Science for the School and Family, Part I. Natural PhilosophyHooker, Worthington
Science
Science for the School and Family, Part I. Natural Philosophy
Hooker, Worthington
Physics; Science
121. =Pressure of Liquids in Proportion to Depth.=--The pressure of
a fluid is in exact proportion to its depth. For, as the particles
are all under the influence of gravity, the upper layer of them
must be supported by the second, and these two layers together by
the third, and every layer must bear the weight of all the layers
above it. The increase of pressure at great depths produces the
most striking effects. Thus if an empty corked bottle be let down
very deep at sea, either the cork will be driven in or the bottle
will be crushed in. A gentleman tried the following experiment: He
made a pine-wood cork, so shaped that it projected over the mouth
all around. He then covered this with pitch, and fastened over the
whole several pieces of tarpaulin. The bottle, thus prepared, he
let down to a great depth by attaching to it a weight. On raising
it up he found that it contained about half a pint of water
strongly impregnated with pitch, showing that the pressure of the
water forced water through the several pieces of tarpaulin, the
pitch, and the pores of the wooden cork. When a ship founders near
land, the pieces of the wreck, as it breaks up, float to the shore;
but when the accident happens in deep water, the great pressure
forces water into the pores of the wood, and thus makes it so
heavy that no part of the vessel will ever rise again. When a man
dives very deep he suffers much from the pressure on his chest. If
we watch a bubble of air rising in water it is small at first, but
it grows larger as it approaches the surface, because it sustains
less pressure than when it was deep in the water. The force with
which a fluid is discharged from an opening in a vessel depends on
the height of the fluid above the opening. The difference in this
respect between a full barrel and one nearly empty is very obvious.
Most fishes, probably, can not bear the pressure of great depths,
and so are commonly found on the coast, or on banks, as they are
called, in the midst of the ocean.
[Illustration: Fig. 75.]
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