Chemistry 2045 Gasses
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Gases
Our first look at large collections of
particles acting together!
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Gases & Atoms First
The simplest model of a gas has all the
molecules moving and acting independently.
But, with a large number of particles, their
average behavior is strictly delineated.
Only He, Ne, Ar, Kr, Xe, and Rn are atomic
gases.
Really, we are looking at a particles-first
approach here!
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Basic Ideas of This Chapter
We present the ideal gas first.
Gas molecules move independently.
Forces between molecules are nil.
Model seems very simple but it explains a greatdeal!
We shall end with a description of real gases.
Some intermolecular forces enter in. Structural effects (in terms of size) of molecules
also enter into our discussions.
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Studying the Behavior of Substances
To give a more general perspective, there arecertain things we can measure that lead tounderstanding the state of a system.
A short list: Pressure (P)
Volume (V)
Temperature (T) Amount of substance (mass or moles, wor n)
Composition (for mixtures; notation later)
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A Little Analysis
The properties listed on the previous slide arewhat we could call observables.
One thing we try to do in science is connectobservables together if possible.
Ideally, we can get an equation of state.
Having the equation of state, we then try to gofurther and explain itin terms ofindividual
particles. That is one of the main things we shall do in this
chapter.
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Our First Physical Property: P
P stands for pressure.
Pressure = force/unit area
On the average, you have 14.7 lb of air aboveyou.
This exerts the same pressure on you from all
sides! Why? (We explain this verbally.)
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Here is the explanation!
Pressure is caused by
particles (molecules)
hitting you.
When a moleculebounces off you, its
change of momentum is
the force exerted.
An equal number ishitting you from all sides!
Pressure is thus isotropic.
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Needless to say, the more particles,
the higher the pressure!
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Units of Pressure
We usually think of pressure in terms ofstandardatmospheric pressure.
The SI unit of pressure is the pascal (Pa).
This is 1 Pa = 1 N/m2. 1 atm 101325 Pa (exactly!)
The next slide shows some standard pressure
units. Ones with exact defintions are marked with an
asterisk (*).
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Some Pressure Units
Unit Abbreviation Std. Atmospheric Pressure
Pascal Pa (= 1 N/m2) 101325 Pa (*)
Pounds/in2 psi (or ) 14.6959488 psi
Torr (mm Hg) torr 760 torr (*)
Bar bar 1.01325 bar (*)
Inches of mercury in Hg 29.9212598
Atmosphere atm 1 atm (*)
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Measuring Pressure
Various instruments are
used nowadays.
For measuring air
pressure, the traditionalinstrument is the
mercury barometer.
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Measuring Gas Pressures
Pressures are measuredby manometers.
Some of these aremechanical but the
traditional instrumentsuse columns of Hg.
At the right is an open-ended manometer.
Note that we have tocorrect for atmosphericpressure!
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Other types of Manometers
Simple Closed-End Manometer A McLeod Gauge (Low Pressures)
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We now look at some gas laws.
Remember our observable variables:
n, P, V, and T
For the various laws, we keep two of these
constant and note how the remaining two
are related.
We examine these in the next few slides...
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Boyles Law
Tand n held constant.
Vis inversely
proportional to P.
Or, PV = constant.
Boyle is watching us to
the right!
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A Depiction of Boyles Experiment
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For a gas subject to Boyles Law...
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Charless Law
Here, we hold n and P
constant and observe V
vs. T.
V T V= (const) T
Needless to say, Charles
very much approves ofus using his work!
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Here we see the experimental results!
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Note the intercept!
All gases extrapolate to the same point.
This is -273.15C.
This is also 0.00 K. In other words, this is the first place that the
concept ofabsolute zero appears.
T(K) = T(C) + 273.15
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For a gas subject to Charles Law...
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We see something similar for P.
IfVand n are held
constant, we can look at
P vs. T.
P T. Or, P = (const) T.
This the law of Gay-
Lussac (not mentionedin book).
Gay-Lussac...
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Pour Monsieur Gay-Lussac...
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Avogadros Law
Here, we hold P and Tconstant and observe Vvs. n.
