Radioactive Half-Life & Decay Calculator

Calculate radioactive isotope decay, remaining quantity, half-life, or elapsed duration using N(t) = N₀ × (½)^(t/t½). Includes an isotope library, decay constants, and archaeological dating analysis.

Target Parameter

Live calculation
Quick Sample Presets
grams, %, mCi
days
days
Calculated Remaining Amount N(t)
88.6062via N(t) = N₀ × (½)^(t / t½)
Half-Lives Elapsed0.175

% Remaining

88.61%

% Decayed

11.39%

Half-Life

5730.00 years

Elapsed Time

1000.00 years

Residual Activity & Decay Constant (λ)

Remaining: 88.61%Decayed: 11.39%
Decay Constant (λ per day)

3.3119e-7 d⁻¹

Mean Lifetime (τ = t½ / ln 2)

8266.64 years

After 1000.00 years (0.17 half-lives), 88.61% of the initial sample remains intact.

11.39% of the radioactive parent nuclei have transmuted into daughter decay products.

The Mathematics of Exponential Radioactive Decay

Radioactive decay is a first-order stochastic process in which unstable atomic nuclei lose energy by emitting ionizing radiation. Because the probability of decay per unit time is constant for each specific nuclide, macroscopic decay follows an exact exponential decay curve: N(t) = N₀ (½)t/t½ = Net.

Radioactive Decay Governing Equations
1. Remaining Quantity N(t)
N(t) = N₀ · (½)t / t½

Exponential half-life power

2. Decay Constant (λ)
λ =
ln(2)

λ ≈ 0.69315 ÷ t½

3. Elapsed Time (t)
t = t½ · log₂(
N₀N
)

Logarithmic age solver

Half-Life Step Sequence Table
1 t½ = 50.0%|2 t½ = 25.0%|3 t½ = 12.5%|4 t½ = 6.25%|5 t½ = 3.125%
Step-by-Step Calculation Breakdown
Example 1: Carbon-14 Dating of an Ancient Wooden Artifact (2,000 Years Elapsed)
1. Parameters: Initial quantity N₀ = 100.00%, Half-life t½ = 5,730 years, Elapsed t = 2,000 years
2. Calculate half-lives elapsed: n = 2,000 ÷ 5,730 = 0.3490 half-lives
3. Compute remaining: N(2000) = 100 × (0.5)0.3490 = 78.51% (21.49% decayed)
Example 2: Iodine-131 Medical Dose Decay (8.02 Days Half-Life, 24.06 Days Elapsed)
1. Parameters: Initial dose N₀ = 50.00 mCi, Half-life t½ = 8.02 days, Time t = 24.06 days
2. Calculate half-lives: n = 24.06 ÷ 8.02 = 3.00 exact half-lives
3. Compute residual activity: 50.00 × (0.5)³ = 50.00 × 0.125 = 6.25 mCi (87.5% eliminated)

Key Radioactive Nuclides & Clinical/Scientific Roles

Isotope NameHalf-Life DurationScientific / Clinical Application
Carbon-14 (C-14)5,730 yearsArchaeological organic dating
Uranium-238 (U-238)4.468 billion yearsGeological Earth age dating & nuclear fuel
Plutonium-239 (Pu-239)24,110 yearsNuclear energy & space RTG batteries
Radium-226 (Ra-226)1,600 yearsHistorical luminous paints & radiochemistry
Cesium-137 (Cs-137)30.17 yearsIndustrial radiography & medical calibration
Strontium-90 (Sr-90)28.8 yearsIndustrial thickness gauges & RTGs
Tritium (Hydrogen-3)12.32 yearsSelf-powered emergency exit lighting & fusion
Cobalt-60 (Co-60)5.27 yearsMedical cancer radiation therapy & sterilization
Polonium-210 (Po-210)138.4 daysStatic eliminators & alpha emitter research
Iodine-131 (I-131)8.02 daysThyroid medical diagnostic and ablation therapy
Technetium-99m (Tc-99m)6.01 hoursHospital diagnostic SPECT organ imaging
Fluorine-18 (F-18)109.8 minutesOncology PET scan metabolic tracer (FDG)

Frequently Asked Questions

What is half-life and what is the radioactive decay equation?
Half-life (t½) is the statistical duration required for exactly one-half of the unstable radionuclide nuclei in a sample to undergo radioactive decay: N(t) = N₀ × (½)^(t / t½) = N₀ × e^(-λt), where N₀ is the initial quantity, t is elapsed time, and λ = ln(2) / t½ is the characteristic decay constant.
How does Carbon-14 radiometric dating work?
Cosmic rays in the upper atmosphere continuously form Carbon-14 (t½ = 5,730 years), which enters the biosphere and is absorbed by living organisms. When an organism dies, Carbon-14 intake stops, and the isotope decays at a known exponential rate. Measuring the residual C-14 ratio determines the time elapsed since biological death up to ~50,000 years.
What percentage remains after 1, 2, 3, 4, and 5 half-lives?
After 1 half-life: 50.0% remains; 2 half-lives: 25.0% remains; 3 half-lives: 12.5% remains; 4 half-lives: 6.25% remains; 5 half-lives: 3.125% remains; 10 half-lives: ~0.098% remains (virtually 99.9% decayed).
What is the mean lifetime (tau) of a radionuclide?
The mean lifetime (τ = 1 / λ = t½ / ln(2) ≈ 1.443 × t½) is the average lifespan of an individual radioactive nucleus before decaying.

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