what is a fluid? - njit soskenahn/10summer/lecture/lecture13.pdf · 2 mass and density • density...
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Physics 106 Lecture 13
Fluid MechanicsSJ 7th Ed.: Chap 14.1 to 14.5
• What is a fluid?• Pressure• Pressure varies with depth• Pascal’s principle• Methods for measuring pressure• Buoyant forces • Archimedes principle• Fluid dynamics assumptionsy p• An ideal fluid• Continuity Equation• Bernoulli’s Equation
What is a fluid?
Solids: strong intermolecular forcesdefinite volume and shaperigid crystal lattices, as if atoms on stiff springsdeforms elastically (strain) due to moderate stress (pressure) in any direction
Fluids: substances that can “flow”no definite shape molecules are randomly arranged, held by weak cohesive intermolecular forces and by the walls of a containerliquids and gases are both fluids
Liquids: definite volume but no definite shapeoften almost incompressible under pressure (from all sides)can not resist tension or shearing (crosswise) stress
Fluid Statics - fluids at rest (mechanical equilibrium) Fluid Dynamics – fluid flow (continuity, energy conservation)
can not resist tension or shearing (crosswise) stressno long range ordering but near neighbor molecules can be held weakly together
Gases: neither volume nor shape are fixedmolecules move independently of each othercomparatively easy to compress: density depends on temperature and pressure
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Mass and Density
• Density is mass per unit volume at a point:
Vm or
Vm
≡ρΔΔ
≡ρ • scalar• units are kg/m3, gm/cm3..• ρwater= 1000 kg/m3= 1.0 gm/cm3
• Volume and density vary with temperature - slightly in liquids• The average molecular spacing in gases is much greater than in liquids.
Force & Pressure
• The pressure P on a “small” area ΔA is the ratio of the magnitude of the net force to the area
A/FP or AF P =
ΔΔ
=n̂PΔA
• Pressure is a scalar while force is a vector• The direction of the force producing a pressure is perpendicular
to some area of interest
n̂APAPF Δ=Δ=ΔnPΔA
• At a point in a fluid (in mechanical equilibrium) the pressure is the same inequilibrium) the pressure is the same in any directionh
Pressure units:1 Pascal (Pa) = 1 Newton/m2 (SI)1 PSI (Pound/sq. in) = 6894 Pa.1 milli-bar = 100 Pa.
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Forces/Stresses in Fluids
• Fluids do not allow shearing stresses or tensile stresses (pressures)
Tension Shear Compression
• The only stress that can be exerted on an object submerged in a static fluid is one that tends to compress the object from all sides
• The force exerted by a static fluid on an object is always• The force exerted by a static fluid on an object is always perpendicular to the surfaces of the object
Question: Why can you push a pin easily into a potato, say, using very little force, but your finger alone can not push into the skin even if you push very hard?
A sensor to measure absolute pressure
• The spring is calibrated by a known force• Vacuum is inside• The force due to fluid pressure presses on the top of the piston and
compresses the spring until the spring force and F are equal.• The force the fluid exerts on the piston is then measured
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Pressure in a fluid varies with depth
Fluid is in static equilibrium The net force on the shaded volume = 0
• Incompressible liquid - constant density ρ
• Horizontal surface areas = A y1 F1
y=0
P1Horizontal surface areas A• Forces on the shaded region:
– Weight of shaded fluid: Mg– Downward force on top: F1 =P1A– Upward force on bottom: F2 = P2A
y2 Mg
F2 P2
h
MgAPAP F 2y −−==∑ 10
AhVM ρ=Δρ=
• In terms of density, the mass of the shaded fluid is:
The extra pressure at extra depth h is:
ghPPP ρ=−=Δ 12 yyh 21 −≡ghAAP AP 2 ρ+≡∴ 1
Pressure relative to the surface of a liquid
ghPP h ρ+= 0
air
P0
h
Example: The pressure at depth h is:
P is the local atmospheric (or ambient)
All points at the same depth are at the same pressure; otherwise, the fluid could not be in equilibriumThe pressure at depth h does not depend
Ph
liquid
P0 is the local atmospheric (or ambient) pressurePh is the absolute pressure at depth hThe difference is called the gauge pressure
P di ti l The pressure at depth h does not depend on the shape of the container holding the fluid
P0
Ph
Preceding equations also hold approximately for gases such as air if the density does not vary much across h
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Atmospheric pressure and units conversions
• P0 is the atmospheric pressure if the liquid is open to the atmosphere.
