Interpretation of Environmental Isotope and Hydrochemical Data in Groundwater Hydrology
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Interpretation of Environmental Isotope and Hydrochemical Data in Groundwater Hydrology Proceedings of an Advisory Group Meeting Organized by the International Atomic Energy Agency and Held in Vienna, 27-31 Jan.75. by International Atomic Energy Agency.

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Published by s.n in S.l .
Written in English


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SeriesInternational Atomic Energy Agency. Panel proceedings series -- 76-01-27
ID Numbers
Open LibraryOL21757030M

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Interpretation of Environmental Isotope Data in Hydrology (Vienna, Austria, June ). They have not been edited formally, so that minor changes have not been cleared with the original authors. They are reproduced for informal dis-tribution as they may be helpful to hydrologists and- others interested in the application of en-File Size: 2MB.   The hydrochemistry of major ions and environmental isotope compositions (18O, 2H and tritium) of water samples have been used to investigate the characteristics of rainfalls, surface water and groundwater in the Damascus Ghotta basin. The groundwater salinity in the Damascus Ghotta basin gradually increases, as the groundwater moves from western to south-eastern and north-eastern parts Cited by: EnvironmEntal isotopEs in thE hydrological cyclE Principles and Applications Water r esources Programme ed beyond the classical applications of Isotope Hydrology and today, a growing number of other scientific disciplines, ranging from atmospheric the statistical treatment of data, should be treated in the first volume. This series of 6. Isotopes in Groundwater Hydrology Storm runoff analyses using environmental isotope and major ions. In: Interpretation of environmental isotope and hydrochemical data in groundwater hydrology. IAEA, Vienna, pp. P., Importance of infiltration from the Chimbo River in Ecuador to groundwater. In: Isotope Hydrology , Vol.

UNESCO – EOLSS SAMPLE CHAPTERS GROUNDWATER – Vol. II – Environmental Isotopes in Groundwater Studies - Pradeep K. Aggarwal, Klaus Froehlich, Kshitij M. Kulkarni ©Encyclopedia of Life Support Systems (EOLSS) Isotopic standards used for the other elements are a fossil shell, VPDB for 13C/12C, atmospheric nitrogen for 15N/14N, and a naturally occurring sulfide mineral, CDT. Wallick, EI Isotopic and chemical considerations in radiocarbon dating of groundwater within the semi-arid Tucson Basin, Arizona. In Interpretation of Environmental Isotope and Hydrochemical Data in Groundwater Hydrology. Vienna, IAEA: – Google ScholarCited by: BASIC CHEMICAL PRINCIPLES OF GROUNDWATER L. Candela Department of Geotechnical Enginnering and Geo-Sciences. Technological University of Catalonia. Spain I. Morell Department of Experimental Sciences. University Jaume I. Castellón. Spain. Keywords: groundwater, chemical behavior, pollution, sampling, data interpretation. Contents 1 File Size: KB. Assessment of groundwater–surface water interaction using long-term hydrochemical data and isotope hydrology: Headwaters of the Condamine River, Southeast Queensland, Australia Article Jul

Environmental Isotope Hydrology Environmental isotope hydrology is a relatively new field of investigation based on isotopic variations observed in natural waters. These isotopic characteristics have been established over a broad space and time scale. They cannot be controlled by man, but can be observed and interpreted to gain valuable regional. Handbook of Environmental Isotope Geochemistry, Volume 2: The Terrestrial Environment, B focuses on the processes, methodologies, principles, and approaches involved in isotope geochemistry. The selection first elaborates on mathematical models for the interpretation of environmental radioisotopes in groundwater systems; isotopes in cloud. This chapter discusses the scientific background of applications of environmental isotope techniques to groundwater hydrology. The stable isotope composition of groundwater reflects that of the precipitation in the recharge area that seeps through the soil and the unsaturated zone to reach the water by: This study establishes the surface water evaporation line in theory and numerically simulates the δ D and δ 18 O value distribution interval of the recharge source of deep groundwater in the Jiaozuo mining area. The recharge elevation is calculated based on hydrogen and oxygen isotope tracer theory. Theoretical calculation and experimental data indicate that the surface water evaporation Cited by: 4.