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Hydrogen and Oxygen Isotopic Composition of Groundwater in Volcanic Regions
2012Groundwaters of modern volcanic regions are of interest to specialists as are the deep groundwaters of sedimentary basins, using isotope techniques in their studies, in order to elucidate the problems of their formation and solve a number of applied problems of interest concerning their utilization.
V. I. Ferronsky, V. A. Polyakov
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Oxygen and Hydrogen Isotope Measurements in Plant Cellulose Analysis
1989Isotopes are atoms containing the same number of protons but a different number of neutrons in their nucleus. Most of us are familiar with unstable isotopes (e.g., Carbon-14) which decay to another element (e.g., Carbon-14 decays to Nitrogen-14).
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Oxygen and Hydrogen Isotope Ratios in Sedimentary Rocks and Minerals
1967O18/O16 and D/H measurements were made on a variety of sedimentary rocks and minerals, with special emphasis on the fine-grained, predominantly clay mineral fraction of the sediments. The interlayer water was removed from clay minerals prior to the isotopic analyses.
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Stable Oxygen and Hydrogen Isotopes in Precipitation
2005L.L. Gourcy, M. Groening, P.K. Aggarwal
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Fractionation of the isotopes of hydrogen and of oxygen in a commercial electrolyzer
Journal of Research of the National Bureau of Standards, 1934E.W. Washburn, E.R. Smith, F.A. Smith
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Introduction to Isotope Hydrology. Stable and Radioactive Isotopes of Hydrogen, Oxygen and Carbon
2005The application of natural isotopes, stable as well as radioactive, has become a widespread tool for hydrological research, especially surface- and groundwater behaviour and exploration. By far the most common isotopes applied are those of the elements of hydrogen, oxygen and carbon, crucial in the water cycle.
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