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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...
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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.
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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.
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The most common types of radioactivity are α decay, β decay, γ decay, neutron emission, and electron capture.
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Nuclear Fission

Many heavier elements with smaller binding energies per nucleon can decompose into more stable elements that have intermediate mass numbers and larger binding energies per nucleon—that is, mass numbers and binding energies per nucleon that are closer to the “peak” of the binding energy graph near 56. Sometimes neutrons are also produced. This decomposition of a large nucleus into smaller pieces is called fission. The breaking is rather random with the formation of a large number of different...
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The process of converting very light nuclei into heavier nuclei is also accompanied by the conversion of mass into large amounts of energy, a process called fusion. The principal source of energy in the sun is a net fusion reaction in which four hydrogen nuclei fuse and ultimately produce one helium nucleus and two positrons.
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Preparing an Isotopically Pure 229Th Ion Beam for Studies of 229mTh
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First results on 236U levels in global fallout.

A Sakaguchi1, K Kawai, P Steier

  • 1Research Institute for Radiation Biology and Medicine, Hiroshima University, Hiroshima, Japan. aya-s@llrl.ku-unet.ocn.ne.jp

The Science of the Total Environment
|May 2, 2009
PubMed
Summary
This summary is machine-generated.

Researchers estimated global fallout of Uranium-236 (236U) using soil samples. This study found approximately 900 kg of 236U fallout, aiding geo-resource and waste management research.

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Area of Science:

  • Environmental Science
  • Nuclear Chemistry
  • Geochemistry

Background:

  • Global fallout of radionuclides, including Uranium-236 (236U), impacts soil composition.
  • Understanding the distribution of 236U is crucial for environmental monitoring and resource management.

Purpose of the Study:

  • To quantify the global fallout level of 236U in soil.
  • To establish a method for estimating 236U fallout using other radionuclide ratios.

Main Methods:

  • Analysis of 12 soil cores from Japan, measuring 236U, Plutonium-239+240 (239+240Pu), and Cesium-137 (137Cs).
  • Determination of 239+240Pu and Uranium-238 (238U) concentrations via alpha-particle spectrometry.
  • Measurement of the 236U/238U ratio using accelerator mass spectrometry (AMS).

Main Results:

  • Consistent 236U/239Pu ratios ranging from 0.212 to 0.253 were observed in the soil samples.
  • The total global fallout of 236U is estimated to be approximately 900 kg.
  • The findings provide a baseline for 236U levels in fallout.

Conclusions:

  • The study successfully estimated global 236U fallout using soil measurements and radionuclide ratios.
  • This research contributes valuable data for geo-resources, waste management, and geochemistry.
  • Further research into U isotopes like 236U is encouraged.