The half-life (T₁/₂) is the time required for a quantity to reduce to half its initial value. The decay process follows first-order kinetics and is described by the exponential decay law:
N(t) = N₀ · (½)t / T₁/₂ = N₀ · e-λt
where λ = ln(2) / T₁/₂ is the decay constant, N₀ is the initial amount, and N(t) is the remaining amount after time t.
This fundamental equation governs not only nuclear decay but also chemical reaction rates, drug elimination in pharmacokinetics, and even capacitor discharge. By knowing any three parameters, the fourth can be derived analytically.
All calculations use double-precision floating point arithmetic, validated against standard nuclear data tables. The interactive graph plots the full decay curve from t=0 up to a dynamic range (typically 3× half-life or until near-zero). The current time point is highlighted, providing an intuitive visual understanding of the decay process.
Carbon-14 has a half-life of 5,730 ± 40 years (NIST data). By measuring the remaining ¹⁴C in organic artifacts, archaeologists calculate the time since death. This calculator reproduces the standard decay formula used by radiocarbon laboratories (Stuiver & Polach, 1977). For a sample with initial 100% modern carbon, after 5,730 years exactly 50% remains – a cornerstone of Quaternary geochronology.
Iodine-131 (half-life ≈ 8.02 days, IAEA Live Chart of Nuclides) is used to treat hyperthyroidism and thyroid cancer. Medical physicists calculate the activity remaining in the patient’s thyroid to ensure therapeutic dose while minimizing radiation exposure. The calculator helps estimate residual activity, crucial for radiation safety planning (ICRP Publication 107, ICRP).
Following nuclear accidents, Cs-137 (half-life ≈ 30.17 years, NIST Physical Reference Data) is a key contaminant. Environmental scientists use decay calculations to predict long-term soil contamination levels and to assess remediation needs. Our tool reflects the official decay data from IAEA and UNSCEAR reports.
The decay constant λ = ln(2)/T₁/₂ represents the probability of decay per unit time. The mean lifetime τ = 1/λ = T₁/₂ / ln(2) ≈ 1.4427 × T₁/₂ is the average lifespan of a radioactive atom. These parameters are fundamental in reactor physics, dosimetry, and radiometric dating.
| Isotope / Substance | Half-Life | Typical Application | Decay Constant λ (approx) |
|---|---|---|---|
| Carbon-14 (¹⁴C) | 5,730 years | Archaeological dating | 1.209 × 10⁻⁴ yr⁻¹ |
| Iodine-131 (¹³¹I) | 8.02 days | Thyroid therapy | 0.0864 day⁻¹ |
| Uranium-238 (²³⁸U) | 4.468 × 10⁹ years | Geochronology | 1.551 × 10⁻¹⁰ yr⁻¹ |
| Technetium-99m (⁹⁹ᵐTc) | 6.01 hours | Medical imaging | 0.1153 h⁻¹ |
| Radon-222 (²²²Rn) | 3.82 days | Indoor air quality | 0.1814 day⁻¹ |
Data integrity & updates: The tool is reviewed periodically to ensure consistency with authoritative sources. The last verification was performed in March 2026 using NIST and IAEA data releases.