fluids. introduction the 3 most common states of matter are: –solid: fixed shape and size (fixed...
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Fluids
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Introduction• The 3 most common states of matter are:
– Solid: fixed shape and size (fixed volume)– Liquid: takes the shape of the container and
has a fixed volume (incompressible)– Gas: expands to fill its container and volume
is not fixed (compressible)
Fixed Shape Fixed Volume
Solid
Liquid No
Gas No No
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Introduction (cont.)
• A fluid is a substance that flows– Liquids and gases are fluids
because they do not have a fixed shape
• Fluids exert pressure on the walls of their containers– Pressure is force per area– Examples: party balloons,
garden hose
Gas
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Introduction (cont.)
• Fluid mechanics is the branch of physics that studies fluids and the forces on them– Fluid statics: study of fluids at rest
• Hydrostatic pressure• Hydraulics• Buoyancy
– Fluid dynamics: study of fluids in motion• Continuity equation• Bernoulli equation
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Introduction (cont.)
• Fluid mechanics assumes that matter is a continuum (“the continuum hypothesis”)– Fluids are continuous and continuously
dividable– The fact that matter is composted of atoms
and molecules is ignored– Properties such as density, pressure,
temperature and velocity are taken to be well-defined at infinitely small points
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Introduction (cont.)
• Fluid mechanics assumes every fluid obeys– conservation of mass– conservation of energy– conservation of momentum– Newton’s laws of motion
• Fluids have a property called viscosity which is a measure of resistance to flow– Viscosity is related to friction– Syrup has high viscosity, water has low viscosity– An inviscid fluid has zero viscosity
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Density
• The density of a solid, liquid, or gas is defined as mass per unit volume:
density = = m/V is the Greek letter “rho”– SI unit for density: kg/m3
– m and V are mass and volume, respectively
• Another common unit for density is g/cm3
– 1 g/cm3 = 1000 kg/m3
• The density of liquid water is 1.00 g/cm3
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Specific Gravity
• The specific gravity of a substance is defined as the ratio of the density of that substance to the density of liquid water:
SG =
– Example: The density of gold is 19300 kg/m3 SG of gold is gold/ H2O = 19300/1000 = 19.3
– Note: SG is a dimensionless quantity– Note: SG of any substance is equal
numerically to its density in g/cm3
substance
liquid water
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Pressure
• Pressure is defined as force per unit area:
pressure = P = F/A– F is the force acting perpendicular to the
surface area A– SI unit for pressure is the pascal (Pa)
1 Pa = 1 N/m2
– The American unit for pressure is “pounds per square inch” or “psi”
1 psi = 1 lbf/in2 = 6,900 Pa
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Pressure (cont.)
• Example: What is the pressure exerted on the ground by a 60-kg person whose two feet cover an area of 500 cm2?P = F/A = mg/A
= (60 kg)(9.8 m/s2)/(0.050m2)= 12,000 N/m2
= 12 kPaIf the person stands on one foot, what will the pressure will be? 24 kPa!
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Atmospheric Pressure
• Atmospheric pressure (P0) is the pressure of the air around us– P0 = 101.3 kPa (14.7 psi) at sea level
– Atmospheric pressure decreases with increasing altitude (height above sea level)
– The cells of living organisms maintain an internal pressure that counter balances atmospheric pressure
– A common unit of pressure is the atmosphere (atm):
1.000 atm = 101.3 kPa
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Gauge Pressure• Gauge pressure (PG) is the pressure over
and above atmospheric– Tire gauges read “zero” when open to the air
because they read gauge pressure
• The total or absolute pressure is abs. pressure = P0 + PG = 1.0 atm + PG
• For many problems in fluids, only gauge pressure is needed– Decide for each problem whether “P” is gauge
or absolute
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Compressibility of Fluids
• A gas will readily change volume and density when it experiences a change in pressure– We say gases are compressible fluids
• Most liquids do not readily change volume and density, even under a wide range of pressures– Such liquids are called incompressible fluids – Incompressible = constant
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Fluid Statics (Hydrostatics)
