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  • 1
    Online Resource
    Online Resource
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Keywords: Hydrogeology. ; Hydrology. ; Coasts. ; Geochemistry. ; Geophysics. ; Israel ; Grundwasser ; Grundwasserleiter ; Hydrogeochemie ; Hydrogeologie
    Description / Table of Contents: Introduction Hydrogeology of Israel -- The mountain carbonate aquifers of Israel -- The coastal aquifers of Israel, including seawater intrusion and SGD -- The vast regional desert Nubian Sandstone aquifer -- The hydrogeological system of the Dead Sea Rift base level -- Recharge processes in the desert and Mediterranean environments -- Groundwater contamination and environmental aspects -- Dating of different groundwater bodies -- Monitoring of groundwater level and salinity changes, related to tides, exploitation and earthquakes -- Paleohydrology of Israel -- Engineering and infrastructural aspects related to groundwater processes (watering, subsidence, sinkholes) -- Hydrogeophysics (borehole logging, TDEM, TEM) -- Ancient groundwater exploitation systems discovered in archaeological sites -- Groundwater resources management. .
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XI, 511 p. 262 illus., 203 illus. in color.)
    Edition: 1st ed. 2021.
    ISBN: 9783030511487
    Series Statement: Springer Hydrogeology
    Language: English
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Hydrology-Israel. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (504 pages)
    Edition: 1st ed.
    ISBN: 9783030511487
    Series Statement: Springer Hydrogeology Series
    DDC: 333.910095694
    Language: English
    Note: Intro -- Acknowledgements -- Contents -- About the Editors -- Introduction -- 1 Climate -- 2 Groundwater Base Levels -- 3 Groundwater Resources -- 4 Salinization and Pollution of the Groundwater System -- References -- The Yarkon-Taninim Basin-An Example of a Major Carbonate Aquifers in Israel -- 1 Background and Purpose of the Article -- 1.1 The Jurassic Arad Group Aquifer -- 1.2 The Eocene Avedat Group Aquifer or Aquitard -- 1.3 The Judea Group Carbonate Aquifer -- 2 Hydrogeology of the Yarkon-Taninim Basin -- 3 Management Issues and Policy -- References -- The Coastal Aquifers of Israel -- Introduction to Studies of Coastal Aquifers of Israel -- General Information and Hydrogeology of the Mediterranean and Dead Sea Coastal Aquifers and Their Relation with Their Base Level -- 1 General Background -- 2 The Israeli Mediterranean Coastal Aquifer -- 3 The Dead Sea Coastal Aquifer -- 4 Seawater Intrusion Monitoring -- References -- Dynamic Relationship Between the Sea and the Aquifer -- 1 Mediterranean Coastal Aquifer -- 2 DS Coastal Aquifer -- 2.1 Current Hydraulic Connection Between the DS and Groundwater -- 3 Past and Future -- 4 The Groundwater System Next to a Stratified Lake -- References -- Geochemical Aspects of Seawater Intrusion into the Mediterranean Coastal Aquifer -- 1 Introduction -- 2 Methodology -- 3 Behavior of Major Ions During Salinization and Freshening Processes -- 4 Behavior of Minor and Trace Elements During Salinization and Freshening Processes -- 5 Behavior of Nutrients During Salinization and Freshening Processes -- 6 Summary and Conclusions -- References -- Geochemical Aspects of Groundwater in the Dead Sea Coastal Aquifer -- 1 General Introduction About the Geochemistry of the Dead Sea -- 2 Groundwater Geochemistry and Flow Mechanisms -- 3 Circulation of the Dead Sea Brine in the Aquifer. , 4 14C Evolution and Tritium in the Dead Sea Groundwater -- 5 Oxidation of Organic Matter in the Dead Sea Coastal