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  2. Decay correction - Wikipedia

    en.wikipedia.org/wiki/Decay_correction

    If the radiation measured has dropped by half between the 4 hour sample and the 24 hour sample we might think that the concentration of compound in that organ has dropped by half; but applying the decay correct we see that the concentration is 0.5*2.82 so it has actually increased by 40% in that period.

  3. Bateman equation - Wikipedia

    en.wikipedia.org/wiki/Bateman_equation

    (this can be adapted to handle decay branches). While this can be solved explicitly for i = 2, the formulas quickly become cumbersome for longer chains. [3] The Bateman equation is a classical master equation where the transition rates are only allowed from one species (i) to the next (i+1) but never in the reverse sense (i+1 to i is forbidden).

  4. Rubidium–strontium dating - Wikipedia

    en.wikipedia.org/wiki/Rubidium–strontium_dating

    The ratio 87 Sr/ 86 Sr in a mineral sample can be accurately measured using a mass spectrometer. If the amount of Sr and Rb isotopes in the sample when it formed can be determined, the age can be calculated from the increase in 87 Sr/ 86 Sr. Different minerals that crystallized from the same silicic melt will all have the same initial 87 Sr/ 86 ...

  5. Calculation of radiocarbon dates - Wikipedia

    en.wikipedia.org/wiki/Calculation_of_radiocarbon...

    These ratios are used to calculate F m, the "fraction modern", defined as = where R norm is the 14 C / 12 C ratio for the sample, after correcting for fractionation, and R modern is the standard 14 C / 12 C ratio for modern carbon. [12]

  6. Radiometric dating - Wikipedia

    en.wikipedia.org/wiki/Radiometric_dating

    N(t) is number of atoms of the parent isotope in the sample at time t (the present), given by N(t) = N 0 e −λt, and; λ is the decay constant of the parent isotope, equal to the inverse of the radioactive half-life of the parent isotope [17] times the natural logarithm of 2.

  7. Uranium–thorium dating - Wikipedia

    en.wikipedia.org/wiki/Uranium–thorium_dating

    Thorium-230 is itself radioactive with a half-life of 75,000 years, [4] so instead of accumulating indefinitely (as for instance is the case for the uranium–lead system), thorium-230 instead approaches secular equilibrium with its radioactive parent uranium-234. At secular equilibrium, the number of thorium-230 decays per year within a sample ...

  8. Radioactive decay - Wikipedia

    en.wikipedia.org/wiki/Radioactive_decay

    A material containing unstable nuclei is considered radioactive. Three of the most common types of decay are alpha, beta, and gamma decay. The weak force is the mechanism that is responsible for beta decay, while the other two are governed by the electromagnetic and nuclear forces. [1] Radioactive decay is a random process at the level of ...

  9. Radiochemistry - Wikipedia

    en.wikipedia.org/wiki/Radiochemistry

    Radiochemistry is the chemistry of radioactive materials, where radioactive isotopes of elements are used to study the properties and chemical reactions of non-radioactive isotopes (often within radiochemistry the absence of radioactivity leads to a substance being described as being inactive as the isotopes are stable).