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☢️ Half-Life Calculator

Calculate radioactive decay, remaining quantity, elapsed time, and half-life values using the exponential decay formula. Supports scientific notation for precise isotope calculations in nuclear physics, chemistry, and radiometric dating.

Select which value you want to calculate, then enter the known values. Leave the field you want to calculate empty.

📦 Remaining Quantity (N)
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units remaining
📊 Decayed Quantity
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units decayed
📈 Decay Constant (λ)
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per unit time
🔄 Half-Lives Elapsed
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number of half-lives

📊 Decay Curve Data

See how the quantity decreases over successive half-lives.

Half-Life # Time Elapsed Remaining Quantity % Remaining
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Please enter valid numeric values. Leave only the field you want to calculate empty.

📐 Exponential Decay Formula

The Half-Life Formula
N(t) = N₀ × (½)^(t / T₁/₂)

Where:

  • N(t) = Quantity remaining after time t
  • N₀ = Initial quantity at time t = 0
  • t = Elapsed time
  • T₁/₂ = Half-life of the substance
Decay Constant (λ)
λ = ln(2) / T₁/₂ ≈ 0.693147 / T₁/₂

The decay constant λ represents the probability of decay per unit time. It is related to the half-life by the natural logarithm of 2.

Alternative Exponential Form
N(t) = N₀ × e^(-λt)

This is the continuous exponential decay form, where e is the base of natural logarithms and λ is the decay constant.

Mean Lifetime (τ)
τ = 1/λ = T₁/₂ / ln(2)

The mean lifetime τ is the average time a particle or nucleus exists before decaying. It is longer than the half-life by a factor of approximately 1.4427.

📊 Common Isotope Half-Lives

Reference table of half-lives for common radioactive isotopes used in science, medicine, and industry.

Isotope Symbol Half-Life Decay Mode Application
Uranium-238²³⁸U4.468 billion yearsAlphaGeological dating
Uranium-235²³⁵U703.8 million yearsAlphaNuclear power, dating
Potassium-40⁴⁰K1.248 billion yearsBeta+, ECRock dating
Carbon-14¹⁴C5,730 yearsBeta-Radiocarbon dating
Plutonium-239²³⁹Pu24,110 yearsAlphaNuclear weapons, fuel
Radium-226²²⁶Ra1,600 yearsAlphaMedical radiotherapy
Cobalt-60⁶⁰Co5.27 yearsBeta-Medical sterilization
Strontium-90⁹⁰Sr28.8 yearsBeta-Nuclear fallout
Caesium-137¹³⁷Cs30.17 yearsBeta-Medical, industrial
Tritium (H-3)³H12.32 yearsBeta-Biolabeling, fusion
Iodine-131¹³¹I8.02 daysBeta-Thyroid treatment
Phosphorus-32³²P14.26 daysBeta-Biological research
Technetium-99m⁹⁹ᵐTc6.01 hoursGammaMedical imaging
Polonium-212²¹²Po299 nanosecondsAlphaResearch

📋 Half-Life Calculation Examples

📌 Example 1: Carbon-14 Dating

Problem: An archaeological sample contains 25% of its original Carbon-14. Carbon-14 has a half-life of 5,730 years. How old is the sample?

Solution: After 1 half-life (5,730 yr): 50% remains. After 2 half-lives (11,460 yr): 25% remains. The sample is approximately 11,460 years old.

📌 Example 2: Medical Isotope Decay

Problem: A patient receives 200 MBq of Technetium-99m (half-life = 6.01 hours). How much remains after 18 hours?

Solution: 18 hours = 3 half-lives. N = 200 × (½)³ = 200 × ⅛ = 25 MBq remains.

📌 Example 3: Finding Half-Life

Problem: A 500 g sample decays to 125 g in 24 years. What is the half-life?

Solution: 500 → 250 → 125 = 2 half-lives in 24 years. Half-life = 24 ÷ 2 = 12 years.

📌 Example 4: Exponential Decay

Problem: Iodine-131 has a half-life of 8.02 days. If you start with 100 mg, how much remains after 20 days?

