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Groundwater Geophysics – a Tool for Hydrogeology |
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Contents |
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Authors |
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1 Petrophysical properties of permeable and lowpermeable rocks |
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1.1 Seismic velocities |
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1.1.1 Consolidated rock |
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1.1.2 Unconsolidated rock |
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1.1.3 Clay and till |
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1.2 Electrical resistivity |
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1.2.1 Archie´s law – conductive pore fluid and resistive rock matrix |
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1.2.2 Limitations of Archie´s law – conducting mineral grains |
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1.3 Electric Permittivity (Dielectricity) |
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1.4 Conclusions |
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1.5 References |
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2 Seismic methods |
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2.1 Introduction |
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2.1.1 What type of waves is applied in seismic exploration? |
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2.1.2 How can seismic waves image geological structure? |
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2.1.3 How are seismic waves generated and recorded in the field? |
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2.1.4 What kind of seismic measurements can be performed? |
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2.1.5 What kind of hydro-geologically relevant information can be obtained from seismic prospecting? |
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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? |
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2.2 Seismic refraction measurements |
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2.2.1 Targets for seismic refraction measurements |
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2.2.2 Body wave propagation in two-layer media with a plane interface |
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2.2.3 Seismic refraction in laterally heterogeneous two-layer media |
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2.2.4 Consistency criteria of seismic refraction measurements |
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2.2.5 Field layout of seismic refraction measurements |
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2.2.6 Near surface layering conditions and seismic implications |
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2.2.7 Seismic interpretation approaches for heterogeneous subsurface structures |
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2.2.8 Structural resolution of seismic refraction measurements |
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2.3 Seismic reflection imaging |
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2.3.1 Targets for seismic reflection measurements |
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2.3.2 Seismic reflection amplitudes |
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2.3.3 Concepts of seismic reflection measurements |
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2.3.4 Seismic migration |
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2.3.5 Field layout of seismic reflection measurements |
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2.3.6 Problems of near surface reflection seismics |
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2.3.7 Structural resolution of seismic reflection measurements |
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2.4 Further reading |
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2.5 References |
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3 Geoelectrical methods |
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3.1 Basic principles |
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3.2 Vertical electrical soundings (VES) |
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3.2.1 Field equipment |
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3.2.2 Field measurements |
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3.2.3 Sounding curve processing |
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3.2.4 Ambiguities of sounding curve interpretation |
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3.2.5 Geological and hydrogeological interpretation |
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3.3 Resistivity mapping |
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3.3.1 Square array configuration |
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3.3.2 Mobile electrode arrays |
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3.3.3 Mise-à-la-masse method |
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3.4 Self- potential measurements |
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3.4.1 Basic principles of streaming potential measurements |
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3.4.2 Field procedures |
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3.4.3 Data processing and interpretation |
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3.5 2D measurements |
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3.5.1 Field equipment |
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3.5.2 Field measurements |
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3.5.3 Data Processing and Interpretation |
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3.5.4 Examples |
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3.6 References |
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4 Complex Conductivity Measurements |
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4.1 Introduction |
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4.2 Complex conductivity and transfer function of waterwet rocks |
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4.3 Quantitative interpretation of Complex conductivity measurements |
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4.3.1 Low Frequency conductivity model |
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4.3.2 Complex conductivity measurements |
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4.4 Relations between complex electrical parameters and mean parameters of rock state and texture |
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4.5 The potential of complex conductivity for environmental applications |
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4.5.1 Organic and inorganic contaminants |
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4.5.2 Monitoring subsurface hydraulic and migration processes |
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4.5.3 Geohydraulic parameters |
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4.6 References |
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5 Electromagnetic methods – frequency domain |
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5.1 Airborne techniques |
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5.1.1 Introduction |
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5.1.2 Theory |
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5.1.3 Systems |
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5.1.4 Data Processing |
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5.1.5 Presentation |
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5.1.6 Discussion and Recommendations |
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5.2 Ground based techniques |
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5.2.1 Slingram and ground conductivity meters |
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5.2.2 VLF, VLF-R, and RMT |
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5.3 References |
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6 The transient electromagnetic method |
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6.1 Introduction |
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6.1.1 Historic development |
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6.1.2 Introduction |
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6.1.3 EMMA - ElectroMagnetic Model Analysis |
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6.2 Basic theory |
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6.2.1 Maxwell’s equations |
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6.2.2 Schelkunoff potentials |
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6.2.3 The transient response over a layered halfspace |
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6.2.4 The transient response for a halfspace |
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6.3 Basic principle and measuring technique |
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6.4 Current diffusion patterns |
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6.4.1 Current diffusion and sensitivity, homogeneous halfspace |
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6.4.2 Current densities, layered halfspaces |
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6.5 Data curves |
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6.5.1 Late-time apparent resistivity |
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6.6 Noise and Resolution |
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6.6.1 Natural background noise |
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6.6.2 Noise and measurements |
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6.6.3 Penetration depth |
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6.6.4 Model errors, equivalence |
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6.7 Coupling to man-made conductors |
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6.7.1 Coupling types |
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6.7.2 Handling coupled data |
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6.8 Modelling and interpretation |
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6.8.1 Modelling |
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6.8.2 The 1D model |
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6.8.3 Configurations, advantages and drawbacks |
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6.9 Airborne TEM |
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6.9.1 Historical background and present airborne TEM systems. |
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6.9.2 Special considerations for airborne measurements |
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6.10 Field example |
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6.10.1 The SkyTEM system |
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6.10.2 Inversion of SkyTEM data |
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6.10.3 Processing of SkyTEM data |
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6.10.4 The Hundslund Survey |
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6.11 References |
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7 Ground Penetrating Radar |
