Hydrogeological Geophysics


Introduction

Surface and borehole geophysics methods are utilised for delineation of various phenomena including; profiling of bedrock topography and structure, mapping of the water table, fracture systems, permeability of aquifers, salt water - fresh water boundaries, groundwater contamination, perched groundwater, confining layers, and migration pathways. The primary motivation for using geophysics as a tool in resource exploration and aquifer management is to target areas for detailed investigation and/or as follow up to conventional SI techniques, for example to interpolate between boreholes.

Techniques

SURFACE geophysical methods used include; seismic refraction and reflection, ground penetrating radar, electromagnetic conductivity profiling / sounding and imaging using the new Strataghem, 2D resistivity imaging, resistivity sounding, electrokinetic sounding (EKS), microgravity, magnetics, self potential and radon prospecting. BOREHOLE geophysical methods used include; crosshole seismics, seismic tomography, and wireline logging.


Mapping fractures / sinkholes
Terrain conductivity profiling survey used to map a fault (bounded by linear conductivity highs in yellow/orange) and sinkholes shown as localised conductivity lows (in blue)


Permeability Mapping using EKS
Electrokinetic sounding (EKS) surface survey result for site in South Africa - 2 channels of electric potential data acquired using a pair of antennae and a hammer source for P-waves - calculated hydraulic conductivities / permeabilities also shown as a function of depth



Remote Sensing Page

Copyright 1995-1999 Geo-Services International (UK) Ltd



Geo-Services Home Page