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Properties of Gases

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A balloon racer uses the Charles law. ... Aneroid barometer Aneroid Barometer Slide 16 Open- tube manometer Slide 18 Slide 19 Ideal Gas Laws Boyle's Law ... – PowerPoint PPT presentation

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Title: Properties of Gases


1
Properties of Gases
  • Compiled by
  • Mr. Walia

2
Gas form is an essential form of the matter
  • O2, O3, N2, CO2 are essential gases in the
    atmosphere.
  • O2, and N2 provide the plants essential compounds
    for photosynthesis.
  • O3 protects us from the harmful solar radiations.

3
The proportion of these gases in the atmosphere
is measured using balloons by meteorologists
everyday.
4
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5
11 of the periodical table elements are in the
gas form.
6
Many inorganic and organic compounds are gases
NO2, SO2, N2O, CH4 , C2H6 , C3H8 , CH3NH2
7
Pressure of the Gases
  • Pressure (P) is the force exerted on a surface
    divided by the area of the surface

8
Properties of Pressure
  • Pressure increases as more gas is added
  • Conclusion - Pressure (P) is directly
    proportional to moles of gas (n)
  • Pressure due to a gas is the same in all
    directions whereas pressure due to weight is
    directional
  • Pressure unit in SI is Pascal
  •  

9
Theres another way to measure the gas pressure

Gas pressure can be measured by relating to the
atmospheric pressure.
  • Barometer
  • An apparatus used to measure pressure  derived
    from the Greek "baros" meaning "weight. 
  • Created by Evangelista Torricelli in 1646.

10
  • Torricelli inverted a tube filled with mercury
    into a dish until the force of the Hg inside the
    tube balanced the force of the atmosphere on the
    surface of the liquid outside the tube.
  • The hight of the mercury
  • in the tube is a measure of
  • the atmospheric pressure.
  • At sea level and 0C
  • this height  is 760 mmHg
  • and the pressure supporting this height is
    called 1 atmosphere.

11
Atmospheric Pressure is measured by different
units
  • Atmospheric pressure is equal to 760 mmHg and is
    called 1 atm.
  • 1 atm 760 mmHg
  • 1 mmHg 1 torr so 1atm 760
    torr
  • 1 atm 101.325 kPa
  • 1 bar 10 5 Pa so 1 atm 1
    bar

12
Change in average atmospheric pressure with
altitude
13
Why Mercury?
  • In theory, any liquid can be used in abarometer.
  • Mercury is so dense that can form a usable height
    in the tube. A similar barometer made of water,
    in comparison, would have to be more than 34 feet
    (100 meters) high.
  • Mercury also has a low vapor pressure, meaning it
    does not evaporate very easily. Water has a
    greater vapor pressure. Because of this, the
    pressure exerted by water vapor at the top of the
    barometer would affect the level of the mercury
    in the tube and the barometric reading.

14
Aneroid barometer
  • A major disadvantage of the mercury barometer is
    its bulkiness and fragility. The long glass tube
    can break easily, and mercury levels may be
    difficult to read under unsteady conditions, as
    on board a ship at sea.
  • To resolve these difficulties, the French
    physicist Lucien Vidie invented the aneroid
    ("without liquid") barometer in 1843.

15
Aneroid Barometer
  • An aneroid barometer is a container that holds a
    sealed chamber from which some air has been
    removed, creating a partial vacuum. An elastic
    disk covering the chamber is connected to a
    needle or pointer on the surface of the container
    by a chain, lever, and springs. As atmospheric
    pressure increases or decreases, the elastic disk
    contracts or expands, causing the pointer to move
    accordingly.

16
  • This type of aneroid barometer has a pointer that
    moves from left to right in a semicircular motion
    over a dial, reflecting low or high pressure. The
    simple clock-like aneroid barometer hanging on
    the wall of many homes operates on this basis.

17
Open- tube manometer
  • The open-tube manometer is another device that
    can be used to measure pressure. The open-tube
    manometer is used to measure the pressure of a
    gas in a container.

18
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19
  • Atmospheric pressure pushes on the mercury from
    one direction, and the gas in the container
    pushes from the other direction. In a manometer,
    since the gas in the bulb is pushing more than
    the atmospheric pressure, you add the atmospheric
    pressure to the height difference
  • gas pressure atmospheric pressure h
  • h is the difference in mercury levels.
  • Gas pressure will be in units of torr or
    mmHg.

20
Ideal Gas Laws
  • There are some laws that explain
  • (a) the relationship between the pressure and
    volume of the gas at a fixed temperature,
  • (b) the relationship between the volume and
    temperature of it in a fixed pressure and,
  • (c) the relationship between the pressure and
    temperature of a gas in a fixed volume.

21
Boyle's Law (1662)
  • The relationship between the pressure and the
    volume of a given sample of gas at fixed
    temperature.
  • A sample of gas compresses if the external
    pressure applied to it increases and the product
    PV is constant.
  • The Pressure (P) of a gas is inversely
    proportional to Volume (V) at constant
    Temperature (T) and moles of gas (n). 

