Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)
-
Upload
peter-townsend -
Category
Documents
-
view
226 -
download
1
Transcript of Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)
![Page 1: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/1.jpg)
Methane (CH4)
Ozone (O3)
Carbon Dioxide (CO2)Ammonia (NH3)
Nitrogen (N2)
Water Vapor (H2O)
![Page 2: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/2.jpg)
MOLECULAR ABSORPTION
From Previous lectures we know how to use absorption coefficients & cross sections to calculate absorption and emission by gases in the atmosphere.
BUT:•How do gases absorb radiation?
•Why do only certain gases absorb radiation?
• What dictates the nature of the absorption (wavelength,strength)?
![Page 3: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/3.jpg)
Elementary Molecular Spectroscopy
E1
E2
Absorption emission
E=h
Quantum mechanics dictates that virtually all energy transitions are discrete:•Absorption: molecule increases its energy
•Emission: molecule decreases its energy.
![Page 4: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/4.jpg)
Elementary Molecular Spectroscopy
One of the real clues as to the nature of the absorption emission process (and for that matter the nature of matter itself) came from the realization that bright and dark lines occur in the same spectral location
Bright lines of emission’
Dark lines of absorption
Wavelength or frequency
![Page 5: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/5.jpg)
Molecules can store energy in 4 discrete ways:
1.Translational (kinetic) energy – directly associated with the the TEMPERATURE of the gas. 2.Vibrational : Most molecules are constantly vibrating! (if their structures allow it)3.Rotational: Molecules can rotate on top of vibrating.4.Electronic: Relates to energy states of electrons inside a molecule
Energy storage potential in each type is :A.Electronic : HIGH (associated with visible/UV) B.Vibrational: MEDIUM-LOW (associated with IR/Microwave)C.Rotational: quite low – tacked on as a modified to vibrations, leading to “vibrational-rotational” absorption features.
![Page 6: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/6.jpg)
IMPORTANT NOTES:Because molecules are constantly
colliding when in Local Thermodynamic Equilibrium (LTE), the energies are constantly redistributed amongst kinetic, electronic, vibrational, and rotational modes of energy storage.
TRANSLATIONAL ENERGY is not quantized, but plays an important role in energy redistribution. Molecules that are excited by electronic/vibrational transitions will redistribute some of this extra energy to translational energy (ie HEATING)
EEL > EVIB > ETRANS > EROT
![Page 7: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/7.jpg)
The types of interactions that occurin matter depend on the rate ofoscillations that must be induced (i.e the wavelength of the incident radiation).
On the whole, shorter wavelength, radiation interacts with lighter andsmaller parts of matter whereas moresluggish slower oscillating radiationaffects the larger parts of matter.
We are mainly concerned with mechanisms affecting electrons, and atoms to more bulky molecules - mostly vibrational and rotational spectra
![Page 8: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/8.jpg)
ELECTRONIC TRANSITIONS ARE IMPORTANT IN the UltraViolet – It’s How Ozone protects us!
UV-A
UV-B
UV-C
• N2 generally unimportant in stratospheric chemistry
• Because of O2/O3, no photons make it below mid- stratosphere that can excite more electronic transitions.
![Page 9: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/9.jpg)
The Electric Dipole: Separation of + and - charge
The electric dipole is a characteristic of matter important to how E-M radiation interacts with matter.
The displacement or oscillation of charge in this the dipole creates a time varying dipole moment (ie. dp/dt) and in turn a time varying e-field and thus EM radiation
![Page 10: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/10.jpg)
Dipole Moments (electric or magnetic) ARE REQUIRED to interact with E-M radiation
![Page 11: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/11.jpg)
*
*
*Induced through vibrations
![Page 12: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/12.jpg)
THE OVERALL PICTURE
![Page 13: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/13.jpg)
MODES OF VIBRATION
Degenerate!
![Page 14: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/14.jpg)
Analog Models: Vibration of a Diatomic Molecule“It’s like a spring!”
Restoring Force F=-k(r-re)
harmonic oscillator predicts
the vibrationalquantum #
k=Spring constant
m’=“reduced mass”
![Page 15: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/15.jpg)
VIBRATION INFORMATION!
• Linear diatomic molecules have a single mode of vibration at fundamental frequency ν1.
• Triatomic (linear& nonlinear) have : ν1, ν2, ν3
• Energy of vibration E = (v+½) hν; v=0,1,2,3…
• QM rules require Δv=±1 !!!
• SO ΔE = hν (for a given vibrational mode)
• If you could only change one mode at a time, CO2 (e.g.) could only have 3 absorption regions. In reality it has a lot more!
