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    1Ir. Chong Kok Chung UEME 2123 Fluid Mechanics I

    Basic Properties of Fluids

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    Reference BooksMain textbook : Fundamental of Fluid Mechanics

    (7 th Edition SI

    !uthor(s : Munson" #kiishi" $oun% and

    Rothma&er

    Publisher : 'ile& !sia Student Edition

    2

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    3

    !ssessment est ) : )*+ ('eek 7" )7 th ,ul& -*)." Sunda&"/:0* to 1:0*am

    est - : )*+ ( entati2el& 'eek ))

    !ssi%nment : )*+ ('eek )0" -- nd !u%ust -*).

    3ab Report : )*+

    Final Exam : .*+ (4losed book examination

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    4on2entional !reas

    !erospace!utomoti2ePropulsion

    'h& Stud& Fluid Mechanics

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    'ind En%ineerin%

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    !ir 4ond and 5entilation

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    !ero6acoustics

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    Biotechnolo%&

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    Irri%ation and &droelectric

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    10

    Main opicsSome 4haracteristics of Fluids8imensions and 9nits!nal&sis of Fluid Beha2iorsIdeal as 3a;

    Fluid Properties4ompressibilit& of Fluids5apor PressureSurface ension

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    11

    4haracteristics of Fluids'hat is a Fluid<

    'hat is the di=erence bet;een a Solid and a Fluid<

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    Fluids comprise the liquid and gas (or apor! phase o" the ph#sical "orms.

    $ "luid is a su%stance that de"orms continuousl# under theapplication o" a shear stress no matter ho& small the shear stressma# %e.

    $ shearing stress is created &hene er a tangential "orce acts on a

    sur"ace.

    12

    8e>nition of Fluid

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    'hen a constant shear "orce is applied

    )olid de"orms or %ends

    Fluid continuousl# de"orms.

    13

    Fluid and Solid

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    *ague idea

    Fluid is so"t and easil# de"ormed.)olid is hard and not easil# de"ormed.

    Molecular structure)olid has densel# spaced molecules &ith large intermolecularcohesi e "orce allo&ed to maintain its shape.

    14

    Fluid and Solid

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    )ome materials+ such as slurries+ tar+ putt#+ toothpaste+ and so on+

    are not easil# classi"ied since the# &ill %eha e as solid i" theapplied shearing stress is small+ %ut i" the stress e,ceeds somecritical alue+ the su%stance &ill "lo&. -he stud# o" such materialsis called rheology .

    15

    Fluid and Solid

    h

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    ualitati e aspect

    uantitati e aspect

    'hat is ualitati e and 'hat is uantitati e/'hat is ualitati e and 'hat is uantitati e/

    16

    4haracteristic 8escription" 8imensionand 9nits

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    ualitati e aspect ser es to identi"# the nature+ or t#pe+ o" thecharacteristics ( such as length+ time+ stress+ and elocit#! .

    ualitati e description is gi en in terms o" certain primaryquantities, such as Length, L, time, T, mass, M, andtemperature, θ . -he primar# quantities are also re"erred to as

    %asic dimensions .

    -hese primar# quantities can then used to pro ide a qualitati edescription o" an# other secondary quantity : "or e,ample+ area 0

    2+ elocit# 0 - 1 +densit# 0 M 3.

    17

    ?ualitati2e !spect

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    ro ide a numerical measure o" the characteristics.

    4equire %oth a num%er and a standard.

    $ standard "or length might %e a meter or "oot+ "or time an houror second+ and "or mass a slug or kilogram.

    )uch standards are called units.

    18

    ?uantitati2e !spect

    d d

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    rimar# quantities also re"erred as %asic dimensions

    )uch as ength+ + time+ -+ mass+ M+ and temperature+ 5.

    Used to pro ide a qualitati e description o" an# othersecondar# quantit#.

    )econdar# quantitiesFor e,ample+ area 0 2+ elocit# 0 - 1 +densit# 0 M 3.

    19

    Primar& and Secondar&?uantities

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    Mass6M7+ ength6 7+ time6-7+ and -emperature6Mass6M7+ ength6 7+ time6-7+ and -emperature6 θ 77

    MLT systemMLT system

    Force6F7+ ength6 7+ time6-7+ and -emperature6Force6F7+ ength6 7+ time6-7+ and -emperature6 θ 77FLT systemFLT system

    Force6F7+ Mass6M7+ ength6 7+ time6t7+ and -emperature6Force6F7+ Mass6M7+ ength6 7+ time6t7+ and -emperature6θ 77FMLTFMLTθ systemsystem

    20

    S&stem of 8imensions

    8imensions !ssociated ;ith 4ommon Ph&sical

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    21

    8imensions !ssociated ;ith 4ommon Ph&sical?uantities

    8i i ll&

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    2

    2 gt d =

    22

    $ll theoreticall# deri ed equations are dimensionally

    homogeneous 8 that is+ the dimensions o" the le"t side o" theequation must %e the same as those on the right side+ and alladditi e separate terms ha e the same dimensions.

