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Transcript of Physics 201 Chapter 13 Lecture 1 - UW-Madison … Physics 201, UW-Madison 1 Physics 201 Chapter 13...
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11/30/2009 Physics 201, UW-Madison 1
Physics 201Chapter 13Lecture 1
Fluid Statics Pascal’s Principle Archimedes Principle (Buoyancy)
Fluid Dynamics Continuity Equation Bernoulli Equation
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11/30/2009 Physics 201, UW-Madison 2
Fluids
Atmospheric PressureEven when there is no breeze air molecules are continuously
bombarding everything around - results in pressure
normal atmospheric pressure = 1.01 x 105 Pa (14.7 lb/in2)
Pressure (P)P = Force/Area [N/m2]
1 N/m2 = 1 Pascal (Pa)
Density = Mass/Volumeρ = M / V units = kg/m3
Pressure variation with depthP = ρ g h
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11/30/2009 Physics 201, UW-Madison
Densities of substances
3
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11/30/2009 Physics 201, UW-Madison 4
Density & Pressure are related by the Bulk Modulus
LIQUID: incompressible (density almost constant)
GAS: compressible (density depends a lot on pressure)
Compressiblity
B =Δp
(−ΔV /V )
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11/30/2009 Physics 201, UW-Madison 5
Variation of pressure with depth
m = ρV; V = Ah⇒ m = ρAh
P =FA=mgA
; i.e., P =ρAh( )gA
⇒ P = hρg
True for all shapes of containers
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11/30/2009 Physics 201, UW-Madison
Pressure difference of 3 m of water compares to the change of descending 3000m in air
6
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Pascal’s Principle A change in pressure in an enclosed fluid is
transmitted undiminished to all the fluid and to its container.
This principle is used in hydraulic system P1 = P2
(F1 / A1) = (F2 / A2)
F2
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Pascal’s Principle
This principle is used in hydraulic system P1 = P2
(F1 / A1) = (F2 / A2) Can be used to achieve a mechanical advantage F2 = F1 (A2 / A1)
» Work done is the same: height by which the surface A2 rises is smaller than the change in the height of surface with area A1.
F1
A1
F2A2
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Using Fluids to Measure Pressure
1 atm = 760 mm (29.9 in) Hg = 10.3 m (33.8 ft) H20
• Use Barometer to measure Absolute Pressure
Barometer Top of tube evacuated (p=0) Bottom of tube submerged into pool of mercury
open to atmosphere (p=p0) Pressure dependence on depth:
• Use Manometer to measure Gauge Pressurep0
Δh
Manometerp1
Measure pressure of volume (p1) relative to the atmospheric pressure (≡ gauge pressure )
The height difference (Δh) measures the gauge pressure:
Δh =(p1 − p0 )
ρg
h =p0
ρg
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Measurement of Pressure
Manometer If both sides of an U-tube are open to atmosphere
the levels of the fluid are the same on both sides If one side is connected to a “pressurized side” the
level difference between the two sides can be used to measure pressure.
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11/30/2009 Physics 201, UW-Madison 11
Measuring the tire pressure:Is this a manometer or a barometer?
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Measuring Blood Pressure Blood pressure is quite high, 120/80 mm of Hg Use higher density fluid in a manometer: Mercury
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11/30/2009 Physics 201, UW-Madison
Atmosphere - pressure vs height
13
P = P0e−ρ0P0
gh
--> whiteboard
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Pressure in a fluidPressure in a fluid
• Impulse to wall:
Fx!t = !px = !(Mvx)
Fx = !(Mvx)/ !t
• Force is perpendicular to surface
• Force proportional to area of surface
• pressure (p)
p = Force/area [N/m2]
1 N/m2 = 1 Pascal (Pa)
v
v
Fx
wall
molecule
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PressurePressurey
Atmospheric PressureAtmospheric Pressure
Even when there is no breeze air molecules are continuously
bombarding everything around - results in pressure
normal atmospheric pressure = 1.01 x 105 Pa (14.7 lb/in2)
average vertical force = fy
=
!py
!t=
! mvy
"
#$$
%
&''
!t
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ArchimedesObject immersed in a fluid is subject to a “buoyant force”.
