The following tools can generate any one of the values from the other three in the half-life formula for a substance undergoing decay to decrease by half.

Half-Life Calculator

The most suitable types of sample for radiocarbon dating are charcoal and well-preserved wood, although leather, cloth, paper, peat, shell and bone can also be used. Because of the somewhat short half-life of 14C, radiocarbon dating is not applicable to samples with ages greater than about 50,000 years, because the remaining concentration would. Here of some of the well-tested methods of dating used in the study of early humans: Potassium-argon dating, Argon-argon dating, Carbon-14 (or Radiocarbon), and Uranium series. All of these methods measure the amount of radioactive decay of chemical elements; the decay occurs in a consistent manner, like a clock, over long periods of time.

Please provide any three of the following to calculate the fourth value.

Half-Life, Mean Lifetime, and Decay Constant Conversion

Please provide any one of the following to get the other two.

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Definition and Formula

Half-life is defined as the amount of time it takes a given quantity to decrease to half of its initial value. The term is most commonly used in relation to atoms undergoing radioactive decay, but can be used to describe other types of decay, whether exponential or not. One of the most well-known applications of half-life is carbon-14 dating. The half-life of carbon-14 is approximately 5,730 years, and it can be reliably used to measure dates up to around 50,000 years ago. The process of carbon-14 dating was developed by William Libby, and is based on the fact that carbon-14 is constantly being made in the atmosphere. It is incorporated into plants through photosynthesis, and then into animals when they consume plants. The carbon-14 undergoes radioactive decay once the plant or animal dies, and measuring the amount of carbon-14 in a sample conveys information about when the plant or animal died.

Below are shown three equivalent formulas describing exponential decay:

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where
N₀ is the initial quantity
N_t is the remaining quantity after time, t
t_1/2 is the half-life
τ is the mean lifetime
λ is the decay constant

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If an archaeologist found a fossil sample that contained 25% carbon-14 in comparison to a living sample, the time of the fossil sample's death could be determined by rearranging equation 1, since N_t, N₀, and t_1/2 are known.

This means that the fossil is 11,460 years old.

Derivation of the Relationship Between Half-Life Constants

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Using the above equations, it is also possible for a relationship to be derived between t_1/2, τ, and λ. This relationship enables the determination of all values, as long as at least one is known.