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Most of these have half-lives that are less than five minutes, except 94 Ru (half-life: 51.8 minutes), 95 Ru (half-life: 1.643 hours), and 105 Ru (half-life: 4.44 hours). The primary decay mode before the most abundant isotope, 102 Ru, is electron capture and the primary mode after is beta emission .
Ruthenium is a chemical element; it has symbol Ru and atomic number 44. It is a rare transition metal belonging to the platinum group of the periodic table . Like the other metals of the platinum group, ruthenium is unreactive to most chemicals.
English: A diagram showing the isotope signatures of natural ruthenium and fission product ruthenium from U-235 which had been subjected to thermal neutrons. Note that the Mo-100 (a long lived double beta emitter) has not had time to decay to Ru-100 over the time since the reactors stopped working.
Printable version; In other projects Wikidata item; Appearance. move to sidebar hide. Help Pages in category "Isotopes of ruthenium" ... Ruthenium-125 This page was ...
This page uses the meta infobox {{Infobox isotopes (meta)}} for the element isotopes infobox.. This infobox contains the table of § Main isotopes, and the § Standard atomic weight.
The ruthenium in PUREX raffinate can become oxidized to form volatile ruthenium tetroxide which forms a purple vapour above the surface of the aqueous liquor. The ruthenium tetroxide is very similar to osmium tetroxide; the ruthenium compound is a stronger oxidant which enables it to form deposits by reacting with other substances. In this way ...
Printable version; In other projects ... 1.6 einsteinium-248: 27 1.6 ... 10 6 seconds ruthenium-106: 1.023 32.3 neptunium-235: 1.0845
Isotope geochemistry is an aspect of geology based upon the study of natural variations in the relative abundances of isotopes of various elements.Variations in isotopic abundance are measured by isotope-ratio mass spectrometry, and can reveal information about the ages and origins of rock, air or water bodies, or processes of mixing between them.