Radioactivity Kinetics
Radioactive decay is a spontaneous nuclear process in which an unstable nucleus loses energy by emitting radiation — alpha particles (), beta particles (), or gamma rays (). Unlike ordinary chemical reactions, radioactive decay is entirely unaffected by temperature, pressure, or the chemical state of the element. The driving force is purely nuclear instability: certain combinations of protons and neutrons are energetically unfavorable, and the nucleus rearranges itself to reach a more stable configuration. A profound mathematical feature of radioactive decay is that it follows first-order kinetics — the rate at which nuclei decay at any instant is directly proportional to the number of radioactive nuclei present at that instant. This single fact leads to an exponential decrease in the number of radioactive atoms over time, described by the radioactive decay law . Three interrelated quantities characterise this behavior: the decay constant (), the half-life (), and the mean (average) life (). Understanding radioactivity kinetics has enormous practical consequences. It underlies radiometric dating techniques such as carbon-14 dating (archaeology) and uranium-lead dating (geology), guides the safe handling and disposal of nuclear waste, determines the therapeutic window of radioactive isotopes used in nuclear medicine, and allows physicists to identify unknown isotopes by measuring their characteristic half-lives. This article develops each concept from first principles and connects them through precise mathematical relationships.
- The Rate Equation (First-Order Kinetics)
- Separating Variables and Integrating
- Half-Life ()
- Mean (Average) Life ()
- Activity and the Becquerel
The Rate Equation (First-Order Kinetics)
Let be the number of undecayed radioactive nuclei at time . The fundamental empirical observation is that the rate of decay is proportional to :\n\[-\frac{dN}{dt} = \lambda N\]\nThe negative sign indicates is decreasing. The proportionality constant is the decay constant, unique to each radioactive nuclide, with SI unit s. A large means rapid decay; a small means slow decay. This is exactly analogous to a first-order chemical reaction rate law .
Separating Variables and Integrating
Rearrange the differential equation and integrate both sides:\n\[\frac{dN}{N} = -\lambda\, dt \implies \int_{N_0}^{N} \frac{dN'}{N'} = -\lambda \int_0^t dt'\]\n\[\ln N - \ln N_0 = -\lambda t \implies \ln\frac{N}{N_0} = -\lambda t\]\nExponentiating both sides gives the Radioactive Decay Law:\n\[N(t) = N_0\, e^{-\lambda t}\]\nwhere is the number of radioactive nuclei at . Because mass and activity are both proportional to , the same exponential law applies to mass and activity .
Half-Life ()
The half-life is the time required for exactly half the radioactive nuclei to decay. Set :\n\[\frac{N_0}{2} = N_0 e^{-\lambda t_{1/2}} \implies \frac{1}{2} = e^{-\lambda t_{1/2}}\]\n\[\ln 2 = \lambda t_{1/2} \implies \boxed{t_{1/2} = \frac{\ln 2}{\lambda} = \frac{0.693}{\lambda}}\]\nAfter each successive half-life, the quantity remaining is halved: . After half-lives, . Half-life is the most intuitively accessible measure of decay rate and varies enormously across nuclides — from microseconds (, ) to billions of years (, yr).
Mean (Average) Life ()
The mean life is the statistical average time a single nucleus survives before decaying. Each nucleus that decays at time contributes a lifetime of . The number decaying in interval is . Averaging over all nuclei:\n\[\tau = \frac{1}{N_0}\int_0^{\infty} t\,\lambda N_0 e^{-\lambda t}\,dt = \lambda \int_0^{\infty} t e^{-\lambda t}\,dt = \lambda \cdot \frac{1}{\lambda^2} = \frac{1}{\lambda}\]\nSo , and since :\n\[\tau = \frac{t_{1/2}}{\ln 2} = \frac{t_{1/2}}{0.693} \approx 1.443\, t_{1/2}\]\nThe mean life is always slightly longer than the half-life. At , the number of nuclei remaining is .
Activity and the Becquerel
Activity is the number of disintegrations per second: . The SI unit is the becquerel (Bq), where . An older unit, the curie (Ci), is defined as , originally chosen as the activity of 1 gram of . Since and decreases exponentially, activity also falls as . In nuclear medicine, the activity of a radiopharmaceutical must be carefully scheduled relative to its half-life so the dose reaches the patient at the right moment.
The Key Equation
- N(t) — Number of undecayed nuclei at time t (dimensionless (count)): The remaining number of radioactive nuclei at elapsed time t.
- N_0 — Initial number of nuclei (dimensionless (count)): The number of radioactive nuclei present at t = 0.
- \lambda — Decay constant (s (or yr, min, etc.)): The probability per unit time that a single nucleus will decay; unique to each nuclide.
- t — Time (s (or any consistent time unit)): Elapsed time since t = 0.
- t_{1/2} — Half-life (s (or yr, min, etc.)): The time for half the nuclei to decay; inversely proportional to .
- \tau — Mean (average) life (s (or yr, min, etc.)): The average time a nucleus exists before decaying; equals 1/ and is about 1.443 times the half-life.
Worked Example
Problem. A freshly prepared sample of iodine-131 (), used in thyroid cancer treatment, has an initial activity of Bq. The half-life of is 8.02 days. (a) Calculate the decay constant in s. (b) Find the activity after 24.06 days. (c) Calculate the mean life in days.
Answer. λ = 1.00 × 10⁻⁶ s⁻¹; Activity after 24.06 days = 1.0 × 10⁸ Bq; Mean life τ = 11.57 days
Origins · 1 minMarie Skłodowska Curie and how this was discovered
Marie Curie pioneered the scientific study of radioactivity — a term she coined. Working with her husband Pierre in Paris, she discovered the radioactive elements polonium () and radium () in 1898. She demonstrated that radioactivity is an atomic property, not a molecular or environmental one, providing the conceptual foundation for the decay law. She remains the only person to have won Nobel Prizes in two different sciences: Physics (1903, shared with Pierre Curie and Henri Becquerel) and Chemistry (1911, for the isolation of pure radium). Marie Curie's personal notebooks from the 1890s are still so radioactively contaminated that they are stored in lead-lined boxes in the Bibliothèque nationale de France, and researchers must sign a liability waiver to view them.
Related Concepts
- First-Order Reactions and Half-Life in Chemical Kinetics — Radioactive decay is mathematically identical to a first-order chemical reaction; the same integrated rate law and half-life formula apply, making the analogy a powerful bridge between nuclear and chemical kinetics.
- Alpha, Beta, and Gamma Decay — Understanding what kind of radiation is emitted (α, β, γ) and how nuclear equations are balanced is the qualitative complement to the quantitative decay-rate mathematics studied here.
- Nuclear Binding Energy and Mass Defect — The stability of a nucleus — and hence the value of λ — is determined by its binding energy per nucleon. This concept explains why some nuclides decay rapidly while others are stable for billions of years.
- Radiometric Dating (Carbon-14 and Uranium-Lead) — Radiometric dating is the most important applied use of the radioactive decay law, directly using the equation N(t) = N₀e^(−λt) to calculate the age of archaeological and geological samples.