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GRADES 1-8
AIR AND WATER PRESSURE
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BACKGROUND INFORMATION:
Fluid dynamics is the study of how gases and liquids behave.
A fluid can be either a gas or a liquid.
All substances have three states of matter: solid, liquid, and gas.
When a substance is in a solid state, its molecules
are all lined up and rigid.
Its volume and shape are fixed.
An ice cube (solid water) remains an ice cube no matter
what size or shape a container you put it in.
A liquid, on the other hand, has molecules that are more fluid and moveable.
It has a fixed volume, but it can take the shape of its new container.
You can pour a quantity of water from a glass to a cube,
but if the cube has a smaller volume than the glass,
the water will run over the top! A gas has
molecules that are completely free to move about,
contracting and expanding at will.
A gas has no fixed volume or shape. If you take a
deep breath of air (a gas), the air you take in expands
to fill all the compartments of your lungs. If you
blow that breath into a balloon, for instance,
the volume in the balloon is much smaller
than the volume in your lungs.
We measure the number of molecules in a given volume of
fluid and call it density. Since the volume of a
liquid is constant, its density, the mass (measured
by the number of molecules) in a fixed volume,
is also constant. A liquid is considered to be incompressible;
the density is constant and you can't squeeze more mass into
the same volume. With a gas, you can continue
to add molecules into a given volume, or you can
squeeze the same number of molecules into a smaller volume.
When you do this, the density changes and the gas
is called a compressible fluid.
A fluid exerts a pressure on the container holding it. Pressure
is a series of small forces acting on all the surfaces
the fluid touches. A force is a push; it
is a vector, meaning it has both a magnitude
(the amount) and a direction in which it is
acting. Pressure is measured as the force per area.
The pressure is not a vector because it exists in all
directions. We can measure the pressure of a gas like
air at sea level on a still day, and show
that the pressure is constant and equal to 14.7
pounds per square inch (psi). This is called atmospheric
pressure. An open, flat balloon has the same atmospheric
air pressure on both the inside and the outside. When
we blow into the balloon, however, we increase the
pressure above atmospheric pressure. The increased pressure inside the
balloon causes the sides of the balloon to bulge outward.
In Activity 2, we used the increased air pressure in
our balloon to raise the book off the table surface.
In Activity 5, when we put the lid with the
hole taped up on the tub, we took away the
atmospheric pressure acting on the water in the tub. When
we took the tape off the bottom hole, the atmospheric
pressure acting on the bottom of the tub was much greater
than the pressure inside the tub, so the water stayed
in the tub! Even the weight of the water in
the tub wasn't enough to overcome the pressure difference. Once
the tape was removed from the top hole, however,
the pressure on both the top surface and the bottom surface
of the tub were equal, and the weight of the
water forced it to run out the hole!
When we analyze fluids in motion, we will often do
our calculations for 'idealized' flows. This means we make assumptions
about the flow to simplify our equations of fluid motion to
algebraic equations. We can get a good idea of the
fluid behavior for these idealized conditions. Usually, the negatives
we are ignoring are small and don't affect the answer too
much.
When we can define our fluid flow along fixed lines
(along a pipe, for example) and with no
energy changes, we can use the Bernoulli equation. By
energy changes we mean something that takes an effort, work,
or chemical catalyst to change. For example, we talk
about how things flow in nature: water runs downhill,
not uphill. It takes energy, or some type effort,
to go against nature. When we are following nature and
not using any energy, we can use the Bernoulli equation
to compute values in our flow. Daniel Bernoulli was a
Swiss mathematician who lived in the early 1700's. He developed
a series of mathematical expressions to explain basic fluid flow phenomena.
He is most famous for developing an expression for idealized flows.
In its most common form, the Bernoulli equation states that
the local pressure plus the dynamic pressure (caused by the
motion of the air) is equal to a constant.
In Activity 1, we are using the Bernoulli principle to
hold up the balloon or the ping pong ball. As
you blow upwards around the ball, the air splits into
multiple air streams around it. At the bottom of the
ball, the velocity is actually 0; the velocity on
the sides of the ball is increasing. Bernoulli's equation says
that as the velocity increases, the local pressure decreases!
Where there is no velocity the pressure is at its highest.
So the pressure at the bottom of the ball is higher
than the pressure on the sides, and the ball is
held up by the airstream.
Activity 4 demonstrates the Bernoulli equation also. When you blow
into the spool, the air coming out the bottom moving
over the card is at a fairly high velocity, so
the local pressure on the top side of the card is
lower than the atmospheric pressure pressing up from the bottom of
the card, where there is no air moving. The
pressure difference keeps the card in place!
Buoyancy is the final concept we want to discuss here.
When an object is immersed in a fluid, what makes
it float? Archimedes' principle states that the fluid exerts an
upward force on the object equal to the weight of the
fluid that is displaced by the object. This means that
if you have an object whose mass is less than that
of the fluid, the fluid forces will push that object
up! This is why a boat floats or a hot
air balloon floats through the air. The weight of the
boat (its mass times gravity) is less than the
weight of the water it displaces. In Activity 3,
the students built boats and placed pennies in them. As
long as the boats displaced a large volume of water,
multiple pennies could be placed in them. If the foil
boats didn't displace much water, then they wouldn't be able
to hold many pennies. The wadded up piece of foil
didn't displace very much water at all, and the weight
of the wad was greater than the weight of the water
it displaced, so it sunk to the bottom.
Hot air balloons also work on the buoyancy principle. As
the air heats up, its density decreases. Once the
balloon is expanded to its full size, its volume is
fixed. As the density continues to decrease, that means
the mass is decreasing. Since weight is the mass times
gravity, the weight of the hot air is less than
the weight of the cooler air it is displacing, and
the balloon rises into the air!
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