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The history of the barometer (and how it works) - Asaf Bar-Yosef

  • 0:07 - 0:11
    Aristotle famously said,
    "Nature fears of empty space"
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    when he claimed that a true vacuum,
    a space devoid of matter, could not exist
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    because the surrounding matter
    would immediately fill it.
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    Fortunately, he turned out to be wrong.
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    A vacuum is a key component
    of the barometer,
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    an instrument for measuring air pressure.
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    And because air pressure
    correlates to temperature
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    and rapid shifts in it can contribute to
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    hurricanes, tornadoes
    and other extreme weather events,
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    a barometer is one of the
    most essential tools
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    for weather forecasters and scientists alike.
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    How does a barometer work,
    and how was it invented?
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    Well, it took awhile.
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    Because the theory of Aristotle
    and other ancient philosophers
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    regarding the impossibility of a vacuum
    seemed to hold true in everyday life,
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    few seriously thought to question it
    for nearly 2,000 years --
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    until necessity raised the issue.
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    In the early 17th century,
    Italian miners faced a serious problem
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    when they found that their pumps
    could not raise water
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    more than 10.3 meters high.
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    Some scientists at the time,
    including one Galileo Galilei,
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    proposed that sucking air out of the pipe
    was what made water rise to replace the void.
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    But that its force was limited and could lift
    no more than 10.3 meters of water.
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    However, the idea of a
    vacuum existing at all
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    was still considered controversial.
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    And the excitement over
    Galileo's unorthodox theory,
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    led Gasparo Berti to conduct a simple
    but brilliant experiment
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    to demonstrate that it was possible.
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    A long tube was filled with water
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    and placed standing in a shallow pool
    with both ends plugged.
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    The bottom end of the tube
    was then opened
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    and water poured out into the basin
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    until the level of the water remaining
    in the tube was 10.3 meters.
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    With a gap remaining at the top,
    and no air having entered the tube,
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    Berti had succeeded in
    directly creating a stable vacuum.
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    But even though the possibility
    of a vacuum had been demonstrated,
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    not everyone was satisfied
    with Galileo's idea
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    that this empty void
    was exerting some mysterious
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    yet finite force on the water.
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    Evangelista Torricelli,
    Galileo's young pupil and friend,
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    decided to look at the problem
    from a different angle.
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    Instead of focusing on the
    empty space inside the tube,
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    he asked himself,
    "What else could be influencing the water?"
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    Because the only thing in contact
    with the water was the air surrounding the pool,
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    he believed the pressure from this air
    could be the only thing preventing
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    the water level in the tube
    from dropping further.
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    He realized that the experiment
    was not only a tool to create a vacuum,
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    but operated as a balance
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    between the atmospheric pressure
    on the water outside the tube
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    and the pressure from the
    water column inside the tube.
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    The water level in the tube decreases
    until the two pressures are equal,
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    which just happens to be
    when the water is at 10.3 meters.
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    This idea was not easily accepted,
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    as Galileo and others
    had traditionally thought
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    that atmospheric air has no weight
    and exerts no pressure.
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    Torricelli decided to
    repeat Berti's experiment
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    with mercury instead of water.
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    Because mercury was denser,
    it fell farther than the water
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    and the mercury column stood
    only about 76 centimeters tall.
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    Not only did this allow Torricelli to make
    the instrument much more compact,
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    it supported his idea that weight
    was the deciding factor.
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    A variation on the experiment used two tubes
    with one having a large bubble at the top.
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    If Galileo's interpretation had been correct,
    the bigger vacuum in the second tube
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    should have exerted more suction
    and lifted the mercury higher.
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    But the level in both tubes was the same.
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    The ultimate support for Torricelli's theory
    came via Blaise Pascal
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    who had such a mercury tube
    taken up a mountain
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    and showed that the mercury level dropped
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    as the atmospheric pressure
    decreased with altitude.
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    Mercury barometers based on
    Torricelli's original model
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    remained one of the most common ways
    to measure atmospheric pressure until 2007
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    when restrictions on the use of
    mercury due to its toxicity
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    led to them no longer
    being produced in Europe.
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    Nevertheless, Torricelli's invention,
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    born of the willingness to question
    long accepted dogmas
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    about vacuums and the weight of air,
    is an outstanding example
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    of how thinking outside of the box
    -- or the tube --
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    can have a heavy impact.
Title:
The history of the barometer (and how it works) - Asaf Bar-Yosef
Description:

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Video Language:
English
Team:
closed TED
Project:
TED-Ed
Duration:
04:46

English subtitles

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