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. Author manuscript; available in PMC: 2018 Dec 15.
Published in final edited form as: J Environ Manage. 2017 Apr 20;204(Pt 2):709–720. doi: 10.1016/j.jenvman.2017.04.033

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