• Atmospheric pressure varies locally due to altitude, temperature, motion of air masses, other factors.
• Sea level atmospheric pressure P0 = 1.00 atm= 1.01325 x 105 Pa = 101.325 kPa = 1013.25 mb (millibars)= 29.9213” Hg = 760.00 mmHg ~ 760.00 Torr= 14.696 psi (pounds per square inch)
Pascal (Pa)
bar (bar) atmosphere(atm)
torr(Torr)
pound-force persquare inch (psi)
1 Pa ≡ 1 N/m2 10−5 9 8692×10−6 7 5006×10−3 145 04×10−61 Pa ≡ 1 N/m 10 9.8692×10 7.5006×10 145.04×10
1 bar 100,000 ≡ 106 dyn/cm2
0.98692 750.06 14.5037744
1 atm 101,325 1.01325 ≡ 1 atm 760 14.696
1 torr 133.322 1.3332×10−3 1.3158×10−3 ≡ 1 Torr; ≈ 1 mmHg
19.337×10−3
1 psi 6.894×103 68.948×10−3 68.046×10−3 51.715 ≡ 1 lbf/in2
Pressure Measurement: Barometer
• Invented by Torricelli (1608-47)• Measures atmospheric pressure P0 as it varies
with the weather• The closed end is nearly a vacuum (P = 0)• One standard atm = 1.013 x 105 Pa.
near-vacuum
Mercury (Hg) ghP Hgρ=0
One 1 atm = 760 mm of Hg= 29.92 inches of Hg
m 0.760 )m/s .)(m/kg10(13.6
Pa 101.013 g
Ph 23
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Hg
=×
×=
ρ=
80930
How high is the Mercury column?
m 10.34 )m/s .)(m/kg10(1.0
Pa 101.013 g
Ph 23
5
water=
××
=ρ
=8093
0
How high would a water column be?
Height limit for a suction pump
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Pressure Measurements: Manometer
• Measures the pressure of the gas in the closed vessel
• One end of the U-shaped tube is open to the atmosphere at pressure P0
• The other end is connected to theThe other end is connected to the pressure PA to be measured
• Points A and B are at the same elevation.• The pressure PA supports a liquid
column of height h• The Pressure of the gas is:
ghPP P BA ρ+== 0 What effect would increasing P have on
Absolute vs. Gauge Pressure• The gauge pressure is PA – P0= ρgh
– What you measure in your tires• Gauge pressure can be positive or negative.• PA is the absolute pressure – you have to add the ambient pressure P0 to
the gauge pressure to find it.
increasing P0 have on the column height?
Example: Blood Pressure
• Normal Blood pressure is: 120 (systolic = peak) over 70 (diastolic = resting) – in mmHg.
• What do these numbers mean?• How much pressure do they correspond to in Pa. and psi?
Recall: 760.00 mmHg = 1.01325 x 105 Pa =14.696 psi
(101,325/760.00) = 133.322 Pa./mmHg
(101,325/14.696) = 6894. Pa./psi
Systolic pressure of 120= 16,000 Pa.= 2 32 psi
Mercury Sphygmomanometer
Aneroid Sphygmomanometer
= 2.32 psi
Diastolic pressure of 70= 9333 Pa.= 1.354 psi
Gauge or absolute?
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Pascal’s PrincipleA change in the pressure applied to an enclosed incompressible fluid is transmitted undiminished to every point of the fluid and to the walls of the container.
