The DOI matches its Crossref record; 4 of the 4 references it cites were found in a registry or an index.
OXYGEN AND HYDROGEN ISOTOPES IN THE HYDROLOGIC CYCLE
Abstract
▪ Abstract Changes of the isotopic composition of water within the water cycle provide a recognizable signature, relating such water to the different phases of the cycle. The isotope fractionations that accompany the evaporation from the ocean and other surface waters and the reverse process of rain formation account for the most notable changes. As a result, meteoric waters are depleted in the heavy isotopic species of H and O relative to ocean waters, whereas waters in evaporative systems such as lakes, plants, and soilwaters are relatively enriched. During the passage through the aquifers, the isotope composition of water is essentially a conservative property at ambient temperatures, but at elevated temperatures, interaction with the rock matrix may perturb the isotope composition. These changes of the isotope composition in atmospheric waters, surface water, soil, and groundwaters, as well as in the biosphere, are applied in the characterization of hydrological system as well as indicators of paleo-climatological conditions in proxy materials in climatic archives, such as ice, lake sediments, or organic materials.
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Citations
Cites
The thermodynamic properties of isotopic substances
Urey, H. C. (1947) · Journal of the Chemical Society (Resumed) · doi:10.1039/jr9470000562 · Cited by 2,544
Standard for Reporting Concentrations of Deuterium and Oxygen-18 in Natural Waters
Craig, H. (1961) · Science · doi:10.1126/science.133.3467.1833 · Cited by 2,013
Calculation of Equilibrium Constants for Isotopic Exchange Reactions
Bigeleisen, J., & Mayer, M. G. (1947) · The Journal of Chemical Physics · doi:10.1063/1.1746492 · Cited by 1,893
Oxygen isotope enrichment of sea water by evaporation
Lloyd, R. M. (1966) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(66)90133-5 · Cited by 153
Cited by
Modification and preservation of environmental signals in speleothems
Fairchild, I. J., Smith, C. L., Baker, A., Fuller, L., Spötl, C., Mattey, D., McDermott, F., & E.I.M.F. (2006) · Earth-Science Reviews · doi:10.1016/j.earscirev.2005.08.003 · Cited by 852
Distribution of oxygen-18 and deuterium in river waters across the United States
Kendall, C., & Coplen, T. B. (2001) · Hydrological Processes · doi:10.1002/hyp.217 · Cited by 831
Lagrangian ocean analysis: Fundamentals and practices
van Sebille, E., Griffies, S. M., Abernathey, R., Adams, T. P., Berloff, P., Biastoch, A., Blanke, B., Chassignet, E. P., Cheng, Y., Cotter, C. J., et al. (2018) · Ocean Modelling · doi:10.1016/j.ocemod.2017.11.008 · Cited by 601
Fundamentals of Isotope Geochemistry
Kendall, C., & Caldwell, E. A. (1998) · Isotope Tracers in Catchment Hydrology · doi:10.1016/b978-0-444-81546-0.50009-4 · Cited by 530
The global monsoon across time scales: Mechanisms and outstanding issues
Wang, P. X., Wang, B., Cheng, H., Fasullo, J., Guo, Z., Kiefer, T., & Liu, Z. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.07.006 · Cited by 508
Metadata
- Authors
- Gat, J. R.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1996-05
- Volume
- 24
- Issue
- 1
- Pages
- 225-262
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2160156450
- Cited by
- 2,454
- References
- 4
- FWCI
- 0.72
- Type
- journal article
- Language
- en
- Open access
- closed
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- Gat, J. R. (1996). OXYGEN AND HYDROGEN ISOTOPES IN THE HYDROLOGIC CYCLE. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.24.1.225
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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