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  • 1
    Keywords: Hydraulic engineering ; Environmental pollution ; Sustainable development ; Hydrogeology ; Water pollution. ; Environmental sciences. ; Angewandte Hydrogeologie ; Grundwasseranreicherung ; Infiltration ; Versickerung ; Grundwasserleiter ; Methode ; Hydrogeologie ; Hydrogeochemie ; Hydrochemie
    Description / Table of Contents: Introduction to Anthropogenic Aquifer Recharge -- Hydrogeology Basics – Aquifer Types and Hydraulics -- Vadose Zone Hydrology Basics -- Groundwater Recharge and Aquifer Water Budgets -- Geochemistry and Managed Aquifer Recharge Basics -- Anthropogenic Aquifer Recharge and Water Quality -- Contaminant Attenuation and Natural Aquifer Treatment -- MAR Project Implementation -- MAR Hydrogeological and Hydrochemistry Evaluation Techniques -- Vadose Zone Testing Techniques Clogging -- Pretreatment.-ASR and Aquifer Recharge Using Wells -- Groundwater Banking -- Surface-Spreading Systems – Infiltration Basins -- Surface-Spreading Systems (Non-Basin) -- Vadose Zone Infiltration Systems -- Recharge and Recovery Treatment Systems -- Soil-Aquifer Treatment -- Riverbank Filtration -- Saline-Water Intrusion Management -- Wastewater MAR and Indirect Potable Reuse -- Low Impact Development and Rainwater Harvesting -- Unmanaged and Unintentional Recharge
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (XXV, 861 p)
    ISBN: 9783030110840
    Series Statement: Springer Hydrogeology
    Language: English
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  • 2
    Keywords: Water. ; Physical geography. ; Natural disasters.
    Description / Table of Contents: 1. Introduction to Climate Change and Groundwater -- 2. Climate and Groundwater Primer -- 3. Historical Evidence for Anthropogenic Climate Change and Climate Modeling Basics -- 4. Intergovernmental Panel on Climate Change and Global Climate Change Projections -- 5. Modeling of Climate Change and Aquifer Recharge and Water Levels -- 6. Sea Level Rise and Groundwater -- 7. Climate Change and Small Islands -- 8. Groundwater Related Impacts of Climate Change on Infrastructure -- 9. Adaptation and Resilience Concepts -- 10. Adaptation Options -- 11. Conjunctive Use -- 12. Climate Change Adaptation - Water Management Decision Making Process -- 13. Regional Hydrological Impacts to Climate Changes and Adaptation Actions and Options -- 14. Applied Climate Change Assessment and Adaptation.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XV, 350 p. 54 illus., 49 illus. in color.)
    Edition: 1st ed. 2021.
    ISBN: 9783030668136
    Series Statement: Springer Hydrogeology
    Language: English
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  • 3
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Groundwater. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (357 pages)
    Edition: 1st ed.
    ISBN: 9783030668136
    Series Statement: Springer Hydrogeology Series
    DDC: 333.9104
    Language: English
    Note: Intro -- Preface -- Contents -- About the Author -- 1 Introduction to Climate Change and Groundwater -- 1.1 Introduction -- 1.2 Climate Change and Groundwater -- 1.3 Climate Change Modeling -- 1.4 Projected Global Climate Changes -- 1.5 Climate Change and Groundwater Recharge and Use -- 1.6 Sea Level Rise and Groundwater -- 1.7 Evaluating Climate Change Impacts on Groundwater Storage -- 1.8 Adaptation Options -- 1.9 Water Planning and Governance -- 1.10 Climate Change Adaptation Planning Process -- 1.11 Case Studies of Adaptation to Climate Change in High Groundwater Use Area -- References -- 2 Climate and Groundwater Primer -- 2.1 Aquifer Water Budgets -- 2.2 Potential, Reference, and Actual Evaporation -- 2.3 Infiltration -- 2.4 Recharge -- 2.4.1 Recharge Types -- 2.4.2 Anthropogenic Aquifer Recharge -- 2.4.3 Quantification