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7.1 Electromagnetic wave propagation |
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7.1.1 Electric permittivity and conductivity |
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7.1.2 Electromagnetic wave propagation |
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7.1.3 Reflection and refraction of plane waves |
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7.1.4 Scattering and diffraction |
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7.1.5 Horizontal and vertical resolution |
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7.1.6 Wave paths, traveltimes, and amplitudes |
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7.1.7 Estimation of exploration depth |
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7.2 Technical aspects of GPR |
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7.2.1 Overview of system components |
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7.2.2 Antennas and antenna characteristics |
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7.2.3 Electronics |
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7.2.4 Survey practice |
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7.3 Processing and interpretation of GPR data |
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7.3.1 General processing steps |
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7.3.2 Examples for GPR profiling and CMP data |
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7.4 References |
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8 Magnetic Resonance Sounding |
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8.1 Introduction |
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8.2 NMR-Principles and MRS technique |
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8.3 Survey at Waalwijk / The Netherlands |
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8.4 Survey at Nauen / Germany with 2D assessment |
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8.5 Current developments in MRS |
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8.6 References |
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9 Magnetic, geothermal, and radioactivity methods |
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9.1 Magnetic method |
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9.1.1 Basic principles |
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9.1.2 Magnetic properties of rocks. |
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9.1.3 Field equipments and procedures |
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9.1.4 Data evaluation and interpretation |
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9.2 Geothermal method |
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9.2.1 The underground temperature field |
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9.2.2 Field procedures |
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9.2.3 Interpretation of temperature data |
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9.3 Radioactivity method |
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9.4 References |
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10 Microgravimetry |
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10.1 Physical Basics |
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10.2 Gravimeters |
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10.3 Gravity surveys and data processing |
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10.3.1 Preparation and performance of field surveys |
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10.3.2 Data processing |
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10.4 Interpretation |
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10.4.1 Direct methods |
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10.4.2 Indirect methods |
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10.4.3 Density estimation |
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10.5 Time dependent surveys |
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10.6 References |
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11 Direct Push-Technologies |
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11.1 Logging tools |
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11.1.1 Geotechnical tools |
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11.1.2 Geophysical tools |
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11.1.3 Hydroprobes |
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11.1.4 Hydrogeochemical tools |
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11.1.5 Miscellaneous other tools |
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11.2 Sampling tools |
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11.2.1 Soil sampling tools |
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11.2.2 Soil gas sampling tools |
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11.2.3 Groundwater sampling tools |
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11.3 Tomographic applications |
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11.4 Permanent installations |
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11.5 Conclusions |
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11.6 References |
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12 Aquifer structures – pore aquifers |
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12.1 Pore aquifers – general |
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12.1.1 Definition |
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12.1.2 Porosity – a key parameter for hydrogeology |
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12.1.3 Physical properties of pore aquifers |
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12.1.4 Geophysical survey of pore aquifers |
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12.2 Buried valley aquifer systems |
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12.2.1 Introduction |
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12.2.2 Geological and hydrological background |
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12.2.3 Methods |
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12.2.4 Discussion and Conclusion |
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12.3 A Large-scale TEM survey of Mors, Denmark |
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12.3.1 Study area – the island of Mors |
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12.3.2 Hydrogeological mapping by the use of TEM |
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12.3.3 Data collection and processing |
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12.3.4 Results and discussions |
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12.3.5 Conclusions |
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12.4 Groundwater prospection in Central Sinai, Egypt |
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12.4.1 Introduction |
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12.4.2 Geological and hydrogeological aspects |
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12.4.3 Field work and interpretation |
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12.4.4 Groundwater occurrence |
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12.5 References |
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13 Aquifer structures: fracture zones and caves |
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13.1 Hydraulic importance of fracture zones and caves |
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13.2 Geophysical exploration of fracture zones: seismic methods |
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13.3 Geophysical exploration of faults and fracture zones: geoelectrical methods |
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13.4 Geophysical exploration of fracture zones: GPR |
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13.5 Exploration of faults and fracture zones: Geophysical passive methods (self-potential, gravity, magnetic, geothermal and radioactivity methods) |
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13.6 Geophysical exploration of caves |
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13.7 References |
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14 Groundwater quality - saltwater intrusions |
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14.1 Definition |
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14.2 Origin of saltwater intrusions |
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14.3 Electrical conductivity of saline water |
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14.4 Exploration techniques |
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14.5 Field examples |
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14.5.1 Saltwater intrusions in the North Sea region |
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14.5.2 Saline groundwater in the Red Sea Province, Sudan |
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14.6 References |
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15 Geophysical characterisation of aquifers |
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15.1 Definition of hydraulic conductivity and permeability |
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15.2 Hydraulic conductivity related to other petrophysical parameter |
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15.3 Geophysical assessment of hydraulic conductivity |
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15.3.1 Resistivity |
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15.3.2 Seismic velocities |
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15.3.3 Nuclear resonance decay times |
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15.4 Case history: Hydraulic conductivity estimation from SIP data |
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15.5 References |
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16 Groundwater protection: vulnerability of aquifers |
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16.1 General |
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16.2 Vulnerability maps |
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16.3 Electrical conductivity related to hydraulic resistance, residence time, and vulnerability |
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16.4 Vulnerability maps based on electrical conductivity |
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16.5 References |
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17 Groundwater protection: mapping of contaminations |
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17.1 The brownfields problem |
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17.2 Mapping of waste deposits |
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17.3 Mapping of abandoned industrial sites |
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17.4 Mapping of groundwater contaminations |
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17.4.1 Anorganic contaminants |
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17.4.2 Organic contaminants |
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17.5 References |
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Index |
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