Emanuel Mazor's Global Water Dynamics: Shallow and Deep Groundwater, PDF

By Emanuel Mazor

ISBN-10: 0824753224

ISBN-13: 9780824753221

Acknowledging in his preface that hydrology has been nearly taken over by way of mathematical modeling, Mazor (emeritus, Weizmann Institute of technological know-how, Rehovot, Israel) however makes the case for box observations and measurements. Filling this article with a number of case examples, he discusses observation-based examine methods to the research of the dynamic habit of world water structures and the underlying variables affecting international water stability and provide, specifically the administration of fossil groundwaters. assurance comprises groundwater exploitation and upkeep, petroleum genesis and exploration, thermal water sport and effort creation, and nuclear waste repositories. The solutions to routines are behind the publication.

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Extra info for Global Water Dynamics: Shallow and Deep Groundwater, Petroleum Hydrology, Hydrothermal Fluids, and

Example text

The DD values of formation waters indicate these are meteoric waters, formed on exposed continents. Observation: The isotopic composition of the hydrogen of formation waters is light; the yD values are in the range of À160% to À20%. , continental, groundwater (Figs. 14). This implies that by and large formation waters were formed on paleocontinents during repeated stages of sea regressions. The continental groundwater was preserved within the host rocks that were covered by the alternating sea transgressions, which laid down new shallow marine sediments that confined the underlying rock strata (Fig.

3. 4. 5. Chloride contained in concentrations that are significantly below saturation with regard to halite, indicating that it originates from outside the rock system. All the ions that are correlated with the Cl concentration are external as well. Seawater ion/Cl ratios indicate an origin from airborne sea spray. The external ions occur in the same relative abundances, irrespective of the nature of the host rocks. The external ions are washed in by the recharge water. Internal sources of ions, introduced by water–rock interactions.

2 Underground Flow Patterns The following observations can best be made in regions that are not disturbed by human activity: Aerated and saturated zones and the water table. Observation: In all wells there is an upper part empty of water, and beneath which there is water. Conclusion and nomenclature: There is a zone at which the voids between the soil and rock fragments contain air—the aerated zone; and beneath it there is a zone at which the voids of the rocks are filled with water—the saturated zone.

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Global Water Dynamics: Shallow and Deep Groundwater, Petroleum Hydrology, Hydrothermal Fluids, and by Emanuel Mazor

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