CL 15- haloalkanes Flashcards
ozone also
why do haloalkanes have higher boiling points than alkanes?
- contain london forces and permanent-permanent dipole forces which are stronger than just london forces in alkanes
- requires more energy to overcome (still have low boiling points)
experiment to measure the rates of hydrolysis of haloalkanes
AgNO₃ and ethanol
- set up 3 test tubes with 1cm³ of ethanol
- add 2 drops of one of the haloalkanes to each test tube (R-Cl, R-Br, R-I)
- warm to 60°C in water bath
- warm 3 test tubes containing 1cm³ of AgNO₃
- mix a silver nitrate and haloalkane test tube
- time how long it takes for a precipitate to form
why do we need ethanol in the experiment?
haloalkanes are insoluble, so using ethanol ensures that they dissolve and can react with the water molecules
nucleophile
definition
electron pair donor
explain the trend in the rates of hydrolysis of primary haloalkanes
in terms of carbon-halogen bonds
bond strength decreases
C-F > C-Cl > C-BR > C-I
the weaker the bond strength, the faster the hydrolysis
when is ozone good?
when it’s in the stratosphere, prevents harmful UV light reaching organisms on earth
when is ozone bad?
when it’s in the troposphere, harmful on respiratory tracts of animals
what is ozone’s job?
think UV with lower wavelengths
entirely screen out 200-280nm wavelength UV-c
high energy so potentially very damaging
UV-a reaches earth’s surface and is responsible for skin aging
UV-b is partially filtered out by ozone and causes sunburn and cancer
why is there a problem concerning ozone levels?
- the rate of removal of ozone used to equal the rate of production of ozone
- humans have added substances to the atmosphere that have disrupted the rate of removal
uses of CFC’s
chlorofluorocarbon
- refrigerants, cools fridge down
- propellants (aerosol sprays)
- fire extinguishing (removed oxygen)
equation for the production of halogen radicals (by the action of UV radiation on CFC’s in the upper atmosphere)
CF₂Cl₂ –> CF₂Cl. + Cl.
the equation for the resulting catalysed breakdown of the earth’s protective ozone layer
O₃ + O –> 2O₂
catalysed breakdowns of ozone by Cl.
propagation steps
Cl. + O₃ –> ClO. + O₂
ClO. + O –> Cl. + O₂
catalysed breakdown of ozone by NO .
propagation steps
NO. + O₃ –> NO₂. + O₂
NO₂. + O –> NO. + O₂