This is really where theconcept of the molewas first proposed.
Credit for this goes toAvogadro...
...who, of course, is alsowatching us!
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Avogadros Law is also a simple
graph...
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For a gas obeying Avogadros Law...
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Here are the 3 laws as in the book...
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These can be combined to give...
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We make this an equation by putting
in a constant...
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How the text looks at this...
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Another view of the constant...
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Values ofR
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Note these exactconversion factors...
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We can exploit this sometimes to get a
combined gas law (verbal discussion)...
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We write the combined gas law on the
board...
We look at how this handles the following
Boyles Law case...
Charles Law case...
Avogadros Law case...
Single gas sample at different P, V, and T(same n)
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In all this...
Watch your units!
We especially need to
watch R!
Also, how do we besthandle changes in
pressure, temperature,
and energy units.
We shall now discuss
some of these topics!
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We have two definitions of the mole
we shall be using...
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How many particles in a mole?
NA = 6.0221415 1023 mol-1
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Some Delightful Applications!
I. Molar Volume
II. Gas Density
III. Molar Mass (molecular weight) of a Gas
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Molar Volume
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Special Condition: STP
STP means standard temperature at pressure
P = 1 atm (exactly)
T= 0.00C = 273.15K
Under these conditions, V= 22.4Lfor all idealgases!
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A More Precise Calculation (n = 1)
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All IdealGases the Same! (AIGATS!)
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Density: General Definition pHirst!
density = mass/volume
Units:
g/L (gases)
g/mL (liquids & solids)
kg/m3 (SI unit)
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Density of a gas...
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Molar Mass of a Gas
This is important!
This is a method of
determining molar mass
(aka molecularweight)
The equation is to the
right...
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Gas Mixtures & Partial Pressures
Ideal gases in a mixture exert their pressures
independently.
This is called Daltons Law of Partial Pressures.
We show some math in the next slide...
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Look at a mixture of gases A, B, C, & D
Thi l d i i
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This leads to a concentration unit,
mole fraction (for a given gas, i)
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Useful Relations...
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Collecting Gases over Water
A common method of
collecting gaseous
products of reactions.
Works well as long asthe gas is not soluble in
water!
This is the first time that
we encounter vapor
pressure.
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Yes, water is a liquid but...
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Example: Collecting H2 over water
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Gas Stoichiometry
Before we get started on
this, please remember
that we have two
definitions for a mole:
In terms of mass.
In terms of the ideal gas
law.
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A Thank You to John Dalton!
In his prime! After too much pHun with gases!
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Shortcut Method for Stoichiometry
1) Write the balanced chemical equation.
2) Place the relevant coefficients below theequation.
3) Place the relevant number of moles abovethe equation.
4) Construct the needed equation from ratios.
5) Solve this equation for whatever you arelooking for (pressure, moles, mass, volume,etc.)
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A Picture of the Shortcut Method
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Comparing Moles via Ratios
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An Abstract Example
How many grams ofB are
needed to produce VmL
of a gas, C, at a given P
and T?
The way to set this up is
shown to the right.
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Two ways to do these problems!
I. Write the balanced chemical equation (BCE)
and construct the algebraic solution for a
given problem by use of ratios.
II. Use conversion factors as shown in the book.
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The Kinetic Theory of Gases
This is a very simple model.
But it gives a lot of profound conclusions.
Coupled with quantum mechanics, it actually
predicts the ideal gas law.
We shall skip the QM however!
And look at other things more relevant to us!
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Some Postulates...
I. The size of gas particles is negligibly small.
II. The average kinetic energy of a particle is
proportional to the temperature (in K).
III. All collisions between particles and with the
walls of the container are completely elastic.
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pHun with equations!
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pHun (continued)...
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pHun (it goes on!)...
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pHeeling the Pressure?
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Remember the 2nd Postulate?
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Lets put it in!
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And...................
pHinally putting in THE constant
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pHinally, putting in THE constant
gives...
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Lets Look at a Gas in Action...
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Time to Call in Some Mechanics!
