11.7 - Exponential Decay Equations
- 1The equation linking undecayed nuclei, original nuclei, decay constant, and time
- 2Calculating remaining activity using initial activity, decay constant, and time
- 3Using radioactive carbon-14 for archaeological dating
Mathematical model for radioactive decay
The relationship between the number of undecayed radioactive nuclei (N) remaining from an original number (N0) can be determined by:
Where:
- N = number of nuclei remaining
- N0 = initial number of nuclei
- = decay constant (s-1)
- t = time (s)
As the nuclei decay over time, their activity (A) also changes. The activity at any given time t is:
Where:
- A = activity at time t (Bq)
- A0 = initial activity at t = 0 (Bq)
Worked example - Calculating the number of remaining nuclei
Calculate the number of undecayed nuclei remaining after 10,000 years given the initial number of nuclei is 1.0 x 106 and the decay constant for the substance is 1.209 x 10-4 per year.
Step 1: Formula
Step 2: Substitution and correct evaluation
Radioactive dating using carbon-14
The radioactive isotope carbon-14 is extensively used in archaeological dating because:
- Living organisms absorb carbon-14 from the atmosphere.
- Upon death, the decay of carbon-14 in the organisms begins.
- The comparison of the remaining carbon-14 enables the dating of archaeological samples.
Key Points:
- Carbon-14 has a half-life of approximately 5,730 years.
- The measurement of the carbon-14 percentage facilitates the calculation of the sample's age.
- This method is applicable to materials that were once living, such as wood or bone.
Worked example - Calculating the age of an archaeological artefact
Estimate the age of an archaeological sample if the initial activity of carbon-14 was 0.25 Bq and has now decayed to 0.1 Bq, with the decay constant for carbon-14 being 1.21 x 10-4 per year.
Step 1: Formula
Step 2: Rearranged formula
Step 3: Substitution and correct evaluation