💡 N = remaining amount | N₀ = initial amount | λ = decay constant (per unit time) | t = elapsed time | T½ = half-life
📖 What is Radioactive Decay?
Radioactive decay is the process by which an unstable atomic nucleus loses energy by emitting radiation.
The rate of decay is exponential — meaning the amount of radioactive material decreases by a constant
fraction over equal time intervals. This calculator uses the standard exponential decay equation:
N = N₀ × e−λt
Where:
• N = Remaining amount after time t
• N₀ = Initial amount
• λ (lambda) = Decay constant (per unit time)
• t = Elapsed time
• e = Euler's number (≈ 2.71828)
Example: Carbon-14 Dating (Half-Life = 5730 years)
Given: Half-life T½ = 5730 years | Initial C-14 N₀ = 100% | Remaining N = 25%
Step 1: λ = ln(2) / 5730 = 0.00012097 per year Step 2: t = [ln(100/25)] / 0.00012097 Step 3: t = [1.3863] / 0.00012097 Step 4: t ≈ 11,460 years (two half-lives)
💡 Explanation: If 25% of C-14 remains, the sample has undergone 2 half-lives (100% → 50% → 25%),
which equals 2 × 5730 = 11,460 years.
🎯 Common Half-Life Values
Carbon-14 (¹⁴C): 5,730 years — archaeology / carbon dating
Uranium-238 (²³⁸U): 4.47 billion years — geology / rock dating
Potassium-40 (⁴⁰K): 1.25 billion years — geological dating
Iodine-131 (¹³¹I): 8.02 days — medical imaging
Technetium-99m (⁹⁹ᵐTc): 6.01 hours — medical scans
Fluorine-18 (¹⁸F): 109.7 minutes — PET scans
💡 Real-World Applications
Carbon Dating: Determining the age of archaeological artifacts up to ~50,000 years.
Medical Imaging: Radioisotopes with short half-lives used in PET and SPECT scans.
Nuclear Waste Management: Calculating safe storage times for radioactive materials.
Geological Dating: Determining the age of rocks and Earth's formations.
Radiometric Dating: Using decay chains to date fossils, minerals, and meteorites.
Radiation Safety: Estimating dose decay over time for medical and industrial use.
⚠️ Limitations & Assumptions
📌 Important Notes
Assumes a constant decay constant λ throughout the time period.
Assumes no external source of the radioactive isotope (closed system).
Does not account for radiogenic daughter products that may also decay.
Carbon-14 dating is only reliable up to ~50,000 years.
Results are theoretical estimates — real-world samples may have contamination.
Units of λ and t must match (e.g., both in years, or both in seconds).
📚 Sources & References
Authoritative Sources
NIST — Atomic and Nuclear Physics Data
IAEA — Radioactive Decay and Half-Life Tables
OpenStax — University Physics, Volume 3 (Nuclear Physics)
US EPA — Radioactive Decay Basics
IAEA — Nuclear Data Services (NuDat)
❓ Frequently Asked Questions
What is half-life?
Half-life (T½) is the time required for half of a radioactive substance to decay.
It's a constant for each isotope and is independent of the initial amount or external conditions
(temperature, pressure, chemical state).
What is the difference between decay constant and half-life?
Decay constant (λ) is the probability per unit time that a given nucleus will decay.
Half-life (T½) is the time for half the sample to decay. They are related by:
λ = ln(2) / T½.
How does carbon dating work?
Living organisms continuously absorb carbon-14 (¹⁴C) from the atmosphere. When they die, the ¹⁴C begins to
decay with a half-life of 5,730 years. By measuring the remaining ¹⁴C, scientists can estimate the age
of the sample — up to about 50,000 years.
Why does decay follow an exponential curve?
Because each nucleus has a fixed probability of decaying per unit time, the number of decays per second
is proportional to the current number of nuclei. This leads to an exponential decay equation
N = N₀ × e−λt.
Can I use this for medical radioisotopes?
Yes — the same formula applies to medical isotopes like Iodine-131 (8.02 days) or Technetium-99m (6.01 hours).
Simply enter the half-life in the same units as your time.
This Decay Calculator is provided for informational and educational purposes only.
Results are based on the standard exponential decay formula and assumed constant decay constants.
Real-world samples may be affected by contamination, external radiation sources, or measurement uncertainty.
For medical, industrial, or safety-critical applications, always consult a qualified nuclear physicist,
radiation safety officer, or authoritative data source.