Kansas Geological Survey, Current Research in Earth Sciences, Bulletin 247, part 1
Modeling Dielectric-constant Values of Geologic Materials: An Aid to Ground-Penetrating Radar Data Collection and Interpretation--Fig. 10A

Fig. 10A. Dry and water-saturated dielectric constant versus helium porosity. These values are based on laboratory measurements from carbonate samples collected at the Martinez, Kruger et al. (1998) study site. The TP-model results for wet and dry calcite ( = 8.5) and quartz ( = 4.5) are also shown.