Title: Topics for Today
1Topics for Today
- Greenhouse Gases How do they keep us warm?
2Readings for Today
- 3.4 Vibrating Molecules and the Greenhouse Effect
3Topics for Friday
- Climate Change A Global Problem?
- Quiz 7 (of 11)!!
4Readings for Friday
May even bleed into Monday.
- 3.8 Methane and other greenhouse gases
- 3.10 Responding to science with policy changes
- 3.11 The Kyoto Protocol on Climate Change
- 3.12 Global warming and ozone depletion
5Announcements!!!
6Bring back your radon disks!!
7Announcements!
Nice, warm weather
Please remember Do not wear shorts or sandals to
lab!!
8Exam Regrading
Same process as Exam 1.
9Topics for Today
- Greenhouse Gases How do they keep us warm?
10Review from Monday
11Review
The Greenhouse Effect
12Review from a long time ago.
(
Lecture 15.
(
13What happens when a molecule absorbs light?
14(No Transcript)
15(No Transcript)
16(No Transcript)
17What happens to a molecule when it absorbs IR?
18Among other motions, this includes stretching and
bending!
Figure 3.17
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20What happens to a molecule when it absorbs IR?
21Q When will IR cause a molecule to vibrate?
A When there is a dipole moment!
22- Dipole Moment Unequal distribution of charge!
Where have we seen dipole moments before?
23- Polar Bonds Unequal sharing of electrons in a
chemical bond. Still a covalent bond!
RESULTS IN AN UNEQUAL DISTRIBUTION OF CHARGE!!
From Lecture 19 or so
24A bunch of polar molecules
d-
d
H
Cl
N
d-
That is, they have dipoles
H
H
d
d
H
d
d-
O
H
H
d
d
25What about some other molecules?
..
..
O
C
O
..
..
26Carbon Dioxide
Polar or nonpolar bonds?
..
..
O
C
O
..
..
27Carbon Dioxide
Polar bonds
..
..
d
O
C
O
d-
d-
..
..
28Carbon Dioxide
Polar or nonpolar molecule?
..
..
d
O
C
O
d-
d-
..
..
29So, no overall dipole moment
Carbon Dioxide
Nonpolar Molecule
..
..
Why does it absorb IR radiation?
d
O
C
O
d-
d-
..
..
But CO2 is a greenhouse gas!
30The IR can cause (or induce) a dipole moment!
31Possible Vibrations for CO2
Think ELECTRONEGATIVITY!!!
32- Symmetric Stretch
- Both out, both in
- Keeps linear shape
33- Symmetric Stretch
- Both out, both in
- Keeps linear shape
34Does this induce a dipole moment?
- Symmetric Stretch
- Both out, both in
- Keeps linear shape
35- Asymmetric Stretch
- One in and one out
- Keeps linear shape
36- Asymmetric Stretch
- One in and one out
- Keeps linear shape
37Does this induce a dipole moment?
- Asymmetric Stretch
- One in and one out
- Keeps linear shape
38- Bend
- Bends in one plane
- Loses linear shape
39- Bend
- Bends in one plane
- Loses linear shape
40- Bend
- Bends in one plane
- Loses linear shape
Does this induce a dipole moment?
41- Bend
- Bends in another plane
- Loses linear shape
Same as the other bend, just in a different plane
42IR vibrations for a linear 3 atom molecule
Figure 3.17
43Bending in each plane
http//chemistry.boisestate.edu/rbanks/spectroscop
y/co2vibrations.gif
44CO2 bending and stretching
- Summary
- Symmetric Stretch
- Asymmetric Stretch
- Bend 1
- Bend 2
Which of these is able to produce a dipole moment?
CO2 has THREE possible ways to absorb IR!!
How do we measure this?
45Spectrophotometry
Sort of
46What are wavenumbers?
Figure 3.15 in your Text
47What is transmittance?
4 µm 4000 nm!
48Absorbance
The opposite of absorbance!
49Review
The Greenhouse Effect
50http//www.spaceguarduk.com/cd/dict/dictionary/inf
rared.htm
51Where is visible light?
Higher Energy
Lower Energy
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53What happens when a molecule absorbs light?
It depends on the wavelength
54What happens to a molecule when it absorbs IR?
55What happens when a molecule absorbs light?
It depends on the wavelength
AND on the molecule.
