Buoyancy Experiments
Buoyancy
In physics, buoyancy is the upward force on an object produced by the surrounding fluid (i.e., a liquid or a gas) in which it is fully or partially immersed, due to the pressure
difference of the fluid between the top and bottom of the object. The
net upward buoyancy force is equal to the magnitude of the weight of
fluid displaced by the body. This force enables the object to float or
at least to seem lighter. Buoyancy is important for many vehicles such as boats, ships, balloons, and airships, and plays a role in diverse natural phenomenon such as sedimentation.
Forces and equilibrium
Pressure increases with depth below the surface of a liquid. Any
object with a non-zero vertical depth will see different pressures on
its top and bottom, with the pressure on the bottom being higher. This
difference in pressure causes the upward buoyancy force.
The hydrostatic pressure at a depth h in a fluid is given by

where
is the density of the fluid,
is the depth (negative height), and
is the standard gravity ( −9.8 N/kg on Earth)
The force due to pressure is simply the pressure times the area.
Using a cube as an example, the pressure on the top surface (for
example) is thus

where d is the length of the cube's edges. The buoyant force is then the difference between the forces at the top and bottom

which reduces to

in the case of a cube, the difference in between the top and bottom is , so

or

- where V is the volume of the cube,

The negative magnitude implies that it is in the opposite direction
to gravity. It can be demonstrated mathematically that this formula
holds true for any submerged shape, not just a cube.
The buoyancy of an object depends, therefore, only on two factors: the object's submerged volume, and, the density
of the surrounding fluid. The greater the object's volume and
surrounding density of the fluid, the more buoyant force it
experiences. Thus the magnitude of the buoyant force is simply equal to
the weight of the displaced fluid. In this context, displacement is the term used for the weight of the displaced fluid and, thus, is an equivalent term to buoyancy.
The total force on the object is thus the net force of buoyancy and the object's weight

If the buoyancy of an (unrestrained and unpowered) object exceeds
its weight, it tends to rise. An object whose weight exceeds its
buoyancy tends to sink.
It is common to define a buoyant mass mb that represents the effective mass of the object with respect to gravity

where is the true (vacuum) mass of the object, whereas ρo and ρf are the average densities of the object and the surrounding fluid, respectively. Thus, if the two densities are equal, ρo = ρf,
the object appears to be weightless. If the fluid density is greater
than the average density of the object, the object floats; if less, the
object sinks.
Compressive fluids
The atmosphere's density depends upon altitude. As an airship
rises in the atmosphere, its buoyancy reduces as the density of the
surrounding air reduces. The density of water is essentially constant:
as a submarine
expels water from its buoyancy tanks (by pumping them full of air) it
rises because its volume stays the same (the volume of water it
displaces if it is fully submerged) while its weight is decreased.
Compressible objects
As a floating object rises or falls the forces external to it change
and, as all objects are compressible to some extent or another, so does
the object's volume. Buoyancy depends on volume and so an object's
buoyancy reduces if it is compressed and increases if it expands.
If an object at equilibrium has a compressibility
less than that of the surrounding fluid, the object's equilibrium is
stable and it remains at rest. If, however, its compressibility is
greater, its equilibrium is then unstable, and it rises and expands on the slightest upward perturbation, or falls and compresses on the slightest downward perturbation.
Submarines rise and dive by filling large tanks with seawater. To
dive, the tanks are opened to allow air to exhaust out the top of the
tanks, while the water flows in from the bottom. Once the weight has
been balanced so the overall density of the submarine is equal to the
water around it, it has neutral buoyancy and will remain at that depth.
Normally, in order to balance the density closely, some air has to be
left in the tanks. This gives the submarine a static stability; if the
submarine descends even slightly, the increased pressure of the water
will compress the air in the tanks, reducing its volume. Since buoyancy
is a function of volume, this implies a decrease in buoyancy, and the
submarine will continue to decend.
The height of a balloon tends to be stable. As a balloon rises it
tends to increase in volume with reducing atmospheric pressure, but the
balloon's cargo does not expand. The average density of the balloon
decreases less, therefore, than that of the surrounding air. The
balloon's buoyancy reduces because the weight of the displaced air is
reduced. A rising balloon tends to stop rising. Similarly a sinking
balloon tends to stop sinking.
Archimedes' principle
The Falkirk Wheel
boat lift relies on Archimedes principle. A boat in the wheel always
displaces its weight in water so the two sides of the wheel remain
balanced even if there is a boat only in one side.
Archimedes' principle, or the law of upthrust, is:
- "a body immersed in a fluid is buoyed up by a force equal to the weight of the displaced fluid."
In other words, when a body is partially or completely immersed in a
liquid, then it experiences an upward buoyant force which is equal to
the weight of the fluid displaced by the immersed part of the body.
It is named after Archimedes of Syracuse, who first discovered this law. Vitruvius (De architectura IX.9–12) recounts the famous story of Archimedes making this discovery while in the bath (for which see eureka) but the actual record of Archimedes' discoveries appears in his two-volume work, On Floating Bodies. The ancient Chinese child prodigy Cao Chong also applied the principle of buoyancy in order to measure the accurate weight of an elephant, as described in the Sanguo Zhi.
This is true only as long as one can neglect the surface tension (capillarity) acting on the body.[1]
The weight of the displaced fluid is directly proportional to the
volume of the displaced fluid (specifically if the surrounding fluid is
of uniform density). Thus, among objects with equal masses, the one
with greater volume has greater buoyancy.
Suppose a rock's weight is measured as 10 newtons
when suspended by a string in a vacuum. Suppose that when the rock is
lowered by the string into water, it displaces water of weight 3
newtons. The force it then exerts on the string from which it hangs
will be 10 newtons minus the 3 newtons of buoyant force:
10 − 3 = 7 newtons. This same principle even reduces the
apparent weight of objects that have sunk completely to the sea floor,
such as the sunken battleship USS Arizona at Pearl Harbor, Hawaii. It is generally easier to lift an object up through the water than it is to finally pull it out of the water.
The density of the immersed object relative to the density of the fluid is easily calculated without measuring any volumes:

Density
If the weight of an object is less than the weight of the fluid the
object would displace if it were fully submerged, then the object has
an average density less than the fluid and has a buoyancy greater than
its weight. If the fluid has a surface, such as water in a lake or the
sea, the object will float at a level where it displaces the same
weight of fluid as the weight of the object. If the object is immersed
in the fluid, such as a submerged submarine or air in a balloon, it
will tend to rise. If the object has exactly the same density as the
fluid, then its buoyancy equals its weight. It will tend neither to
sink nor float. An object with a higher average density than the fluid
has less buoyancy than weight and it will sink. A ship floats because
although it is made of steel, which is more dense than water, it
encloses a volume of air and the resulting shape has an average density
less than that of the water.
References
See also
External links
This article is licensed under the GNU Free Documentation License. It uses material from Wikipedia Encyclopedia article "Buoyancy"
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