Sigma Calculator — 543+ Free Calculator Tools
Find the remaining quantity after any elapsed time, plus half-lives elapsed and the amount decayed.
Enter the initial quantity, the half-life, and the elapsed time — all in matching units (e.g. years and years). The calculator divides elapsed time by the half-life to get the number of half-lives, then applies exponential decay.
Formula
Remaining = initial × (1/2)^(elapsed ÷ half-life). Example: 100 units with a 5-year half-life after 15 years → 3 half-lives → 100 × (1/2)³ = 12.5 remaining.
Half-life is the clock that governs everything from radioactive dating to how long your morning coffee keeps you alert. It answers a simple question: how long until half of something is gone? Because the answer stays constant no matter how much you start with, a single half-life value unlocks predictions across archaeology, medicine, nuclear physics, and environmental science. This guide shows you how to use the calculator above, explains what half-life really means, derives the decay formula with two fully worked numerical examples, applies it to carbon-14 dating and drug elimination, and flags the five mistakes people make most often.
Follow these steps to compute the remaining quantity with the calculator above:
Tip: the three time inputs must share units. Mixing a half-life in hours with an elapsed time in days silently produces a wrong answer — convert first (24 hours = 1 day) so both use the same unit.
Before you trust any result, sanity-check the half-lives elapsed. If the elapsed time is shorter than one half-life, more than half must remain; if it spans exactly three half-lives, exactly one-eighth must remain. These quick mental checks catch unit mix-ups instantly.
The half-life of a substance is the time required for half of its atoms or molecules to decay, transform, or be eliminated. After one half-life, 50% remains; after two, 25%; after three, 12.5% — each half-life multiplies the survivors by another factor of one-half. This multiplicative pattern is called exponential decay, and it arises whenever each unit has a constant probability of decaying per unit time, independent of the others.
The defining feature of half-life is that it does not depend on the starting amount. Whether you begin with 10 grams or 10 kilograms of a radioisotope, half is gone after one half-life. Mathematically this happens because the initial quantity cancels out of the fraction remaining: N/N₀ = (1/2)^(t/T) contains no N₀ on the right-hand side. The process is first-order, meaning the decay rate is proportional to the amount present, so the fraction lost per unit time stays constant even as the absolute loss shrinks.
Half-lives span an astonishing range. Francium-223 decays with a half-life of about 22 minutes, so a sample is essentially gone within a day. Carbon-14, the archaeologist’s clock, has a half-life of 5,730 years, making it ideal for dating artifacts up to ~50,000 years old. Uranium-238, used to date the Earth itself, has a half-life of 4.468 billion years — comparable to the age of the planet. In medicine, the relevant half-lives are hours: caffeine’s ~5-hour half-life explains why an afternoon espresso can still disturb midnight sleep, and many drugs are dosed at intervals chosen relative to their half-lives.
It helps to distinguish half-life from two related ideas. The mean lifetime (average time before decay) equals the half-life divided by ln(2), i.e., about 1.4427 half-lives — longer than the half-life because a few long-lived stragglers pull the average up. The decay constant λ = ln(2)/T is the per-unit-time decay probability used in the continuous form N(t) = N₀e^(−λt). All three describe the same process; half-life is simply the most intuitive packaging.
A subtle point: the amount never mathematically reaches zero. After 10 half-lives, (1/2)^10 = 1/1024 ≈ 0.098% remains; after 20 half-lives, about one-millionth remains. In practice the substance becomes undetectable or negligible long before that, which is why we speak of “effectively gone” after 7–10 half-lives (less than 1% to 0.1% remaining).
The remaining quantity after elapsed time t is:
N(t) = N₀ × (1/2)^(t/T)
Where N₀ is the initial quantity, T is the half-life, and t is the elapsed time (t and T in the same units). The exponent t/T counts how many half-lives have elapsed — it need not be a whole number. Equivalent forms include N(t) = N₀e^(−λt) with λ = ln(2)/T ≈ 0.6931/T.
Worked example 1 — whole number of half-lives. N₀ = 100 grams, T = 5 years, t = 15 years.
These are exactly the calculator’s defaults, so you can verify the tool by entering 100, 5, and 15. The halving sequence is visible: 100 → 50 → 25 → 12.5.
Worked example 2 — fractional half-lives. N₀ = 80 mg, T = 10 hours, t = 25 hours.
Fractional exponents are handled the same way — the formula does not require whole half-lives. As a check via the continuous form: λ = 0.6931/10 = 0.06931 per hour, and 80 × e^(−0.06931×25) = 80 × e^(−1.7328) = 80 × 0.17678 = 14.14 mg. Both forms agree.
To solve for the half-life itself from two measurements, rearrange: T = (t₂ − t₁) × ln(2) / ln(N₁/N₂). This is how laboratories determine half-lives experimentally, as shown in the FAQ below.
Radiocarbon dating is the most famous application of half-life. Cosmic rays continually create carbon-14 in the atmosphere, so living organisms contain a steady ratio of C-14 to ordinary C-12. When the organism dies, C-14 intake stops and the existing C-14 decays with a half-life of T = 5,730 years. Measuring the remaining fraction reveals the time since death.
