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Lesson 8 of 10

Chemical Kinetics · Lesson 8 of 10

Arrhenius Calculations and Experimental Data

“Derive logarithmic and two-temperature Arrhenius relationships, extract parameters from data and make conditional kinetic predictions.”

Learning Objectives

• Derive the natural-log and base-10 Arrhenius forms. • Use two rate constants to determine activation energy and the prefactor. • Fit an Arrhenius line using all measured data and interpret scatter. • Combine conversion-time or half-life observations with temperature dependence.

Turn an exponential dependence into a straight line

The Arrhenius equation contains a product Aexp(−E_a/RT). Taking natural logarithms turns that product into a sum: ln k=ln A−E_a/(RT). For a fixed unit chosen for k, this is a straight-line relationship between the logarithm of its numerical value and reciprocal absolute temperature. The intercept gives the prefactor in the same rate-constant unit.

Natural-log and decimal-log formsLaTeX
Strictly, logarithms refer to k/kref and A/kref with a fixed rate-constant reference unit. For the ln plot against 1/T, slope=−E_a/R; for log₁₀, slope=−E_a/[(ln10)R].

A negative slope means a positive activation energy: moving to the right increases 1/T, which means lowering temperature, so k becomes smaller. The reciprocal-temperature axis reverses the intuitive direction of warming. If the horizontal axis is scaled as 1000/T, the slope becomes −E_a/(1000R), so the scale factor must be restored before calculating E_a.

Eliminate A between two temperatures

Write ln k₁=ln A−E_a/(RT₁) and ln k₂=ln A−E_a/(RT₂). Subtract the first from the second. If A and E_a can be treated as constant over the interval, ln A cancels. Combine the logarithms into ln(k₂/k₁) and collect reciprocal temperatures. Both rate constants must use the same units and the same definition of measured rate.

Two-temperature relationshipLaTeX
For T₂>T₁ and positive E_a, both sides are positive because k₂>k₁. Use ln10 in the denominator if the logarithm is converted to base ten.
Solve for the unknown parameterLaTeX
A has the same units as k₁. If R uses joules, the calculated E_a is J mol⁻¹ and can then be divided by 1000 for kJ mol⁻¹.
Two rate constants determine E_a and A

Problem
A first-order process has k₁=0.0200 s⁻¹ at 500 K and k₂=0.0700 s⁻¹ at 700 K. Determine E_a and A.

  1. 1.Ratio k₂/k₁=3.5 and reciprocal-temperature difference=1/500−1/700. Substitution gives E_a=18227.1 J mol⁻¹≈18.23 kJ mol⁻¹.
  2. 2.A=0.0200exp[E_a/(8.314×500)]=1.60424 s⁻¹.
  3. 3.Check at 700 K: Aexp[−E_a/(8.314×700)] reproduces 0.0700 s⁻¹. This tests both the sign and the units.
  4. 4.The numerical value of A does not become a concentration or an energy; its inverse-time unit follows from the first-order k used here.
Predict an ethyl iodide rate constant

Problem
For C₂H₅I(g)→C₂H₄(g)+HI(g), k₁=1.60×10⁻⁵ s⁻¹ at 600 K and E_a=209 kJ mol⁻¹. Predict k₂ at 700 K.

  1. 1.Convert the barrier to 209000 J mol⁻¹. Then ln(k₂/k₁)=(209000/8.314)(1/600−1/700).
  2. 2.Exponentiating gives k₂=1.60×10⁻⁵×exp[(209000/8.314)(1/600−1/700)]=0.00636076 s⁻¹.
  3. 3.The result exceeds k₁ because the temperature is higher and the activation energy positive. Using Celsius or reversing the temperature difference would give an unphysical result for this model.
Infer a barrier from doubling over 10 K

Problem
If k doubles from 298 K to 308 K, estimate E_a in the constant-parameter Arrhenius model.

  1. 1.Use the ratio 2 and the actual temperature pair: E_a=8.314ln2/(1/298−1/308)=52893.5 J mol⁻¹≈52.89 kJ mol⁻¹.
  2. 2.The result is specific to the temperature interval. A doubling over a different interval can imply a different barrier.
  3. 3.No concentration values are required because the observation concerns rate constants, rather than a rate change caused by composition.

Use all the data when a graph is requested

Temperature / °CTemperature / KMeasured k / s⁻¹
0273.157.87×10⁻⁷
20293.151.70×10⁻⁵
40313.152.57×10⁻⁴
60333.151.78×10⁻³
80353.152.140×10⁻²
Arrhenius fit to a five-temperature dataset

Problem
Fit ln k against 1/T for the table and predict k at 30 °C and 50 °C.

  1. 1.Convert every Celsius temperature to kelvin and use all five measured rate constants. Fit a straight line by minimising the sum of squared vertical logarithmic residuals; do not assume that rounded experimental points lie exactly on one line.
  2. 2.The fitted line is ln(k/[1 s⁻¹])≈30.3124−12115.2 K/T. Thus E_a=100.726 kJ mol⁻¹ and A=1.46046e+13 s⁻¹.
  3. 3.At 30 °C=303.15 K, fitted k≈6.42972e-05 s⁻¹. At 50 °C=323.15 K, fitted k≈0.000762758 s⁻¹.
  4. 4.The points show scatter around the line, especially the 60 °C datum. These are model-based predictions from the chosen all-point fit, not exact values implied independently by every pair of measurements.
  5. 5.Using only two endpoints or rounding temperatures to integer kelvin yields somewhat different parameter estimates. State the method so the result is reproducible.

