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Groundwater Geophysics : A Tool for Hydrogeology.
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Applied Geoscience
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ISBN
9783540884057
-- 9783540884040
Author
Kirsch, Reinhard
Title
Groundwater Geophysics : : A Tool for Hydrogeology.
2nd ed.
Description
1 online resource (564 pages)
Contents
Intro -- CONTENTS -- 1 Petrophysical properties of permeable and low-permeable rocks -- 1.1 Seismic Velocities -- 1.1.1 Consolidated rock -- 1.1.2 Unconsolidated rock -- 1.1.3 Clay and till -- 1.2 Electrical resistivity -- 1.2.1 Archie´s law - conductive pore fluid and resistive rock matrix -- 1.2.2 Limitations of Archie´s law - conducting mineral grains -- 1.3 Electric Permittivity (Dielectricity) -- 1.4 Conclusions -- 1.5 References -- 2 Seismic methods -- 2.1 Introduction -- 2.1.1 What type of waves is applied in seismic exploration? -- 2.1.2 How can seismic waves image geological structure? -- 2.1.3 How are seismic waves generated and recorded in the field? -- 2.1.4 What kind of seismic measurements can be performed? -- 2.1.5 What kind of hydro-geologically relevant information can be obtained from seismic prospecting? -- 2.1.6 What are the advantages and disadvantages of seismic measurements compared to other methods? How do seismics and other geophysical measurements complement each other? -- 2.2 Seismic refraction measurements -- 2.2.1 Targets for seismic refraction measurements -- 2.2.2 Body wave propagation in two-layer media with a plane interface -- 2.2.3 Seismic refraction in laterally heterogeneous two-layer media -- 2.2.4 Consistency criteria of seismic refraction measurements -- 2.2.5 Field layout of seismic refraction measurements -- 2.2.6 Near surface layering conditions and seismic implications -- 2.2.7 Seismic interpretation approaches for heterogeneous subsurface structures -- 2.2.8 Structural resolution of seismic refraction measurements -- 2.3 Seismic reflection imaging -- 2.3.1 Targets for seismic reflection measurements -- 2.3.2 Seismic reflection amplitudes -- 2.3.3 Concepts of seismic reflection measurements -- 2.3.4 Seismic migration -- 2.3.5 Field layout of seismic reflection measurements.
2.3.6 Problems of near surface reflection seismics -- 2.3.7 Structural resolution of seismic reflection measurements -- 2.4 Further reading -- 2.5 References -- 3 Geoelectrical methods -- 3.1 Basic principles -- 3.2 Vertical electrical soundings (VES) -- 3.2.1 Field equipment -- 3.2.2 Field measurements -- 3.2.3 Sounding curve processing -- 3.2.4 Ambiguities of sounding curve interpretation -- 3.2.5 Geological and hydrogeological interpretation -- 3.3 Resistivity mapping -- 3.3.1 Square array configuration -- 3.3.2 Mobile electrode arrays -- 3.3.3 Mise-à-la-masse method -- 3.4 Self- potential measurements -- 3.4.1 Basic principles of streaming potential measurements -- 3.4.2 Field procedures -- 3.4.3 Data processing and interpretation -- 3.5 2D measurements -- 3.5.1 Field equipment -- 3.5.2 Field measurements -- 3.5.3 Data Processing and Interpretation -- 3.5.4 Examples -- 3.6 References -- 4 Complex conductivity measurements -- 4.1 Introduction -- 4.2 Complex conductivity and transfer function of water-wet rocks -- 4.3 Quantitative interpretation of Complex conductivity measurements -- 4.3.1 Low Frequency conductivity model -- 4.3.2 Complex conductivity measurements -- 4.4 Relations between complex electrical parameters and mean parameters of rock state and texture -- 4.5 The potential of complex conductivity for environmental applications -- 4.5.1 Organic and inorganic contaminants -- 4.5.2 Monitoring subsurface hydraulic and migration processes -- 4.5.3 Geohydraulic parameters -- 4.6 References -- 5 Electromagnetic methods - frequency domain -- 5.1 Airborne techniques -- 5.1.1 Introduction -- 5.1.2 Theory -- 5.1.3 Systems -- 5.1.4 Data Processing -- 5.1.5 Presentation -- 5.1.6 Discussion and Recommendations -- 5.2 Ground based techniques -- 5.2.1 Slingram and ground conductivity meters -- 5.2.2 VLF, VLF-R, and RMT -- 5.3 References.
6 The transient electromagnetic method -- 6.1 Introduction -- 6.1.1 Historic development -- 6.1.2 Introduction -- 6.1.3 EMMA - ElectroMagnetic Model Analysis -- 6.2 Basic theory -- 6.2.1 Maxwell's equations -- 6.2.2 Schelkunoff potentials -- 6.2.3 The transient response over a layered halfspace -- 6.2.4 The transient response for a halfspace -- 6.3 Basic principle and measuring technique -- 6.4 Current diffusion patterns -- 6.4.1 Current diffusion and sensitivity, homogeneous halfspace -- 6.4.2 Current densities, layered halfspaces -- 6.5 Data curves -- 6.5.1 Late-time apparent resistivity -- 6.6 Noise and Resolution -- 6.6.1 Natural background noise -- 6.6.2 Noise and measurements -- 6.6.3 Penetration depth -- 6.6.4 Model errors, equivalence -- 6.7 Coupling to man-made conductors -- 6.7.1 Coupling types -- 6.7.2 Handling coupled data -- 6.8 Modelling and interpretation -- 6.8.1 Modelling -- 6.8.2 The 1D model -- 6.8.3 Configurations, advantages and drawbacks -- 6.9 Airborne TEM -- 6.9.1 Historical background and present airborne TEM systems -- 6.9.2 Special considerations for airborne measurements -- 6.10 Field example -- 6.10.1 The SkyTEM system -- 6.10.2 Inversion of SkyTEM data -- 6.10.3 Processing of SkyTEM data -- 6.10.4 The Hundslund Survey -- Acknowledgements -- 6.11 References -- 7 Ground penetrating radar -- 7.1 Electromagnetic wave propagation -- 7.1.1 Electric permittivity and conductivity -- 7.1.2 Electromagnetic wave propagation -- 7.1.3 Reflection and refraction of plane waves -- 7.1.4 Scattering and diffraction -- 7.1.5 Horizontal and vertical resolution -- 7.1.6 Wave paths, traveltimes, and amplitudes -- 7.1.7 Estimation of exploration depth -- 7.2 Technical aspects of GPR -- 7.2.1 Overview of system components -- 7.2.2 Antennas and antenna characteristics -- 7.2.3 Electronics -- 7.2.4 Survey practice.