Solution: N = 100 × (½)^(20/8.02) = 100 × (½)^2.494 ≈ 100 × 0.177 = 17.7 mg remains.

☢️ Half-Life Calculator Features

🧮
Four Calculation Modes
Calculate any missing variable — remaining quantity, half-life, elapsed time, or initial quantity — from the other known values.
📊
Decay Curve Data Table
View how the quantity decreases over successive half-lives in an easy-to-read table format showing remaining quantity and percentage.
🔬
Scientific Notation
Supports very small and very large numbers using JavaScript floating-point arithmetic, ideal for isotope calculations.
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Full Formula Reference
Complete formulas including exponential decay, decay constant (λ), mean lifetime (τ), and all their relationships.
📱
Mobile Friendly
Fully responsive design that works seamlessly on smartphones, tablets, and desktop computers.
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Privacy Protected
All calculations are performed locally in your browser. No data is transmitted to any server.

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What is Half-Life?

Understanding Radioactive Decay

Half-life (T₁/₂) is the time required for a quantity of a radioactive substance to reduce to half of its initial value. This concept is fundamental in nuclear physics, chemistry, and radiometric dating. The key insight is that radioactive decay follows an exponential pattern — the amount of substance decreases by a constant factor (half) over each equal time interval. This means that after one half-life, 50% remains; after two, 25%; after three, 12.5%; and so on.

The Exponential Decay Formula

The mathematical foundation of half-life calculations is the exponential decay formula: N(t) = N₀ × (½)^(t/T₁/₂). This formula can be used to solve for any variable — the remaining quantity, the half-life, the elapsed time, or the initial quantity — as long as the other three values are known. The decay constant λ = ln(2)/T₁/₂ provides an alternative formulation: N(t) = N₀ × e^(-λt), which is particularly useful in differential equation models of decay processes.

Applications in Science and Medicine

Half-life calculations have wide-ranging practical applications. In archaeology, carbon-14 dating uses the 5,730-year half-life of ¹⁴C to determine the age of organic materials up to about 50,000 years old. In nuclear medicine, isotopes like technetium-99m (6-hour half-life) are used for diagnostic imaging because they decay quickly enough to minimize patient radiation exposure while providing clear images. In geology, uranium-lead dating relies on the 4.5-billion-year half-life of ²³⁸U to date the oldest rocks on Earth and in the solar system. In environmental science, understanding the half-lives of nuclear fallout isotopes like ¹³⁷Cs (30 years) and ⁹⁰Sr (29 years) is crucial for assessing long-term contamination risks.

Half-Life vs. Doubling Time

Half-life and doubling time are mathematically related concepts. While half-life describes exponential decay (quantities decreasing by half), doubling time describes exponential growth (quantities doubling). The formulas are structurally identical: N(t) = N₀ × 2^(t/T_d) for doubling, compared to N(t) = N₀ × (½)^(t/T_½) for halving. The doubling time T_d can be calculated from a growth rate using the rule of 70 (T_d ≈ 70/growth rate %), while half-life uses the same mathematics in reverse. This symmetry makes the same calculator useful for modeling both radioactive decay and population growth when adjusted appropriately.

Frequently Asked Questions (FAQ)