Aquifer -- 6 The Thermal Brines (Ein Qedem Brine) -- References -- Submarine Groundwater Discharge Along the Israeli Eastern Mediterranean Coast and in Inland Basins -- 1 Submarine Groundwater Discharge (SGD)-General Background -- 2 Methodology -- 3 The Role of SGD in Oceanic Mass Balances and Water Quality -- 4 SGD Along the Israeli Coast -- 5 SGD in Dor Bay -- 6 SGD in the Mediterranean -- 7 SGD in Inland Basins -- 8 Remaining Questions -- References -- The Nubian Sandstone Aquifer in the Sinai Peninsula and the Negev Desert -- 1 Preface -- 2 The Study of the Nubian Sandstone Aquifers of North Africa -- 3 The Study of the Nubian Sandstone Aquifer of the Sinai-Negev Basin -- 3.1 Hydrogeological Background -- 3.2 Evolution of Studies of the NSA -- 4 Epilogue -- References -- The Eastern Dead Sea Rift Continental Groundwater Base Level -- 1 General -- 2 The Hydrogeology of Different Segments of the DSR Base Level -- 2.1 The Hula Basin Segment (HB on Fig. 1) -- 2.2 The Sea of Galilee-Lower Jordan Valley Segment -- 2.3 The Arava Valley Segment (AR on Fig. 1) -- 2.4 The Dead Sea Segment -- References -- Paleohydrogeology of Israel -- 1 Introduction -- 2 The Paleohydrogeology of Israel Prior to, and During Neogene Times -- 3 The Paleo-Eastern Mediterranean Sea Base Level -- 4 The Paleo-Eastern DSR Base Level -- 5 Paleo-Salinity, Salinization, and Interface Configuration -- 5.1 The Eastern Mediterranean Base Level -- 5.2 The Eastern DSR Base Level -- 6 Paleo-Groundwater Divide Locations, and Flow Gradients -- 7 The Hydrological Connection Between the Western and Eastern Base Levels -- 8 Paleo-Natural Recharge -- 9 The Paleo-Nubian Sandstone Groundwater System -- References -- Unsaturated-Zone Hydrology in Israel: A Subjective Review. , 1 Introduction -- 2 Recent History of the UZH in Israel -- 3 Organization of the Review -- 4 Groundwater Recharge and Flow in the Unsaturated Zone -- 4.1 Steady-State Annual Recharge Estimates Using Deep Unsaturated-Zone Data -- 4.2 Unsaturated Flow Models, Transient Recharge Estimates and Annual Averages -- 4.3 Recharge Under Ponding Conditions -- 4.4 Matrix Flow Versus Flow Along Preferential Paths in the Unsaturated Zone of the Coastal Aquifer -- 4.5 Unsaturated Zone Flow in Rocky Vadose Zone -- 5 UZH and the Investigation of Aquifer Salinization -- 6 UZH and the Investigation of Aquifer Contamination with Nitrate -- 6.1 UZH Nitrate-Leaching Studies Based on Deep Sampling -- 6.2 UZH Nitrate-Leaching Studies Based on Vadose-Zone Monitoring Systems (VMS) -- 7 UZH and the Investigation of Organic-Compounds Contamination -- 8 Unsaturated-Zone Geochemistry -- 9 Concluding Remarks -- References -- Dating of Groundwater in Israeli Aquifers and Determination of Groundwater Flow Velocities -- 1 Introduction -- 2 The Dating Tools -- 3 Dating of Fresh Groundwater -- 3.1 Radiocarbon and Tritium -- 3.2 Noble Gases -- 3.3 Radon -- 3.4 Artificial Tracers -- 3.5 CFCs and SF6 -- 3.6 Depleted 18O -- 3.7 Uranium Isotopes -- 4 Dating of Saline Groundwater and Brines-Determination of Rate of Seawater Intrusion -- 4.1 General -- 4.2 Radiocarbon and Tritium -- 4.3 Noble Gases -- 4.4 Radium and Radon -- 4.5 Artificial Tracers -- References -- Engineering and Infrastructural Aspects, Related to Groundwater Regime and Processes -- Soil Aquifer Treatment System Performance: Israel's Shafdan Reclamation System as an Ultimate Case Study -- 1 Introduction -- 2 The Shafdan Plant Main Components -- 3 Hydrogeological Setting and the Related SAT System Structure -- 4 Hydrological Management of the SAT System -- 4.1 Goals and Constrains. , 4.2 Means and Principles for the Shafdan