Under Pressure - Free Educational videos for Students in K-12 | Lumos Learning

Under Pressure - Free Educational videos for Students in k-12


Under Pressure - By MITK12Videos



Transcript
00:13 do you feel that do you feel the weight of
00:16 the atmosphere pushing down on you ? Actually , you
00:20 like most people have probably not thought about how heavy
00:24 the atmosphere actually is and about the pressure it pushes
00:29 on you every day . In fact , You have
00:33 about 14.7 lbs of force pushing on you per every
00:39 square inch of you . But where does this pressure
00:43 come from ? For the answer to that question .
00:46 Science had a way to the middle of the 17th
00:48 century when Pascal had hypothesis . You see , he
00:51 thought that the atmospheric pressure that we experience every day
00:54 is actually due to the massive column of air ,
00:57 the towers above us , and the way that it
00:59 exerts by gravity . To test this , He devised
01:02 a very simple experiment . He took an instrument called
01:06 a barometer , the measures atmospheric pressure , and made
01:09 measurements at several locations in the lowest part of town
01:11 , at the top of a church tower , and
01:13 even climbed a local mountain to measure the pressure at
01:15 the top with the idea that if the height of
01:18 the column of air stayed , the same pressure should
01:21 stay the same each of those locations . But at
01:24 the height of the column decreases at each location ,
01:27 then the pressure should decrease as well . I'm gonna
01:31 show you how to build a simple pressure measuring device
01:33 called a manama Ter . First I need to relatively
01:36 stiff tubes . I use to plastic pipettes I had
01:38 lying around the lab . I cut one end off
01:42 to make room for the plug . You also need
01:45 a plug to plug one end and a piece of
01:48 relatively stiff tube . Now to make the manama ter
01:52 , you need to connect the tubing to each of
01:54 the pipe . It's or plastic tubes . Once they're
01:59 connected , you'll have a U . Shaped device .
02:01 You can then fill it with water , add some
02:03 food coloring if you like , and then plug one
02:05 end to fix the pressure . There you go .
02:08 You have a phenomena and you're ready to make pressure
02:10 measurements at the beginning , the pressure exerted on each
02:13 column of liquid is equal so the liquid levels and
02:16 tube A . And B . Are equal as well
02:19 . If the pressure on tube A . Increases the
02:22 water and tube , they will fall and the water
02:24 and to be will rise . If the pressure over
02:27 tube A decreases then the water and to be will
02:30 fall and the water and tube they will rise .
02:34 For our first measurement we went to Constitution Park in
02:36 boston here we show that the pressure is greater than
02:39 it was in the lab . But using our phenomena
02:41 to show that column A . Is 12 millimeters below
02:44 column B . But what's the pressure going to be
02:47 up on bunker hill monument ? Well let's find out
02:51 After climbing 275 stairs were able to take from measurement
02:56 at the top of Bunker Hill Monument Here , we're
02:59 able to show that the column a . Is just
03:01 six below column B . For our final measurement ,
03:05 we drove about 20 miles south to the Great Blue
03:07 Hill . After climbing for about a mile and a
03:10 half , we reached the top with stunning views of
03:13 boston and the ocean . Here we get our lowest
03:16 measurement yet . Column a is actually three above column
03:20 B . Now , for some results in calculations getting
03:24 from changes in water levels to pressure calculations for starters
03:29 , the air and to be is constrained by the
03:31 plug Because of this , it's an ideal gas and
03:34 obeys the ideal gas law , which states the pressure
03:37 times volume equals . NRT . Now NRT remains constant
03:41 through all measurements . Because of this , we can
03:44 then produce a nice relationship and that is P one
03:47 times V one equals P . T becomes V .
03:49 Two . Or in other words , the pressure times
03:51 volume at one state must equal the pressure and volume
03:55 at another state . But how do we get from
03:59 differences in water levels that we measured in the field
04:01 to changes in volume of to be . Which is
04:04 what we need for our actual calculations . Well ,
04:07 from my device , I've calculated that for each one
04:10 millimeter change in water level , that corresponds to a
04:14 change in volume of 0.133 mills with half of that
04:19 volume change occurring in column A . And the other
04:21 half occurring in column B . So to calculate the
04:24 change in volume of to be only , we can
04:26 take my conversion factor of 0.133 mils per millimeter and
04:30 multiply it by half of the high change , Therefore
04:34 the final volume in to be that we saw in
04:36 the field is V two equals the initial volume .
04:40 V one of 22 mills minus the change in volume
04:44 . So using this formula , I went ahead and
04:46 calculated the final volume to be each of our locations
04:50 . A Constitution Park . The final volume of to
04:52 be was 20.4 mills at Bunker Hill Monument 21.2 mills
04:57 and at Great Blue Hill 22.4 miles . Now we
05:00 can take this relationship and rearrange it to actually solve
05:04 for the pressure in each of these locations using the
05:06 initial conditions of the air and to be a P
05:09 one equals 101.6 killer pascal's , which is the pressure
05:13 the day that I built my manama Ter and the
05:15 initial volume of to be That is the air volume
05:19 of 22 mills . Using this equation , we get
05:22 an actual atmospheric pressure , a Constitution Park 109.6 killer
05:26 Pascal's at Bunker Hill Monument . 105.5 killer pascal's another
05:30 Great Blue hill of 99.8 killer pascal's . But how
05:34 do these atmospheric pressures relate to the elevations that we
05:38 measured them ? Well , Just as pascal showed ,
05:41 we see that the pressure decreases with increased elevation at
05:45 a very linear relationship over the elevations that we measured
05:49 . Finally , I'd like to leave you with some
05:51 tips for when you make your own measurements . First
05:53 . Be patient . It can take time for the
05:56 manama tower to reach equilibrium as you change pressures .
06:00 Second , take multiple measurements . This will greatly increase
06:03 your accuracy . And third pay attention to whether as
06:06 things like changes in temperature or incoming weather systems can
06:10 have a dramatic effect on the pressures that you measure
06:14 . Some final questions to think about , based on
06:15 what you've learned today . First , what would happen
06:19 to the water in the Manama as I went to
06:20 5000 m ? Or what about the moon ? And
06:23 second ? What would happen if you made a measurement
06:26 on an airplane at 10,000 m ? Think about these
06:29 things , as you think about pressure .
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