7.3 Processing and interpretation of GPR data -- 7.3.1 General processing steps -- 7.3.2 Examples for GPR profiling and CMP data -- 7.4 References -- 8 Magnetic resonance sounding -- 8.1 Introduction -- 8.2 NMR-Principles and MRS technique -- 8.3 Survey at Waalwijk / The Netherlands -- 8.4 Survey at Nauen / Germany with 2D assessment -- 8.5 Current developments in MRS -- 8.6 References -- 9 Magnetic, geothermal, and radioactivity methods -- 9.1 Magnetic method -- 9.1.1 Basic principles -- 9.1.2 Magnetic properties of rocks -- 9.1.3 Field equipments and procedures -- 9.1.4 Data evaluation and interpretation -- 9.2 Geothermal method -- 9.2.1 The underground temperature field -- 9.2.2 Field procedures -- 9.2.3 Interpretation of temperature data -- 9.3 Radioactivity method -- 9.4 References -- 10 Radiomagnetotellurics -- 10.1 Introduction -- 10.2 Basic principles of the RMT - method -- 10.3 RMT Devices -- 10.4 Interpretation of RMT data -- 10.5 Case studies -- 10.5.1 Contaminated site exploration -- 10.5.2 Waste site exploration -- 10.6 References -- 11 Microgravimetry -- 11.1 Physical basics -- 11.2 Gravimeters -- 11.3 Gravity surveys and data processing -- 11.3.1 Preparation and performance of field surveys -- 11.3.2 Data processing -- 11.4 Interpretation -- 11.4.1 Direct methods -- 11.4.2 Indirect methods -- 11.4.3 Density estimation -- 11.5 Time dependent surveys -- Acknowledgement -- 11.6 References -- 12 Direct push-technologies -- 12.1 Logging tools -- 12.1.1 Geotechnical tools -- 12.1.2 Geophysical tools -- 12.1.3 Hydroprobes -- 12.1.4 Hydrogeochemical tools -- 12.1.5 Miscellaneous other tools -- 12.2 Sampling tools -- 12.2.1 Soil sampling tools -- 12.2.2 Soil gas sampling tools -- 12.2.3 Groundwater sampling tools -- 12.3 Tomographic applications -- 12.4 Permanent installations -- 12.5 Conclusions -- 12.6 References.
13 Vertical flows in groundwater monitoring wells -- 13.1 Forced convective flow -- 13.1.1 Field equipment and procedures -- 13.1.2 Data Processing and interpretation -- 13.1.3 Examples -- 13.2 Free convective flow -- 13.2.1 Classification of density driven convective transport processes -- 13.2.2 Field equipments and procedures -- 13.2.3 Data processing and interpretation -- 13.2.4 Examples -- 13.3 References -- Further readings -- 14 Aquifer structures - pore aquifers -- 14.1 Pore aquifers - general -- 14.1.1 Definition -- 14.1.2 Porosity - a key parameter for hydrogeology -- 14.1.3 Physical properties of pore aquifers -- 14.1.4 Geophysical survey of pore aquifers -- 14.2 Buried valley aquifer systems -- 14.2.1 Introduction -- 14.2.2 Geological and hydrological background -- 14.2.3 Methods -- 14.2.4 Discussion and Conclusion -- 14.3 A Large-scale TEM survey of Mors, Denmark -- 14.3.1 Study area - the island of Mors -- 14.3.2 Hydrogeological mapping by the use of TEM -- 14.3.3 Data collection and processing -- 14.3.4 Results and discussions -- 14.3.5 Conclusions -- 14.4 Groundwater prospection in Central Sinai, Egypt -- 14.4.1 Introduction -- 14.4.2 Geological and hydrogeological aspects -- 14.4.3 Field work and interpretation -- 14.4.4 Groundwater occurrence -- 14.5 References -- 15 Aquifer structures: fracture zones and caves -- 15.1 Hydraulic importance of fracture zones and caves -- 15.2 Geophysical exploration of fracture zones: seismic methods -- 15.3 Geophysical exploration of faults and fracture zones: geoelectrical methods -- 15.4 Geophysical exploration of fracture zones: GPR -- 15.5 Exploration of faults and fracture zones: Geophysical passive methods (self-potential, gravity, magnetic, geothermal and radioactivity methods) -- 15.6 Geophysical exploration of caves -- 15.7 References -- 16 Groundwater quality - saltwater intrusions.
16.1 Definition.
Subject
Geological Mapping
Geophysics
Groundwater -- Research
Hydrogeology -- Methodology
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