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Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter Atkins • Julio de Paula

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Page 1: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Atkins’ Physical ChemistryEighth Edition

Chapter 22 – Lecture 3

The Rates of Chemical Reactions

Copyright © 2006 by Peter Atkins and Julio de Paula

Peter Atkins • Julio de Paula

Page 2: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Rate Law: An experimentally determined law of nature

Mechanism: A theory of the sequence of events that may be occurring at the molecular level

The mechanism must agree with the rate law!!

Page 3: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Example of a mechanism once believed to be correct

H2 (g) + I2 (g) ⇌ 2 HI (g)

Rate law proposed in 1894:

ratef = kf [H2] [I2]

rater = kr [HI]2

Mechanism: Step (1) H2 + I2 ⇌ H2I2

Step (2) H2I2 → 2 HI

Rate law proposed in 1967:

]I[]HI['k

1

]I][H[krate

2

222

1

appears to be a simplebimolecular mechanism

Page 4: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Reaction Mechanisms

The overall progress of a chemical reaction can be represented at the molecular level by a series of simple elementary steps or elementary reactions

The sequence of elementary steps that leads to product formation is the reaction mechanism.

2NO (g) + O2 (g) 2NO2 (g)

N2O2 is detected during the reaction!

Elementary step: NO + NO N2O2

Elementary step: N2O2 + O2 2NO2

Overall reaction: 2NO + O2 2NO2

+

Page 5: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Elementary step: NO + NO N2O2

Elementary step: N2O2 + O2 2NO2

Overall reaction: 2NO + O2 2NO2

+

Intermediates - species that appear in a reaction mechanism but not in the overall balanced equation

An intermediate is always formed in an early elementary step and consumed in a later elementary step.

Molecularity of a reaction - the number of molecules reacting in an elementary step.

• Unimolecular reaction – elementary step with 1 molecule

• Bimolecular reaction – elementary step with 2 molecules

• Termolecular reaction – elementary step with 3 molecules

Page 6: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Unimolecular reaction A products rate = k [A]

Bimolecular reaction A + B products rate = k [A][B]

Bimolecular reaction A + A products rate = k [A]2

Rate Laws and Elementary Steps

Writing plausible reaction mechanisms:

• The sum of the elementary steps must give the overall balanced equation for the reaction.

• The rate-determining step should predict the same rate law that is determined experimentally.

Rate-determining step - the slowest step in the sequence of steps leading to product formation.

Page 7: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.16 Diagrams of possible reaction schemes

Page 8: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.17 Reaction profile when 1st step is RDS

Page 9: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

The experimental rate law for the reaction between NO2 and CO to produce NO and CO2 is rate = k[NO2]2. The reaction is believed to occur via two steps:

Step 1: NO2 + NO2 NO + NO3

Step 2: NO3 + CO NO2 + CO2

What is the equation for the overall reaction?

NO2+ CO NO + CO2

What is the intermediate?

NO3

What can you say about the relative rates of steps 1 and 2?

rate = k[NO2]2 is the rate law for step 1 so step 1 must be slower than step 2

Page 10: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.8 Approach of concentrations to their equilibrium values

For the reaction: A ⇌ B

• In practice, most kineticstudies are on reactionsfar from equilibrium

• ∴ Reverse reactionsare unimportant

Page 11: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.13 Concentrations of A, I and P with time

A → I → P

Consumption of A is ordinary1st-order decay:

tko

ae]A[]A[

Note that the concentration of Irises to a maximumthen falls to zero...

Page 12: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.14 Basis of steady-state approximation

[I] remains negligibly small

A → I → P

Assumption:

0dt

]I[d

Page 13: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.15 Comparison of the exact result for the concentrations

of a reaction and concentrations from steady-state approximation

Page 14: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

How do we postulate a plausible mechanism?

• Common approach is to use the kinetic isotope effect

• Process facilitates identification of bond-breaking events

• Decrease in reaction rate is observed when an atom isreplaced with a heavier isotope

• Primary kinetic isotope effect – the RDS requires scissionof a bond involving that isotope

• Secondary kinetic isotope effect – bond scission occursin a bond NOT involving that isotope

Page 15: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

How do we postulate a plausible mechanism?

• Effect arises from change in activation energy when atomis replaced with a heavier isotope

• Change is in zero-point vibrational energy of bond

νh)v(E 21

vib

Page 16: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.18 Changes in reaction profile when a C−H

bond is replaced with C−D

Page 17: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.19 Protons can tunnel through the activation barrier

• Effective barrierheight is reduced

• Important only atlow temperatureswhen most of thereactant moleculesare left of the barrier

• More important inelectron transferreactions even at roomtemperature

Page 18: Atkins’ Physical Chemistry Eighth Edition Chapter 22 – Lecture 3 The Rates of Chemical Reactions Copyright © 2006 by Peter Atkins and Julio de Paula Peter

Fig. 22.20 Difference in zero-point vibrational energies to describe the secondary kinetic isotope effect

λe)H(k

)D(k

where λ is anexperimentallydetermined parameter

• If λ > 1 then the deuteratedform reacts more slowly

• If λ < 1 then the undeuteratedform reacts more slowly