ΔFΔP
• The pressure in a fluid depends on depth h and on the value of P0 at the surface
• All points at the same depth have the same pressure.
Example: open container
ghPP h ρ+= 0
p0
ph
Add i t f A ith l d b ll it & i ht W• Add piston of area A with lead balls on it & weight W. Pressure at surface increases by ΔP = W/A
gh P P exth ρ+=
• Pressure at every other point in the fluid (Pascal’s law), increases by the same amount, including all locations at depth h.
PPP ext Δ+= 0
Ph
Pascal’s Law Device - Hydraulic pressA small input force generates a large output force
• Assume the working fluid is incompressible• Neglect the (small here) effect of height on pressure
• The volume of liquid pushed down on th l ft l th l h d
xA xA 21 Δ=Δ 21
• Assume no loss of energy in the fluid no friction etc
the left equals the volume pushed up on the right, so:
AA
xx
1
2
2
1=ΔΔ
∴
xF Work xF Work 2 21 Δ==Δ= 211
the fluid, no friction, etc.
Other hydraulic lever devices using Pascal’s Law:
• Squeezing a toothpaste tube• Hydraulic brakes• Hydraulic jacks• Forklifts, backhoes
AA
xx
FF
2
1
1
2
1
2=ΔΔ
=∴
mechanical advantage
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Archimedes Principle C. 287 – 212 BC• Greek mathematician, physicist and engineer• Computed π and volumes of solids• Inventor of catapults, levers, screws, etc.• Discovered nature of buoyant force – Eureka!
Why do ships float and sometimes sink?Why do objects weigh less when submerged in a fluid?Why do objects weigh less when submerged in a fluid?
ball of liquidin equilibrium
hollow ball same
upward force
identical pressures at every point
• An object immersed in a fluid feels an upward buoyant force that equals the weight of the fluid displaced by the object. Archimedes’s Principle
– The fluid pressure increases with depth and exerts forces that are the same whether the submerged object is there or not.
– Buoyant forces do not depend on the composition of submerged objects. – Buoyant forces depend on the density of the liquid and g.
Archimedes’s principle - submerged cube
• The extra pressure at the lower surface compared to the top is:
fltb t ghPPP ρ=−=Δ
A cube that may be hollow or made of some material is submerged in a fluidDoes it float up or sink down in the liquid?
• The pressure at the top of the cube causes a downward force of Ptop A
• The larger pressure at the bottom of the cube causes an upward force of Pbot A
• The upward buoyant force B is the weight of the fluid displaced by the cube:
fltopbot ghPPP ρ=−=Δ
gMgVghAPA B flfl fl =ρρ=Δ= =
• The weight of the actual cube is:gV gM F cubecubeg ρ==
Similarly for irregularly shaped objects
ρcube is the average density
The cube rises if B > Fg (ρfl > ρcube)The cube sinks if Fg> B (ρcube > ρfl)
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Archimedes's Principle: totally submerged object
Object – any shape - is totally submerged in a fluid of density ρfluid
The upward buoyant force is the weight of displaced fluid:
fluiduidfl gV B ρ=The downward gravitational force on the
The direction of the motion of an object
The downward gravitational force on the object is:
objectobjectobjectg gV gM F ρ==The volume of fluid displaced and the object’s volume are equal for a totally submerged object. The net force is:
objectobjectuidfl[ gnet V g ] FBF ρ−ρ=−=
The direction of the motion of an object in a fluid is determined only by the densities of the fluid and the object– If the density of the object is less than
the density of the fluid, the unsupported object accelerates upward
– If the density of the object is more than the density of the fluid, the unsupported object sinks
The apparent weight is the external force needed to restore equilibrium, i.e.
netgapparent F B F W −=−=
Archimedes’s Principle: floating object
At equilibrium the upward buoyant force is balanced by the downward weight of the object:
An object sinks or rises in the fluid until it reaches equilibrium. The fluid displaced is a fraction of the object’s volume.
ggnet F B 0 FBF =⇒=−=
The volume of fluid displaced Vfluid corresponds to the portion of the object’s volume below the fluid level and is always less than the object’s volume.Equate:
objectobjectgfluiduidfl gVFgV B ρ==ρ=
Solving:
objectobjectfluiduidfl VV ρ=ρ
VV
uidfl
object
object
fluid ρ
ρ=
Objects float when their average density is less than the density of the fluid they are in.