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Major Point!
In a gas at a given temperature, lighter particles
travel faster (on average) than do heavier ones!
BUT, all have the same (average) kinetic energy!
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Remember...
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Root Mean Square Velocity
To make sense of this we need the
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To make sense of this, we need the
MOLE!
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Some Razzle-Dazzle Math!
f
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pHinal Equation for RMS Speed...
h h !!!
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Watch your units here!!!
R = 8.314472 J/molK
MSIis in kg/mol (!)
(This is the SI unit for MW)
Tis in Kelvins.
( )
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Example: Nitrogen gas (N2) at 25.00C
l 2 00C
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Example: He gas at 25.00C
F S k f C l
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For Sake of Completeness...
Average Velocity Most Probable Velocity
A C i
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A Comparison...
A G hi l Vi
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A Graphical View
A d th i
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And another view...
T P t L k At N
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Two Processes to Look At Now
Diffusion
This is the process whereby
two gases mix.
Basically, the molecules mix
while colliding.
This is influenced by the meanfree path (discussed shortly).
Effusion
This is the rate of escape of
molecules through a pin hole
into a vacuum.
How this (and diffusion) are
handled by kinetic theory is
shown in the next slide.
O Pi t f Diff i
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One Picture of Diffusion...
A d th (dj ?)
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And another (dj vu?)...
A Pi t f Eff i
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A Picture of Effusion
B th P F ll G h L
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Both Processes Follow Grahams Law
The rate of effusion(diffusion) is inversely
proportional to the
square root of the
molar mass.
Derivation on next slide.
In the meantime, meet
Thomas Graham!
A Sh t D i ti
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A Short Derivation
Mean Free Path
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Mean Free Path
Until now, we havebeen ignoring molecular
size.
But molecules docollide and do have size.
The distance a molecule
travels between
collisions is called themean free path.
An Equation for Mean Free Path ()
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An Equation for Mean Free Path ()
is the molecularcollision diameterin m.
P is the pressure in
pascals. R is in J/molK.
This is just a bonus
equation and will not be
on exams!
Example: Mean free path in O
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Example: Mean free path in O2
We shall assume STP. The molecular diameter
of O2 is 361 pm.
We shall analyze theunits on the board.
(Under the conditionsof this problem, O2travels about 180molecular diametersbefore colliding.)
A Bonus: The Speed of Sound
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A Bonus: The Speed of Sound
Monatomic Gas Diatomic Gas
Examples (25 00C)
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Examples (25.00 C)
Helium Nitrogen
Real Gases
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Real Gases
These differ from ideal gases in the followingways:
Real molecules are not pointsthey have size.
There are attractive forces between the molecules.
Conditions for a gas to behave like an
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ideal gas...
High temperature (explain why!)
Low pressure (again, explain this!)
Experimental Molar Volumes (STP)
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Experimental Molar Volumes (STP)
We look at Ar and pressure
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We look at Ar and pressure...
Correcting for Molecular Volume
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Correcting for Molecular Volume
Ideal Gas Volume Correction
We look at Xe and Pressure
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We look at Xe and Pressure...
Correcting Pressure for Effects of
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Intermolecular Forces
Ideal Behavior Pressure Correction
Multiplying the Corrected Values Together Gives
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the van der Waals Equation
Ifn = 1, this takes on a simpler form!
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(Vm is the molar volume.)
This is a semi-empirical equation
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This is a semi-empirical equation...
The form of theequation comes from
good physical
arguments.
But, a and b must be
obtained
experimentally.
A table of these is tothe right...
A little chalk talk
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A little chalk talk ...
The vdw equation is anequation of state forreal gases.
It is about the simplest
one that works well. But, it is not perfect!
There are many otherequations!
As you can see, van derWaals was proud of it!
Another view of real gas behavior
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Another view of real gas behavior
Z = PV/RT is called thecompressibility factor
of a gas.
Z = 1 for an ideal gas.
Real gases are much
more interesting!
See the slide to the
right (gases at 273K)...
The End of Gases!
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The End of Gases!
Yes, that
is
enough!