Chemical kinetics is the study of how fast chemical reactions happen and what factors speed them up or slow them down.
It does not tell you whether a reaction will happen (that’s thermodynamics – ΔG). It tells you how quickly it happens once it starts.
Kitchen analogy: Thermodynamics tells you that bread will eventually go stale. Kinetics tells you it happens in 3 days on the counter vs. 3 weeks in the freezer.
C3H8(g) + 5O2(g) → 3CO2(g) + 4H2O(g)
Imagine a factory that makes candles.
The recipe: burn 1 batch of wax + 5 batches of oxygen to produce 3 batches of CO2 + 4 batches of water vapor.
If wax burns at 1 batch/min, oxygen is consumed 5× faster.
CO2 forms at 3× the rate, and water at 4×.
Each species moves at a different absolute speed.
But divide each speed by its coefficient and they all agree: 1 batch/min.
The rate expression is the official scorecard.
It converts every species’ individual speed into one agreed-upon reaction rate.
It does not matter which molecule you choose to watch.
→ Q3 applies the same scorecard to a new reaction — watch for the subscript-vs-coefficient trap with FeCl3.
Grading: Each term is worth 2 pts. Deduct for missing negative signs, missing coefficient denominators, or wrong coefficients.
Reaction: 2Fe(s) + 6HCl(aq) → 2FeCl3(aq) + 3H2(g)
The AnalogyPicture a sushi conveyor belt with a fixed rule: for every 2 salmon rolls eaten, 6 miso soups are sipped, 2 soy sauce packets are used, and 3 napkins are taken. Your eating speed and sipping speed look completely different — but divide each by its “per-roll” number (coefficient) and every measurement points to the same overall rate of dining.
Iron and HCl do the same thing: they disappear and appear at different absolute speeds, but the coefficients are the conversion factors that normalize everything to a single reaction rate.
Reaction: NO2(g) + O3(g) → NO3(g) + O2(g)
The AnalogyYou want to know what makes your car go faster: fuel quality or tire pressure?
You can’t test both at once — that makes it impossible to isolate which change helped.
So you run one test changing only the fuel.
Then another changing only the tires.
The method of initial rates works exactly the same way.
Hold one reactant constant.
Change the other.
See how the rate responds.
That response tells you the order.
• Double [X] → rate doubles → 1st order in X
• Double [X] → rate quadruples → 2nd order in X
• Double [X] → rate unchanged → 0th order in X
→ Q5 uses the same method — but watch what happens when doubling [NO] quadruples the rate. That second pattern is where the 2nd-order twist reveals itself.
| Rate law | An equation that shows how the rate depends on concentration: Rate = k[A]a[B]b. The exponents (a, b) must be found experimentally – they are NOT the stoichiometric coefficients! |
| Order | The exponent for a specific reactant. “First order in NO2” means the rate is directly proportional to [NO2]. “Second order” means proportional to [NO2]2. |
| Overall order | The sum of all individual orders. If a=1 and b=1, overall order = 2. |
| k (rate constant) | A number specific to this reaction at a specific temperature. Bigger k = faster reaction. Its UNITS depend on the overall order. |
| Initial rate | The rate measured at the very START of the reaction, before products build up and complicate things. |
| M·s−1 | Molarity per second – the standard unit for reaction rate. |
| Experiment | [NO2] (M) | [O3] (M) | Initial Rate (M·s−1) |
|---|---|---|---|
| 1 | 5.0 × 10−5 | 1.0 × 10−5 | 0.022 |
| 2 | 5.0 × 10−5 | 2.0 × 10−5 | 0.044 |
| 3 | 2.5 × 10−5 | 2.0 × 10−5 | 0.022 |
The core formula to keep in mind:
Step 1 — Pick the right pair of experiments.
We need two experiments where only [NO2] changes and [O3] stays constant.
That’s Experiments 2 and 3 — both have [O3] = 2.0 × 10−5 M.
Step 2 — Calculate the rate multiplier.
The rate doubled — a multiplier of 2.
Step 3 — Calculate the concentration multiplier.
The concentration also doubled — a multiplier of 2.
Step 4 — Plug into the formula and solve.
What power do you raise 2 to in order to get 2?
The answer is 1, because 21 = 2.
Step 1 — Pick the right pair of experiments.
We need two experiments where only [O3] changes and [NO2] stays constant.
That’s Experiments 1 and 2 — both have [NO2] = 5.0 × 10−5 M.
Step 2 — Calculate the rate multiplier.
The rate doubled — a multiplier of 2.
