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2. Behavior of nuclear fuel during a reactor accident - Wikipedia

   en.wikipedia.org/wiki/Behavior_of_nuclear_fuel...

   The uranium to zirconium for different parts of the solid differs a lot, in the brown lava a uranium rich phase with a U:Zr ratio of 19:3 to about 38:10 is found. The uranium poor phase in the brown lava has a U:Zr ratio of about 1:10. [24] It is possible from the examination of the Zr/U phases to know the thermal history of the mixture.

3. Uranium–lead dating - Wikipedia

   en.wikipedia.org/wiki/Uranium–lead_dating

   Since the exact rate at which uranium decays into lead is known, the current ratio of lead to uranium in a sample of the mineral can be used to reliably determine its age. The method relies on two separate decay chains , the uranium series from 238 U to 206 Pb, with a half-life of 4.47 billion years and the actinium series from 235 U to 207 Pb ...

4. Detrital zircon geochronology - Wikipedia

   en.wikipedia.org/wiki/Detrital_zircon_geochronology

   Zircon is a strong tool for uranium-lead age determination because of its inherent properties: [8] Zircon contains high amount of uranium for machine recognition, commonly 100–1000 ppm. [8] Zircon has a low amount of lead during crystallization, in parts per trillion. [8] Thus, lead found in zircon can be assumed as daughter nuclei from ...

5. Corium (nuclear reactor) - Wikipedia

   en.wikipedia.org/wiki/Corium_(nuclear_reactor)

   The uranium to zirconium ratio in different parts of the solid differs a lot, in the brown lava a uranium-rich phase with a U:Zr ratio of 19:3 to about 19:5 is found. The uranium-poor phase in the brown lava has a U:Zr ratio of about 1:10. [37] It is possible from the examination of the Zr/U phases to determine the thermal history of the mixture.

6. Decay chain - Wikipedia

   en.wikipedia.org/wiki/Decay_chain

   The three long-lived nuclides are uranium-238 (half-life 4.5 billion years), uranium-235 (half-life 700 million years) and thorium-232 (half-life 14 billion years). The fourth chain has no such long-lasting bottleneck nuclide near the top, so almost all of the nuclides in that chain have long since decayed down to just before the end: bismuth-209.

7. Uranium–thorium dating - Wikipedia

   en.wikipedia.org/wiki/Uranium–thorium_dating

   Uranium–thorium dating, also called thorium-230 dating, uranium-series disequilibrium dating or uranium-series dating, is a radiometric dating technique established in the 1960s which has been used since the 1970s to determine the age of calcium carbonate materials such as speleothem or coral.

8. Yttrium-90 - Wikipedia

   en.wikipedia.org/wiki/Yttrium-90

   Yttrium-90 is produced by the nuclear decay of strontium-90 which has a half-life of nearly 29 years and is a fission product of uranium used in nuclear reactors. As the strontium-90 decays, chemical high-purity separation is used to isolate the yttrium-90 before precipitation.

9. Technetium-99m - Wikipedia

   en.wikipedia.org/wiki/Technetium-99m

   The underlying principle is, under conditions of stress, diseased myocardium receives less blood flow than normal myocardium. MPI is one of several types of cardiac stress test. As a nuclear stress test, the average radiation exposure is 9.4 mSv, which when compared with a typical 2 view chest X-ray (.1 mSv) is equivalent to 94 Chest X-rays. [83]