Half-Life
| Formula / Notation | A(t) = A₀e^(−λt); t½ = ln2/λ |
|---|---|
| Also Known As | Radioisotope half-life, Decay half-life, Biological half-life |
What is Half-Life?
The time required for half of the atoms in a radioactive sample to decay. Different radioactive isotopes have characteristic half-lives ranging from fractions of a second to billions of years. Half-life is also used in pharmacokinetics to describe drug elimination rates.
Formula & Notation
Other Names / Synonyms: Radioisotope half-life, Decay half-life, Biological half-life
Properties & Characteristics
Uses & Applications
Safety Information
Always consult the SDS/MSDS before handling any chemical. This information is for educational purposes only.
Key Facts
Frequently Asked Questions
The time required for half of the atoms in a radioactive sample to decay. Different radioactive isotopes have characteristic half-lives ranging from fractions of a second to billions of years. Half-life is also used in pharmacokinetics to describe drug elimination rates.
Radiocarbon dating (C-14 t½ = 5730 yr, dates objects up to 50,000 yr). Geological dating (U-238/Pb-206, K-40/Ar-40). Medical radioisotopes: Tc-99m (6 hr, imaging), I-131 (8 days, thyroid treatment), F-18 (110 min, PET scan). Nuclear waste storage calculations. Pharmacokinetics and drug dosing interv…
Short half-life isotopes have high activity (high radiation dose rate) but shorter environmental persistence. Long half-life isotopes (Pu-239: 24,100 yr, U-238: 4.47 billion yr) require permanent geological storage. Never dispose of radioactive materials in regular waste — specialized licensed dispo…
The formula or notation for Half-Life is: A(t) = A₀e^(−λt); t½ = ln2/λ