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14.2 What is a Fluid?14.2 What is a Fluid?
•A fluid, in contrast to a solid, is a substance that can flow.
•Fluids conform to the boundaries of any container in which we put them. They do so because a fluid cannot sustain a force that is tangential to its surface. That is, a fluid is a substance that flows because it cannot withstand a shearing stress.
•It can, however, exert a force in the direction perpendicular to its surface.)
33
Stresses in Solids
The level of stress required to obtain a givenThe level of stress required to obtain a given
deformation ※ ※Tensile stress(Tensile stress( 拉伸應力拉伸應力 )) ,, Tensile strain (Tensile strain ( 拉伸應變拉伸應變 ))
and and Young’s modulus (Young’s modulus ( 楊氏模數楊氏模數 ))
※ ※Shear stress(Shear stress( 剪應力剪應力 )) , , Shear strain (Shear strain ( 剪應變剪應變 )) and and
Shear modulus (Shear modulus ( 剪力模數剪力模數 ))
※ ※ Volume stress(Volume stress( 體積應力體積應力 )) ,, Volume strain (Volume strain ( 體積應變體積應變 ))
and Bulk modulus (and Bulk modulus ( 體積彈性模量體積彈性模量 ))
12.7: Elasticity
A stress is defined as deforming force per unit area, which produces a strain, or unit deformation.
Stress and strain are proportional to each other. The constant of proportionality is called a modulus of elasticity.
55
Strain unit deforTensile = matio n
= L
L
2
Normal forcstre
e NTensile = =
Ass ( S )
rea m
F
A
Tensile stressTensile stress(( 拉伸應力拉伸應力 )) ,, Tensile strain Tensile strain (( 拉伸應拉伸應變變 ) and ) and Young’s modulusYoung’s modulus ( ( 楊氏模數楊氏模數 ))
Tensile stress Young's modulus ( E ) =
Tensile strain
F /AE =
ΔL/L
66
Stress-strain relationship
A stress–strain curve for a steel test specimen. The specimen deforms permanently when the stress is equal to the yield strength of the specimen’s material. It ruptures when the stress is equal to the ultimate strength of the material.
77
Thin cylinder under internal pressure
Resisting force F S 2 { S Longitudinal Tensile stress }R 1 1
2Pressure force F { Pressure in the tube along the longitudinal axis }
p
Rt
p R p
{ Shear stress at wall }
2 S 2 { For equilibrium }1
S 1 2
p
Rt p R
pRt
88
FR = S2 Lt
F = p L2R
FR = S2 Lt
p
p
Resisting force F S 2 { S Transverse Tensile stress }R 2 2
Pressure force F 2
S 2 2 { For equilibrium }2
S 2
Lt
p RL
Lt p RL
pRt
99
Shear stressShear stress(( 剪應力剪應力 )) ,, Shear strain Shear strain (( 剪應變剪應變 )) and and Shear modulus Shear modulus (( 剪力模數剪力模數 ))
Shear stress
Shear st ( G )
i=
ra n
F/AShear modulus
/Lx
2
Tangential force N = =
Area m
FShear stress
A
= Fractional change in length
=
Shear strain
L
xL
1111
Volume stress(( 體積應力體積應力 )) , Volume strain (( 體積應體積應變變 )) and Bulk modulus (( 體積彈性模量體積彈性模量 ))
2
force NVolume stress ( change in pressure ) =
Area m
P = F
A
Voulme strain = Fractional change in volume
= V
V
Volume stressBulk modulus ( B ) =
Volume strain
> 0 Generally < 0 /
- P VB
V V P
Note : Compressibility ( k ) = 1 / B
1212
YYoung’soung’s modulusmodulus ( ( 楊氏模數 )) ,, SShear modulushear modulus ( ( 剪力模數 ) ) ,,BBulk modulusulk modulus ( ( 體積彈性模量 ) )
1313
Stresses in FluidsStresses in Fluids Normal stress ( pressure )Normal stress ( pressure ) Tangential or shearing stressTangential or shearing stress shear the fluid particle and deform its shapeshear the fluid particle and deform its shape
1414
The Nature of FluidsThe Nature of Fluids
The fluids The fluids cannot cannot support support Tensile stressesTensile stresses and and Shear stresses Shear stresses ..