Step 3 — Calculate the concentration multiplier.
The concentration doubled — a multiplier of 2.
Step 4 — Plug into the formula and solve.
The concentration doubled and the rate also doubled.
What power do you raise 2 to in order to get 2?
The answer is 1, because 21 = 2.
Rearrange: k = Rate / ([NO2]a[O3]b) = Rate / ([NO2][O3])
✓ Verified: k = 4.4 × 107 for all three experiments (consistent k confirms the rate law is correct)
| If conc ratio is: | And rate ratio is: | Then order = |
|---|---|---|
| 2× | 1× (no change) | 0 |
| 2× | 2× | 1 |
| 2× | 4× | 2 |
| 2× | 8× | 3 |
| 3× | 9× | 2 |
| 3× | 27× | 3 |
If the ratio isn’t clean, use: order = ln(rate ratio) / ln(conc ratio)
Reaction: 2NO(g) + Cl2(g) → 2NOCl(g)
The AnalogyThink of a car crash.
The chance of a crash depends on how many cars are on the road.
Double the cars, and you roughly quadruple the crash risk.
Every pair of cars is a potential collision — that’s what makes it 2nd order.
In this reaction, two NO molecules must collide simultaneously.
So the rate is 2nd order in NO.
Cl2 only needs to show up once — that makes it 1st order.
Pack more NO in, and the rate doesn’t just double — it quadruples.
| Exp | [NO] (M) | [Cl2] (M) | Initial Rate (M·s−1) |
|---|---|---|---|
| 1 | 0.10 | 0.10 | 2.53 × 10−6 |
| 2 | 0.10 | 0.20 | 5.06 × 10−6 |
| 3 | 0.20 | 0.10 | 10.1 × 10−6 |
| 4 | 0.30 | 0.10 | 22.8 × 10−6 |
The core formula to keep in mind:
Step 1 — Pick the right pair of experiments.
We need two experiments where only [NO] changes and [Cl2] stays constant.
That’s Experiments 1 and 3 — both have [Cl2] = 0.10 M.
Step 2 — Calculate the rate multiplier.
The rate quadrupled — a multiplier of 4.
Step 3 — Calculate the concentration multiplier.
The concentration doubled — a multiplier of 2.
Step 4 — Plug into the formula and solve.
The concentration doubled, but the rate quadrupled — not just doubled.
As a comparison: if the rate had only doubled, the order would be 1 (because 21 = 2).
But since the rate quadrupled, the order must be 2 (because 22 = 4).
Step 1 — Pick the right pair of experiments.
We need two experiments where only [Cl2] changes and [NO] stays constant.
That’s Experiments 1 and 2 — both have [NO] = 0.10 M.
Step 2 — Calculate the rate multiplier.
The rate doubled — a multiplier of 2.
Step 3 — Calculate the concentration multiplier.
The concentration doubled — a multiplier of 2.
Step 4 — Plug into the formula and solve.
What power do you raise 2 to in order to get 2?
The answer is 1, because 21 = 2.
✓ Verified: k = 2.53 × 10−3 for all four experiments
Start with: Rate = k × [stuff]. The units must balance.
| This problem: | M/s = k × M2 × M = k × M3 |
| Solve for k: | k = (M/s) / M3 = M−2·s−1 |
Shortcut: For overall order n: k units = M(1−n)·s−1. Here n=3: M(1−3) = M−2s−1 ✓
Zero order = an IV drip in a hospital. The drug enters your bloodstream at a constant rate — the amount already in your system doesn’t matter. Concentration plays zero role in the speed.
First order = a leaky bucket. The more water inside, the faster it drips out. But every hour it loses the same fraction of what’s left — that’s why radioactive half-lives are constant. Today you lose half. Next period you lose half of that half.
Second order = two strangers trying to find each other at a marathon finish line. When thousands of runners are present, bumping into each other is easy. As the crowd thins, finding your friend gets dramatically harder — rate drops off much faster than first order.
