Module 6
PlanningGuide

Lesson 2.5


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Concepts
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Equations
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Examples
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Exercises
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Answers
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Definitions

Lesson 2.5
Lesson 2.6
Lesson 2.7
Lesson 2.8
Lab 2.5
Lab 2.6
Lab 2.7
Lab 2.8
Project 6


Lesson 2.5 Gases

Overview
This lesson deals with gases, atmospheric pressure, Boyles law and Bernoulli’s principle. On completion of the lesson, you should be able to discuss the behavior of gases in terms of the kinetic theory. You should also be able to explain variations in atmospheric pressure with altitude, explain the relationship between pressure and and volume and pressure and velocity in venturis and aircraft wings.

MINI LAB

CHOICE OF ACTIVITIES

  1. Crush can: Boil some water inside a soda can and quickly invert it into a container with cold water in it.
  2. Barometer: Make a barometer with a glass jar and a thin sheet of rubber sealed around the edge of the opening. Attach a pointer to the surface of the sheet.
  3. Make a hot air balloon
  4. Venturi: Cut a drinking straw in half. Place the end of one piece in some water. Use the other half of the straw to direct a jet if air over the open end of the straw. This should create a spray as the air "draws" the water up towards the stream of air.

 

Kinetic Theory
Gas molecules fill whatever container they are in. They move around rapidly, collide with each other and collide with the surface of the container. The pressure of the gas is caused by the rate at which the molecules collide with the container’s surface. When molecules collide with the surface of a container at a higher rate, the pressure increases

Gases Have Weight
We move about in a sea of gas. This gas occupies space and has mass.
We can demonstrate this by comparing the mass of a sample of compressed gas with a similar sample at normal atmospheric pressure.

Gases And Buoyancy
The air around us has pressure and this pressure can cause buoyancy.
The lifting power of a balloon depends on the difference in density between the gas in the balloon and the air outside the balloon.
For example, helium atoms have four times the mass of hydrogen atoms but the lifting power of a hydrogen balloon is only marginally better than that of a helium balloon. The lifting power of a balloon is equal to the mass of air displaced less the mass of the balloon.
(See Example 2.5.2 below)

Air Pressure
The amount of pressure that the air around us can exert is quite large.
The force that air exerts at sea level, relative to a vacuum, is 101,300 N per square meter.
It can support a column of water 10 meters high. On 1 square meter, this is equivalent to the weight of 10 tons of water. We have seen how air pressure can crush a can and how air pressure holds things in place. In the famous Magdenberg experiment, the mayor of Magdenberg, Otto von Guericke used two teams of horses to try to pull two hemispheres apart after the air between them was evacuated.

Barometers
We use barometers to measure changes in air pressure.
A mercury barometer consists of a tube that is closed at one end. It is filled with mercury and tipped upside down with its open end below the surface of the mercury in a small reservoir. The pressure on the liquid in the reservoir keeps the liquid in the tube. (Or we could say that the vacuum above the liquid keeps it in place but a vacuum is just the absence of pressure.) Normal atmospheric pressure at sea level will keep the top of the column of mercury at a level of 760 mm above the level of the mercury in the reservoir. The level of the mercury in the column changes as the atmospheric pressure changes.

Theoretically, we could use water in a similar type of barometer but the lower density of water would require the tube to be that over 10 meters high. The main problem is however that water boils when the pressure gets too low and the closed end of the tube will contain a lot of water vapor that will affect the reading quite considerably.

A type of water barometer consists of a sealed container with water and air in it. The level of water in a side tube changes as the air pressure changes and this can be used to give an indication of the atmospheric pressure.

Aneroid Barometer
Changes in atmospheric pressure help us to predict changes in the weather. It’s useful to have a barometer but water barometers or mercury barometers are not practical for household use.
Mercury is very dangerous and water barometers are bulky and inaccurate. The most practical barometer is the aneroid barometer.
This is just a closed container that changes its shape as the air pressure around it changes. A system of levers and a pointer are used to amplify the movement of the surface of the container and give an indication of the change in pressure.