Force on sides cancel
Force on top Ft = ρghT A
Force on bottom Fb = ρghB A
ΔF = ρg A Δh
FB = (mg)disp
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11/30/2009 Physics 201, UW-Madison 17
ArchimedesObject immersed in a fluid is subject to a “buoyant force”.
Force on sides cancel
Force on top Ft = ρghT A
Force on bottom Fb = ρghB A
ΔF = ρg A Δh
FB = (mg)disp
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11/30/2009 Physics 201, UW-Madison 18
The pressure is a function of the depth only (for a givendensity of the fluid and of g)
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11/30/2009 Physics 201, UW-Madison 19
Float
Weight of object = ρ0gV
Buoyant force is the weight of the displaced fluid
Weight of fluid = ρfgV
Displace just enough fluid such that forces = 0!
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Archimedes PrincipleBuoyant Force (B)
weight of fluid displaced (P=F/A, P=ρgh)» B = ρfluid g Vdisplaced
» W = ρobject g Vobject
» object sinks if ρobject > ρfluid
» object floats if ρobject < ρfluid
» Eureka!
If object floats….» B=W» Therefore ρfluid g Vdisplaced = ρobject g Vobject
» Therefore Vdisplaced/Vobject = ρobject / ρfluid
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11/30/2009 Physics 201, UW-Madison 21
Float Buoyant force is the weight of the displaced fluid Weight of object = ρIceVtotal gWeight of fluid = ρSeaWatergVsubmersed
Displace just enough fluid such that forces = 0!
General solution: Vdisplaced/Vobject = ρobject / ρfluid
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The weight of a glass filled to the brim with water is Wb. A cube of ice is placed in it, causing some water to spill. After the spilled water is cleaned up, the weight of the glass with ice cube is Wa. How do the weights compare: 1. Wb > Wa. 2. Wb < Wa.3. Wb = Wa.
Archimedes’ Principle: The buoyant force on an object equals the weight of the fluid it displaces.
Weight of water displaced = Buoyant force = Weight of ice
Archimedes Principle
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11/30/2009 Physics 201, UW-Madison 23
QuestionSuppose you float a large ice-cube in a glass of water, and that after you place the ice in the glass the level of the water is at the very brim. When the ice melts, the level of the water in the glass will: 1. Go up causing the water to spill. 2. Go down.3. Stay the same.
Archimedes’ Principle: The buoyant force on an object equals the weight of the fluid it displaces.
Weight of water displaced = Buoyant force = Weight of ice
When ice melts it will turn into water of same volume
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11/30/2009 Physics 201, UW-Madison 24
Buoyancy
Two cups hold water at the same level. One of the two cups has plastic balls (projecting above the water surface) floating in it. Which cup weighs more?
Archimedes principle tells us that the cups weigh the same. Each plastic ball displaces an amount of water that is exactly
equal to its own weight.
Cup I Cup II
1) Cup I2) Cup II3) Both the same
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Two identical glasses are filled to the same level with water. Solid steel balls are at the bottom in one of the glasses. Which of the two glasses weighs more? 1. The glass without steel balls 2. The glass with steel balls 3. Both glasses weigh the same
The steel balls sink. The buoyant force equal to the weight of the displaced water is not sufficient to counter the weight of the steel balls. Therefore, the glass with steel balls weighs more.
Sunken Balls
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Imagine holding two identical bricks under water. Brick A is just beneath the surface of the water, while brick B is at a greater depth. The force needed to hold brick B in place is:
1. larger
2. the same as
3. smaller
than the force required to hold brick A in place.
The buoyant force on each brick is equal to the weight of the water it displaces and does not depend on depth.
Buoyant force and depth
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Fluid Flow
• Volume flow rate: ΔV/Δt = A Δd/Δt = Av (m3/s)
• Continuity: A1 v1 = A2 v2
i.e., flow rate the same everywhere
e.g., flow of river
Fluid flow without friction
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ProblemTwo hoses, one of 20-mm diameter, the other of 15-mm diameter are connected one behind the other to a faucet. At the open end of the hose, the flow of water measures 10 liters per minute. Through which pipe does the water flow faster? 1. The 20-mm hose 2. The 15-mm hose 3. Water flows at the same speed in both cases4. The answer depends on which of the two hoses comes first in the flow
When a tube narrows, the same volume occupies a greater length. For the same volume to pass through points 1 and 2 in a given time, the velocity must be greater at point 2. The process is reversible.