The fluids flow and The fluids flow and deform continuously deform continuously and permanently under and permanently under Shear stresses Shear stresses ..
1515
Fluid Mechanics Fluid Mechanics (Liquids and Gases)(Liquids and Gases)
Fluid StaticsFluid Statics Fluid PropertiesFluid Properties Density (ρ=m/vDensity (ρ=m/v )) Pressure Pressure (( P=F/AP=F/A )) Variation of Pressure with DepthVariation of Pressure with Depth Pascal’s PrinicplePascal’s Prinicple Archimedes’ PrincipleArchimedes’ Principle
20A
2
m
N
A
FlimP
1m
1N)1Pa(Pascal
14.3 Density and Pressure
To find the density of a fluid at any point, we isolate a small volume element V around that point and measure the mass m of the fluid contained within that element. If the fluid has uniform density, then
Density is a scalar property; its SI unit is the kilogram per cubic meter.
If the normal force exerted over a flat area A is uniform over that area, then the pressure is defined as:
The SI unit of pressure is the newton per square meter, which is given a special name, the pascal (Pa).
1 atmosphere (atm) = 1.01x105 Pa =760 torr =14.7 lb/in.2.
2
1N 1Pa(Pascal
m )
1
2A 0
NFP lim
A m
14.4: Fluids at Rest
Above: A tank of water in which a sample of water is contained in an imaginary cylinder of horizontal base area A.
Below: A free-body diagram of the water sample.
The balance of the 3 forces is written as:
If p1 and p2 are the pressures on the top and the bottom surfaces of the sample,
Since the mass m of the water in the cylinder is, m =V, where the cylinder’s volume V is the product of its face area A and its height (y1 -y2), then m =A(y1-y2). Therefore,
If y1 is at the surface and y2 is at a depth h below the surface, then
(where po is the pressure at the surface, and p the pressure at depth h).
The pressure at a point in a fluid in static equilibrium depends on the depth of that point but not on any horizontal dimension of the fluid or its container.
F2
F1
1919
14.5: Measuring Pressure: The Mercury Barometer
Fig. 14-5 (a) A mercury barometer. (b) Another mercury barometer. The distance h is thesame in both cases.
A mercury barometer is a device used to measure the pressure of the atmosphere. The long glass tube is filled with mercury and the spaceabove the mercury column contains only mercury vapor, whose pressure can be neglected.If the atmospheric pressure is p0 , and is the density of mercury,
(Pascal) Pa101.013
m
N101.013
0.76ms
m9.8
m
Kg1013.6
m
N10760g
760mmHg
e)(atmospher 1atm
5
25
233
23
Hg
2020
14.5: Measuring Pressure: The Open-Tube Manometer
An open-tube manometer measures the gauge pressure pg of a gas. It consists of a U-tube containing a liquid, with one end of the tube connected to the vessel whose gauge pressure we wish to measure and the other end open to the atmosphere.
If po is the atmospheric pressure, p is the pressure at level 2 as shown, and is the density of the liquid in the tube, then
2121
Blood pressure is measured using an inflatable cuffBlood pressure is measured using an inflatable cuff
systolic
diastolic
Pgauge (mmHg)
t
2323
Pressure Change within a Gas Change within a Gas
Mt.Everest
10km
20km
30km
40km
90% of the Atom is below here
99% of the Atom is below here
Ozone layer
50% of the atmosphere is below 5.6km
Atmospheric pressure as Atmospheric pressure as a function of a function of elevation?elevation?
2424
P+△ P
y+△ y△ y
Py
P0
0 0
0
0
PV nRT
mRT M
Mm RT
PV M
RTP air density
MIf T constant P
P sea level
y P yP
空氣之分子量
Ideal gasIdeal gas
PP00≡Atmospheric ≡Atmospheric
Pressure at sea levelPressure at sea level
2525
P
y
P0
0
0
0
air
air
air
0
0
P y y0
0P y 0
gyP
0
P g y
uniform
P g y
P y g yP
dPg dy
P P
P y P e
2626
14.6: Pascal’s Principle
A change in the pressure applied to an enclosed incompressible fluid is transmitted undiminished to every portion of the fluid and to the walls of its container.
2727
14.6: Pascal’s Principle and the Hydraulic Lever
The force Fi is applied on the left and the downward force Fo from the load on the right produce a change p in the pressure of the liquid that is given by
If we move the input piston downward a distance di, the output piston movesupward a distance do, such that the same volume V of the incompressible liquid isdisplaced at both pistons.