![Page 16: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/16.jpg)
Analog Models: Rotation of a ‘Diatomic Molecule’
Rotating MoleculeCenter of mass: m1r1=m2r2
Moment of Inertia: I=m1r12+ m2r2
2
Energy: E=1/2 I2 =L2/2IAngular Momentum, L= I
![Page 17: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/17.jpg)
The more complex the molecule geometry, the more rotational degrees of freedom exist, and thus the more complex is the rotational absorption spectrum.
Linear molecules (CO2, N2O) - only one I, simple evenly spaced distribution of lines)
Symmetric top molecules (NH3, CF3Cl) - non linear, I1=I2,I3
Spherical symmetric top (CH4) - non linear, I1=I2=I3
Asymmetric top (H2O) - non linear and all moments of inertia are different - complex (random) spectrum
![Page 18: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/18.jpg)
ROTATION INFORMATION!• In reality, most atmospheric gas molecules
have one or two nonzero moments of inertia
• Angular momentum is quantized by
• E = ½L2/I =
• QM rules require • Usually: ΔJ=±1 only• Degenerate: ΔJ=±1, or 0 (not J=00)
• SO ΔE =
• Leads to equally spaced lines (J=0,1,2,3 etc)
• Rotations are often a perturbation on vibrational transitions
![Page 19: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/19.jpg)
Fundamental Vibrational Mode
First Harmonic VibrationalMode
ΔJ= -1
ΔJ= 0
ΔJ= +1
ROATIONAL-VIBRATIONAL Transitions
![Page 20: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/20.jpg)
Rotation-Vibration Modes
vibrations + rotations typically occurtogether - at least < 20 m
selection rules (from q-theory) establishwhich transitions are permitted
Diatomic molecule v= 1, J= 1 P&R Branch
Triatomic (linear) molecule (CO2) v= 1, J= 1 P&R Branch v= 1, J= 0 Q Branch
![Page 21: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/21.jpg)
IMPORTANT SOLAR ABSORPTION BANDS
From Liou, Chapter 3
• Most useful in remote sensing! Can often derive column-integrated quanties of these gases.
• Can be important for energy balance (H2O especially)
![Page 22: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/22.jpg)
P-Branch
R-Branch
Q-Branch
15 μm ν2 CO2 Transition
![Page 23: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/23.jpg)
15 μm CO2 Transitions (mainly ν2)
![Page 24: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/24.jpg)
The thermal IR spectrum, again
![Page 25: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/25.jpg)
Isotopologues Matter!
![Page 26: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/26.jpg)
Summary electricPermanent magnetic dipole - yes
Insert fig. 8.9
![Page 27: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/27.jpg)
![Page 28: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/28.jpg)
VERY LITTLE RHYME OR REASON
![Page 29: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/29.jpg)
Summary in Words of Gas Transitions (1)
• 3 types of quantized transitions important to us:• Electronic (highest energy: UV-Vis)• Vibrational (medium energy: Vis-NIR-Thermal IR)• Rotational (Far IR & Microwave)
• Other types of absorption are not quantized:• Photo-Ionization : Ripping electronic off to make ion
(Occurs when photon energy > ionization energy of molecule)• Photo-Dissociation: Tearing an atom off a molecule
(E.g. O3 O2 + O* - critical for stratospheric chemistry)(Occurs when photon energy > dissociation energy of molecule)
• Pure rotational transitions can happen ONLY if molecule has a permanent electric dipole moment: (e.g. H2O, CO, O3).
• Symmetric linear molecules (N2, CO2, N2O) do not have a permanent dipole moment.
![Page 30: Methane (CH4) Ozone (O3) Carbon Dioxide (CO2) Ammonia (NH3) Nitrogen (N2) Water Vapor (H2O)](https://reader036.fdocuments.us/reader036/viewer/2022062309/56649dff5503460f94ae6bff/html5/thumbnails/30.jpg)
Summary in Words of Gas Transitions (2)
• Rotational transitions often accompany vibrational transitions
• Rotational quantum number J changes by (-1,0, or 1) when vibrational quantum number v changes by ± 1. • ΔJ = -1 “P-branch”• ΔJ = 0 “Q-branch” if it exists! Only allowed if the vibrational
transition is “degenerate” , e.g. the ν2 transition of CO2!• ΔJ = +1 “R-branch”
• The energy associated with ΔJ = ±1 is proportional to the starting J state For example: J = 34 takes 3 times more energy than J = 01 !
• The energy associated with Δv = ±1 does not depend on starting v state: they all take the same energy.