Plant Hydrological Management -- 4.3 Water Balance and Groundwater Levels -- 4.4 Regions of High Hydrological Sensitivity and Relating Production Priorities -- 4.5 Recharged Effluent Migration in the Aquifer -- 4.6 Numerical Modeling as a Management Tool -- 5 Water Quality Performance of the Shafdan SAT System -- 5.1 Overview -- 5.2 Retention Time, Regulation and Water Quality -- 5.3 Suitability of the Shafdan Reclaimed Effluent for Unlimited Irrigation -- References -- Hydrological and Geological Controls on the Evolution of the Dead Sea Sinkholes -- 1 Introduction -- 1.1 Background -- 1.2 Geological and Hydrological Background of the Dead Sea Region -- 2 The Dead Sea Sinkholes-Mechanism of Formation -- 3 Controls on Rates of Sinkholes Propagation Along the Dead Sea Coast -- 3.1 Control of Sediments Properties and Thickness on Final Sinkhole Occurrence and Technics of Precursors for Sinkhole Collapses -- 3.2 Controls on Dissolution Rates of the Salt Layer Along the Dead Sea Coast-Precipitation in the Judea Mountains (JM) Versus DS Level Drop -- 3.3 Acceleration of Salt Layer Dissolution and Sinkhole Appearance in Stream Tributaries by Penetration of Floodwater Through Existing Sinkholes -- 4 Summary -- References -- Geoelectric, Geoelectromagnetic and Combined Geophysical Methods in Groundwater Exploration in Israel -- 1 Introduction -- 2 Methods -- 2.1 The DC Resistivity Soundings -- 2.2 The Electrical Resistance Tomography (ERT) -- 2.3 The Time Domain Electromagnetic (TDEM) Method -- 2.4 The Surface Nuclear Magnetic Resonance (SNMR) Method -- 3 Geoelectric Characterization of Groundwater Salinity in Clastic Coastal Aquifers -- 3.1 The Mediterranean Coastal Aquifer -- 3.2 The Gulf of Eilat (Aqaba) Coastal Aquifer. , 4 Geoelectric Characterization of Groundwater Salinity Along and Close to the Dead Sea Rift (DSR) -- 4.1 The Sea of Galilee -- 4.2 The Dead Sea Coast -- 4.3 Geophysical Delineation of Sinkhole Development in the Dead Sea Coastal Plain -- 5 Integrated Geophysical Surveys in the Mediterranean and Dead Sea Coastal Aquifers -- 5.1 SNMR-TDEM -- 5.2 Reflection Seismics-TDEM -- 6 TDEM Characterization of Groundwater Salinity in Deep Carbonate Aquifers -- 6.1 Mount Carmel-Central Coastal Plain Area -- 6.2 Mediterranean Sea-Northern DSR Traverse -- 6.3 Mediterranean-Dead Sea Traverse -- 6.4 Dead Sea-Gulf of Eilat Traverse -- 7 Evaluating Porosity/Storativity of Saline Ground Water-Saturated Aquifers Using TDEM Method -- 7.1 General -- 7.2 Porosity Calculations -- References -- Numerical Modeling of Groundwater in Israel -- 1 Introduction -- 2 Survey of Models -- 3 Regional Aquifers Management -- 4 Groundwater Salinization -- 4.1 Sharp Interface Models -- 4.2 Models Taking into Account Transport -- 5 Contaminant Fate and Transport -- 6 Vadoze Zone -- 7 Summary and Conclusions -- References -- Hydrogeology in Archeological Perspective: What Did People in Ancient Times Know About Hydrogeology? -- 1 Introduction -- 2 The Coastal Plain -- 2.1 The Hydrogeology of the Coastal Aquifer -- 2.2 Submerged Neolithic Settlements off the Carmel Coast -- 2.3 The Submerged Pottery Neolithic Wells -- 2.4 Coastal Wells from the Historical Periods -- 2.5 The Mawasi Agriculture in Coastal Areas -- 3 The Inland Zone -- 3.1 Spring Flow Tunnels of the Iron Age II -- 3.2 Inland Wells -- 4 The Southern Part of Israel-The Negev Wells -- 4.1 Abu Hof Site (Fig. 1) (Between Kibutz Lahav and Lehavim) -- 4.2 Tel Beer Sheba (Fig. 1) -- 4.3 Tel Arad (Fig. 1) -- 4.4 Water Wells in the Negev During the Roman and Byzantine Periods -- 5 Qanats in the Jordan and Arava Valleys -- 6 Discussion. , 7 Summary.
