Table 1.
List of surface-based geophysical methods commonly used in fractured rock. The extent and depth of the survey region and the resolution are all approximate ranges. The measured parameters can be derived directly from the acquired data. The recovered properties are obtained through processing and/or inversion of the acquired data.
| Method | Lateral Extent of Survey Region (meters) | Depth of Survey Region (meters) | Resolution (meters) | Measured Parameters | Recovered Properties of Interest | Potential Fractured Rock Targets |
|---|---|---|---|---|---|---|
| Electrical Resistivity | 1 to 100 | 1 to 100 | 0.5 to 10 | Electrical potential from applied current | DC electrical conductivity | Fracture zones, Amendment monitoring |
| Ground Penetrating Radar | 1 to 1000 | 1 to 50 | 0.1 to 10 | Amplitude and arrival time of reflected EM energy | Dielectric constant at frequencies of 1MHz to 1GHz | Major fractures, fracture zones, transport in fractures |
| Electro-magnetic induction | 1 to 10000 | 1 to 100 | 0.5 to 10 | Induced magnetic fields due to sub-surface conductors | Electrical conductivity | Contaminant plume delineation |
| Very low frequency EM | 1 to 10000 | 5 to 75 | 1 to 10 | Secondary fields from navigational signals | Electrical conductivity | Faults, fracture zones |
| Magnetometry | 1 to 10000 | 1 to 100 | 0.5 to 10 | Magnitude and/or gradient of Earth’s magnetic field | Magnetization, magnetic susceptibility | Treatment monitoring (metals) |
| Seismic Reflection/Refraction | 1 to 1000 | 1 to 500 | 1 to 10 | Amplitude and arrival time of reflected elastic energy | Elastic wave velocities, attenuation | Depth of weathered zone, major fractures |
| Induced Polarization | 1 to 1000 | 1 to 100 | 0.5 to 10 | Decay in electrical potential following current pulse; frequency dependence of complex impedance | Imaginary part of the complex electrical conductivity at frequencies from mHz to kHz | Permeability estimation, amendment monitoring |
| Surface Nuclear Magnetic Resonance | 10 to 100 | 1 to 100 | 1 to 10 | Decay in nuclear magnetization following radiofrequency pulse | Relaxation time constant | Depth to groundwater, permeability, water content |
| Self Potential | 1 to 1000 | 1 to 100 | 0.5 to 10 | Electrical potentials arising from current sources in the earth | Electrodiffusion potential, redox potential, streaming potential | Groundwater flow directions |