→ Q7 puts you in the detective seat: real N2O5 data, three columns to compute, and one plot that tells the truth.
| Integrated rate law | An equation linking concentration to time directly. Instead of “rate = ...”, it says “[A] at time t = ...”. Useful for predicting how much is left after a certain time. |
| [A]t | Concentration of A at time t (the moment you’re interested in) |
| [A]0 | Concentration of A at time 0 (the starting concentration) |
| ln | Natural logarithm (base e = 2.718...). On your calculator: the “ln” button. NOT log (which is base 10). |
| Linear plot | When data falls on a straight line. We try three different y-axes ([A], ln[A], 1/[A]) to see which gives a straight line. |
| Slope | The steepness of the line (rise/run = Δy/Δx). For kinetics, the slope equals k or −k. |
| Order | Integrated Rate Law | Linear Plot (y vs. x) | Slope = | Units of k |
|---|---|---|---|---|
| Zero | [A]t = −kt + [A]0 | [A] vs. t | −k | M·s−1 |
| First | ln[A]t = −kt + ln[A]0 | ln[A] vs. t | −k | s−1 |
| Second | 1/[A]t = kt + 1/[A]0 | 1/[A] vs. t | +k | M−1·s−1 |
Only ONE of these three will be linear. That’s how you identify the order. Then the slope gives you k.
Reaction: 2N2O5 → 4NO2 + O2
The AnalogyYou’re a detective with three suspects: zero order, first order, second order. Each has a telltale signature. Run three “forensic tests” on your data:
• Plot [N2O5] vs. time → straight line? Zero order caught.
• Plot ln[N2O5] vs. time → straight line? First order caught.
• Plot 1/[N2O5] vs. time → straight line? Second order caught.
Only ONE of the three will give a truly straight line. That’s your suspect — and the slope of that line hands you k on a silver platter.
| ln[N2O5] | Press the ln button on your calculator, then enter the concentration. Example: ln(5.00) = 1.6094. For values less than 1, ln gives a negative number: ln(0.61) = −0.4943. That’s OK! |
| 1/[N2O5] | Just divide 1 by the concentration. Example: 1/5.00 = 0.200. As concentration gets smaller, 1/[A] gets larger. |
| “Linear” | The differences between consecutive values are approximately constant. If Δ(ln[A]) per 500s is always ~−0.35, that’s linear. |
| Time (s) | [N2O5] (M) | ln[N2O5] | 1/[N2O5] (M−1) |
|---|---|---|---|
| 0 | 5.00 | 1.6094 | 0.2000 |
| 500 | 3.52 | 1.2585 | 0.2841 |
| 1000 | 2.48 | 0.9083 | 0.4032 |
| 1500 | 1.75 | 0.5596 | 0.5714 |
| 2000 | 1.23 | 0.2070 | 0.8130 |
| 2500 | 0.87 | −0.1393 | 1.1494 |
| 3000 | 0.61 | −0.4943 | 1.6393 |
How to tell: Check if the change between consecutive values is constant:
| Interval | Δ(ln[N2O5]) | Δ(1/[N2O5]) |
|---|---|---|
| 0 → 500 | −0.351 | 0.084 |
| 500 → 1000 | −0.350 | 0.119 |
| 1000 → 1500 | −0.349 | 0.168 |
| 1500 → 2000 | −0.353 | 0.242 |
| 2000 → 2500 | −0.346 | 0.336 |
| 2500 → 3000 | −0.355 | 0.490 |
| Verdict | CONSTANT (~−0.35) ✓ | NOT constant (grows 6×) ✗ |
For first order: slope of ln[A] vs t = −k
Since slope = −k: k = −(−7.01 × 10−4) = 7.01 × 10−4
Linear regression R² = 0.999996 – essentially a perfect straight line.
Imagine a bouncer at a club who only lets in people who are “energetic enough.” That minimum energy requirement is Ea. At room temperature, most molecules are tired and subdued — few make the cut, reaction is slow. Raise the temperature and suddenly everyone is hyped up and bouncing — more molecules clear the threshold, reaction is fast.
A is how many people show up to the door per second (collision frequency × proper orientation). e−Ea/RT is the fraction the bouncer actually lets in. Even a 10°C rise can double or triple that fraction — which is why warm reactions go so much faster.
→ Q9 takes this further: the Arrhenius plot tells you exactly how high the bouncer’s energy threshold is — in kJ/mol.
