The rate constant for the decomposition of at various temperatures is given below:
| T/°C | 0 | 20 | 40 | 60 | 80 |
|---|---|---|---|---|---|
| / | 0.0787 | 1.70 | 25.7 | 178 | 2140 |
Draw a graph between and and calculate the values of and . Predict the rate constant at 30° and 50°C.
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Start your 14-day free trial to unlock the full solution →Using the Arrhenius equation , we plot vs to get a straight line. From its slope () and intercept (), we find and . Then we predict and .
The Arrhenius equation is the backbone of temperature-dependent kinetics. It tells us that the rate constant depends exponentially on temperature:
Taking natural logs gives a linear form:
This is of the form , where , , slope , and intercept . So if we plot against , we get a straight line — and from its slope and intercept we can extract both and .
Temperature must be in kelvin when using in the Arrhenius plot. A common mistake is to use Celsius directly — that gives a completely wrong slope.
Let’s work through it step by step.
1. Convert temperatures to kelvin and compute and
| (°C) | (K) | (K) | (s) | |
|---|---|---|---|---|
| 0 | 273.15 | |||
| 20 | 293.15 | |||
| 40 | 313.15 | |||
| 60 | 333.15 | |||
| 80 | 353.15 |
Notice that values are given as , so we divide by to get actual in s.
2. Plot vs
On a graph, the points fall beautifully on a straight line. The slope is negative (since increases with , increases as decreases). We can calculate the slope using any two well-separated points, but for accuracy, use the first and last:
Using the two extreme points gives a quick estimate. For exam problems, this is usually sufficient — but if you have time, a least-squares fit (or averaging slopes from multiple pairs) gives a more reliable result.
3. Calculate from the slope
Since slope , we have:
4. Calculate from the intercept
The intercept . From the graph, the line crosses the axis at (theoretical). Using the point-slope form with any data point, say at C:
So:
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