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  • 3
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Water table. ; Electronic books.
    Description / Table of Contents: This book deals with the role of changing groundwater base level on the adjacent hydrological systems. It summarizes, compiles and compares results of current and paleo base levels, using examples from all over the world.
    Type of Medium: Online Resource
    Pages: 1 online resource (175 pages)
    Edition: 1st ed.
    ISBN: 9783642139444
    DDC: 551.492
    Language: English
    Note: Intro -- Groundwater Base Level Changes and Adjoining Hydrological Systems -- Acknowledgements -- Contents -- Chapter 1 Introduction -- References -- Chapter 2 The Main Types of Groundwater Base-Level -- Chapter 3 Factors Controlling Base-Level Elevation Changes -- 3.1 General -- 3.2 Global, Regional and Local Climate Changes -- 3.3 Tectonic Movements -- 3.4 Isostatic and Glacio-Isostatic Movements -- 3.5 Land Subsidence Through Compaction and Dewatering -- 3.6 Groundwater Cones of Depression Caused by Natural Processes of Evapotranspiration -- 3.7 Groundwater Cones of Depression Caused by Groundwater Exploitation -- References -- Chapter 4 Methods and Techniques to Define Base-Level Elevation and to Measure and Assess the Effect of Their Variation on Adjoining Groundwater Systems -- 4.1 Base-Level Elevation -- 4.1.1 Current Ground Level Measurements -- 4.1.1.1 Precise Geodetic Leveling -- 4.1.1.2 The GPS Technique -- 4.1.1.3 The INSAR Technique -- 4.1.2 Current Sea and Lake Level Measurements -- 4.1.3 Paleo- and Historic Shorelines -- 4.1.3.1 Near-Shore Marine Terraces -- 4.1.3.2 Karstification and Cave Formation -- 4.1.3.3 Erosional and Other Geomorphological Evidence -- 4.1.3.4 Sedimentological Indicators -- 4.1.3.5 Submerged Archaeological Sites -- 4.2 Methods to Determine Groundwater Systems´ Response to Base-Level Changes -- 4.2.1 Current Field Measurement -- 4.2.2 Indirect Estimation -- 4.2.3 Hydrological Simulations -- References -- Chapter 5 Capturing of Groundwater Basins and Shifts of Divides -- 5.1 General -- 5.2 Climate Changes -- 5.3 Tectonically Induced Elevation Changes of Base-Levels -- 5.4 Karst Systems -- 5.5 Stream Piracy by Groundwater Sapping -- 5.6 Groundwater Exploitation -- References -- Chapter 6 Salinity, Salination and Freshening of the Different Base-Levels and Their Adjoining Groundwater Sytems -- 6.1 General. , 6.2 The Global Marine Base-Level -- 6.2.1 Base-Level Salinity -- 6.2.2 Adjoining Groundwater Systems Salinity -- 6.3 Continental Endorheic Base-Levels Distant from the Sea -- 6.3.1 Base-Level Salinity -- 6.3.2 Adjoining Groundwater Systems Salinity -- 6.4 Flow-Through, Intermediate, Base-Levels -- 6.4.1 Base-Level Salinity -- 6.4.2 Adjoining Groundwater Systems Salinity -- 6.5 Salinity of Endorheic Base-Levels Below Sea Level, Close to the Sea -- 6.6 Freshening of Coastal Aquifers -- References -- Chapter 7 Paleo, Current and Future Marine Base-Levels -- 7.1 General -- 7.2 The Neogene Marine Mediterranean Base-Level -- 7.3 The Black Sea Neogene to Holocene Base-Levels -- 7.4 Quaternary and Holocene Marine Base-Levels -- 7.5 Current and Future Marine Base-Levels -- References -- Chapter 8 Characteristics of Current Continental Endorheic Base-Levels -- References -- Chapter 9 Current