User:Limulus

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Thorium

By 1946, only eight years after the discovery of nuclear fission, three fissile isotopes had been publicly identified for use as nuclear fuel:[1][2]

Th-232, U-235 and U-238 are primordial nuclides, having existed in their current form for over 4.5 billion years, predating the formation of the Earth; they were forged in the cores of dying stars through the r-process and scattered across the galaxy by supernovas.[4] Their radioactive decay produces about half of the earth's internal heat.[5]

For technical (outlined in a section below) and historical reasons, the three are each associated with different reactor types. U-235 is the world's primary nuclear fuel and is usually used in light water reactors. U-238/Pu-239 has found the most use in liquid sodium fast breeder reactors. Th-232/U-233 is best suited to molten salt reactors (MSR).[3]

Alvin M. Weinberg pioneered the use of the MSR at Oak Ridge National Laboratory. The Aircraft Reactor Experiment in 1954 and Molten-Salt Reactor Experiment from 1965 to 1969 both used liquid fluoride salts; the latter notably demonstrated the use of U-233 as a fuel source.[6] Unfortunately for MSR research, Weinberg was fired and the MSR program closed down in the early 1970s,[7] after which research stagnated in the United States.[8][9]

Sorensen-related

Thorium in India (map)

For Occurrence of thorium based on File:India-locator-map-thorium2012.svg updated with

India's thorium is mostly located in a contiguous belt of eastern coastal states as placer sands. 2016 monazite reserve estimates:[10]
  Andhra Pradesh (31%)
  Tamil Nadu (21%), and Odisha (20%)
  Kerala (16%), and West Bengal (10%)
  Jharkhand (2%)

Selected Pictures I've Taken

RFID chip
Sisyrinchium montanum

References

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