Ozone

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  • Created by: Science
  • Created on: 20-04-21 16:16

Ozone

Troposphere - bottom layer    Stratosphere - ozone

Gas percentages in air

  • 78% Nitrogen
  • 21% oxygen 
  • 399ppm CO2
  • 0.93% Argon

Converting between % and ppm

  • % - ppm multiple by 10000
  • ppm - % divide by 10000

Solar energy

  • Radiowaves stopped by atomosphere
  • x rays and gamma rays lost in magnetosphere
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Ozone

UV light

  • high energy UV radiation absorbed by ozone 
  • breaks DNA bonds (photodissociation) causing mutation/skin cancer

Ozone

  • highly reaction
  • tropospheric ozone formed from exhaust gases and unburnt hydrocarbons

Energy equations

  • wave speed = frequency x wavelength
  • energy = plank constant x frequency

Molecule behaviour

  • visible light/UV promotoes electrons
  • infrared causes vibration
  • Microwaves causes rotation
  • Temperature above Kelvin causes translation
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Ozone

Calculating frequency from bond enthalpy

  • Divide by Avogadro's constant
  • Convert energy to joules
  • use E=hv to work out frequency

Heterolytic bond fission - forms ions

Homolytic bond fission - forms radicals 

Radicals - species with an upaired electron

Chain reaction

  • Initiation
  • propagation
  • Termination

Steady state reaction - rate of formation = rate of destruction 

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Ozone

Forming ozone

  • O2 + high energy UV --> 2O
  • O+ O --> O3
  • O + O --> O2

Destruction of ozone

  • O + O3 --> 2O2
  • O3 + high energy UV --> O2 O
Factors affecting rates of reaction
  • temperature
  • surface area
  • catalyst
  • radiation intensity
  • pressure
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Ozone

Activation energy - minimum amount of energy required to break bonds

Maxwell - Boltzmann distribution curve

  • area under graph = number of particles
  • increase in temperature - graph moves to right and is lower down
  • catalyst changes Ea line

General rule- increase by 10 derees, rate is doubled

Polarity

  • when one atom higher charge denisty then the other 
  • due to a difference in electronegative

Electronegativity

  • measure of ability of an atom in a molecule to attract electrons in a chemical bond to itself
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Ozone

Intermolecule forces

  • Instantaneous dipole - induced dipole
  • permanent dipole - induced dipole
  • permanent dipole - permanent dipole

Boiling points

  • increased carbon chain = stronger bonds due to larger number of electrons
  • branching decreases strength of bonds reducing contact points

Hydrogen bonding

  • type of permanent dipole - permanent dipole 
  • molecule 1: H atom attached to highly electronegative atom
  • molecule 2: highly electronegative atom with at least one lone pair of electron
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Ozone

Chlorofluorocarbons

  • low toxicity
  • non-flammable 
  • high stability

Hydrofluorocarbons (HFC) - fluorine radicals aren't formed in stratosphere

Hydrochlorofluorocarbons (HCFCs) - C-H bond broken in low troposphere 

Haloalkanes

  • C-F bonds can't undergo photodissociation 
  • C-Br / C-I broken lower in troposphere 

Chlorine

  • CH3Cl undergoes photodissociation to create Cl radical
  • homogeneous catalysts 
  • X + O3 --> O2 + XO
  • XO + O --> O2 + X
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