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Geochimica et Cosmochimica Acta, 1951
Abstract Natural silicates vary in their O18/O16ratios by as much as 2–4%. This difference is largely due to an exchange reaction between silica and water during the processes of erosion and sedimentation, as a result of which sedimentary rocks are richer in O18 than are the igneous rocks. The temperature coefficient for the silica-water exchange has
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Abstract Natural silicates vary in their O18/O16ratios by as much as 2–4%. This difference is largely due to an exchange reaction between silica and water during the processes of erosion and sedimentation, as a result of which sedimentary rocks are richer in O18 than are the igneous rocks. The temperature coefficient for the silica-water exchange has
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2019
The 'detective' power of stable isotopes for processes that occurred in the past, and for elucidating mechanisms at the molecular level, has impressed researchers over the past 100 years, since the time when isotopes of elements were first discovered.
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The 'detective' power of stable isotopes for processes that occurred in the past, and for elucidating mechanisms at the molecular level, has impressed researchers over the past 100 years, since the time when isotopes of elements were first discovered.
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Source partitioning using phosphate oxygen isotopes and multiple models in a large catchment
Water Research, 2023Ziteng Wang
exaly
Trivalent chromium isotopes in the eastern tropical North Pacific oxygen-deficient zone
Proceedings of the National Academy of Sciences of the United States of America, 2021Tianyi Huang, Edward A Boyle
exaly
Bacterial Fractionation of Oxygen Isotopes
Journal of the American Chemical Society, 1947M, DOLE, R C, HAWKINGS, H A, BARKER
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