Interpret experimental data (tables, graphs, calculations) from rate‑of‑reaction investigations and explain how the five key factors affect the rate of a chemical reaction.
The rate of a chemical reaction is the change in amount (or concentration) of a reactant or product per unit time.
Rate = \(\displaystyle\frac{\Delta[\text{A}]}{\Delta t}\) or \(\displaystyle\frac{\Delta V}{\Delta t}\) or \(\displaystyle\frac{\Delta m}{\Delta t}\)
Raising the temperature gives particles more kinetic energy, so a larger proportion can overcome \(E_a\); this explains the temperature effect on the rate.
| Factor | Effect on rate (with example) |
|---|---|
| Concentration (or pressure) of reactants |
More particles per unit volume → more collisions per second. Example: Doubling the concentration of \(\ce{HCl}\) in the reaction \(\ce{NaCl + HCl → NaCl + HCl}\) roughly doubles the rate. For gases, increasing pressure has the same effect as increasing concentration because the number of gas‑phase collisions rises. |
| Temperature |
Increases average kinetic energy → larger fraction of molecules possess energy ≥ \(E_a\). Empirical rule: The rate roughly doubles for every 10 °C rise in temperature (for many reactions). Example: The reaction between \(\ce{Mg}\) and \(\ce{HCl}\) proceeds noticeably faster at 50 °C than at 20 °C. |
| Surface area of a solid |
Smaller particles expose more surface → more sites for collisions. Example: Powdered calcium carbonate reacts much faster with \(\ce{HCl}\) than a single chunk of the same mass. |
| Catalyst |
Provides an alternative pathway with a lower activation energy. The catalyst is not consumed; it appears unchanged at the end of the reaction. Example: Manganese(IV) oxide (\(\ce{MnO2}\)) speeds up the decomposition of \(\ce{H2O2}\). |
| Nature of the reactants |
Reactivity depends on bond strength, ionic vs. covalent character, etc. Example: Acids react rapidly with active metals (e.g., \(\ce{Zn}\)), whereas gases such as \(\ce{N2}\) are inert at room temperature because the N≡N bond is very strong. |
| Method | What is measured | Typical set‑up (apparatus) |
|---|---|---|
| Volume of gas collected (e.g., \(\ce{CO2}\), \(\ce{H2}\)) | \(\Delta V\) over time | Gas syringe or measuring cylinder attached to the reaction flask via a delivery tube; stop‑watch; thermometer to record temperature. |
| Loss of mass of a solid | \(\Delta m\) over time | Analytical balance, weighing boat (or crucible), stop‑watch; the solid is weighed before the reaction and at regular intervals. |
| Change in pressure (closed system) | \(\Delta P\) over time | Sealed reaction vessel, pressure sensor or manometer, thermometer; pressure is recorded at set time intervals. |
| Colour change (spectrophotometry) | \(\Delta\) absorbance over time | Colourimeter or spectrophotometer, cuvettes, stop‑watch; the absorbance of the reaction mixture is measured at regular intervals. |
| Titration of a product | Volume of titrant used per time interval | Burette, pipette, suitable indicator, stop‑watch; aliquots are taken at set times and titrated immediately. |
If a measured quantity (volume, mass, pressure, absorbance) varies linearly with time, the gradient \(\displaystyle\frac{\Delta y}{\Delta x}\) is the average rate.
Gradient = \(\frac{y_2-y_1}{x_2-x_1}\) = \(\frac{\Delta\text{quantity}}{\Delta t}\)
For gases collected at room temperature and pressure Cambridge uses the molar volume:
\(24\ \text{dm}^3\ \text{mol}^{-1}\) ≈ \(24\,000\ \text{cm}^3\ \text{mol}^{-1}\)
Thus:
\[ \text{Rate (mol s}^{-1}) = \frac{\Delta V\ (\text{cm}^3)}{\Delta t\ (\text{s})}\times\frac{1\ \text{mol}}{24\,000\ \text{cm}^3} \]| Time (s) | Volume of \(\ce{CO2}\) (cm³) |
|---|---|
| 0 | 0 |
| 10 | 12 |
| 20 | 24 |
| 30 | 36 |
Gradient (ΔV/Δt) = \(\frac{12\ \text{cm}^3}{10\ \text{s}} = 1.2\ \text{cm}^3\text{s}^{-1}\).
Convert to moles s⁻¹:
\[ \text{Rate} = 1.2\ \frac{\text{cm}^3}{\text{s}} \times \frac{1\ \text{mol}}{24\,000\ \text{cm}^3} = 5.0\times10^{-5}\ \text{mol s}^{-1} \]If the reaction occurs in 0.500 L of solution, the change in concentration per second is:
\[ \Delta[\ce{CO2}] = \frac{5.0\times10^{-5}\ \text{mol s}^{-1}}{0.500\ \text{L}} = 1.0\times10^{-4}\ \text{mol L}^{-1}\text{s}^{-1} \]Data (mass of Mg remaining):
| Time (s) | Mass of Mg remaining (g) |
|---|---|
| 0 | 0.500 |
| 20 | 0.460 |
| 40 | 0.420 |
| 60 | 0.380 |
| 80 | 0.340 |
Mass of Mg lost in the first 20 s = 0.500 g – 0.460 g = 0.040 g.
Moles of Mg lost:
\[ n_{\ce{Mg}} = \frac{0.040\ \text{g}}{24.3\ \text{g mol}^{-1}} = 1.65\times10^{-3}\ \text{mol} \]Reaction: \(\displaystyle \ce{Mg + 2HCl -> MgCl2 + H2}\)
1 mol Mg produces 1 mol \(\ce{H2}\). Hence moles of \(\ce{H2}\) formed = \(1.65\times10^{-3}\) mol.
Using the molar volume (24 000 cm³ mol⁻¹):
\[ V_{\ce{H2}} = 1.65\times10^{-3}\ \text{mol}\times24\,000\ \text{cm}^3\text{mol}^{-1}=39.6\ \text{cm}^3 \]If the experiment actually collected 35 cm³, the percentage yield is:
\[ \%\,\text{yield}= \frac{35}{39.6}\times100 = 88\% \]Plot the *initial* rate (taken from the first few data points) against a variable such as concentration, pressure or temperature. The shape of the plot reveals the order with respect to that variable:
When experimental points are not perfectly collinear, draw a straight line of best fit through them. State the uncertainty in the gradient (e.g., “\(0.85\pm0.05\ \text{cm}^3\text{s}^{-1}\)”). This satisfies AO3 – evaluating the reliability of the result.
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