Thursday Sept. 7, 2006

The first of the optional assignments was handed out in class.  It will be due next Thursday (Sept. 14).  You can earn a little bit of extra credit on optional assignments.  Optional assignments should be ready to be turned in when you come to class.  Don't let the instructor see you finishing an optional assignment or working with a friend in the last few minutes before the start of class (he is likely to take your unfinished assignment and that of your friend).




Air pressure is a force that pushes downward, upward, and sideways.  The bottom person in the people pyramid below must push upward with enough force to support the other people.  The air pressure in the four tires on your automobile push down on the road (that's something you would feel if the car ran over your foot) and push upward with enough force to keep the 1000 or 2000 pound vehicle off the road.





Three layers of air in the atmosphere are shown above (each layer contains the same amount of air, 10% of the air in the atmosphere).  This picture reminds you that air pressure decreases with increasing altitude.

The layer at the ground and at the bottom of the atmosphere is "squished" by the weight of the air above.  Squeezing all of this air into a thin layer or small volume increases the air's density.  The highest air density is found at the bottom of the atmosphere.

The next layer up is also squished but not as much as the bottom layer.  The density of the air in the second layer is lower than in the bottom layer.  The air in the 3rd layer has even lower density.  It is fairly easy to understand that air density decreases with increasing altitude. 

Finally if you look closely at the figure you can see that pressure decreases most rapidly with increasing altitude in the dense air at the bottom of the atmosphere.

Next we'll do a little demonstration (the demonstration doesn't involve dropping water balloons as shown below).


All of the forces acting on the water balloon are shown in the next figure.

The figure at left shows air pressure (red arrows) pushing on all the sides of the balloon.  Because pressure decreases with increasing altitude, the pressure pushing downward on the top of the balloon is a little weaker than the pressure pushing upward at the bottom of the balloon.  The two sideways forces cancel each other out.  The total effect of the pressure is a weak upward force (shown on the right figure, you might have heard this called a bouyant force).  Gravity exerts a downward force on the water balloon.  In the figure at right you can see that the gravity force is stronger than the upward pressure difference force.  The balloon falls as a result.

In the demonstration a wine glass is filled with water.  A small plastic lid is used to cover the wine glass.  You can then turn the glass upside down without the water falling out.


Now we'll look again at all of the forces and see how this is possible.

All the same forces are shown again in the left most figure.  In the right two figures we separate this into two parts.  First the water inside the glass isn't feeling the downward and sideways pressure forces (because they're pushing on the glass).  Gravity still pulls downward on the water but the upward pressure force is able to overcome the downward pull of gravity.

Some of the historical information on pps. 31 & 32 in the photocopied class notes was mentioned briefly. 

Between 1926 and 1936 several courageous teams of scientists and adventurers competed to see who could travel the highest in the atmosphere by balloon.  In May 1926 Captain Hawthorne Charles Grey reached 28,510 ft. altitude.  He was in an open gondola; note the many layers of clothing that he needed in order to survive the cold temperatures found at those altitudes.

Capt. Grey reached 42, 249 ft.  At those heights, the air is too thin to support life and supplementary oxygen is required.  Grey made another trip in November, 1926, but was killed when he ran out of oxygen during the descent.

A short video tape segment documenting Auguste Piccard's and Paul Kipfer's trip to 51,775 ft altitude was shown in class.


One of the test descents in the Trieste (the bathyscaph designed and built by Auguste Piccard) and a portion of  Bertrand Piccard's non-stop voyage around the globe by balloon will be shown in the next week or two.

The Practice Quiz was administered in the final portion of the class.