Continental Base-Levels Above Sea Level -- 9.1 General -- 9.2 Lake Chad Basin -- 9.3 The Great Salt Lake Basin -- 9.4 The Andean Altiplano Basin -- 9.5 The Aral Sea Basin -- 9.6 The Mono Lake Basin, California -- 9.7 The Main Ethiopian Rift Basin -- References -- Chapter 10 Current Continental Base-Levels Below Sea Level and Distant from the Sea -- 10.1 General -- 10.2 The Great Artesian Basin and Lake Eyre Basin, Australia -- 10.3 The Death Valley Basin -- 10.4 Central Asia Closed Endorheic Basins -- 10.5 The Caspian Sea-Kara Bogaz Gol Basin -- References -- Chapter 11 Current Continental Base-Levels Below Sea Level, Located Close to the Sea -- 11.1 General -- 11.2 The Dead Sea Rift Endorheic Base-Level -- 11.2.1 General -- 11.2.2 Structure and Tectonics -- 11.2.3 The Hydrological History of the DSR Base-Level -- 11.2.4 Current Groundwater Flow Regime -- 11.2.5 Water Salinities of the DSR Base-Levels and Their Adjoining Groundwater Systems. , 11.2.6 The Response of the Groundwater System to the DSR Base-Level Changes -- 11.2.6.1 General -- 11.2.6.2 Paleo-Groundwater System -- 11.2.6.3 Current Groundwater System -- 11.2.6.4 Future Groundwater System -- 11.3 The Afar Depression-Lake Asal -- 11.4 The Qattara Depression -- 11.5 The Salton Trough Base-Level -- 11.6 The Chotts of Tunisia and Algeria -- 11.7 Sabkhat Ghuzayyil, Sirte Basin, Libya -- 11.8 Lago Enriquillo, Dominican Republic -- 11.9 The Argentine Salinas Close to the Atlantic Coast -- 11.10 Sebkha Paki Tah, Morocco -- 11.11 Salination Mechanism -- References -- Index.
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 38 (2000), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: The interface between fresh and saline ground water was studied in the Dead Sea area, using in situ profiles of electrical conductivity (EC) of water. The slope of the interface was found to be 10 times shallower than normally expected near the ocean because of the greater density contrast (the density of the Dead Sea is 1.23 g/cc). Although the Dead Sea system is extremely dynamic, the Ghyben-Herzberg approximation was still found to be relevant. The shallow interface is expected to cause Dead Sea water to intrude much farther inland than does sea water adjacent to oceans. This extremely shallow interface needs to be taken into account when exploiting ground water in this area in order to avoid upconing of brines and salinization.In recent times, the hydrologic system of the Dead Sea area has changed in water levels and salinity. Simulations using SUTRA code were run for a confined subaquifer to examine the effects of such change on the location of the fresh-saline water interface. Following the changes, the new interface is not parallel to the previous one because the increase in density causes a decrease in the interface's slope.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 374 (1995), S. 803-805 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Vegetation at the study site (Fig. 1) was sparse, and the existence of small stumps reflected unsuccessful attempts by plants to establish themselves in the area. The well established plants that were sampled in the restricted study area were individuals of Sueda fruticosa, Anabasis articulata, A ...
    Type of Medium: Electronic Resource
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