22
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23
  • Boyle's law, stated in mathematical terms for a
    gas whose pressure and volume is measured at two
    different pressure/volume states at a constant
    temperature is then,
  • P1V1 P2V2

24
Boyles Mathematical Law
What if we had a change in conditions
since PV k
P1V1 P2V2
Eg A gas has a volume of 3.0 L at 2 atm. What
is its volume at 4 atm?
25
  1. determine which variables you have
  • P1 2 atm
  • V1 3.0 L
  • P2 4 atm
  • V2 ?
  1. determine which law is being represented

P and V Boyles Law
26
3) Rearrange the equation for the variable you
dont know
4) Plug in the variables and chug it on a
calculator
V2 1.5L
27
Example 1
  • At 0 C and 5.00 atm, a given sample of a gas
    occupies 75.0 L. The gas is compressed to a final
    volume of 30.0 L at 0 C. What is the final
    pressure?
  • Answer 12.5 atm

28
Charles' Law (1787)
  • (It was developed by Guy Lussac in 1802)
  • The volume of any gas increases directly with
    increasing temperature at constant pressure.
  • If we plot a graph of the volume of a sample of
    gas versus the temperature at constant pressure
    we get something that looks like the following

29
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30
Absolute Temperature
  • Experimental data show that 1C increase in the
    temperature of an ideal gas would increase its
    volume as 1/273 of the volume at 0C .
  • So if the volume in 0C was 273 mL, it would
    increase 1/273 x 273 mL 1 mL at 1C and the
    total volume will be 274 mL.
  • A 10C increase will increase the volume
  • 10 x 1/273 x 273 mL 10 mL, the total volume
    283 mL.
  • A 273C increase will increase the volume
  • 273 x 1/273 x 273 mL 273 mL, the total
    volume 546 mL.

31
  • Although the the volume increases in a regular
    manner with increase in temperature, it is not
    directly proportional to the Celsius temperature.
    An increase in temperature from 1C to 10 C ,
    eg., does not increase the volume 10- fold, but
    only from 274 mL to 283 mL.
  • An absolute temperature scale, kelvin
    temperature, is defined in such a way the volume
    is directly proportional to kelvin temperature.
  • A 2-fold increase in the absolute temperature
    would increase the volume the same an increase
    from 273 K (0C) to 546 K (273 C) increases the
    volume from 273 mL to 546 mL.
  • A Kelvin reading is (T) is obtained by adding 273
    to the Celsius temperature (t)
  • T t 273

32
  • From the extrapolated line, we can determine the
    temperature at which an ideal gas would have a
    zero volume. Since ideal gases have infinitely
    small atoms the only contribution to the volume
    of a gas is the pressure exerted by the moving
    atoms bumping against the walls of the container.
    If no volume then there must be no kinetic energy
    left. Thus, absolute zero is the temperature at
    which all kinetic energy (motion) has been
    removed. NOTE This does not mean all energy has
    been removed, merely all kinetic energy.

33
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34
To avoid the need to know k, we use ratios. The
ratio of V to T of an ideal gas at constant
pressure is constant over all temperatures. Or...

35
  • A balloon racer uses the Charles law. When the
    air in the balloon gets warmer it expands and
    will become less dense and balloon floats in the
    air. When the air gets colder it will become more
    dense and it will come down in the air.

36
Example 2
  • A sample of a gas has a volume of 79.5 mL at 45
    C. What volume will the sample occupy at 0 C
    when the pressure is held constant?
  • Answer 68.2 mL

37
Amonton's Law (1703)
  • The Pressure of a gas is directly proportional
    to the Temperature (Kelvin) at constant V and n.
  • Example 3
  • A 10.0 L container is filled with a gas to a
    pressure of 2.00 atm at 0 C. At what temperature
    will the pressure inside the container be 2.50
    atm?
  • Answer 341 K 68 C

38
Molar Volume
  • Molar volume (Vm) is the volume that every mole
    of the material occupies (L. mol-1)
  • Vm V. occupied by the material/ No. of moles
    of it
  • Vm V / n
  • Physical data show that molar volumes of gases
    are equal at the same pressure and temperatures.
    Vm for some gases at 0 C and 1 atm
  • Argon
    22.09
  • Carbon dioxide
    22.26
  • Nitrogen
    22.40
  • Oxygen
    22.40
  • Hydrogen
    22.43

39
Avogadro's Law(1811)
  • The Volume of a gas is directly proportional to
    the moles of the gas, n at constant P and T. 
  • According to Avogadro, equal volumes of different
    (ideal) gases at the same temperature and
    pressure contain equal numbers of molecules
    (moles) of the different gases.

40
Ideal Gas Law
  • If we take the three of the gas laws we've
    studied so far, we can combine them into a single
    law called the Ideal Gas law. This law covers the
    relationship between temperature, pressure,
    volume and number of moles of an Ideal gas.
  • Avogadro's Law V k1n T,P
  • Boyle's Law V k2/P T,n
  • Charles' Law V k3T n,P

41
  • After some consideration and algebra, we arrive
    at
  • V koverall nT/P
  • where koverall turns out to be the Ideal gas
    constant
  • (or universal gas constant) 
  • We're more familiar with the equation written as
  • PV nRT
  • This is the Ideal Gas Law or the equation of
    state for an ideal gas. At ordinary conditions of
    temperature and pressure, most gases conform well
    to the behavior described by this equation.
    Deviations occur, however, under extreme
    conditions (low temperature and high pressure).

42
  • The molar volume of an ideal gas at STP (0 C and
    1 atm) 22.4136 L
  • So we can calculate the ideal gas constant
  • R PV / nT
  • (1 atm) (22.4136 L) / (1 mol) (273.15 K)
  • 0.082056 8.2056 x 10 2 L.atm / K.mol
  • Another form of the equation of state for an
    ideal gas
  • Since n g / MW
  • So PV (g/MW) RT

43
  • Example 4
  • The volume of a sample of gas is 462 mL at 35 C
    and 1.15 atm. Calculate the volume of the sample
    at STP.
  • Example 5
  • What is the density of NH3 (g) at 100 C and 1.15
    atm?
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