Chapter 9 Fluid Mechanics
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Transcript Chapter 9 Fluid Mechanics
Chapter 9
Topics:
9-1
9-2
9-3
9-4
Fluid Mechanics
Fluids & Buoyant Force
Fluid Pressure & Temperature
Fluids in Motion
Properties of Gases
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Fluids
A fluid is a non-solid state of matter in which atoms or
molecules are free to move past each other; a liquid or a
gas
Liquids have a definite volume, but an indefinite shape
Gases have indefinite volume and shape
Density is mass per unit volume
D = m/V
or
ρ =m/V
(Where ρ is mass density)
Density of gases is measured at certain temperature &
pressure – usually 0C & 1atm
Temperature & pressure influence gas density
Solids & liquids are virtually incompressible, so
their densities are pressure-independent
Density of water is 1g/mL or 1.0 x 103kg/L or
1.0 x 103kg/m3
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Buoyancy & Archimedes’Principle
The upward force a fluid exerts on objects
partially or completely submerged in it –
the buoyant force
Buoyant force acts in direction opposite
gravity
Thus objects submerged in water, have a weight
less than that when on solid ground; this is
called the object’s apparent weight
The buoyant force = the weight of the fluid
displaced by the object in the fluid
Any object placed into a fluid will displace some
of the fluid & take its place; it is the weight of
that displaced fluid that provides the upward
buoyant force on the object
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Mass, density, buoyancy
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Buoyancy
http://www.youtube.com/wat
ch?v=eQsmq3Hu9HA
http://www.youtube.com/wat
ch?v=vJ36urazDu4
Note apparent decrease in mass
of rock
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Buoyant Force
The magnitude of buoyant force = to amount of fluid
displaced by the object that is submerged or partially
submerged in a fluid
FB = Fg = mfg
FB = buoyant force
Fg = force of displaced fluid
mfg = mass of displaced fluid x accel due to gravity
mfg is the weight of the displaced fluid
The relative densities of substances will determine
what floats, what becomes submerged, & what sinks
An floating object cannot be denser than the fluid in
which it floats
For floating objects
ρf/ρo = Vo/Vf
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Altering buoyancy
Devices that alter buoyancy change
the object’s average density
Examples include, life jackets, ballast
tanks, ship’s hollow hulls, swim bladders
Submarines use ballast
tanks to change their
depth
7
How organisms use buoyancy
Swim bladders inflate to change the overall density of the fish
when air is gulped at the surface or gas secreted by a gas gland
and the gas goes into the swim bladder; the fish can adjust the
gas content to control its diving trim
Sharks do not have swim bladders; their liver is huge and lipidrich; they adjust the lipid content to adjust their diving trim
Cephalopods (squid, octopus) have no swim bladder; they alter
buoyancy and thus diving trim by adjusting body fluids to alter
body density; also these organisms can withstand depths which
would crush other organisms (they have no swim bladders that
would implode, they have not internal bones which would be
crushed)
Human brain has a density of 1040kg/m3; the cerebro-spinal fluid
bathing the brain and spinal cord has a density of 1007kg/m3.
This fluid supports the brain with a buoyant force within the cranial
cavity. This is why when various spinal tap or other clinical
procedures are performed, the brain experiences great stress after
the procedure. Patients must stay in prone positions with medical
care until the brain fluid volume is restored.
8
Floating objects
Buoyant force = object’s weight for
floating objects
FB = Fg =mog
The force of gravity (object’s weight)
is in equilibrium with the buoyant
force acting against the Fg
Since the 2 forces are equal and
opposite, the object floats at the
surface of the fluid
9
Submerged objects
If the 2 forces are not in equilibrium
& the densities differ, the object will
become submerged
The degree of submergence depends on
the FB (buoyant force upwards) and
apparent weight of object (downwards)
Fg/FB = ρo/ρf
This equation is used to solve
buoyancy problems
10
Pressure & Temperature
Pressure = force/area
P=F/A
unit is N/m2
Atmospheres (atm)
Millimeter of mercury (mmHg)
Pounds per square inch (lb/in2)
105 Pa or 105 N/m2
1 atm
101 mmHg
14.8 lb/in2
A N/m2 is also called a Pascal (Pa)
Pressure can also be measured in:
At sea level atmospheric pressure is:
For each 33 feet an object is submerged in the ocean, they
experience an additional 1 atm of pressure
http://www.madsci.org/posts/archives/1998-11/912136521.Ph.r.html
If you have that much pressure on you at this instant at sea level,
how is it that you feel no pressure difficulties?
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Fluids exert pressure
Fluids exert force equally in all directions when inside
an object
Pascal’s Principle
P 1 = P2
F1/A1 = F2/A2
This relationship is useful to understand how
pressure, force, & area are related
Consider how a barber chair works
Little Louie steps on a small lever at the base of the
chair (applying a small force) which raises Big Bubba
in the chair.
How does a small force applied by Louie’s foot raise
massive Bubba in the barber chair?