What is half-life?
Half-life is the time required for a quantity of a radioactive substance to decay to half of its initial value. It is a characteristic property of each radioactive isotope and is constant regardless of the starting amount or external conditions. For example, carbon-14 has a half-life of 5,730 years — meaning a 100g sample of ¹⁴C will become 50g after 5,730 years, then 25g after another 5,730 years, and so on. The concept applies to any exponential decay process, including chemical reactions, drug metabolism in the body, and capacitor discharge in electronics.
How to calculate half-life?
To calculate half-life, use the formula: N(t) = N₀ × (½)^(t/T₁/₂). If you know the initial quantity (N₀), the remaining quantity (N), and the elapsed time (t), you can solve for T₁/₂. Rearranged: T₁/₂ = t × ln(2) / ln(N₀/N). For example, if a 200g sample decays to 50g in 30 years: T₁/₂ = 30 × ln(2) / ln(200/50) = 30 × 0.693 / 1.386 = 15 years. Our calculator handles this automatically — just select "Half-Life (T₁/₂)" as the calculation mode and enter the other three values.
What is exponential decay?
Exponential decay is a process where a quantity decreases at a rate proportional to its current value. This means the quantity decreases by a constant fraction (not a constant amount) over equal time intervals. The mathematical form is N(t) = N₀ × e^(-λt), where λ is the decay constant. Exponential decay is characterized by its half-life — the time needed for the quantity to reduce by half. Unlike linear decay (where the same amount decreases each period), exponential decay slows down over time but never reaches zero mathematically. In practice, the substance is considered effectively gone after about 10 half-lives (0.1% remaining).
Half-life vs doubling time: what's the difference?
Half-life and doubling time are mathematically inverse concepts. Half-life measures how long it takes for a quantity to decrease by half (radioactive decay, drug elimination). Doubling time measures how long it takes for a quantity to double (population growth, compound interest, bacterial growth). The formulas are structurally identical: N(t) = N₀ × (½)^(t/T_½) for decay and N(t) = N₀ × 2^(t/T_d) for growth. The decay constant λ is related to half-life by λ = ln(2)/T_½, while the growth rate r is related to doubling time by r = ln(2)/T_d. Understanding both concepts provides a complete picture of exponential processes in nature.
What are real-world applications of half-life?
Half-life has numerous practical applications: Radiometric dating — carbon-14 (5,730 yr) for archaeology, uranium-lead (4.47 billion yr) for geology. Nuclear medicine — technetium-99m (6 hr) for imaging, iodine-131 (8 days) for thyroid treatment. Nuclear waste management — understanding storage requirements based on isotope half-lives. Food irradiation — cobalt-60 (5.27 yr) for sterilizing food. Environmental science — tracking nuclear fallout isotopes. Pharmacokinetics — drug half-life determines dosing schedules. Industrial radiography — using iridium-192 (74 days) for non-destructive testing of welds and pipelines.
Is half-life affected by temperature or pressure?
For nuclear decay processes, half-life is not affected by temperature, pressure, chemical state, or any other environmental conditions. This is because radioactive decay is a quantum mechanical process that occurs at the atomic nucleus level, and the strong nuclear force governing decay is unaffected by external conditions. This property makes radioactive decay an exceptionally reliable clock for dating purposes. However, for some chemical decay processes (like drug metabolism or chemical decomposition), half-lives can be affected by temperature, pH, and other environmental factors. Our calculator models the nuclear decay scenario with constant half-life.

About This Half-Life Calculator

Our Half-Life Calculator is a comprehensive tool for modeling radioactive decay and exponential decay processes. Whether you're a student studying nuclear physics, a researcher working with radioactive isotopes, or a medical professional calculating dosage decay, this calculator provides accurate results using the standard exponential decay formula N(t) = N₀ × (½)^(t/T₁/₂).

Why Choose Our Half-Life Calculator?

🧮 Four-Way Calculation

Calculate remaining quantity, half-life, elapsed time, or initial quantity from any three known values. Complete flexibility for any decay problem.

📊 Detailed Decay Tables

View complete decay curve data showing remaining quantity and percentage after each successive half-life, helping visualize the exponential pattern.

📐 Formula Reference

Full mathematical reference including exponential decay formula, decay constant (λ), mean lifetime (τ), and their relationships with worked examples.

🔬 Isotope Reference

Built-in reference table of common radioactive isotopes with their half-lives, decay modes, and practical applications in science and medicine.

🔒 Privacy First

All calculations are performed in your browser. No data is stored, transmitted, or shared with any third parties.

🆓 Always Free

Complete access to all features with no registration, no hidden fees, and no usage limits. Use it as often as you need for study or work.

Important Disclaimer: This Half-Life Calculator provides mathematical estimates based on the exponential decay model. Results should be verified against authoritative sources for critical applications in nuclear medicine, radiation safety, or scientific research. This tool is for educational and informational purposes only and should not replace professional consultation in matters involving radioactive materials or health and safety decisions.