    9eneral homogeneous equation alid in an# s#stem o" units.

    4estricted homogeneous equation restricted to a particulars#stem o" units.

    21.1: t d =

    Valid only for the system ofValid only for the system of

    units using feet and secondsunits using feet and seconds

    8imensionall&omo%eneous

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    In addition to the qualitati e description o" the arious quantities

    o" interest+ it is generall# necessar# to ha e a quantitati e measureo" an# gi en quantit#.

    For e,ample+ i" &e measure the &idth o" this page in the %ook and sa#that it is 1; units &ide+ the statement has no meaning until the unit o"

    length is de"ined.

    I" &e indicate that the units o" length is a meter+ and de"ine themeter as some standard length+ a unit s#stem "or length has %een

    esta%lished.$ unit must %e esta%lished "or each o" the remaining %asic quantities.

    23

    S&stems of 9nits

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    ength "t

    -ime secondForce l%-emperature oF or o4 o4 0 oF=>?@.:AMass slug 1 l% 1 slug B 1 "t sec 2

    9ra it# g 32.1A> "t sec2 'eight ' (l%! 0 m (slug!B g ("t sec 2!

    25

    British ra2itationalS&stem

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    ength m

    -ime secondMass Kg-emperature o K o K o C=2A3.1?Force De&ton 1 D 1 KgB1 m sec 2

    'ork oule ( ! 1 DBmo&er 'att ('! ' sec DBm sec

    9ra it# g 0 @.G;A m sec2 'eight ' (D! 0 m (Kg! B g (m sec 2 ! 1 kg mass &eights @.G1D

    26

    International S&stem (SI

    En%lish En%ineerin% (EE

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    Mass l%m

    Force l%"

    ength "t

    -ime second

    -emperatureo

    4 (a%solute temperature!

    27

    En%lish En%ineerin% (EES&stem

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    Ma@or En%ineerin% Blunders 4aused b& Fault&

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    29

    Ma@or En%ineerin% Blunders 4aused b& Fault&Measurement

    4on2ersion Factor

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    30

    4on2ersion Factor

    4on2ersion Factor

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    31

    4on2ersion Factor

    S& f 9 i

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    M -t

    International )#stem (kg+ m+ s+ oK!

    F -t

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    )I (kg+ m+ s+oK!

    1D 0 1kgm s 2

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    34

    $ tank o" liquid ha ing a total mass o" 3: kg rests on a support in theequipment %a# o" the )pace )huttle. Hetermine the "orce (in ne&tons! thatthe tank e,erts on the support shortl# a"ter li"t o"" &hen the shuttle isaccelerating up&ards as sho&n in the "igure at 1?"t s 2 .

    Example )A) B and SI9nits

    Example )A) B and SI

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    35

    $ tank o" liquid ha ing a total mass o" 3: kg rests on a support in theequipment %a# o" the )pace )huttle. Hetermine the "orce (in ne&tons! thatthe tank e,erts on the support shortl# a"ter li"t o"" &hen the shuttle isaccelerating up&ards as sho&n in the "igure at 1?"t s 2 .

    Example )A) B and SI9nits

    N

    a g m F

    maW F or am F

    f

    f

    ?1G

    7!3;>G.;61?G1.@(3:

    !(

    =

    +=

    +=

    =−=∑

    ! l& i f Fl id B h 2i

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    $nal#sis o" an# pro%lem in "luid mechanics necessaril# includesstatement o" the %asic la&s go erning the "luid motion. -he %asicla&s+ &hich applica%le to an# "luid+ are

    Conser ation o" mass

    De&ton s second la& o" motion

    -he "irst la& o" thermod#namics

    -he second la& o" thermod#namics

    36

    !nal&sis of Fluid Beha2iors

    Measurement of Fluid Mass and

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    Hensit#

    )peci"ic &eight

    )peci"ic 9ra it#

    37

    Measurement of Fluid Mass and'ei%ht

    8ensit&

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    38

    -he densit# o" a "luid+ designated %# the 9reek s#m%ol ρ (rho! + isde"ined as its mass per unit olume .

    Hensit# is used to characteriJe the mass o" a "luid s#stem.In the

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    39

    -he speci"ic &eight o" a "luid+ designated %# the 9reek s#m%ol γ

    (gamma! + is de"ined as its &eight per unit olume.