Altimeters
We can also us a barometer to measure the height above sea level. Airplanes have altimeters which have the same structure as an aneroid barometer. The scale on the altimeter is graduated to show the height above sea level.
The air expands as its pressure decreases. This means that the density of the air decreases as it gets further away from the earth. Because of this, the relationship between altitude and pressure is not simply proportional. Pressure at a certain depth of fluid depends on the density of the fluid. In liquids, the density is the same at all depths but with gases, the density changes with depth.

Bernoulli & Venturi
Speed affects pressure. Aircraft stay in the sky because air speeds up as it goes over the top of the aircraft’s wing. The increase causes a drop in pressure on the top of the wing. When the kinetic energy of the air increases, its pressure energy must decrease and visa versa.
The wing is also shaped so that the air slows down slightly as it passes under the wing and this causes a slight increase in pressure below the wing. This difference in pressure acting over a large area, provides the lift needed to keep the aircraft in the air.

Stalling
Its important that the air flows smoothly over the wing of an aircraft for the lift forces to work.
If the speed drops too much or if the angle of the wing is too large, we get turbulence on the wing that messes up the flow patterns, stops the lift and the airplane stalls.

Boyles Law:

P1V1 = P2V2 The pressure of a sample of an ideal gas multiplied by its volume is constant if the temperature remains constant.

P1 = Initial pressure (Pa)
V1 = Initial volume (m3)
P2 = Final pressure (Pa)
V2 = Final volume (m3)

Example 2.5.1 Boyle’s Law
If a 5-liter container filled with air at 101300 Pa. is squashed until the volume of the air 2 liters, what will be pressure inside the container?

Solution
P1V1 = P2V2 P2 = 5/2 x 101300 Pa

P2 = 253250 Pa

 

Example 2.5.2 Buoyancy
Calculate the lifting power of a 20 m3 helium-filled bag in air that has a density of 1.2 kg.m-3. The density of the helium may be taken as 0.19 kg.m-3.

Assume that the mass of the empty bag is 5 kg.

Solution
The mass of air displaced by the helium bag is = 20 x 1.2 = 24 kg.

The mass of helium in the bag = 20 x 0.19 = 3.8 kg

The mass of the bag is = 5 kg

The lift created by the balloon is therefore equivalent to the weight of:

24 kg – 3.8 kg – 5 kg = 15.2 kg

This is equivalent to 15.2 kg x 9.81 N/kg = 149 N

Questions

  1. How is the rate at which gas molecules collide with the inner surface of a container related to the pressure of the gas in the container?
  2. Why does the rate of collision between gas molecules and the inner surface of a container increase if the amount of gas in the container is increased?
  3. Why does the rate of collision between gas molecules and the inner surface of a container increase if the temperature of the gas in the container is increased?
  4. If the atmosphere exerts a pressure of 101300 N on a square meter of surface at the earth’s surface, what is the mass of a column of air with a base of 1 m2 that extends all the way to the top of the atmosphere?
  5. What is the difference between a mercury barometer and an aneroid barometer?
  6. How could a barometer be used to estimate the height of a very tall building?
  7. If we assume that 99% of the atmosphere is in a 30-kilometer deep layer around the earth, what is the average density of the earth’s atmosphere?
  8. If 50% of the earth’s atmosphere is below 5600 meters, what is the average density of the air at elevations between 0 and 5600 meters?
  9. How does Boyle’s law describe the relationship between the pressure and volume of a fixed amount of gas?
  10. If a 2-liter bottle filled with air at 101300 Pa. is squashed until the volume of the air in the bottle is 1 liter, what will be pressure inside the bottle?
  11. If treasure hunters use a large bag filled with air to lift a bronze cannon from the ocean floor to the surface, why is this potentially dangerous?
  12. If a dirigible is filled with hydrogen that has roughly half the density of helium, why does it not have twice the lifting power?
  13. If the air in a large warehouse has a density of 1.18 kg/m3, what mass of air in the building is displaced by a bag of helium with a volume of 10 m3? If the bag has a mass of 1 kg and the helium in the bag has a density of 0.185 kg/m3, what is its lifting power?
  14. A fluid flowing through a pipe speeds up as it flows into a narrower section of pipe. Why does the pressure of the fluid decrease as its speed increases?
  15. Will the pressure increase if the fluid moves into a pipe with a larger diameter?