of Recharge -- 2.4.3.1 Water Fluctuation Method -- 2.4.3.2 Environmental Tracers -- 2.4.3.3 Water Budget Methods -- 2.4.3.4 Flow-Tube Method -- 2.4.4 Climate Change, Land Use Land Cover Change, and Groundwater Recharge -- 2.4.5 Effects of Temperature on Recharge -- 2.4.6 Climate Change and Recharge -- 2.5 Climate Change and Water Demand -- 2.5.1 Plant Evapotranspiration Rates and Irrigation Water Demands -- 2.5.2 Climate Change and Domestic and Industrial Water Demands -- References -- 3 Historical Evidence for Anthropogenic Climate Change and Climate Modeling Basics -- 3.1 Introduction -- 3.2 Historical Climate Trends -- 3.2.1 Temperature -- 3.2.2 Precipitation -- 3.2.3 Drought -- 3.3 Historic Sea Level Rise -- 3.4 Tropical Storm Frequency and Intensity -- 3.5 Atmospheric Carbon Dioxide Concentration -- 3.6 General Circulation Models (GCMs) -- 3.6.1 GCM History -- 3.6.2 Coupled Model Intercomparison Project -- 3.6.3 CMIP and IPCC Emissions Scenarios -- 3.6.4 Accessing GCM and RGM Results -- 3.6.4.1 Climate Wizard. , 3.6.4.2 U.S. Geological Survey Viewers -- References -- 4 Intergovernmental Panel on Climate Change and Global Climate Change Projections -- 4.1 Intergovernmental Panel on Climate Change -- 4.2 Global Climate Change Predictions -- 4.2.1 Introduction -- 4.2.2 Global Temperature Change -- 4.2.3 Precipitation -- 4.2.4 Droughts and Aridity -- 4.2.5 Snow and Glacier Dominated Water Systems -- 4.2.6 Global Sea Level Rise -- 4.2.7 Extreme Storms -- References -- 5 Modeling of Climate Change and Aquifer Recharge and Water Levels -- 5.1 Introduction -- 5.2 Modeling Approaches -- 5.3 Bias Correction -- 5.4 Downscaling -- 5.4.1 Scaling and Change Factors -- 5.4.2 Dynamical Downscaling -- 5.4.3 Statistical Downscaling -- 5.4.4 Stochastic Weather Generators -- 5.5 Hydrologic Modeling -- 5.6 Aquifer Heterogeneity and Modeling Results -- 5.7 Bottom-Up (Decision-Scaling, Sensitivity Analysis) Approach -- 5.8 Published Modeling Studies -- 5.8.1 Edwards Aquifer, Texas -- 5.8.2 Rhenish Massif, Germany -- 5.8.3 Southern High Plains, New Mexico and Texas -- 5.8.4 High Plains Aquifer, Western United States -- 5.8.5 Serral-Salinas Aquifer, Southeastern Spain -- 5.8.6 Galicia-Costa, Spain -- 5.8.7 West Bengal, India -- 5.8.8 Grand Forks, South Central British Columbia, Canada -- 5.8.9 Mediterranean Coastal Aquifers -- 5.8.10 Suwannee River Basin, Northern Florida -- 5.9 Conclusions -- References -- 6 Sea Level Rise and Groundwater -- 6.1 Introduction -- 6.2 Direct Inundation -- 6.2.1 Introduction -- 6.2.2 Future Inundation Mapping -- 6.3 Extreme Sea Level Events (Storm Surges) -- 6.3.1 Climate Change and ESLs -- 6.3.2 Historical Impacts of ESLs on Fresh Groundwater Resources -- 6.4 Saline Water Intrusion -- 6.4.1 Basics -- 6.4.2 Theoretical Modeling -- 6.4.3 Evaluation of Location of Fresh-Saline Water Interface -- 6.4.4 Saline Water Intrusion Vulnerability Assessments. , 6.4.5 Site Specific Modeling of SLR Impacts on Saline Water Intrusion -- 6.4.5.1 Monterey County, California -- 6.4.5.2 Hilton Head, South Carolina -- 6.4.5.3 Shelter Island, New York -- 6.4.5.4 Dutch Delta, The Netherlands -- 6.4.5.5 Island of Faster, Denmark -- 6.4.5.6 Borkum, German North Sea -- 6.4.5.7 Broward County, Southeastern Florida -- 6.4.5.8 Laccadive Islands, India -- 6.5 Rising Water Tables-Groundwater Inundation -- 6.5.1 Coastal Groundwater Inundation Vulnerability Mapping Methods -- 6.5.1.1 Three-Dimensional Groundwater Modeling Approach -- 6.5.1.2 Empirical Water Table Elevation Surface and Hydrostatic Rise Approach -- 6.5.1.3 Simple Hydrostatic Rise with No Hydraulic Gradient Approach -- 6.5.2 Coastal Groundwater Inundation Studies -- 6.5.2.1 Oahu, Hawaii -- 6.5.2.2 Northern California -- 6.5.2.3 Honolulu, Hawaii -- 6.5.2.4 Coastal New Hampshire -- 6.5.2.5 San Francisco Bay Area -- References -- 