Therefore, if holes are drilled at = 30and 150, they can be used to measurefree stream static pressure.

    (iii)

    sin= lTherefore

    At = 6

    (. .30) 56

    (. . 150)sin

    =

    1

    2 sin

    =

    1

    4

    CP= 0 i.e. P= P

    At

    =

    2(

    .

    .90)and

    3

    2(

    .

    . 270)

    CP= -3

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    Lift = sin0 Drag = cos0

    It can be shown that for a potential flow past a circular cylinder that

    Lift = 0

    Drag = 0

    The above results, which is based on ideal-flow analysis, show that a cylinder

    placed in a free stream experiences no drag force. In fact, it can be shown from

    the above theory that any SYMMETRICAL BODY placed in a free stream along

    the axis of symmetry should experience no drag force.

    D'Alembert Paradox:

    Even though the above analysis shows that a cylinder or any symmetrical body

    placed in a free stream experiences no drag force, however, in real life (viscous

    fluid), the body does experience a drag. This paradoxical behaviour is referred

    to asD'AlembertParadox

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    FLOW WITH CIRCULATION ROUND A CIRCULAR

    CYLINDER IN UNIFORM FLOW

    As discussed earlier, flow past a circular cylinder generates no lift. In order to get

    lift, we need to introduce circulation to the cylinder. This can be achieved by

    using point vortex.

    + =

    Flow past a cylinder Point vortex Flow past rotating cylinder

    For flow past a circular cylinder:(note: the flow is from right to left)

    For a point vortex (anticlockwise):

    = 1

    =

    2

    ln

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    Combined flow:

    On the surface of cylinder, r = a

    u' = 0

    At stagnation point u' = v' = 0

    Put = 0

    =

    sin

    1

    2

    ln

    (

    )

    u = 1 =cos 1 v =

    =sin 1 +

    + 2

    1

    v = 2sin + 2

    2

    sin

    0+

    2= 0

    =A +B

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    or sin0 =4 ()

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    ||

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    || =

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    No real solution exist on r = a,

    :. we need to go somewhere else for stagnation point

    If r a, cos = 0 or sin= 1.In other words, stagnation point lies on y-axis,

    but why on y-axis??

    v' = 0

    For sin= -1

    This has real roots if > 4Ua

    For || >

    At stagnation point, u = 0 = 1 cos

    sin 1 + + 2 = 0

    1 + + 2 = 01 + 2 = 0

    2+

    = 0

    = b b 42 where b =2 , = 1, =

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    For sin = 1, no real roots (exercise: show this)

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    =sin20

    =sin + 12 4sin3 + 2sin + 4 sin0 d

    =

    sin

    +

    1

    2

    (3sin

    sin3

    ) +

    (1

    cos2

    ) +

    4

    sin

    0d

    =1

    2 []0

    =1

    2 2

    Therefore

    Hence for finite span b

    (28)

    Note:

    (a) L generated by circulation here is called Magnus Effect.(b) L is perpendicular to U.

    L = U (lift per unit length)

    L = U b

    L = U (lift per unit length)

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    (c) L is independent of the radius "a" of the cylinder. Therefore a linevortex of strength , moves with velocity U will also experience a

    lateral force (perpendicular to U) of U /unit length of vortex.

    (d) Real life examples of Magnus Effect are spinning of a golf ball, or tabletennis ball or lawn tennis ball.

    137

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    The experimental Flettner rotor sailboat at the University of Rhode Island.

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    THE CONCEPT OF VELOCITY POTENTIAL

    The velocity potential is represented by (Greek letter phi) and is defined by the

    following expression

    d

    =

    sin

    d

    Then = sind or

    dd

    =sin(in streamline coordinate)

    In Cartesian coordinate, it can be shown that

    dd =; dd =; dd =

    Alternatively, the velocity potential

    can be defined from the condition of

    irrotationality.

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    If the flow is irrotational, the vorticity () = 0

    but =x V = 0 (curl of velocity)

    where

    =

    +

    +

    From vector algebra x V = 0 where is a scalar function. Compare thisequation with the one above show that

    V = dd =; dd =; dd =

    Hence is the potential function of velocityQuestion: What equation does

    obey?

    From the continuity equation

    + = 0Since u =

    and

    =

    Therefore = and =

    substituting these into the continuity equation, we get

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    or

    Same rules apply, i.e

    (1) It is linear

    (2) Complex solutions can be obtained from the addition of simple solutions.

    Note:

    (1)By definition, the existence of potential function implies that the flow isirrotational, i.e. vorticity = 0.

    (2)and are given byCartesian Co-ordinates:

    Polar Co-ordinates:

    Hence like , follows LAPLACE'S EQUATION.

    (30)

    (31)

    (32)

    (33)

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    Relationship between stream function () and potential function ()

    In the previous section, it was learned that lines of constant formed a set of

    streamlines. We are now going to show that lines of constant or potential lines,

    form a family of curves which intersect the streamlines at right angle.

    From calculus, it can be shown that,

    For a line of constant , d=0.

    Solving for the slope, we get

    Similarly, for stream function

    For the line of constant (streamline), we get

    x dx + y d y = 0

    d = x dx + y dy

    dydxconstant =

    xy =u

    v

    d

    =

    xdx +

    ydy

    x dx + y d y = 0

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    Hence

    Therefore lines of constant is perpendicular to lines of constant . The two setsof curves hence form an ORTHOGONAL GRID SYSTEM or FLOW NETS

    dydxconstant = 1dy

    dxconstant

    dydxconstant =

    x

    y

    =v

    u

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    Examples:

    In a uniform flow field

    Sink

    Point vortex

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    Doublet

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    147

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    Method of Images

    The previous solutions have all been for unbounded flows, such as a circular

    cylinder immersed in a broad expanse of uniformly streaming fluid. However,

    many practical problems involve a nearby rigid boundary constraining the flow.

    For example, (1) an aerofoil near the ground, simulating landing or take off, or

    (2) a cylinder mounted in a wind tunnel with narrow walls. In such cases the basic

    unbounded-potential-flow solutions can be modified for wall effects by the

    method of images.

    Consider a line source placed a distance from a wall as shown below. To create

    the desired wall, an image source of identical strength is placed the same distance

    below the wall. By symmetry the two sources create a plane-surface streamline

    between them, which is taken to be the wall.

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    Determination of forces acting on the wall

    Therefore, the combined flow field is given by =1+ = Q2 ( 1+ )tan 1 = y h

    x=

    rsin hrcos

    tan

    =

    y + h

    x

    =rsin

    + h

    rcos

    where

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    A Point Vortex Near A Wall

    For a vortex near a wall, an image vortex of the opposite rotation must be locatedthe same distance below the wall. But of course the pattern could also be

    interpreted as the flow near a vortex pair in an unbounded fluid.

    The pressure distribution, due to the vortex, along the wall can be determined ina similar fashion as the one shown above.

    A Point Sink Near A Wall

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    A Source Trapped In A Corner

    The number of image vortices required to simulate the flow is as shown below.