Scenario. A bone fragment contains 3.125% of the carbon-14 found in a living bone. How old is it?
Step 1 — express the fraction as a power of one-half. 3.125% = 0.03125 = 1/32. Since (1/2)^5 = 1/32, exactly 5 half-lives have elapsed.
Step 2 — convert half-lives to years. Age = 5 × 5,730 = 28,650 years.
Step 3 — sanity check. After each half-life the fraction halves: 100% → 50% (5,730 yr) → 25% (11,460 yr) → 12.5% (17,190 yr) → 6.25% (22,920 yr) → 3.125% (28,650 yr). The chain confirms the answer.
A second illustration with the calculator’s method: a charcoal sample starts with an activity of 240 decays per minute and measures 60 decays per minute today. The fraction remaining is 60/240 = 0.25 = (1/2)², so 2 half-lives elapsed and the sample is 2 × 5,730 = 11,460 years old. Beyond about 9 half-lives (~50,000 years) less than 0.2% remains, which is why radiocarbon dating has a practical age limit.
Pharmacology uses half-life to schedule doses and predict when a drug clears the body. After each half-life, the blood concentration halves (assuming first-order elimination, which holds for most drugs at therapeutic doses).
Scenario. A patient receives a 500 mg dose of a drug with an 8-hour half-life. How much remains after 24 hours, and when is less than 1% left?
Step 1 — half-lives elapsed. 24 / 8 = 3 half-lives.
Step 2 — remaining amount. 500 × (1/2)³ = 500 × 0.125 = 62.5 mg.
Step 3 — time to under 1%. 1% = 0.01 = (1/2)^n gives n = log(0.01)/log(0.5) ≈ 6.64 half-lives. Time = 6.64 × 8 ≈ 53.1 hours (about 2.2 days). In practice clinicians use the rule of thumb “7 half-lives to clear,” i.e., 56 hours here, leaving (1/2)^7 = 1/128 ≈ 0.78%.
This is also why dosing intervals relate to half-life: a drug taken every half-life accumulates to a steady state of about twice the single dose (500 mg → 750 mg → 875 mg → approaching 1,000 mg), because each new dose arrives just as the previous one has halved. Understanding this prevents both underdosing and accidental overdose.
Continue with these companion tools: the Exponent Calculator for evaluating the (1/2)^(t/T) power directly, and the Scientific Calculator for the logarithms used in half-life rearrangements. Browse the full collection in our Math Calculators hub.
This page provides a half-life (exponential decay) calculator. Formula: N(t) = N₀ × (1/2)^(t/T); continuous form N(t) = N₀e^(−λt) with λ = ln(2)/T ≈ 0.6931/T. Verified examples: N₀ = 100, T = 5, t = 15 → 12.5 remaining, 3 half-lives, 87.5 decayed; N₀ = 80, T = 10, t = 25 → 14.14 remaining. Carbon-14: T = 5,730 years; 3.125% remaining → 5 half-lives → 28,650 years. Drug: 500 mg, T = 8 h, t = 24 h → 62.5 mg. Inverse: T = (t₂−t₁)ln2/ln(N₁/N₂). Half-life is independent of N₀ (first-order kinetics); amount never reaches exactly zero.
The time it takes for half of a quantity to decay or be eliminated — used for radioactive isotopes, medicines in the body, and even caffeine.
One-eighth: (1/2)³ = 1/8. After n half-lives, (1/2)^n of the original remains, so the amount never quite reaches zero.
Multiply the initial amount by one-half raised to the number of elapsed half-lives. The calculator above handles any numbers instantly.
Roughly 5–6 hours in most adults — which is why an afternoon coffee can still affect your sleep at midnight.
The classic half-life formula assumes first-order (exponential) decay, which fits radioactive decay and many drug-elimination processes well.
Yes — the same exponential math works for doubling. Replace the (1/2) base with 2 and the half-life with the doubling time: N(t) = N₀ × 2^(t/T_double). For example, bacteria doubling every 20 minutes: starting from 1,000 cells, after 2 hours (6 doublings) you have 1,000 × 2⁶ = 64,000 cells. The formula structure is identical; only the base changes from one-half to two.
Because radioactive decay is a first-order process: each atom has the same probability of decaying per unit time, independent of the others. The initial quantity cancels out of the fraction remaining — N/N₀ = (1/2)^(t/T) has no N₀ on the right side. So 10 g and 10 kg of the same isotope both lose exactly half their atoms in one half-life; only the absolute numbers differ.
By measuring the quantity at two times and solving T = (t₂ − t₁) × ln(2) / ln(N₁/N₂). For example, a sample reading 1,000 Bq drops to 700 Bq over 10 days: T = 10 × 0.6931 / ln(1000/700) = 6.931 / 0.3567 ≈ 19.43 days. Repeating the measurement over several intervals and averaging gives a precise value.
Sources: Decay calculations verified with the calculator above; carbon-14 half-life (5,730 years) is the standard Libby value.
Also try our Exponent Calculator and Scientific Calculator — or browse all Math Calculators.Half-Life Calculator