7 Climate Change and Small Islands -- 7.1 Introduction -- 7.2 Small Island Erosion and Inundation -- 7.3 Fresh Groundwater on Small Islands -- 7.4 Field and Modeling Studies of Freshwater Lenses and Their Vulnerability to Climate Change -- 7.4.1 Theoretical Modeling (Underwood et al. 1992) -- 7.4.2 Home Island, South Keeling Atoll, Indian Ocean -- 7.4.3 Tarawa, Republic of Kiribata -- 7.4.4 Modeling of Impacts of Storm Overwash and SLR on Pacific Atolls -- 7.4.5 Andros Island, Bahamas -- 7.4.6 Modeling of Effects of SLR on Waves and Overwash -- 7.4.7 Roi-Namur Island, Kwajalein Atoll, Republic of the Marshall Island, Overwash -- 7.4.8 Supertyphoon Haiyan, Samar Island, Philippines -- 7.4.9 Distant Source Waves -- 7.5 Small Island Climate Change Adaptation Options -- References -- 8 Groundwater Related Impacts of Climate Change on Infrastructure -- 8.1 Introduction -- 8.2 Urban Rising Groundwater Levels -- 8.3 Stormwater Management Systems. , 8.4 Centralized Sewage Systems -- 8.5 On-Site Sewage Treatment and Disposal Systems -- 8.6 Agricultural and Changing Groundwater Levels -- 8.7 Land Subsidence -- References -- 9 Adaptation and Resilience Concepts -- 9.1 Introduction -- 9.2 Vulnerability Assessments -- 9.3 Adaptation Planning Under Uncertainty -- 9.4 Adaptative Capacity -- 9.5 Effectiveness of Adaptation -- References -- 10 Adaptation Options -- 10.1 Introduction -- 10.2 Demand Management -- 10.2.1 Demand Management Basics -- 10.2.2 Irrigation Demand Management -- 10.2.3 Residential Water Demand Management -- 10.2.3.1 Economic Incentives -- 10.2.3.2 Legal Mandates -- 10.2.3.3 Consumer Education -- 10.2.4 Water Utilities Leakage and Non-revenue Water -- 10.3 Supply Augmentation -- 10.3.1 Desalination -- 10.3.2 Managed Aquifer Recharge -- 10.3.3 Wastewater Reuse -- 10.3.4 Rainwater Harvesting -- 10.3.5 Transferring Water -- 10.4 Adaptations Options for Rural Areas of Developing Countries -- 10.5 Adaptations to Saline-Water Intrusion -- References -- 11 Conjunctive Use -- 11.1 Introduction -- 11.2 Water Governance -- 11.3 Implementation of Conjunctive Use -- 11.3.1 Southern California -- 11.3.2 Arizona -- 11.3.3 Florida -- References -- 12 Groundwater Management and Adaptation Decision Making Process -- 12.1 Introduction -- 12.2 Water Supply Decision Makers -- 12.3 Water Supply Decision-Making Process -- 12.3.1 Basic Decision-Making Process -- 12.3.2 Decision Support Systems -- 12.4 General Public Engagement -- 12.5 Engagement of Decision-Makers with the Climate Change Research Community -- 12.6 Decision-Making Planning Horizon -- 12.6.1 Florida -- 12.6.2 Texas -- 12.6.3 Arizona -- 12.6.4 California -- 12.7 Summary -- References -- 13 Regional Hydrological Impacts of Climate Changes and Adaptation Actions and Options -- 13.1 Introduction -- 13.2 Southwestern North America. , 13.3 High Plains (Western United States) -- 13.4 Florida -- 13.5 Mediterranean Region -- 13.5.1 Alicante, Spain -- 13.5.2 Southern Italy -- 13.5.3 Mediterranean Coastal Aquifers -- 13.5.4 Serral-Salinas Aquifer, Southeastern Spain -- 13.5.5 Adaptation Options in the Mediterranean Region -- 13.6 Africa -- References -- 14 Applied Climate Change Assessment and Adaptation -- 14.1 Introduction -- 14.2 Prediction of Local Climate Changes -- 14.3 Prediction of Sea Level Rise Impacts -- 14.3.1 Prediction of SLR Impacts -- 14.3.2 Sea Level Rise Adaptation -- 14.4 Water Supply Adaptation Options -- 14.4.1 Water Demand Management and Reallocation -- 14.4.2 New Water Supply Options -- 14.4.3 Optimization-Conjunctive Used and Managed Aquifer Recharge -- 14.5 Decision-Making Under Climate Uncertainty -- 14.6 Prognosis and Recommendations -- References.
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  • 4
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Water conservation -- Arid regions. ; Electronic books.