Then the output work is:
2929
1 1
2 2
2 2 1 1
2 1
b
Vertical direction
F P A
F P A
P gy P gy
(Net force) B P -P A
g hAV
f f
f
blockBuoyant Force B gVf
浮力
Net Force on the block = ?Net Force on the block = ?
P1
P2
h
A
A
y2y1
1F
2F
h
Vb : Volume of the fluid that has been displaced by the body
14.7: Archimedes Principle: Floating and Apparent Weight
When a body floats in a fluid, the magnitude Fb of the buoyant force on the body is equal to the magnitude Fg of the gravitational force on the body.
That means, when a body floats in a fluid, the magnitude Fg of the gravitational force on the body is equal to the weight mfg of the fluid that has been displaced by the body, where mf is the mass of the fluid displaced.
That is, a floating body displaces its own weight of fluid.
The apparent weight of an object in a fluid is less than the actual weight of the object in vacuum, and is equal to the difference between the actual weight of a body and the buoyant force on the body.
3131
HomeworkHomework
Chapter 14 ( page 378 )Chapter 14 ( page 378 )
11 , 18, 24, 27, 29, 32, 47, 49, 62, 63, 65, 6611 , 18, 24, 27, 29, 32, 47, 49, 62, 63, 65, 66
67, 71, 82, 83, 8467, 71, 82, 83, 84
3232
Fluid DynamicsFluid Dynamics
Fluid FlowFluid Flow Laminar Flow (Steady Flow)Laminar Flow (Steady Flow)
Flow RateFlow Rate Bernoulli’s Equation and ApplicationBernoulli’s Equation and Application Viscosity and Laminar FlowViscosity and Laminar Flow
(Poiseuille’s Law)(Poiseuille’s Law) Flow in the Circulatory SystemFlow in the Circulatory System
Turbulent FlowTurbulent FlowThe Onset of TurbulenceThe Onset of Turbulence
3333
Fluid in MotionFluid in Motion (Fluid Dynamics) (Fluid Dynamics)
Fluid velocity Fluid velocity
Steady flow (laminar flow) : Steady flow (laminar flow) : the fluid velocity at any point is independent of the fluid velocity at any point is independent of timetime
Non-steady flow (turbulent) : not steady flowNon-steady flow (turbulent) : not steady flow
tz,y,x,v
3434
x y z
yx zx y z
v ( x + x , y + y , z + z ) - v (x, y, z)Acceleration a =
t
But x = v t , y = v t , z = v t
vv vv ( x + x , y + y , z + z ) = v (x, y, z) + ( )(v t) + ( )(v t) + ( )(v t)
x y z
yx zx y z
v + ( )( t)
t vv v v
a = ( )(v ) + ( )(v ) + ( )(v ) + ( )x y z t
v a = ( v ) v +
t
3535
Stream lineStream line
““No two stream lines No two stream lines ever cross.”ever cross.”
