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Published equation contexts

N206N238=eλ238t−1,N207N235=eλ235t−1\frac{N_{206}}{N_{238}} = e^{\lambda_{238} t} - 1, \qquad \frac{N_{207}}{N_{235}} = e^{\lambda_{235} t} - 1

Why this formula appears here

Uranium’s usefulness as a clock is doubled by an accident of nuclear structure: natural uranium consists of two isotopes, uranium-238 and uranium-235, which decay through separate chains to two different stable lead isotopes, lead-206 and lead-207 respectively, at two different, independently measured rates. Uranium-238’s half-life is about four point four seven billion years and uranium-235’s is about seven hundred four million years, values fixed by direct laboratory counting experiments [ 6 ] and formally adopted as the field’s working convention shortly after [ 7 ] . Because both chains run inside the same mineral grain simultaneously, from the same crystallization event, a single zircon…

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N238N_{238}

Symbol N_238

N2N_238 occurs below the fraction bar. The quantity above the bar is divided by this expression; zero is excluded as a denominator.

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eλ238te^{\lambda_{238} t}

Symbol e^lambda_238 t

ele^lambda2a_238 t is one of the signed contributions combined to compute the quantity on the left.

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eλ235te^{\lambda_{235} t}

Symbol e^lambda_235 t

ele^lambda2a_235 t is one of the signed contributions combined to compute the quantity on the left.

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How to interpret it

With a fixed numerator, increasing a nonzero denominator reduces the fraction. Read it with the definitions, units, and assumptions supplied by the article.

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Published contexts (1)

A symbol can carry a different meaning in another article. Each occurrence keeps its own guide and term definitions.

N206N238=eλ238t−1,N207N235=eλ235t−1,\frac{N_{206}}{N_{238}} = e^{\lambda_{238} t} - 1, \qquad \frac{N_{207}}{N_{235}} = e^{\lambda_{235} t} - 1,

Equation 6 · Evolutionary Nuclear Physics

Radioactive Clocks: How Nuclear Physics Gave Evolution Its Time

This equation states an equality: the expressions on both sides have the same value under the article’s assumptions.

Uranium’s usefulness as a clock is doubled by an accident of nuclear structure: natural uranium consists of two isotopes, uranium-238 and uranium-235, which decay through separate chains to two different stable lead isotopes, lead-206 and lead-207 respectively, at two different, independently measured rates. Uranium-238’s half-life is about four point four seven billion years and uranium-235’s is about seven hundred four million years, values fixed by direct laboratory counting experiments [ 6 ] and formally adopted as the field’s working convention shortly after [ 7 ] . Because both chains run inside the same mineral grain simultaneously, from the same crystallization event, a single zircon…

Meanings in this article

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