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Related Concept Videos

Nuclear Transmutation03:20

Nuclear Transmutation

Nuclear transmutation is the conversion of one nuclide into another. It can occur by the radioactive decay of a nucleus, or the reaction of a nucleus with another particle. The first manmade nucleus was produced in Ernest Rutherford’s laboratory in 1919 by a transmutation reaction, the bombardment of one type of nuclei with other nuclei or with neutrons. Rutherford bombarded nitrogen-14 atoms with high-speed α particles from a natural radioactive isotope of radium and observed protons being...
Nuclear Stability03:18

Nuclear Stability

Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively charged protons together in the...
Radioactive Decay and Radiometric Dating02:48

Radioactive Decay and Radiometric Dating

Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
Radioactivity and Nuclear Equations03:18

Radioactivity and Nuclear Equations

Nuclear chemistry is the study of reactions that involve changes in nuclear structure. The nucleus of an atom is composed of protons and, except for hydrogen, neutrons. The number of protons in the nucleus is called the atomic number (Z) of the element, and the sum of the number of protons and the number of neutrons is the mass number (A). Atoms with the same atomic number but different mass numbers are isotopes of the same element.
A nuclide of an element has a specific number of protons and...
Types of Radioactivity03:23

Types of Radioactivity

The most common types of radioactivity are α decay, β decay, γ decay, neutron emission, and electron capture.
Alpha (α) decay is the emission of an α particle from the nucleus. For example, polonium-210 undergoes α decay:
Isotopes and Radioisotopes01:28

Isotopes and Radioisotopes

In the early 1900s, English chemist Frederick Soddy realized that an element could have atoms with different masses that were chemically indistinguishable. These different types are called isotopes — atoms of the same element that differ in mass. Isotopes differ in mass because they have different numbers of neutrons but are chemically identical because they have the same number of protons. Soddy was awarded the Nobel Prize in Chemistry in 1921 for this discovery.
An isotope containing more...

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Related Experiment Video

Updated: Jul 12, 2026

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films
12:22

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films

Published on: November 9, 2015

Plutonium-244: confirmation as an extinct radioactivity.

E C Alexander, R S Lewis, J H Reynolds

    Science (New York, N.Y.)
    |May 21, 1971
    PubMed
    Summary

    Researchers confirmed plutonium-244

    Area of Science:

    • Cosmochemistry
    • Nuclear Astrophysics
    • Geochemistry

    Background:

    • Meteoritic xenon anomalies suggest extinct radioactivities from galactic nucleosynthesis.
    • Plutonium-244 (²⁴⁴Pu) was hypothesized as a source, but direct evidence was lacking.
    • Understanding early solar system composition requires identifying extinct radionuclides.

    Purpose of the Study:

    • To provide definitive evidence for plutonium-244 as an extinct radionuclide of galactic origin.
    • To confirm the predicted mass spectrum of xenon from ²⁴⁴Pu spontaneous fission.
    • To validate the use of ²⁴⁴Pu abundances in galactic nucleosynthesis chronology.

    Main Methods:

    • Laboratory analysis of xenon mass spectra from a plutonium-244 sample.
    • Comparison of measured xenon mass spectrum with predictions for ²⁴⁴Pu fission.

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    Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films
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  • Correlation of findings with existing meteoritic data.
  • Main Results:

    • The measured xenon mass spectrum precisely matched predictions for spontaneous fission of plutonium-244.
    • This confirms ²⁴⁴Pu as a bona fide extinct radioactivity of galactic origin.
    • Meteoritic abundances of ²⁴⁴Pu can now be reliably used for galactic chronology.

    Conclusions:

    • The discovery solidifies the role of ²⁴⁴Pu in early solar system nucleosynthesis.
    • It confirms r-process nucleosynthesis occurred during the sun's birth.
    • The search for anomalous xenon in meteorites can now be focused on other sources.