The ratio of densities equals the fraction of the object’s volume that is below the surface
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Archimedes’s Principle: King’s Crown
King to Archimedes: “Is the crown made of pure gold?”• The crown’s density ρcrown = mcrown/ Vcrown should = ρgold = 19,300 kg/m3
• Weigh the crown in air to find mcrown• But: how to find Vcrown??
• The Buoyant force equals the difference in scale readings...
Solution:• Weigh crown in air to find mcrown• Weigh it again fully submerged in a fluid• The apparent weight T2 is:
B F T g2 −=
crownfl2g gV TF B ρ=−=• solve:
gTF
Vfl
2gcrown ρ
−=
TFF
flg
gcrown ρ
−=ρ∴
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Example: What fraction of an iceberg is underwater?
VV
VV
uidfl
object
object
fluid total
underwater ρ
ρ==
displaced seawaterApply Archimedes’ Principle
glacial fresh water ice
3iceobject kg/m . 3109170 ×=ρ=ρ
3seawaterfluid kg/m . 310031 ×=ρ=ρ
From table:
%. V
V t t l
underwater 0389=∴
Water expands when it freezes. If not.......ponds, lakes, seas freeze to the bottom in winter
Vtotal
What if iceberg is in a freshwater lake?3
freshwaterfluid kg/m . 310001 ×=ρ=ρ
1.7% V
V total
underwater 9=
Floating objects are more buoyant in saltwaterFreshwater tends to float on top of seawater...
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Water has special properties
Maximum density at 4o C.• ρwater= 1000 kg/m3= 1.0 gm/cm3
• turnover of ponds and lakes• ice floats, so bodies of water do not freeze to the bottom
Fluids’ Flow is affected by their viscosity
• Viscosity measures the internal friction in a fluid.
Low viscosity• gases
Medium viscosity• water• other fluids that pour and flow easily
High viscosity• honey• oil and grease• glass
• Viscous forces depend on the resistance that two adjacent layers of fluid have to relative motion.
• Part of the kinetic energy of a fluid is converted to internal energy, analogous to friction for sliding surfaces
y g
Ideal Fluids – four approximations to simplify the analysis of fluid flow:
Th fl id i i i l f i i i l d• The fluid is nonviscous – internal friction is neglected• The flow is laminar (steady, streamline flow) – all particles
passing through a point have the same velocity at any time.• The fluid is incompressible – the density remains constant• The flow is irrotational – the fluid has no angular momentum
about any point. A small paddle wheel placed anywhere does not feel a torque and rotate
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Laminar Flow - Streamlines
Steady state flow – at any point the velocity of particles is constantEach particle of the fluid follows a smooth path called a streamline. Particles’ velocities are tangent to streamlines (field lines).The paths of different particles never cross each otherEvery given fluid particle arriving at a given point has the same velocity
velocity field lines
Every given fluid particle arriving at a given point has the same velocity
Turbulent flow
An irregular flow characterized by small whirlpool-like regionsTurbulent flow occurs when the particles go above some critical (Mach) speedEnergy is dissipated, more work must be done to maintain flow
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Flow of an ideal fluid through a short section of pipe
Constant density and velocity within volume element dVIncompressible fluid means dρ/dt = 0
Mass flow rate = amount of mass crossing area A per unit time= a “current”sometimes called a “mass flux”
length dx
velocity v
cross-section area A
Av dtdxA
)V(dtd
dtdM I rateflow massmass
ρ=ρ=
ρ===
AdxdV cylinder in fluid fo volume ==
length dxAv I rateflow massmass ρ=≡
Av I rateflow volumevol =≡
v J areaflow/unit massmass ρ=≡
Equation of Continuity: conservation of mass• An ideal fluid is moving through a pipe of nonuniform diameter• The particles move along streamlines in steady-state flow• The mass entering at point 1 cannot disappear or collect in the pipe• The mass that crosses A1 in some time interval is the same as the mass that
crosses A2 in the same time interval.
