Why does a 100 gram sample shrink to 12.5 grams after just three half-lives? Each half-life cuts the amount in half, no matter how much you start with. That one steady rule explains carbon dating, medical scans, and many other decay problems. This guide gives you the table, the formula, and the logic behind it.
| Definition | The time for half of a sample to decay |
|---|---|
| Formula | N = N0 x (1/2)^(t / T) |
| After 3 half-lives | 12.5 percent remains |
| After 10 half-lives | About 0.1 percent remains |
| Carbon-14 half-life | About 5,730 years |
Half-Life Quick Reference Table
Each half-life leaves exactly half of what was there before. Start with 100 percent, and the remaining share drops to 50, then 25, then 12.5 percent. The table below shows the first ten steps.
| Half-lives passed | Fraction left | Percent left | From 100 g |
|---|---|---|---|
| 1 | 1/2 | 50% | 50 g |
| 2 | 1/4 | 25% | 25 g |
| 3 | 1/8 | 12.5% | 12.5 g |
| 4 | 1/16 | 6.25% | 6.25 g |
| 5 | 1/32 | 3.125% | 3.125 g |
| 6 | 1/64 | 1.5625% | 1.5625 g |
| 7 | 1/128 | 0.78% | 0.78 g |
| 8 | 1/256 | 0.39% | 0.39 g |
| 9 | 1/512 | 0.20% | 0.20 g |
| 10 | 1/1,024 | 0.098% | 0.098 g |
Notice that the amount never reaches zero on paper. After ten half-lives, less than one part in a thousand remains. Scientists often treat that level as practically gone for everyday purposes.
Four terms come up again and again in decay problems. Here is what each one means in plain words.
- Half-life (T)
- The fixed time it takes for half of the current amount to decay.
- Initial amount (N0)
- The starting quantity, measured in grams, atoms, or percent.
- Remaining amount (N)
- The quantity still present after the elapsed time has passed.
- Decay constant
- The fraction lost per unit of time, equal to 0.693 divided by the half-life.
- Mean lifetime
- The average life of one atom, about 1.44 times the half-life.
What Does Half-Life Actually Mean?
Half-life is the time it takes for half of a sample to decay or change. The EPA defines it as the time for half of the radioactive atoms present to decay. Each isotope has its own fixed half-life.
The key idea is that the rate is steady in proportion, not in amount. A sample loses half its atoms in one half-life, whether it holds a trillion atoms or a few thousand. That is why the curve bends and flattens instead of falling in a straight line.
Why the Rate Never Changes
Half-life stays constant because each atom has the same chance of decaying in a given time. The atoms do not age or wear out. A smaller sample simply has fewer atoms that can decay.
This is what makes decay exponential rather than linear. HyperPhysics writes the law as N = N0 x e^(-kt), where k is the decay constant. For carbon-14, k is about 0.000121 per year.
The constant also explains a common confusion. The average lifetime of one atom is longer than the half-life. For carbon-14, the mean lifetime is about 8,267 years, compared with its 5,730-year half-life.
How Do You Calculate the Amount Remaining?
Multiply the starting amount by one half raised to the number of half-lives passed. The formula is N = N0 x (1/2)^(t / T). Here t is the elapsed time and T is the half-life.
Try a clear example. A substance has a half-life of 5 years, and you start with 100 grams. After 15 years, three half-lives have passed, so 100 x (1/2)^3 leaves 12.5 grams.
The time does not need to be a whole number of half-lives. After 1.5 half-lives, (1/2)^1.5 equals about 0.354, so 35.4 percent remains. The power handles any fraction, which the table above cannot show.
The exponent does most of the work, so a quick review of powers helps. Our guide to exponents and scientific notation covers how fractional and negative powers behave. For fast answers with any three known values, the Half-Life Calculator solves for the missing one.
How Do You Solve for Time or Half-Life?
Count how many halvings separate the start and end amounts, then multiply by the half-life. In formula form, t = T x log2(N0 / N). Base-2 logarithms simply count the halvings for you.
Finding the Elapsed Time
Suppose 100 grams must fall to 10 grams, and the half-life is 5 years. The ratio is 10, and log2 of 10 is about 3.32. Multiply by 5 years, and the answer is about 16.6 years.
