Chemistry The Atmosphere
- Created by: Chloesn
- Created on: 12-03-14 14:34
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- Chemistry Unit 4
- Chloroflurocarbons
- Alternatives
- Global warming
- Human activity
- Molecules and networks
- Diamond
- Silicon(IV) oxide
- CO2
- SiO2
- Newtwork
- (Giant structures)
- Molecular structure
- CO2
- What happens when radiation reacts with matter
- The atmosphere
- Stratosphere
- Trophosphere
- Ionosphere
- 21% Oxygen
- 0.93 Argon
- 78% Nitrogen
- Energy changes the electromagnetic spectrum
- EM order - RMIVUXG
- Visible light order - ROYGBIV
- Richard Of York Gave Battle In Vain
- Electronic changes when molecules absorb radiation
- Energy interacts with matter
- Translational
- Radio
- Rotational
- Micro
- Vibrational
- Infrared
- Electronic
- Visible and Ultraviolet
- Translational
- E = hv
- E = energy
- V = fequency
- h = Plancks constant
- 6.63 x 10-34
- Upside down y = wavelength
- C = speed of light
- 3.00 x 108 ms-1
- The atmosphere
- Radiation and radicals
- Fission (break)
- Heterolytic
- Homolytic
- Radical chain reaction
- Initiation
- Propagation
- Termination
- Reactions of alkanes with halogens
- Formation and destruction of the ozone
- Ozone depletion
- Fission (break)
- Chemical equilibrium
- Dynamic equilibrium
- Changing
- Equal
- Reversible
- Steady state
- Dynamic equilibrium
- Rates of reaction
- Collision theory
- Activation enthalpy
- Enthalpy profile
- The effect of temperature on rate
- Activation enthalpy
- Maxwell-Boltzmann distribution
- How do catalyst work?
- Hetergeneous catalyst
- Homogenous catalyst
- Chloroflurocarbons
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