    Description / Table of Contents: This book presents a comprehensive description of the hydrogeology and hydrologic processes at work in arid lands. It describes the techniques that can be used to assess and manage the water resources of these areas with an emphasis on groundwater resources.
    Type of Medium: Online Resource
    Pages: 1 online resource (1068 pages)
    Edition: 1st ed.
    ISBN: 9783642291043
    Series Statement: Environmental Science and Engineering Series
    Language: English
    Note: Intro -- Arid Lands Water Evaluationand Management -- Preface -- Acknowledgments -- Contents -- Part I Arid Regions Water Management andIssues -- Part II Arid Lands Geology and Hydrogeology:An Overview -- Part III Water Budget and Recharge -- Part IV Water Resources Assessment Methods -- Part V Water Management Techniques -- Part VI Desalination -- Part VII Wastewater Reuse in Arid Lands -- Part VIII Water Policy and Management -- Part IX Global Climate Change -- Part X Conclusions -- Curriculum Vitae -- Index.
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Sedimentology 48 (2001), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Nodular cherts can provide a window on the original sediment composition, diagenetic history and biota of their host rock because of their low susceptibility to further diagenetic alteration. The majority of Phanerozoic cherts formed by the intraformational redistribution of biogenic silica, particularly siliceous sponge spicules, radiolarian tests and diatom frustules. In the absence of a biogenic silica source, Precambrian cherts necessarily had to have had a different origin than Phanerozoic cherts. The Mesoproterozoic Belt Supergroup in Glacier National Park contains a variety of chert types, including silicified oolites and stromatolites, which have similar microtextures and paragenesis to Phanerozoic cherts, despite their different origins. Much of the silicification in the Belt Supergroup occurred after the onset of intergranular compaction, but before the main episode of dolomitization. The Belt Supergroup cherts probably had an opal-CT precursor, in the same manner as many Phanerozoic cherts. Although it is likely that Precambrian seas had higher silica concentrations than at present because of the absence of silica-secreting organisms, no evidence was observed that would suggest that high dissolved silica concentrations in the Belt sea had a significant widespread effect on silicification. The rarity of microfossils in Belt Supergroup cherts indicates that early silicification, if it occurred, was exceptional and restricted to localized environments. The similarity of microtextures in cherts of different ages is evidence that the silicification process is largely controlled by host carbonate composition and dissolved silica concentration during diagenesis, regardless of the source of silica.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2011-03-01
    Description: The Avon Park Formation (middle Eocene) in central Florida, U.S.A., contains shallow-water carbonates that have been replaced by dolomite to varying degrees, ranging from partially replaced limestones, to highly porous sucrosic dolostones, to, less commonly, low-porosity dense dolostones. The relationships between dolomitization and porosity and permeability were studied focusing on three 305-m-long cores taken in the City of Daytona Beach. Stable-isotope data from pure dolostones (mean {delta}18O = +3.91{per thousand} V-PDB) indicate dolomite precipitation in Eocene penesaline pore waters, which would be expected to have been at or above saturation with respect to calcite. Nuclear magnetic log-derived porosity and permeability data indicate that dolomitization did not materially change total porosity values at the bed and formation scale, but did result in a general increase in pore size and an associated substantial increase in permeability compared to limestone precursors. Dolomitization differentially affects the porosity and permeability of carbonate strata on the scale of individual crystals, beds, and formations. At the crystal scale, dolomitization occurs in a volume-for-volume manner in which the space occupied by the former porous calcium carbonate is replaced by a solid dolomite crystal with an associated reduction in porosity. Dolomite crystal precipitation was principally responsible for calcite dissolution both at the actual site of dolomite crystal growth and in the adjoining rock mass. Carbonate is passively scavenged from the formation, which results in no significant porosity change at the formation scale. Moldic pores after allochems formed mainly in beds that experienced high degrees of dolomitization, which demonstrates the intimate association of the dolomitization process with carbonate dissolution. The model of force of crystallization-controlled replacement provides a plausible explanation for key observations concerning the dolomitization process in the Avon Park Formation and elsewhere: (1) volume-for-volume replacement at a crystal scale, (2) coupled growth of dolomite crystals and dissolution of host calcium carbonate matrix, and (3) automorphic replacement by euhedral dolomite crystals. The force-of-crystallization model also does not require an influx of externally derived water that is undersaturated with respect to calcite to dissolve calcite, a fact that could simplify diagenetic models of porosity generation in dolostones. The later addition of external carbonate can result in a substantial reduction in porosity by the precipitation of dolomite cement, which could convert a high porosity sucrosic dolostone into a dense "Paleozoic type" dolostone.
    Print ISSN: 1527-1404
    Topics: Geosciences
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