Spectral induced polarization and the hydraulic properties of New Zealand sands
Thursday, 18 December 2014: 5:15 PM
Laboratory measurements of spectral induced polarization (SIP) and permeability have been made on unconsolidated samples representative of shallow coastal aquifers in New Zealand. The samples consisted of sands sieved into different fractions ranging from a mean grain size of 1.0 mm to 0.125 mm. Although the occurrence in New Zealand natural sands of titomagnetite means that the magnitude of the SIP phase response is significantly greater than is generally found for “clean” sands, the peak in SIP phase shows a clear dependence on grain size. The SIP spectra have been represented in terms of a Cole-Cole model and the relaxation times derived from this show a strong linear correlation with the measured values of permeability. The SIP and permeability measurements are then extended to mixtures of sieved sands, sand with varying amount of clay, samples with varying amount of magnetic minerals and also natural samples from various locations in New Zealand.