Chapter 15 (4.2.2) Flashcards

1
Q

Reactivity of haloalkanes

A
  • 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
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2
Q

What is a nucleophile?

A

An electron pair donor, e.g. :OH⁻, H₂O:, :NH₃

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3
Q

What is nucleophilic substitution?

A

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.

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4
Q

What is hydrolysis?

A

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.

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5
Q

Mechanism of nucleophilic substitution (explanation but know how to draw)

A
  • 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
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6
Q

Conditions of hydrolysis of haloalkanes

A
  • 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
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7
Q

Carbon-halogen bond strength

A
  • 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.
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8
Q

General equation for the rate of hydrolysis with water

A

CH₃CH₂CH₂X +H₂O —-> CH₃CH₂CH₂OH + H⁺ + X⁻

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9
Q

Hydrolysis of haloalkanes with water (reactions and reagents)

A
  • 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
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10
Q

Measuring the rate of hydrolysis of haloalkanes practical

A
  1. Set up 3 test tubes, each with 1cm³ of ethanol and 2 drops of the haloalkane
  2. Stand in a water bath at 60°C
  3. Place test tube of 0.1moldm⁻³ AgNO₃ in bath and allow to reach the constant temperature
  4. Add 1cm³ of the AgNO₃ to each test tube. Start the stop-clock.
  5. Observe and record time for precipitate to form (for 5 minutes)
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11
Q

Observations from hydrolysis practical

A

1-chlorobutane - white precipitate formed very slowly
1-bromobutane - cream precipitate formed at a medium pace
1-iodobutane - yellow precipitate formed rapidly

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12
Q

Uses of organohalogen compounds

A

Pesticides, dry cleaning solvents, refrigerants etc

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13
Q

The ozone layer

A
  • 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
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14
Q

Equations for breakage and forming of ozone

A

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

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15
Q

CFCs and the ozone layer

A
  • 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
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16
Q

Depletion of the ozone layer by CFCs (e.g. CF₂Cl₂)

A
  • UV radiation initiates breakdown - photodissociation
    CF₂Cl₂ —-> (UV) CF₂Cl• + •Cl
  • The Cl• formed is a very reactive intermediate which can react with an ozone molecule, breaking it down into oxygen
    P1: Cl• + O₃ —-> ClO• + O₂
    P2: ClO• + O• —-> Cl• + O₂
  • overall equation: O₃ + O• —-> 2O₂
  • propagation step 2 regenerates a chlorine radical, which can attack and remove another molecule of ozone in step 1. steps repeat in a cycle over and over in a chain reaction.
17
Q

Depletion of ozone layer by other radicals (e.g. NO)

A
  • nitrogen oxide radicals formed naturally during lightning strikes and as a result of aircraft travel in the stratosphere
  • P1: NO• + O₃ —-> NO₂• + O₂
    P2: NO₂• + O• —-> NO• + O₂
  • overall equation: O₃ + O• —-> 2O₂
  • the same overall equation shows the radicals act as a catalyst