Conversion-time comparisons can reveal a rate-constant ratio

For a first-order process, time to leave fraction f is t=ln(1/f)/k. If two different conversion fractions are reached in equal times at two temperatures, equating those expressions determines k₂/k₁. The remaining fractions, rather than percentages consumed, go inside the logarithms. That ratio can then enter the two-temperature Arrhenius equation.

Equal times for different conversion percentages

Problem
The time for 10% consumption at 298 K equals the time for 25% consumption at 308 K. If A=4.0×10¹⁰ s⁻¹, estimate E_a and k at 318 K.

  1. 1.The remaining fractions are 0.90 and 0.75. Equal times give ln(1/0.90)/k₂₉₈=ln(1/0.75)/k₃₀₈. Therefore k₃₀₈/k₂₉₈=ln(1/0.75)/ln(1/0.90).
  2. 2.Insert that ratio into the two-temperature equation: E_a=76.6502 kJ mol⁻¹.
  3. 3.At 318 K, k=Aexp[−E_a/(8.314×318)]=0.0102579 s⁻¹.
  4. 4.This combines a fractional-decay observation with a temperature model; using 0.10 and 0.25 as remaining fractions would reverse the meaning of the data.
A fitted line has conditions and uncertainty

The intercept is an extrapolation to 1/T=0, not a direct measurement at an experimentally attainable infinite temperature. Parameters can be correlated and sensitive to scatter. A useful line supports Arrhenius behaviour over the studied range, rather than guaranteeing it through a phase or mechanism change.

Reciprocal-temperature plotting exposes experimental scatterReciprocal-temperature plotting exposes experimental scatterln(k/[1 s⁻¹])1000 / T, with T in K2.83.03.23.43.6-14-12-10-8-6-4All-point fit: E_a≈100.73 kJ mol⁻¹; A≈1.4605×10¹³ s⁻¹.
Arrhenius line fitted to the five-temperature dataset— The horizontal scale is1000/T, so its fitted slope is −E_a/(1000R). Dots are supplied measurements.

Quick Quiz

Quiz

Quick check

On an ln k versus 1/T plot, what is the slope?

Explanation: Taking natural logarithms of Arrhenius gives slope −E_a/R against unscaled reciprocal temperature.

Quick check

What must be held approximately common to eliminate A in the two-temperature equation?

Explanation: Subtracting cancels the same prefactor only when the constant-parameter approximation is adequate.

Quick check

If k₂>k₁ for T₂>T₁, the calculated E_a in the simple model should be:

Explanation: Both ln(k₂/k₁) and 1/T₁−1/T₂ are positive, so their ratio gives positive E_a.

Quick check

The prefactor A has which units?

Explanation: The exponential is dimensionless, leaving A with the unit of k.

Quick check

Equal times for 10% and 25% consumption at different temperatures require which quantities inside first-order logarithms?

Explanation: The integrated decay law uses initial amount divided by remaining amount.

Practice Problems

Practice Problems
  1. A hydrocarbon decomposition has k=2.418×10⁻⁵ s⁻¹ at 546 K and E_a=179.9 kJ mol⁻¹. Find A.
  2. A law is written k=(4.5×10¹¹ s⁻¹)exp(−28000 K/T). Find E_a.
  3. The numerical first-order constant in s⁻¹ obeys log₁₀(k/[1 s⁻¹])=14.34−1.25×10⁴ K/T. Find E_a and the temperature for a 256 min half-life.
  4. A process has k₁=4.5×10³ s⁻¹ at 10 °C and E_a=60 kJ mol⁻¹. Find the temperature for k₂=1.5×10⁴ s⁻¹.
  5. The rate quadruples from 293 to 313 K at unchanged composition and under one rate law. Estimate E_a.
  6. For the five-temperature dataset, why can different pairs give different E_a values, and what should be reported with an all-point fit?
  7. A decimal-log plot against 1000/T has slope −5.00. Calculate E_a with R=8.314.

Rearrange k=Aexp(−E_a/RT) to A=kexp(E_a/RT). Convert E_a to 179900 J mol⁻¹, giving A=2.418×10⁻⁵exp[179900/(8.314×546)]=3.93298e+12 s⁻¹. The positive sign in the rearranged exponent is essential. Substituting this prefactor back into the original negative-exponent expression must reproduce the measured rate constant.

Key Takeaways

Key Takeaways

• Taking logarithms turns the simple Arrhenius equation into a straight-line relation. • Natural- and decimal-log plots have slopes differing by ln10. • Check whether reciprocal temperature is plotted as 1/T or 1000/T. • The two-temperature equation removes A only under an adequate constant-parameter model. • Use kelvin, matching energy units and the same definition and units of k. • All-point fitting uses the complete dataset but still requires examining scatter. • Conversion-time and half-life information can supply k values or their ratios. • Predictions should be labelled with the fitted model and its experimental range.