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  2. Oxygen isotope ratio cycle - Wikipedia

    en.wikipedia.org/wiki/Oxygen_isotope_ratio_cycle

    Oxygen (chemical symbol O) has three naturally occurring isotopes: 16 O, 17 O, and 18 O, where the 16, 17 and 18 refer to the atomic mass.The most abundant is 16 O, with a small percentage of 18 O and an even smaller percentage of 17 O. Oxygen isotope analysis considers only the ratio of 18 O to 16 O present in a sample.

  3. Isotopes of oxygen - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_oxygen

    As some methods of isotope separation enrich not only heavier isotopes of hydrogen but also heavier isotopes of oxygen when producing heavy water, the concentration of 17 O and 18 O can be measurably higher. Furthermore, the 17 O (n,α) 14 C reaction is a

  4. δ18O - Wikipedia

    en.wikipedia.org/wiki/Δ18O

    In geochemistry, paleoclimatology and paleoceanography δ 18 O or delta-O-18 is a measure of the deviation in ratio of stable isotopes oxygen-18 (18 O) and oxygen-16 (16 O). It is commonly used as a measure of the temperature of precipitation, as a measure of groundwater/mineral interactions, and as an indicator of processes that show isotopic fractionation, like methanogenesis.

  5. Oxygen - Wikipedia

    en.wikipedia.org/wiki/Oxygen

    Paleoclimatologists measure the ratio of oxygen-18 and oxygen-16 in the shells and skeletons of marine organisms to determine the climate millions of years ago (see oxygen isotope ratio cycle). Seawater molecules that contain the lighter isotope , oxygen-16, evaporate at a slightly faster rate than water molecules containing the 12% heavier ...

  6. Category:Isotopes of oxygen - Wikipedia

    en.wikipedia.org/wiki/Category:Isotopes_of_oxygen

    Print/export Download as PDF; Printable version; In other projects ... Pages in category "Isotopes of oxygen" The following 22 pages are in this category, out of 22 ...

  7. Oxygen-18 - Wikipedia

    en.wikipedia.org/wiki/Oxygen-18

    An example of the production cycle is a 90-minute irradiation of 2 milliliters of 18 O-enriched water in a titanium cell, through a 25 μm thick window made of Havar (a cobalt alloy) foil, with a proton beam having an energy of 17.5 MeV and a beam current of 30 microamperes.

  8. Isotopic signature - Wikipedia

    en.wikipedia.org/wiki/Isotopic_signature

    Oxygen isotopic ratios, which may be measured very precisely, yield a unique and distinct signature for each Solar System body. [40] Different oxygen isotopic signatures can indicate the origin of material ejected into space. [41] The Moon's titanium isotope ratio (50 Ti/ 47 Ti) appears close to the Earth's (within 4 ppm).

  9. File:Phase diagram of solid oxygen.svg - Wikipedia

    en.wikipedia.org/wiki/File:Phase_diagram_of...

    Special pages; Printable version; Page information; ... You are free: to share – to copy ... Phase diagram of solid oxygen: Width: 630.45435: