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Invert a small test-tube or pen
cap inside a 1.5 L plastic coke bottle full of water and screw the lid
on.
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Have just enough air trapped in
the tube or cap so it only just floats. You might have to add a blob of
Blu-Tack or Plasticine.
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Screw the cap on and squeeze
the sides. Your "diver" sinks!
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Let the sides go again and the
"diver" rises to the top again.
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Try this:
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PREDICT: Ask your
students "What will happen when I squeeze the sides?"
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OBSERVE: Watch what
happens, remembering to make sure the cap is screwed on tight!
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EXPLAIN: What does this
show us? (by using a glass test-tube you would see that the air bubble
inside seems to get smaller as the tube fills with more water). Seniors
might like to consider the pressure the water exerts on the air space
as you squeeze the sides.
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PREDICT: Ask your
students "What will happen when I release the sides again?"
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OBSERVE: Watch what
happens. If using a glass test-tube, you would see that the air bubble
inside seems to expand pushing the water out of the tube.
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EXPLAIN: What does this
show us?
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If you used a test-tube you will have
noticed that when you squeezed the side of the bottle, the air bubble
inside got smaller and more water entered the test-tube due the
pressure of your hand. It displaced less water, so lost buoyancy and sank.
Letting the sides of the bottle go again
allowed the trapped air (which was compressed) to push the water in the
tube out again, so the tube became more buoyant, so it rose!
A submarine has tanks or compartments that
can be flooded with sea water so it loses buoyancy and sinks.
Compressed air stored in tanks elsewhere on the sub can be used to push
the water back out again, so the submarine can rise to the surface once
more.
The Lava Lamp picture above uses a
different principle - that of density. The lamp has a heater at
the base which heats up blobs of oil. The oil blobs expand slightly
when hot, becoming less dense than the surrounding liquid, so they
float toward the top of the lamp. After a while they cool, contract and
become more dense than the surrounding liquid, so sink.
Some people think this is a good model to
show how Magma (melted rock deep in the Earth, beneath the hard crust
we live on) reaches the surface of the world. When the Magma reaches
gaps in the Earths crust, it pours out as Lava and we have a volcano.