ra·di·um /ˈrediəm/
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ra·di·um /ˈredɪəm/ 名詞
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Ra·di·um n. Chem. An intensely radioactive metallic element found (combined) in minute quantities in pitchblende, and various other uranium minerals. Symbol, Ra; atomic weight, 226.4. Radium was discovered by M. and Mme. Curie, of Paris, who in 1902 separated compounds of it by a tedious process from pitchblende. Its compounds color flames carmine and give a characteristic spectrum. It is divalent, resembling barium chemically. The main isotope of radium found in pitchblende, radium-226, has a half-life of 1620 years, decaying first by alpha emission to radon.
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See also mesothorium.
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radium
n : an intensely radioactive metallic element that occurs in
minute amounts in uranium ores [syn: Ra, atomic number
88]
radium
Symbol: Ra
Atomic number: 88
Atomic weight: (226)
Radioactive metallic transuranic element, belongs to group 2 of the
periodic table. Most stable isotope, Ra-226 has a half-life of 1602 years,
which decays into radon. Isolated from pitchblende in 1898 Marie and
Pierre Curie.