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Free Half-Life Calculator

Calculate the remaining quantity of a radioactive substance after any elapsed time, determine the number of half-lives that have passed, or find the half-life from decay measurements. Free, private — all calculations run in your browser.

⚡ Instant results🔒 100% private🆓 Always free🚫 No signup⚛️ Nuclear-grade precision
250.0
Remaining N(t)
25.0000%
% Remaining
75.0000%
% Decayed
2.0000
Half-Lives Elapsed
3.833e-12
λ Decay Constant
per second
2.609e+11
Mean Lifetime τ
seconds
Decay Progress
Remaining: 25.0000%Decayed: 75.0000%
Formula
N(t) = N₀ × (½)^(t/t½)
N(t) = 1000 × (½)^(2.000) = 250.0
λ = ln(2) / t½ = 3.833e-12 s⁻¹  |  τ = 1/λ = 2.609e+11 s

Scenario: Same Quantity, Different Half-Lives

62.50
t½ × 0.5
6.25% remaining
250.0
t½ × 1
25.00% remaining
500.0
t½ × 2
50.00% remaining
Real-World Applications
Carbon Dating — C-14 half-life 5,730 yr used to date organic material up to ~50,000 yr
Nuclear Medicine — Tc-99m (6h) used in 80%+ of diagnostic imaging procedures
Pharmacokinetics — Drug half-life determines dosing intervals (e.g. aspirin t½ ≈ 6h)

About This Half-Life Calculator

The Half-Life Calculator models exponential radioactive decay — one of nature's most precise and reliable processes. Given the initial quantity, elapsed time, and half-life of a substance, it calculates how much remains. It can also solve backwards: given initial and final quantities, it determines the number of half-lives elapsed and the total time.

The Formula

N(t) = N₀ × (1/2)^(t / t½) Equivalently: N(t) = N₀ × e^(−λt) where λ = ln(2)/t½ Half-lives elapsed: n = t / t½ Fraction remaining: (1/2)ⁿ = e^(−λt)

Half-life is a constant property of each radioactive isotope — it does not change with temperature, pressure, or chemical state. This constancy makes radioactive decay the basis of highly reliable dating methods in archaeology (radiocarbon dating) and geology (uranium-lead, potassium-argon dating).

Notable Half-Lives

  • Carbon-14 (C-14): 5,730 years — used for archaeological dating
  • Uranium-235 (U-235): 703,800,000 years — nuclear reactor fuel
  • Iodine-131 (I-131): 8.02 days — medical imaging and thyroid treatment
  • Radium-226 (Ra-226): 1,600 years — historical radiotherapy source
  • Polonium-210 (Po-210): 138 days — high toxicity; historically in poisoning cases
  • Tritium (H-3): 12.32 years — used in luminescent watch dials and fusion research

Privacy Notice

All calculations run in your browser. No data is transmitted or stored. See our Privacy Policy.

Quick Reference

Input / ParameterDescriptionExample Value
N₀ (initial quantity)Starting amount (grams, atoms, Bq, etc.)100 g
t (elapsed time)Time that has passed5,730 years
t½ (half-life)Time for half to decay5,730 years (C-14)
N(t) (remaining)N₀ × (1/2)^(t/t½)100 × 0.5¹ = 50 g
n (number of half-lives)n = t / t½5,730/5,730 = 1
Fraction remaining(1/2)ⁿ(0.5)¹ = 50%
Decay constant (λ)λ = ln(2) / t½ ≈ 0.6931 / t½0.6931/5730 = 0.000121/yr

When to Use This Calculator

⚛️
Physics and chemistry homework

Calculate remaining quantity after decay, number of half-lives, or determine the half-life from two data points for nuclear physics problems.

🏥
Medical physics and radiology

Calculate radiotracer activity at time of administration vs. imaging, and determine when radioactive waste from medical procedures reaches safe levels.

🌍
Archaeology and geology

Understand the mathematics behind radiocarbon dating and radiometric age dating using isotopes like U-238 and K-40.

💊
Pharmacokinetics

Apply the half-life concept to drug concentration: how long until a dose drops below therapeutic levels or clears the system entirely.

☢️
Nuclear engineering and safety

Calculate how long radioactive waste remains above safe background levels and model reactor fuel consumption over time.

💡 Pro Tips

1

After every half-life, exactly half remains — but this compounds. After n half-lives, the fraction remaining is (1/2)ⁿ. This is why radioactive materials take so long to become safe: carbon-14 has a half-life of 5,730 years, meaning after 57,300 years (10 half-lives) only 0.1% remains. Nuclear waste with half-lives of thousands of years requires geological-timescale storage.

2

The decay constant λ = ln(2)/t½ ≈ 0.693/t½ connects half-life to the continuous exponential decay formula N = N₀e^(−λt). The two formulas are mathematically identical — choose whichever is more convenient for your problem. The (1/2)^(t/t½) form is often more intuitive; the e^(−λt) form is easier to differentiate.

3

In pharmacology, a drug reaches approximately 97% of its steady-state concentration after 5 half-lives of dosing, and decreases to approximately 3% of peak after 5 half-lives post-dose. This is why drug dosing intervals and washout periods are typically expressed as multiples of the drug's half-life.

4

The number of half-lives n = log₂(N₀/N) — or equivalently n = ln(N₀/N) / ln(2). This formula is used to work backwards: given an initial and final quantity, how many half-lives elapsed? Divide by the half-life period to get the total elapsed time. This is the basis of radiocarbon age dating.

Frequently Asked Questions

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