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  • 1 year ago
A barometer is an instrument that measures air pressure, allowing weather forecasters and scientists to better predict extreme weather events. Despite its incredible usefulness, inventing the barometer was no walk in the park. Asaf Bar-Yosef describes the series of scientists and events that contributed to the birth of the barometer -- and explains how it actually works.

Lesson by Asaf Bar-Yosef, animation by Reflective Films.

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Transcript
00:00Aristotle famously said,
00:08nature fears of empty space,
00:11when he claimed that a true vacuum,
00:13a space devoid of matter,
00:15could not exist because the surrounding matter
00:17would immediately fill it.
00:19Fortunately, he turned out to be wrong.
00:22A vacuum is a key component of the barometer,
00:25an instrument for measuring air pressure.
00:27And because air pressure correlates to temperature,
00:30and rapid shifts in it can contribute to hurricanes,
00:33tornadoes, and other extreme weather events,
00:35a barometer is one of the most essential tools
00:38for weather forecasters and scientists alike.
00:41How does a barometer work, and how is it invented?
00:44Well, it took a while.
00:46Because the theory of Aristotle and other ancient philosophers
00:49regarding the impossibility of a vacuum
00:52seemed to hold true in everyday life,
00:54few seriously thought to question it for nearly 2,000 years,
00:58until necessity raised the issue.
01:01In the early 17th century,
01:03Italian miners faced a serious problem
01:05when they found that their pumps
01:07could not raise water more than 10.3 meters high.
01:10Some scientists of the time,
01:12including one Galileo Galilei,
01:15proposed that sucking air out of the pipe
01:17was what made water rise to replace the void,
01:19but that its force was limited,
01:22and could lift no more than 10.3 meters of water.
01:25However, the idea of a vacuum existing at all
01:28was still considered controversial,
01:30and the excitement over Galileo's unorthodox theory
01:33led Gasparo Berti to conduct a simple but brilliant experiment
01:38to demonstrate that it was possible.
01:40A long tube was filled with water
01:42and placed standing in a shallow pool with both ends plugged.
01:46The bottom end of the tube was then opened
01:48and water poured out into the basin
01:51until the level of the water remaining in the tube was 10.3 meters.
01:56With a gap remaining at the top
01:57and no air having entered the tube,
02:00Berti had succeeded in directly creating a stable vacuum.
02:04But even though the possibility of a vacuum had been demonstrated,
02:08not everyone was satisfied with Galileo's idea
02:11that this empty void was exerting some mysterious yet finite force on the water.
02:17Evangelista Torricelli, Galileo's young pupil and friend,
02:21decided to look at the problem from a different angle.
02:23Instead of focusing on the empty space inside the tube,
02:27he asked himself what else could be influencing the water.
02:30Because the only thing in contact with the water
02:32was the air surrounding the pool,
02:34he believed the pressure from this air
02:36could be the only thing preventing the water level in the tube
02:39from dropping further.
02:41He realized that the experiment was not only a tool to create a vacuum,
02:45but operated as a balance
02:47between the atmospheric pressure on the water outside the tube
02:50and the pressure from the water column inside the tube.
02:53The water level in the tube
02:55decreases until the two pressures are equal,
02:58which just happens to be when the water is at 10.3 meters.
03:01This idea was not easily accepted,
03:05as Galileo and others had traditionally thought
03:07that atmospheric air has no weight and exerts no pressure.
03:12Torricelli decided to repeat Berti's experiment with mercury instead of water.
03:17Because mercury was denser, it fell farther than the water,
03:20and the mercury column stood only about 76 centimeters tall.
03:23Not only did this allow Torricelli to make the instrument much more compact,
03:28it supported his idea that weight was the deciding factor.
03:32A variation on the experiment used two tubes,
03:35with one having a large bubble at the top.
03:37If Galileo's interpretation had been correct,
03:40the bigger vacuum in the second tube
03:42should have exerted more suction and lifted the mercury higher.
03:45But the level in both tubes was the same.
03:48The ultimate support for Torricelli's theory came via Blaise Pascal,
03:53who had such a mercury tube taken up a mountain
03:55and showed that the mercury level dropped
03:58as the atmospheric pressure decreased with altitude.
04:02Mercury barometers based on Torricelli's original model
04:05remained one of the most common ways to measure atmospheric pressure,
04:09until 2007,
04:10when restrictions on the use of mercury due to its toxicity
04:13led to them no longer being produced in Europe.
04:16Nevertheless, Torricelli's invention,
04:19born of the willingness to question long-accepted dogmas
04:22about vacuums and the weight of air,
04:24is an outstanding example of how thinking outside of the box,
04:28or the tube,
04:29can have a heavy impact.
04:30For more information,
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