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Faucet
A stream of water gets narrower as it falls from a faucet (try it & see).
The velocity of the liquid increases as the water falls due to gravity. If the volume flow rate is conserved, them the cross-sectional area must decrease in order to compensate
A1
A2
V1
V2
The density of the water is the same no matter where it is in space and time, so as it falls down and accelerates because of gravity,the water is in a sense stretched, so it thins out at the end.
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Types of Fluid Flow
Laminar flow Steady flow Each particle of the fluid follows a smooth path The paths of the different particles never cross each
other The path taken by the particles is called a streamline
Turbulent flow An irregular flow characterized by small whirlpool like
regions Turbulent flow occurs when the particles go above some
critical speed
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Viscosity
Characterizes the degree of internal friction in the fluid This internal friction, viscous force, is associated with the
resistance that two adjacent layers of fluid have to moving relative to each other
It causes part of the kinetic energy of a fluid to be converted to internal energy
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Ideal Fluid Flow
There are four simplifying assumptions made to the complex flow of fluids to make the analysis easier1. The fluid is nonviscous – internal friction is
neglected2. The flow is steady – the velocity of each point
remains constant3. The fluid is incompressible – the density remains
constant4. The flow is irrotational – the fluid has no angular
momentum about any point
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Streamlines
The path the particle takes in steady flow is a streamline
The velocity of the particle is tangent to the streamline
A set of streamlines is called a tube of flow
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Streamlines
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Continuity equation
Volume Flow rate
Mass flow rate
Δm1 = ρ1ΔV1 = ρ1Av1Δt
IM1 =Δm1
Δt= ρ1A1v1
IV =ΔVΔt
= Av
Δm1
Δt=Δm2
Δt
IM 2 − IM1 =dm2
dt−dm1
dt=dm12
dtContinuity equation
In steady state
General case: mass may be accumulated or decreased in the volume between A1 and A2
ρ2A2v2 = ρ1A1v1
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Continuity equationVolume Flow rate
Mass flow rate IM1 =Δm1
Δt= ρ1A1v1
IV =ΔVΔt
= Av
In steady state
Case of incompressible fluid: density constant
ρ2A2v2 = ρ1A1v1
A2v2 = A1v1
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12/01/2009 Physics 201, UW-Madison
Bernoulli’s Equation As a fluid moves through a region
where its speed and/or elevation above the Earth’s surface changes, the pressure in the fluid varies with these changes
Consider the two shaded segments The volumes of both segments are
equal The net work done on the segment
is W =(P1 – P2) V Part of the work goes into changing
the kinetic energy and some to changing the gravitational potential energy
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Bernoulli’s Equation
The change in kinetic energy: ΔK = 1/2 mv2
2 - 1/2 mv12
The masses are the same since the volumes are the same
The change in gravitational potential energy: ΔU = mgy2 – mgy1
The work also equals the change in energy Combining: W = (P1 – P2)V =1/2 mv2
2 - 1/2 mv12 + mgy2 – mgy1
Rearranging and expressing in terms of density: P1 + 1/2 ρv1
2 + mgy1 = P2 + 1/2 ρv22 + mgy2
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Bernoulli’s Equation
Pressure drops in a rapidly moving fluid whether or not the fluid is confined to a tube
For incompressible, frictionless fluid:
P +12ρv2 + ρgh = constant
12ρv2 = 1
2mv2
1V
=KEV
ρgh = mghV
=PEV
Bernoulli equation states conservation of energyFor Static Fluids:P1 + ρgh1 = P2 + ρgh2
Bernoulli's Principle (constant depth):P1 +12ρv1
2 = P2 +12ρv2
2
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What is the pressure of an incompressible fluid in the constricted region?