Stream lines are Stream lines are parallel to each otherparallel to each other
Fluid does not cross Fluid does not cross the side of boundarythe side of boundary
Stream line: Path of the fluid particle in motionStream line: Path of the fluid particle in motion(流線)(流線)
Steady flow (laminar flow)
4040
Compressible and Incompressible FlowCompressible and Incompressible Flow Incompressible: density of fluid is independent Incompressible: density of fluid is independent
of both position and time (of both position and time (ex : ex : liquid)liquid) Compressible: GasesCompressible: Gases
Rotational and Irrotational FlowRotational and Irrotational FlowRotational: non-zero angular velocityRotational: non-zero angular velocity
4242
Steady flowSteady flow Incompressible → density of fluid is constantIncompressible → density of fluid is constant IrrotationalIrrotational Nonviscous flow → no frictionNonviscous flow → no friction
(no relative velocity between flow tubes)(no relative velocity between flow tubes)
Ideal Fluid Flow
4343
time
volumeconstantAv rate Flow
The fluid flow The fluid flow into the tube at into the tube at “1” with Δt“1” with ΔtΔmΔm11=ρ=ρ11ΔvΔv11=ρ=ρ11vv
11ΔtAΔtA11
Steady flowSteady flowΔmΔm11=Δm=Δm22
ρρ11vv11AA11Δt=ρΔt=ρ22vv22AA22ΔtΔt
(incompressible fluid (incompressible fluid ρρ11=ρ=ρ22))
AA11vv11=A=A22vv22
Equation of continuityEquation of continuity
The fluid flow The fluid flow out the tube at out the tube at “2” with Δt“2” with ΔtΔmΔm22=ρ=ρ22ΔvΔv22=ρ=ρ22vv
22ΔtAΔtA22
4545
時間時間 dtdt 期間,流體柱 期間,流體柱 ac (t) → bd (t+dt)ac (t) → bd (t+dt) SteadySteady IncompressibleIncompressible IrrotationalIrrotational NonviscousNonviscous
Bernoulli’s EquationBernoulli’s Equation
22222
211111 v
2
1gyPv
2
1gyP
4646
1 2F F
1 1 1 1 2 2 2 1 1 1 2 2 2
2 2 1
1 1 1 2 2 2
t dt t bd ac
2 22 2 1 1
2 2 2 2 1 1 1 1
W F d Δ K E
i W P A ds P A ds P A v dt P A v dt
ii W mg y y
m A v dt A v dt
iii Δ K.E K.E K.E K.E K.E
1 1 m v m v
2 2 m A v dt ; m A v dt
i
由 1 1 1 2 2 2 2 2 2 2 1 1 1 1
2 22 2 2 2 1 1 1 1
ii iii P A v dt P A v dt A v dtgy A v dtgy
1 1 A v dt v A v dt v
2 2
Work-Energy TheoremWork-Energy Theorem
TheThe Venturi Tube Venturi Tube ( 文氏管 )
4848
2 21 2 L 2 1
1P P (v v ) ;
2 1 1 2 2A v = A v
2 22 1 2
1 2 L 2 21
A A1P P v ( )
2 A
4949
vL > vH PL < PH
VH
VL
2 2H H H L L L
1 1P gy v P gy v
2 2 H H L L
AHvH = ALvL
AH > AL vL > vH
Venturi effect
5050
High speed , Low Pressure regions
Low speed , High Pressure regions
AirfoilStream (Flow) lines are closer together
5151
Motion of air layer due to the viscosityMotion of air layer due to the viscosity
Spinning ballSpinning ball
Low speed , High Pressure regions
High speed , Low Pressure regions
5252
Measurement of fluid velocity based on Measurement of fluid velocity based on Bernoulli’s principleBernoulli’s principle
5353
C D C 1 air 1 D 2 air 2 Hg
1 air 1 2 air 2 Hg
1 2 Hg air
2 21 air 1 air 1 2 air 2 air 2
21 2 air 2 air 2 1
1 222
air
Hg22
air
P P ; P P gh ; P P gh gh
P gh P gh gh
P P gh gh
1 1P v gy P v gy
2 20
1P P v g y y
2 0
2 P Pv
2 ghv 2
gh
5454
2atm D
1P + 0 + v constant
2
2A A
1P gd v
2 constant
2B 1 B
1P gh v
2 constant
D
2C 2 C
1P g(d+h ) v
2 constant
C atm
C D
C 2
B
P P
v
v v >> v
2g(d+h )
maxC atm 1
2atm B
1
atm1,max
2v = (P gh )
0
P vh
g 2g
Ph
g
BP
Siphon( 虹吸管 )
maxc
max1B h ?
v
?
點高度
5555
Real fluid has a certain amount of internal friction, which is called viscosity.
Viscosity exists in both liquids and gases, and is essentially the frictional force between the adjacent layers of fluid as the layers move past one another.
In liquids, viscosity appears due to the cohesive forces between the molecules. In gases, it arises from collisions between the molecules.
黏滯力 黏滯力 ( ( Viscosity )
5656
b c
A a
y1 y2
h
P1 P2
ρ
ρg
1 2 gP P ( )gh
2 21 2 g 2 1
1P P (v v ) ;
2 1 2Av = av
黏滯力 黏滯力 ( ( Viscosity )
5858
A thin layer of fluid is placed between two flat plates. One plate is static and the other is made to move . The fluid directly in contact with each plate is held to the surface by the adhesive force between the molecules of the liquid and those of the plate. Thus the upper surface of the fluid moves with the same speed v as the upper plate, whereas the fluid in contact with the stationary plate remains stationary. The stationary layer of fluid retards the flow of the layer just above it, which in turn retards the flow of the next layer, and so on.
