Chapter 15 (4.2.2) Flashcards
Reactivity of haloalkanes
- in the carbon-halogen bond, the halogen is more electronegative than carbon, so electron pair in the carbon-halogen bond is closer to the halogen atom
- so the bond is polar
- carbon has a slightly positive charge (𝛿+) and can attract species containing a lone pair of electrons
What is a nucleophile?
An electron pair donor, e.g. :OH⁻, H₂O:, :NH₃
What is nucleophilic substitution?
A reaction in which a nucleophile is attracted to an electron-deficient carbon atom and replaces an atom or group of atoms on the carbon atom. Primary haloalkanes undergo this.
What is hydrolysis?
A chemical reaction involving water or an aqueous solution of a hydroxide that causes the breaking of a bond in a molecule.
In hydrolysis of a haloalkane, carbon-halogen bond is broken and the halogen atom is replaced by an -OH group.
Mechanism of nucleophilic substitution (explanation but know how to draw)
- nucleophile, OH⁻, approaches the carbon atom attached to the halogen on the opposite side of the molecule from the halogen atom (to minimise repulsion between the nucleophile and the 𝛿- halogen atom).
- lone pair of electrons on the hydroxide ion is attracted and donated to the 𝛿+ carbon atom.
- new bond formed between O atom of OH⁻ and the C atom
- carbon-halogen bond breaks by heterolytic fission
- alcohol and halide ion formed
Conditions of hydrolysis of haloalkanes
- haloalkanes can be converted into alcohols using aqueous sodium hydroxide
- very slow reaction at room temperature, so heated under reflux to obtain a good yield of product
Carbon-halogen bond strength
- Rate of hydrolysis depends on the strength of the carbon-halogen bond in the haloalkane
- C-F > C-Cl > C-Br > C-I
- Bond enthalpies show that iodoalkanes react the fastest etc; fluoroalkanes are unreactive as a large quantity of energy is required to break the C-F bond.
General equation for the rate of hydrolysis with water
CH₃CH₂CH₂X +H₂O —-> CH₃CH₂CH₂OH + H⁺ + X⁻
Hydrolysis of haloalkanes with water (reactions and reagents)
- Reaction carried out in the presence of aqueous silver nitrate, AgNO₃ (aq).
- Halide ions, X⁻ (aq), are produced which will react with Ag⁺ (aq) ions to form a precipitate of the silver halide:
Ag⁺ (aq) + X⁻ (aq) —-> AgX (s) - the nucleophile is the water present in aqueous silver nitrate
- haloalkanes are insoluble in water, so ethanol solvent is present to allow the water + haloalkane to mix and produce a single solution rather than 2 layers
Measuring the rate of hydrolysis of haloalkanes practical
- Set up 3 test tubes, each with 1cm³ of ethanol and 2 drops of the haloalkane
- Stand in a water bath at 60°C
- Place test tube of 0.1moldm⁻³ AgNO₃ in bath and allow to reach the constant temperature
- Add 1cm³ of the AgNO₃ to each test tube. Start the stop-clock.
- Observe and record time for precipitate to form (for 5 minutes)
Observations from hydrolysis practical
1-chlorobutane - white precipitate formed very slowly
1-bromobutane - cream precipitate formed at a medium pace
1-iodobutane - yellow precipitate formed rapidly
Uses of organohalogen compounds
Pesticides, dry cleaning solvents, refrigerants etc
The ozone layer
- found at the outer edge of the stratosphere
- tiny amount of ozone is enough to absorb UV-B from the suns rays, only allowing a small amount to reach Earth’s surface
- UV-B = linked to sunburn + increases risk of skin cancer and genetic damage
- depletion of ozone layer could allow more UV-B
- in the stratosphere there is continuous formation and breakage of ozone by UV radiation
Equations for breakage and forming of ozone
Initially very high energy UV breaks oxygen molecules into oxygen radicals
O₂ —-> (UV) 2O•
Steady state (where rate of formation of ozone is the same at which it is broken down) set up involving O₂ and oxygen radicals in which ozone forms and then breaks again
O₂ + O• O₃
- production of CFCs has upset the delicate equilibrium
CFCs and the ozone layer
- chlorofluorocarbons are very stable due to strong carbon-halogen bonds
- remain stable until they reach the stratosphere, where they breakdown, forming chlorine radicals which are thought to catalyse the breakdown of the ozone layer