Finding the Half-Life Itself
Now reverse the question. A sample drops from 80 grams to 20 grams in 12 days. That is a ratio of 4, or exactly two halvings, so the half-life is 12 divided by 2, or 6 days.
Here is a handy check for any answer. The elapsed time divided by the half-life should match the number of halvings you counted. When the two numbers disagree, recheck the ratio before trusting the result.
Growth works the same way in reverse. A quantity that doubles has a doubling time, just as a shrinking one has a half-life. Read the mathematics of doubling time to see the growth side of this rule.
How Does Carbon Dating Use Half-Life?
Carbon dating compares the carbon-14 left in old organic material with the level found in living things. Carbon-14 has a half-life of about 5,730 years, so the remaining share reveals the age.
Living plants and animals keep taking in carbon, so their carbon-14 level stays steady. Once they die, intake stops and the clock starts. HyperPhysics notes that living matter shows about 15 decays per minute per gram of carbon.
The math follows the same formula. After 11,460 years, or two half-lives, 25 percent remains. After just 1,000 years, about 88.6 percent is still present. A piece of wood with 60 percent left is about 4,220 years old.
Newer accelerator methods count the atoms more directly. HyperPhysics notes that this approach can stretch the range to about 100,000 years in the best cases.
Which Isotopes Have Useful Half-Lives in Medicine?
Medical isotopes usually have short half-lives, from minutes to days. A short half-life lets a scan or treatment work, then fade quickly. The table uses half-life values listed by OpenStax.
| Isotope | Half-life | Common use | Amount left later |
|---|---|---|---|
| Fluorine-18 | 110 minutes | PET scans | About 10.3% after 6 hours |
| Technetium-99m | 8.01 hours | Organ and bone scans | About 12.5% after 24 hours |
| Iodine-131 | 8.02 days | Thyroid scans and treatment | About 7.5% after 30 days |
| Cobalt-60 | 5.27 years | Cancer treatment | 50% after 5.27 years |
The pattern is easy to read. Technetium-99m loses about seven eighths of its activity in one day. Cobalt-60 lasts for years, so equipment that uses it needs a steady source.
The same table logic helps with storage planning too. A source held for ten half-lives drops below 0.1 percent of its starting activity. For iodine-131, ten half-lives is about 80 days.
Short half-lives also explain why these isotopes are made close to where they are used. A fluorine-18 batch loses half its strength in under two hours, so long shipping times waste most of it.
These figures describe the isotope itself, not a dosing plan. Medical staff decide doses and timing for each patient.
The Half-Life Calculator takes any three of the starting amount, remaining amount, elapsed time and half-life, then solves for the fourth.
Questions People Ask About Half-Life
What Is Half-Life in Simple Terms?
Half-life is the time it takes for half of a substance to decay. After one half-life, 50 percent remains. After two, 25 percent remains, and the pattern continues.
How Much Is Left After Three Half-Lives?
One eighth, or 12.5 percent, remains after three half-lives. A 100 gram sample with a 5-year half-life leaves 12.5 grams after 15 years.
Does a Substance Ever Fully Decay?
On paper, the amount keeps halving and never reaches exactly zero. In practice, after about ten half-lives less than 0.1 percent remains, which is usually treated as effectively gone.
How Do You Find Half-Life From Two Measurements?
Divide the elapsed time by the number of halvings between the two amounts. A drop from 80 grams to 20 grams in 12 days is two halvings, so the half-life is 6 days.
Why Is Carbon-14 Used for Dating Old Objects?
Carbon-14 has a half-life of about 5,730 years, which suits organic objects up to about 50,000 years old. Living things absorb it until death, then it decays at a known rate.
Where These Numbers Come From
References Used in This Article
This article is general science and math education, not medical advice about radiation or treatment. Isotope values are rounded from the cited references. Reviewed for accuracy by Prof. Dr. Khalil Mudassar, PhD. Last updated September 27, 2026.
Author
Shakeel Muzaffar is the Founder and Editor-in-Chief of MultiCalculators.com, bringing over 15 years of experience in digital publishing, product strategy, and online tool development. He leads the platform's editorial vision, ensuring every calculator meets strict standards for accuracy, usability, and real-world value. Shakeel personally oversees content quality, formula verification workflows, and the platform's commitment to publishing tools that are genuinely useful for students, professionals, and everyday users worldwide.