Experiment setup for obtaining of viscosity coefficient
5959
For a given fluid, it is found that the required force F, is proportional to the area of a fluid in contact with each plate A, and to the speed v, but is inversely proportional to the separation , of the plates, what comes down to the following relation
Experiment setup for obtaining of viscosity coefficient
Velocity gradient v
Av
F
6060
The Nature of FluidsThe Nature of Fluids
The fluids The fluids cannot cannot support support Tensile stressesTensile stresses and and Shear stresses Shear stresses ..
The fluids flow and The fluids flow and deform continuously deform continuously and permanently under and permanently under Shear stresses Shear stresses ..
6161
x
x
x
dvF /A )
dy
dv F/A
dy
A:area of moving plate
:coefficient of viscosity
F A
dv dy
切液體 剪應 ( 力 剪應變 率
剪應 力
流體黏滯性
6262
2
2
v AvF A ; F ; F
y y
A:area of moving plate
:coefficient of viscisity
F A
v y
NN-sm SI unit
m 1 ms m
6363
dvdy
Fluid Temperature [oC] Viscosity [Pa.s]
Water 0 1.8 .10-3
Water 20 1.0.10-3
Water 100 0.3.10-3
Ethyl alcohol 20 1.2.10-3
Engine oil 30 200.10-3
Air 20 0.018.10-3
Hydrogen 0 0.009.10-3
Water vapour 100 0.013.10-3
The viscosity coefficients of various fluids at the specified temperatures 玉米粉漿、
矽酸鉀溶液
紙漿、乳膠漆、血漿、糖漿、髮膠
6464
Viscosity Shear Stress ≡ Change in momentum in bulk fluids
Viscosity Stresses tend to decrease the velocity of the flow on the high speed side of the layer, increase the velocity on the low speed side.
黏滯應力 黏滯應力 ( ( Viscosity Stress )
Momentum exchange by molecular mixing
6565
A shear layer near a solid wallA shear layer near a solid wall
Velocity profile in the region near a solid surface.
uyyxdd
du
6666
黏滯性黏滯性
1)1) What is the velocity What is the velocity distribution across the distribution across the radius?radius?
2)2) What is the flow rate? What is the flow rate? (Poiseuille’s Law)(Poiseuille’s Law)
3)3) Human & Biological Human & Biological ApplicationApplication
Laminar flow of viscous fluids in a Laminar flow of viscous fluids in a cylindrical pipecylindrical pipe
6767
Laminar flow of viscous fluids in a Laminar flow of viscous fluids in a cylindrical pipecylindrical pipe
0vWall
6969
0dr
dvrL 2rF0
dr
dvdr
dvrL 2
dr
dvArF
f
f
Rr r PPrF 221p
Viscous force on the fluid of the cylindrical section Viscous force on the fluid of the cylindrical section by the surrounding fluid isby the surrounding fluid is
External “driving force” on this cylindrical sectionExternal “driving force” on this cylindrical section
7070
dr
dvrL 2r PP ; rFrF 2
21fp In steady flow:In steady flow:
1 2
1 2
v r' r r'1 2
v R 0 r R
r r'21 2
0r R
P Pdv 1 r
dr 2 L
P P1 dv - rdr
2 L
P P1dv - rdr
2 L
P P1 rv r' v R -
2 L 2
1 2 2 2P P1 v r' R r'
4η L
7171
1 2 2 2
1 2 2max
Q Av
dQ v r 2 rdr
P P1v r R r
4 L P P1
v v r 0 R4 L
π
η
η
Flow rateFlow rate
r
dr
7272
r
R dr
1 2 2 2
r R r R1 2 2 2
r 0 r 0
r R r R1 2 2 3
r 0 r 0
P P1dQ R r (2 r dr)
4 L
π P P Q dQ R r rdr
2 L
P P R rdr r dr
2 L
π
π
4 4R R
2 4
Poiseuille's Law
4
1 2P P1 RQ
8 LηV
IR
7373
Q PP Av PP Fvt
Fx
t
WP 2121ower
421 R
1PP
1P
2P
R
Power of the driving sourcePower of the driving source
For constant Flow rate QFor constant Flow rate Q