    Under conditions o" standard gra it# (g0 @.G;Am s 2 0 32.1A> "t s2!+ &ater at :;LF has a speci"ic &eight o" :2.>l% "t 3 and

    @.G;kD m3.

    -he densit# o" &ater is 1.@> slug "t 3 or @@@ kg m3.

    Speci>c 'ei%ht

    g ρ γ =

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    Ideal as 3a;

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    9ases are highl# compressi%le in comparison to "luids+ &ith changes ingas densit# directl# related to changes in pressure and temperaturethrough the equation p=ρRT .

    -he ideal gas equation o" state p=ρRT is a model that relates densit#to pressure and temperature "or man# gases under normal conditions.

    -he pressure in the ideal gas la& must %e e,pressed as an a%solute pressure &hich is measured relati e to a%solute Jero pressure.

    -he standard sea le el atmospheric pressure is 1>.:@@: psi (a%s! or1;1.33k a (a%s!.

    41

    Ideal as 3a;

    5iscosit&

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    -he properties o" densit# and speci"ic &eight are measures o" the

    Nhea inessO o" a "luid.

    It is clear+ ho&e er+ that these properties are not su""icient touniquel# characteriJe ho& "luids %eha e since t&o "luids can ha e

    appro,imatel# the same alue o" densit# %ut %eha e quitedi""erentl# &hen "lo&ing.

    -here is apparentl# some additional propert# that is needed to

    descri%e the N"luidit#Oo" the "luid.

    42

    5iscosit&

    Fluidit& of Fluid

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    43

    Po& to descri%e the N"luidit#O o" the "luid/-he %ottom plate is rigid "i,ed+ %ut the upper plate is "ree tomo e.I" a solid+ such as steel+ &ere placed %et&een the t&o platesand loaded &ith the "orce P + the top plate &ould %e displacedthrough some small distance+ δa.-he ertical line $< &ould %e rotated through the small angle+δβ+ to the ne& position $< .

    A p τ =

    Fluidit& of Fluid

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    44

    'hat happens i" the solid is replaced &ith a "luid such as&ater/

    'hen the "orce is applied to the upper plate+ it &ill mo econtinuousl# &ith a elocit# U.-he "luid NsticksO to the solid %oundaries and is re"erred toas the no slip conditions.

    -he "luid %et&een the t&o plates mo es &ith elocit#u=u(y that &ould %eassumed to ar# linearl#+u="y#$ . In such case+ the

    elocit# gradient is du # dy " # $%

    Fluidit& of Fluid

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    γ ∝τ

    45

    In a small time increment+ Qt+ an imaginar# ertical line $< &ouldrotate through an angle+ QR + so that

    tan QR QR≒ Qa %)inceQa U Qt it "ollo&s that QR0 U Qt %QR / SQR QR + t

    He"ining the rate o" shearing strain+ γ + as

    -he shearing stress is increased %# + the rate o" shearing strain isincreased in direct proportion+ or

    d#duµ=τ

    d#

    du

    %

    U

    tlim

    ;t

    ==δ

    δβ=γ →δ

    d#Cdu∝τ

    -he common "luids such as &ater+ oil+ gasoline+ and air. -he shearing-he common "luids such as &ater+ oil+ gasoline+ and air. -he shearingstress and rate o" shearing strain can %e related &ith a relationshipstress and rate o" shearing strain can %e related &ith a relationship

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    5iscosit& and emperature

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    For "luids+ the iscosit#decreases &ith an increasein temperature.For gases+ an increase intemperature causes anincrease in iscosit#.

    'P /'P /molecular structuremolecular structure

    48

    5iscosit& and emperature

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    -he liquid molecules are closel# spaced+ &ith strong cohesi e"orces %et&een molecules+ and the resistance to relati e motion

    %et&een adVacent la#ers is related to these intermolecular "orce.

    $s the temperature increases+ these cohesi e "orce are reduced&ith a corresponding reduction in resistance to motion. )ince

    iscosit# is an inde, o" this resistance+ it "ollo&s that iscosit# isreduced %# an increase in temperature.

    -he $ndrade s equation & 'e (#T

    49

    5iscosit& and emperature

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    In gases+ the molecules are &idel# spaced and intermolecular

    "orce negligi%le.

    -he resistance to relati e motion mainl# arises due to thee,change o" momentum o" gas molecules %et&een adVacent

    la#ers.

    $s the temperature increases+ the random molecular acti it#increases &ith a corresponding increase in iscosit#.