56Summary
For a molecule to absorb IR radiation, it must
1) Permanently have an uneven distribution of
charge (dipole)
57Polar molecules have dipole moments
d-
d
H
Cl
N
d-
H
H
d
d
H
d
d-
O
H
H
d
d
58Summary
For a molecule to absorb IR radiation, it must
1) Permanently have an uneven distribution of
charge (dipole) OR 2) Vibrate in a way that
can CREATE an uneven distribution of charge
(dipole)
Nonpolar molecules MAY or MAY NOT absorb IR
radiation
59CO2 bending and stretching
- Summary
- Symmetric Stretch
- Asymmetric Stretch
- Bend 1
- Bend 2
60Summary
For a molecule to absorb IR radiation, it must
1) Permanently have an uneven distribution of
charge (dipole) OR 2) Vibrate in a way that
can CREATE an uneven distribution of charge
Nonpolar molecules MAY or MAY NOT absorb IR
radiation
61Do N2, O2, or Ar absorb IR radiation?
621) Polar or nonpolar molecules?
Do N2, O2, or Ar absorb IR radiation?
2) Can we vibrate these to produce a dipole
moment?
..
..
..
O
N
N
O
..
Ar
..
..
63These molecules / atoms are NOT GHGs.
1) They are nonpolar 2) They cannot vibrate to
create an unequal distribution of charge.
64Summary
For a molecule to absorb IR radiation, it must
1) Permanently have an uneven distribution of
charge (dipole) OR 2) Vibrate in a way that
can CREATE an uneven distribution of charge -A
molecule with 3 atoms
65How about water?
Is water polar?
..
..
But it can also vibrate!!
O
H
H
66And a very potent GHG!!
Water vapor is an extremely strong absorber of IR
67Water Vapor
Figure 3.16
68CO2
Figure 3.15 in your Text
69Water Vapor
Figure 3.16
CO2 absorbs here
70Water Vapor
Figure 3.16
Different molecules absorb different wavelengths!
CO2 absorbs here
71Does an increase in water vapor lead to an
increase in Earths temperature?
72On one hand
73Water Vapor
Figure 3.16
74On one hand
On the other hand
75Interactions with Clouds
- Clouds Condensed water on a seed particle
- Reflects solar radiation
76Review
What is the Greenhouse Effect?
77The Greenhouse Effect
- Greenhouse gases are transparent to incoming
solar radiation - Greenhouse gases absorb the infrared light which
is emitted from the earth - This traps energy in the earths atmosphere
Long-wave radiation
Greenhouse Gases
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79About 80 of the heat emitted from the surface is
trapped in the atmosphere
80The Earths atmosphere is about 380 ppm CO2
The average temperature is about 59oF
81About -4 oF!
What would the average temperature of Earth be
with no CO2?
82About 80 of the heat emitted from the surface is
trapped in the atmosphere
Any more than this 80 is called the enhanced
greenhouse effect.
83Some people are worried that this will lead to
climate change (global warming)
84Greenhouse gases
- CH4
- CO2
- H2O
- N2O (nitrous oxide)
- CFCs and replacements
85Greenhouse gases
- CH4
- CO2
- H2O
- N2O (nitrous oxide)
- CFCs and replacements
DONE!
86Water Vapor
Figure 3.16
87Water Vapor
- Extremely strong dipole moment (Very good at
absorbing IR) - Most abundant greenhouse gas (varies from 0-4 of
the atmosphere)
88N2O
HCFCs
CH4
CFCs
O3
HFCs
CO2
H2O
89What makes greenhouse gases more potent?
N2O
HCFCs
CH4
CH4
CFCs
O3
HFCs
CO2
H2O
901) Atmospheric Lifetime
91Methane
Atmospheric lifetime about 10 years
Removed by the hydroxyl radical we will see this
reaction Monday!
92CFCs
Atmospheric lifetime gtgt 100 years
Destroyed in the stratosphere by UV-C
931) Atmospheric Lifetime
2) Atmospheric Concentration
94Concentration of CO2 is about 370 ppm.
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96Concentration of CO2 is about 370 ppm.
CFC concentrations are around 0.007 ppm
973) How efficiently can the molecule absorb IR?
1) Atmospheric Lifetime
2) Atmospheric Concentration
98CO2 bending and stretching
CO2 has only 3 vibrations
- Summary
- Symmetric Stretch
- Asymmetric Stretch
- Bend 1
- Bend 2
99CFCs
This is due to the more complicated SHAPE
CFCs have at least 10 possible vibrations!!
CFCs are much more efficient at trapping IR than
CO2.