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  2. Uses of osmium isotopes - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_osmium

    Osmium (76 Os) has seven naturally occurring isotopes, five of which are stable: 187 Os, 188 Os, 189 Os, 190 Os, and (most abundant) 192 Os. The other natural isotopes, 184 Os, and 186 Os, have extremely long half-life (1.12×10 13 years and 2×10 15 years, respectively) and for practical purposes can be considered to be stable as well.

  3. Osmium - Wikipedia

    en.wikipedia.org/wiki/Osmium

    Osmium (from Ancient Greek ὀσμή (osmḗ) 'smell') is a chemical element; it has symbol Os and atomic number 76. It is a hard, brittle, bluish-white transition metal in the platinum group that is found as a trace element in alloys, mostly in platinum ores. Osmium is the densest naturally occurring element.

  4. Rhenium–osmium dating - Wikipedia

    en.wikipedia.org/wiki/Rhenium–osmium_dating

    Rhenium–osmium dating is a form of radiometric dating based on the beta decay of the isotope 187 Re to 187 Os.This normally occurs with a half-life of 41.6 × 10 9 y, [1] but studies using fully ionised 187 Re atoms have found that this can decrease to only 33 y. [2]

  5. Rhenium - Wikipedia

    en.wikipedia.org/wiki/Rhenium

    [28] [29] The beta decay of 187 Re is used for rhenium–osmium dating of ores. The available energy for this beta decay (2.6 keV) is the second lowest known among all radionuclides, only behind the decay from 115 In to excited 115 Sn* (0.147 keV). [30]

  6. Osmium compounds - Wikipedia

    en.wikipedia.org/wiki/Osmium_compounds

    Osmium tetroxide is the most notable compound of osmium, having many uses. The name "osmium" even derives from Greek " ὀσμή, osme, 'smell'" because of the smell of osmium tetroxide. [12] It also has a number of unusual properties, one being that the solid is volatile. Its volatility, along with its strong oxidizing power, is the origin of ...

  7. Category:Isotopes of osmium - Wikipedia

    en.wikipedia.org/wiki/Category:Isotopes_of_osmium

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  8. Carnian pluvial episode - Wikipedia

    en.wikipedia.org/wiki/Carnian_Pluvial_Episode

    The decline is attributed to early phases of the Wrangellia large igneous province enriching the ocean with osmium-188. Osmium-188 is preferentially sourced directly from the mantle, while osmium-187 is a radiogenic isotope supplied from eroded land. [32] [42] [43]

  9. Electrical resistivities of the elements (data page) - Wikipedia

    en.wikipedia.org/wiki/Electrical_resistivities_of...

    use 10.0 nΩm 85.3 nΩm 92.8 nΩm ... use 41.6 nΩm 187 nΩm 205 nΩm 208 nΩm 210 nΩm ... 76 Os osmium; use 81.2 nΩm CRC (10 −8 Ωm)