    -he )utherland equation & CT )#* # (T+S50

    De;tonian and Don6De;tonianl id

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    Fluids "or &hich the shearing stress is linearl# related to the rate

    o" shearing strain are designated as De&tonian "luids a"ter I. De&ton (1:>2 1A2A!.

    Most common "luids such as &ater+ air+ and gasoline are

    De&tonian "luid under normal conditions.

    Fluids "or &hich the shearing stress is not linearl# related to therate o" shearing strain are designated as non De&tonian "luids .

    51

    Fluid

    De;tonian and Don6De;tonianFl id

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    )hear thinning "luids.

    )hear thickening "luids.

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    )hear thinning "luids -he iscosit#

    decreases &ith increasing shear rate 8 the harder the "luid is sheared+ theless iscous it %ecomes. Man#colloidal suspensions and pol#mersolutions are shear thinning. ate,

    paint is e,ample.

    53

    Fluid

    De;tonian and Don6De;tonianFl id

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    )hear thickening "luids -he iscosit#increases &ith increasing shear rate 8 theharder the "luid is sheared+ the more iscous it

    %ecomes. 'ater corn starch mi,ture &atersand mi,ture are e,amples.

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    He"ining kinematic iscosit# ,= ρ

    -he dimensions o" kinematic iscosit# are 2

    -.

    -he units o" kinematic iscosit# in

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    ρ ρ CC d dp

    - - d dp

    . v =−=

    57

    iquids are usuall# considered to %e incompressi%le+&hereas gases are generall# consideredcompressi%le.Compressible of the fluid?$ propert#+ bulk modulus E v+ is used to characteriJecompressi%ilit# o" "luid.

    -he %ulk modulus has dimensions o" pressure. F 2.

    4ompression and Expansion

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    t /o0s p

    tan= ρ

    58

    'hen gases are compressed or e,panded+ the relationship %et&een pressure and densit# depends on the nature o" the process.

    For isothermal process

    For isentropic process t /o0s pk tan= ρ

    , 'here k is the ratio o" the speci"ic heat at constant pressure+ c p+ to the speci"ic

    heat at constant olume+ c ., / p 1 / v 0 R 0 gas constant

    . . vv=p=p

    . . vv=kp=kp

    Speed of Sound

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    ρ ρ v .

    d dp

    / ==

    59

    -he elocit# at &hich small distur%ances propagate in a "luid iscalled the speed of sound .

    -he speed o" sound is related to change in pressure and densit# o"the "luid medium through

    For isentropic process

    For ideal gas

    ρ kP

    / =

    kRT / =

    5apor Pressure and Boilin%

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    I" liquids are simpl# placed in a container open to theatmosphere+ some liquid molecules &ill o ercome theintermolecular cohesi e "orces and escape into theatmosphere.

    I" the container is closed &ith small air space le"t a%o e the

    sur"ace+ and this space e acuated to "orm a acuum+ a pressure &ill de elop in the space as a result o" the apor thatis "ormed %# the escaping molecules.

    'hen an equili%rium condition is reached+ the apor is said to %e saturated and the pressure that the apor e,erts on theliquid sur"ace is termed the VAP ! P!"##$!", p v .

    60

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    Surface ension

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    $t the inter"ace %et&een a liquid and a gas+ or %et&een t&oimmisci%le liquids+ "orces de elop in the liquid sur"ace &hichcause the sur"ace to %eha e as i" it &ere a NskinO or Nmem%raneOstretched o er the "luid mass.

    $lthough such a skin is not actuall# present+ this conceptualanalog# allo&s us to e,plain se eral commonl# o%ser ed

    phenomena.

    62

    Surface ension

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    )ur"ace tension the intensit#o" the molecular attraction perunit length along an# line inthe sur"ace and is designated

    %# the 9reek s#m%ol σ .

    63

    R p p p

    R p R

    e2 σ

    π σ π

    2

    2 2

    =−=∆

    ∆='here'here p p 22 is the internal pressureis the internal pressure

    andand

    p p

    ee is the e,ternal pressureis the e,ternal pressure

    The force due tosurface tension The force due topressure difference=

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    Surface ension E=ects

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    )ur"ace tension e""ects pla# a role in man# "luid mechanics pro%lems including the mo ement o" liquids through soil andother porous media+ "lo& o" thin "ilm+ "ormation o" drops and

    %u%%les+ and the %reakup o" liquid Vets.

    )ur"ace phenomena associated &ith liquid gas+ liquid liquid orliquid gas solid inter"aces are e,ceedingl# comple,.

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    Measurement of Surface ension

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    # L%&

    Liquid'

    l

    # #l

    Measurement of Surface ension

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