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Hydraulic devices utilize Pascal’s
Principle!
Remember fluids exert pressure in all directions
equally
So, how much force does Little Louie have to apply to
a 0.004m2 piston which applies the pressure
throughout the liquid to push the second piston which
lifts Big Bubba in the chair?
FLL = ?N ALL = 0.004m2
FBB = 780N ABB= 0.5m2
F1/A1 = F2/A2
x/0.004 = 780/0.5
X = 780 x 0.004/0.5 = 6.24N
Little Louie needs to apply a mere 6.24N to lift Big
Bubba’s 780N body in the barber chair!
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A natural hydraulic system
14
Man-made hydraulic system
(to make jobs easier)
15
Equations
for Pressure (P) that varies with depth
As objects go deeper into the water, the
pressure increases with depth; the weight (Fg)
of column of H2O above the object exerts a
force on the object
The H2O column has a volume = Ah, where A =
cross-section area of column; h = height of
column
So mass of the H2O column is: m = ρV =ρAh
These relationships can be arranged in the
following sets of equalities for equations to use
in solutions for pressure problems:
P=F/A=mg/A=ρVg/A=ρAhg/A=ρhg
This is called “guage pressure” b/c it
represents the force on the object by the
column of H2O only
What is absolute pressure?
16
Absolute pressure takes into account the
air pressure above the column of H2O
above the obejct
Fluid pressure is a function of depth
P = Po + ρgh; where Po = atmos P
Temperature is an important quality of
fluids; the kinetic theory helps explain
molecular movement of particles which
have a direct influence on pressure;
changes in temperature affect particle
movement
Absolute zero describes the instance
where all molecular movement
theoretically ceases; 0 Kelvin.
17
Some good video links for fluid
topics
Video about pressure on an egg:
http://www.youtube.com/watch?v=4uRnPTQxZtw
Video on Pascal’s Principle Part 1:
http://www.youtube.com/watch?v=dIjAFW02PBM&feature=
related
Video on Pascal’s Principle Part 2:
http://www.youtube.com/watch?v=Skran9E_Cjk&feat
ure=related
Video on atomspheric pressure:
http://www.youtube.com/watch?v=0fy4TLMNb6s&feature=r
elated
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Atmospheric Pressure
& Temperature
The pressure of the atmosphere exerts pressure on the
atmospheric layers below
At sea level, atmospheric pressure is about 14.8lb/in2 or 1 atm
slide 11)
(see
Humans: 2m2 body surface area; so atmospheric force on our
bodies ~200,000N (40,000lbs)
Why do we not collapse or feel this force?
Temperature – a measure of the average kinetic energy of the
particles in a substance
Measure of how hot or cold a substance is; measured using a
thermometer
The higher the energy content of the particles, the higher the
temperature of the substance
Consider the phase change diagrams of substances to help you
visualize this connection
Temperature scales:
Fahrenheit: 32F water freezes; 212F water evaporates
Celsius: 0C water freezes; 100C water evaporates
Kelvin: 273K water freezes; 373K water evaporates (add 273 to Celsius
temp to get Kelvin temp; NO degree symbol used for Kelvin)
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Fluids in Motion
Bernoulli’s Equation
Ideal fluids
Fluids in motion are real fluids, but we will consider the
fluids in our discussion as ideal fluids
Conservation laws apply to moving fluids; when considering
fluids moving through a pipe, then the mass of fluid
entering the pipe during a certain interval must equal the
mass of the fluid exiting the pipe during the same interval
1)incompressible (density remains same)
2)non-viscous (internal friction is zero)
3)have steady flow (velocity, pressure, density at each point in
fluid remain same)
4)non-turbulent flow (no angular speed, ie eddy currents, in
moving fluid)
A1v1 = A2v2
So, as a fluid moves faster its pressure decreases
Look at diagrams on next slide
20
Note how as
fluid speed
changes, its
pressure
changes; in
what natural
instances would
you notice this?
21
Bernoulli’s Principle provides insight
as to why airplanes fly…
B
A
Air hitting wing front (A) splits its stream; top stream
must arrive at wing end (B) at same time the bottom
stream does; thus air speeds differ from top to bottom;
thus pressure differs & providing sufficient lift for plane!
22
23
Bernoulli’s Equation
Compares the energy of a fluid between 2
points:
P1 + ½ ρv12 + ρgh1 = P2 + ½ ρv22 + ρgh2
If fluid movement thru a pipe is at
same height, then the gravitational
potential energy would not change;
the ρgh now is removed from the
equation
24
Ideal Gas Law
PV = NkBT
P = pressure (unit = atm)
V = volume (unit = L)
N = # particles
kB = Boltzmann’s constant = 1.38X10-23 J/K
T = temperature (unit = K)
Real gases act like ideal gases under
normal conditions; so we can apply the
ideal gas law to real gases
Note: in chemistry this law is written:
PV = nRT
Where n is #moles; R is gas constant (8.31
J/molK)
25