vAvA outflowmassinflowmass ρ==ρ=
ρ1
ρ2
222111 vAvA outflow massinflow mass ρ==ρ=• The fluid is incompressible so:
ttancons a =ρ=ρ 21
vA vA 2211 =∴
• This is called the equation of continuityfor an incompressible fluid ρ1
p• The product of the area and the fluid
speed (volume flux) at all points along a pipe is constant.
The rate of fluid volume entering one end equals the volume leaving at the other endWhere the pipe narrows (constriction), the fluid moves faster, and vice versa
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Bernoulli’s Equation – energy conservation
• An ideal fluid flows through a region where its speed, cross-sectional area, and/or altitude changes.
• The pressure in the fluid varies with these changes.• Application of energy conservation yields the Bernoulli Equation
Daniel Bernoulli, Swiss physicist, 1700 – 1782
OPTIONAL TOPIC
12 EEE W mechpressure by done work −=Δ==Δ
Pressure P1speed v1height y1
Pressure P2speed v2height y2
Volume ΔV = A1Δx1
Volume ΔV = A2Δx2
Equal volumes flow in equal timesdue to continuity equation
time ttime t + Δt
Bernoulli’s Equation – energy conservation
The fluid is incompressible. The continuity equation (no leaks) requires:
2211 xAxA V Δ=Δ=ΔThe net work done on fluid volume by external pressures:
V ]P [P dxAPdxAPdxFdxF W 212121 Δ−=−=−=Δ 221121
Vmm m 1 Δρ=≡= 2
The change in the mechanical energy:11
OPTIONAL TOPIC
Pressure P1speed v1
Pressure P2speed v
Equal volumes flow in equal timesd i i i
12212
1222
1 mgymgymvmvEE E 12 −+−=−=Δ
)yy(gvvPP 21 12212
1222
1 −ρ+−=− ρρ
Equate to the net work and divide through by the volume ΔV:
Rearrange:
gyvPgyvP 21 2222
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212
1 ρ++=ρ++ ρρ
time ttime t + Δt
speed v1height y1
speed v2height y2
Volume ΔV = A1Δx1
Volume ΔV = A2Δx2
due to continuity equation
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Bernoulli’s Equation – energy conservation
Bernoulli’s Equation is often expressed as:
gyvPgyvP 21 2222
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212
1 ρ++=ρ++ ρρ
OPTIONAL TOPIC
]y-y[gPP 121 2ρ+=
Constant gyvP =ρ++ ρ 221
For a fluid at rest Bernoulli’s Equation reduces to the earlier result for variation of pressure with depth:
For flow at constant altitude (y1 = y2) the pressure is lower where ther fluid flows faster:
vPvP 21222
1212
1ρρ +=+
Gases are compressible, but the above pressure / speed relation holds true.
Bernoulli effect causes airplane wings to work
• Streamlines 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
OPTIONAL TOPIC
curvature, and the angle between the wing and the horizontal
Low Pressure where flow velocity is high
Higher Pressure where flow velocity is low
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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:
OPTIONAL TOPIC
– 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
Golf Ball
Th b ll i i id b k i• The ball is given a rapid backspin• The dimples increase friction
– Increases lift• It travels farther than if it was not
spinning
Atomizer
• A stream of air passes over one end of an open tube
• The other end is immersed in a liquid
OPTIONAL TOPIC
• The moving air reduces the pressure above the tube
• The fluid rises into the air stream• The liquid is dispersed into a fine
spray of droplets
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