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OverviewThis text deals with deep groundwater in the granite and gneiss basement of the continents. It has become evident during the past years that highly mineralized water is present in an interconnected fracture network of the basement. Thus, the upper part of the crust of the continents can be viewed as an aquifer and investigated with tools common in hydrogeology. This book presents accounts on water-conducting features of crystalline rocks and summarizes the hydraulic properties of the basement. The volume includes reviews, new data and research on the often remarkable chemical composition of deep groundwater. Microbial processes in the deep basement aquifer are probably more important than previously thought. Two contributions focus on this recent extension of research of the biosphere to greater depth in the Earth. This book should be of interest to hydrologists and hydrogeologists working with water in crystalline rocks, but also to solid earth geophysicists, geochemists and petrologists with an interest in fluids in the crust. Scientists involved in nuclear waste disposal programs and geothermal energy development should also find many ideas in this volume useful. Full Product DetailsAuthor: I. Stober , Kurt BucherPublisher: Kluwer Academic Publishers Imprint: Kluwer Academic Publishers Edition: 2000 ed. Volume: 34 Dimensions: Width: 15.50cm , Height: 1.70cm , Length: 23.50cm Weight: 1.290kg ISBN: 9780792360827ISBN 10: 0792360826 Pages: 278 Publication Date: 31 December 1999 Audience: College/higher education , Professional and scholarly , Undergraduate , Postgraduate, Research & Scholarly Format: Hardback Publisher's Status: Active Availability: In Print This item will be ordered in for you from one of our suppliers. Upon receipt, we will promptly dispatch it out to you. For in store availability, please contact us. Table of Contents1. Geological and hydraulic properties of water-conducting features in crystalline rocks.- 2. Alkali feldspars as microtextural markers of fluid flow.- 3. Hydraulic Properties of the Upper Continental Crust: data from the Urach 3 geothermal well.- 4. In-situ petrohydraulic parameters from tidal and barometric analysis of fluid level variations in deep wells: Some results from KTB.- 5. The role of water-conducting features in the Swiss concept for the disposal of high-level radioactive waste.- 6. The scaling of hydraulic properties in Granitic Rocks.- 7. The Composition of Groundwater in the Continental Crystalline Crust.- 8. Evolution of fluid circulation in the Rhine graben: Constraints from the chemistry of present fluids.- 9. Occurrence and origin of Cl-rich amphibole and biotite in the Earth’s crust — implications for fluid composition and evolution.- 10. Rare earth elements and yttrium as geochemical indicators of the source of mineral and thermal waters.- 11. The hydrogen driven intra-terrestrial biosphere and its Influence on the Hydrochemical Conditions in Crystalline Bedrock Aquifers.- 12. Ancient microbial Activity in Crystalline Bedrock — Results from stable isotope analyses of fracture calcites.ReviewsAuthor InformationTab Content 6Author Website:Countries AvailableAll regions |
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