• Hydrostatics is the study of fluids at rest
• Most hydrostatic issues take place on EarthThe fluid is in a gravitational fieldUsually we are interested in gauge pressure
(over and above Earth atmospheric pressure)Usually we assume the fluid is incompressible
(such as a liquid)
• Because the fluid is at rest, we know the pressure is always perpendicular to container walls
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Hydrostatic Pressure
• Earth’s gravitational field causes the pressure inside a fluid to increase with depth– At the surface: P = 0 (gauge)– At a depth of h below the
surface we have hydrostatic pressure:
P = gh
– This formula assumes = constant (incompressibility)
g
h
P
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Pascal’s Principle
• If a fluid in a confined space is squeezed, the added pressure shows up everywhere in the fluid
• This is called Pascal’s principle:
Pressure applied to a confined fluid increases the pressure throughout by the same amount
• Pascal’s principle is the basis of hydraulics
F
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Hydraulic Systems• Hydraulic systems use an incompressible
fluid under pressure to amplify force
• Pascal’s principle says Pin = Pout so:
Fin/Ain = Fout/Aout
Fout/Fin = Aout/Ain
FinFout
Ain Aout
Pin
Pout
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Buoyancy• Any object partially or totally submerged in
a fluid in a gravitational field experiences a buoyancy force upward
• Archimedes principle states that the buoyancy force on an object is equal to the weight of the displaced fluid:
FB = FgV
– F is the density of the fluid
– V is the volume of the object
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Apparent Weight• A dense object submerged in a fluid
appears to weigh less – This is called apparent weight, Fg
– Apparent weight is equal to the weight (Fg) minus the buoyant force (FB)
Fg = Fg FB
• An object is said to be neutrally buoyant if the weight and the buoyant force are equal– In other words, apparent weight is zero
• If the weight is less than the buoyant force, the object floats
Fg
m
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Fluid Dynamics
• Fluid dynamics is the study of fluids in motion under the influence of forces
• Simplifying assumptions:
– Fluid is incompressible ( = constant)
– Fluid is inviscid (viscosity = 0)– Laminar, steady-state flow
• We will assume incompressibility for some problems involving air even though air is a gas and thus compressible
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Continuity Equation• We can apply conservation of mass to a
fluid flowing through a pipe of changing size:
• Mass flowing into the left side (per time) equals mass flowing out of the right side:
V1/t = V2/t
A1v1 = A2v2
A1v1 = A2v2 (incompressible)
A1
v1
A2
v2
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Continuity (Example)
Water flows at a velocity 14 cm/s out of a circular pipe of diameter 1.5 cm into a rectangular trough 3.3 cm wide. If the velocity of the water in the trough is 6.2 cm/s, what is the water level in the trough?
A1 = d2/4 = (1.5cm)2/4 = 1.76 cm2
A1v1 = A2v2 = whv2
h = A1v1/wv2
= {(1.76 cm2)(14 cm/s)} / {(3.3 cm)(6.2 cm/s)}
= 1.2 cm
h = ?
v2
v1
d
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Bernoulli Equation
• Bernoulli’s principle states that
where the velocity of a fluid is high, the pressure is low, and where the velocity is low, the pressure is high
• Consider an inviscid, incompressible fluid in steady-state, laminar flow:– Pressure (P) may change from point to point– Velocity (v) may change from point to point– Elevation (y) above a reference level may
change from point to point
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Bernoulli Equation (cont.)
• Bernoulli’s equation is a statement of conservation of energy between two points:
P1 + ½(v12) + gy1 = P2 + ½(v2
2) + gy2
– P elastic potential energy (per volume)
– ½(v2) kinetic energy (per volume)
gy gravitational potential energy (per volume)
P1
P2v1
v2
y1
y2
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Bernoulli Eqn. (Example)Water flows from a large water main (20.0 cm diameter) under the street into a house and up 6.50 m of elevation to a 0.750-cm diameter faucet on the second floor. The velocity of the water is 1.10 m/s as it comes out of the faucet. What is the pressure in the main?
Main: d1 = 20.0 cm, v1 0 (continuity says its 0.0015 m/s)
y1 = 0.00 m (ref. level), P1 = ?
Faucet: d2 = 0.750 cm, v2 = 1.10 m/s, y2 = 6.50 m,
P2 = 0 (gauge pressure is zero in atmospheric air)
P1 + ½(v12) + gy1 = P2 + ½(v2
2) + gy2
P1 = ½(v22) + gy2 = [½v2
2 + gy2]=(1000 kg/m3)[½(1.10 m/s)2 + (9.80 m/s2)(6.50m)]= 6.43 104 N/m2 = 64.3 kPa