Continuity equation gives velocity in the constricted region (increases with A1/A2)):
Bernoulli equation
says that pressure drops as 40
P1 +12ρv1
2 = const
A2v2 = A1v1
P ∝1v2
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Applications of Bernoulli’s Principle
Wings and sails Higher velocity on one side of sail versus the
other results in a pressure difference that can even allow the boat to sail into the wind
Entrainment Reduced pressure in high velocity fluid pulls in
particles from static or lower velocity fluid» Bunsen burner, Aspirator, …
Velocity measurement
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Problem(a) Calculate the approximate force on a square meter of sail, given the horizontal velocity of the wind is 6 m/s parallel to its front surface and 3.5 m/s along its back surface. Take the density of air to be 1.29 kg/m3. (b) Discuss whether this force is great enough to be effective for propelling a sail boat.
Force, F = (P1 − P2 )A =12ρ(v2
2 − v12 )A = 15.3 N
The force is small. However, when the sails are large, the force can be high enough to propel a sail boat. For larger boats, one can add more than one sail to increase the surface area.One can even sail into the wind, where (P1 − P2 ) is small.
P1 +12ρv1
2 = P2 +12ρv2
2Bernoulli eq.for constant height
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Applications of Fluid Dynamics
Streamline flow around a moving airplane wing
Lift is the upward force on the wing from the air
Drag is the resistance The lift depends on the
speed of the airplane, the area of the wing, its curvature, and the angle between the wing and the horizontal
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Lift – General
In general, an object moving through a fluid experiences lift as a result of any effect that causes the fluid to change its direction as it flows past the object
Some factors that influence lift are: The shape of the object The object’s orientation with respect to the fluid flow Any spinning of the object The texture of the object’s surface
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Golf Ball
The ball is given a rapid backspin
The dimples increase friction Bernoulli says: Higher relative
velocity will reduce the pressure. Increases lift
It travels farther than if it was not spinning
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Problem(a) What is the pressure drop due to Bernoulli effect as water goes into a 3 cm diameter nozzle from a 9 cm diameter fire hose while carrying a flow of 40 L/s? (b) To what maximum height above the nozzle can this water rise neglecting air resistance.
v1 =F1A1
=40 ×10−3m3 /sπ (0.045)2 = 6.29 m/s
v2 =F2A2
=40 ×10−3m3 /sπ (0.015)2 = 56.6 m/s
P1 − P2 =12ρ(v2
2 − v12 ) = 1.58 ×106 N/m2
h =v2
2g=
(56.6)2
2 × 9.8m=163 m
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Torricelli’s Theorem
P1, v1, h1
P2=P1 , v2 , h2
Bernoulli's equation at constant pressure (P1 = P2 )
P1 +12ρv1
2 + ρgh1 = P2 +12ρv2
2 + ρgh2
12ρv1
2 + ρgh1 =12ρv2
2 + ρgh2
v22 = v1
2 + 2g(h1 − h2 )h = h1 − h2 Same as kinematics equation for any object falling with negligible friction.
h1
h2
Density is constant
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Viscosity
V0
V=0
F
η =
FAvL
L
•Friction in fluids
shearing stress
“strain”
Newton’s lawLaminar flow -- no turbulence
Pressure, τ = η dvdz
η is the coefficient of viscosity'A' is the moving surface
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Real fluid flow
At constant velocity net force is zero.F = P1 − P2( )πr2 and the area on which the force is acting is A = 2πrL
τ = F A =ΔPr2L
η =τ
−ΔvΔror dv =
− P1 − P2( )r2Lη
dr
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More Viscosity
for a given situation P1,P2 ,η, and L are constant
let b =ΔP2ηL
and dv = −brdr and integrating
v = −br2
2+ C
v = 0 at the boundary r = R and, substituting,
v =P1 − P2( )4ηL
R2 − r2( )
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Flow and Viscosity
ΔV = vt( )2πrΔr and again let B = π tb
and, then dV = BR2rdr − Br3dr
V = BR2 rdr0
R
∫ − B r3dr0
R
∫ = BR4
2− B
R4
4= B
R4
4Finally,
Vt=π P1 − P2( )R4
8ηLPoiseuille’s Eqn.
•no turbulence•no sized particles•constant η