| Variable | Name | What It Means (Simply) | Units |
|---|---|---|---|
| k | Rate constant | How fast the reaction goes at this temperature. Bigger k = faster reaction. | Depends on order |
| A | Pre-exponential (frequency) factor | How often molecules collide with the RIGHT orientation. Think of it as the “maximum possible k” if every collision worked. | Same as k |
| Ea | Activation energy | The energy “hill” molecules must clear. Higher Ea = harder to start = slower reaction. | J/mol or kJ/mol |
| R | Gas constant | A universal conversion factor between energy and temperature. | 8.314 J/(mol·K) |
| T | Temperature | MUST be in Kelvin. K = °C + 273.15. Never use Celsius in this equation. | K (Kelvin) |
Take the natural log of both sides of k = Ae−Ea/RT:
This has the form y = mx + b:
| Equation part | Corresponds to | What you do |
|---|---|---|
| y | ln(k) | Plot this on the y-axis |
| x | 1/T | Plot this on the x-axis (T in Kelvin!) |
| m (slope) | −Ea/R | Measure from the line; multiply by −R to get Ea |
| b (y-intercept) | ln(A) | Read from the graph; take eb to get A |
Given: slope of Arrhenius plot (ln k vs. 1/T) = −15,200 K
Formula: slope = −Ea / R, where R = 8.314 J/(mol·K)
The AnalogyThe Arrhenius plot is like a ski slope profile: the steeper the run, the higher the mountain. A steep negative slope means a large Ea — temperature has a huge effect on how fast the reaction goes. A gentle slope means a small Ea — the reaction proceeds at roughly the same speed no matter the temperature.
Reading the slope and multiplying by −R gives you the height of the energy mountain in joules per mole. That’s all this problem is asking you to do.
→ Q10 removes the graph entirely: just two temperature measurements, and you can still calculate the height of that same hill.
The slope has units of Kelvin. Here’s why: slope = Δy / Δx = Δ(ln k) / Δ(1/T). ln k is unitless. 1/T has units of K−1. So slope = unitless / K−1 = K.
When you multiply slope (K) × R (J·mol−1·K−1), the K cancels and you get J/mol. That’s your Ea.
Start with: slope = −Ea / R
Rearrange: Ea = −slope × R
Plug in: Ea = −(−15,200 K) × 8.314 J/(mol·K) = 15,200 × 8.314
Calculate: Ea = 126,373 J/mol
Convert J → kJ: 126,373 ÷ 1000 = 126.4 kJ/mol
The units of k are like a reaction’s ID card. Just as a job title instantly tells you what someone does (s−1 = “first-order reaction,” M−1s−1 = “second-order reaction”), the units reveal the order without running a single experiment.
And the two-point Arrhenius is chemistry’s version of: “if bread goes stale in 3 days at 20°C but only 6 hours at 37°C, how high is the energy hill?” Two temperature measurements are all you need to calculate Ea — no graph required.
← Full circle from Q1: that bread on the counter is back — now you’re not just observing the rate difference, you’re calculating the activation energy responsible for it.
| Temperature | k |
|---|---|
| 300 K | 1.5 × 10−3 s−1 |
| 350 K | 4.2 × 10−2 s−1 |
When you only have TWO temperatures (not enough to make a full graph), you use the two-point form. It’s derived by writing the Arrhenius equation at both temperatures and subtracting:
| k1, T1 | Rate constant and temperature at the FIRST condition |
| k2, T2 | Rate constant and temperature at the SECOND condition |
| ln(k2/k1) | Natural log of the ratio of rate constants. If k got bigger, this is positive. |
For an nth-order reaction, the units of k follow the pattern:
| Order (n) | k units | Reasoning | Match? |
|---|---|---|---|
| 0 | M·s−1 | M(1−0) = M1 | |
| 1 | s−1 | M(1−1) = M0 = 1 | ✓ Match! |
| 2 | M−1·s−1 | M(1−2) = M−1 | |
| 3 | M−2·s−1 | M(1−3) = M−2 |
Assign values:
T1 = 300 K, k1 = 1.5 × 10−3 s−1
T2 = 350 K, k2 = 4.2 × 10−2 s−1
Tip: It doesn’t matter which you call “1” and “2” as long as you’re consistent.
Left side – the rate constant ratio:
k2 / k1 = (4.2 × 10−2) / (1.5 × 10−3) = 28.0
ln(28.0) = 3.332
Right side – the temperature term:
1/T2 = 1/350 = 0.002857 K−1
1/T1 = 1/300 = 0.003333 K−1
1/T2 − 1/T1 = 0.002857 − 0.003333 = −4.762 × 10−4 K−1
Plug into the equation and solve:
3.332 = −(Ea / 8.314) × (−4.762 × 10−4)
3.332 = Ea × (4.762 × 10−4) / 8.314
Ea = (3.332 × 8.314) / (4.762 × 10−4)
Ea = 27.71 / 4.762 × 10−4 = 58,178 J/mol
Convert to kJ: 58,178 ÷ 1000 = 58.2 kJ/mol
All numerical answers computationally verified • CHM 152 Workshop 2 • Chemical Kinetics