Effects of changes in metallic mineral to time domain induced polarization (TDIP) response on physical modeling fieldscale

Induced Polarization (IP) is one of the Geophysical methods that utilize the polarization properties of the rocks. This method is widely used in metallic mineral exploration. In this method, it is known a specific method that called as Time Domain Induced Polarization (TDIP). The physical modeling of IP is used to study the behavior of TDIP response to the subsurface parameters. The fieldscale physical modeling is the development of the laboratory physical model. This modeling is realized by burying objects with a specific geometry that have contrasting physical parameter to host medium in the area that is not too extensive. Soil is used as host medium, sphere and block object which has variation in metallic mineral content as a target. The extreme targets was also made to evaluate the electrodes measurements. Data acquisitions are using the Dipole-dipole and Wenner configurations. The purpose of this study is obtaining the relations between TDIP response to changes of metallic minerals content. Res2DInv ...