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The estimation of humidity in the unsaturated zone of soils and NAPL saturation in contaminated aquifers may be based on the interpretation of electrical resistivity index logs.
Along with the characterization and interpretation of electrical properties of the established conductive antenna patterns, the performance of the printed antennas were analyzed in detail by measuring the scattering parameter S11 and the antenna gain.
In this work, these issues are theoretically investigated and their implications on the interpretation of electrical measurements on GNR-based systems are discussed.
The present study focuses on the electrical properties of active modern submarine hydrothermal deposits, in order to provide constraints on the interpretation of electrical structures obtained from marine electromagnetic surveys.
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We give new results which confirm the interpretation of an electrical equivalent network, consisting of three RC circuits in series, proposed in a previous paper: this electrical network corresponds to the junction resistance and the cell capacitance, to the extracellular matrix structure and to that of the macromolecular layer adsorbed on the luminal side of the cell.
A new approach to interpretation of shallow electrical resistivity tomography (ERT) data discussed for the case of the Olkhon area (western Baikal region) stems from tectonophysical ideas of faulting phases and deformation levels in rocks.
The interpretation of the electrical conductivity (σmix) of natural sand deposits, which contain varying amounts of fine-grained soils, is very complicated due to the presence of surface conduction.
The description above is one of the key results for the interpretation of the electrical C-AFM data.
From an analysis of the conductance spectra, we can derive same general features which can be useful for the interpretation of the electrical characterization of real GNRs.
The present study concentrates on the interpretation of Vertical Electrical Soundings (VES) and well logs to understand the geometry and the functioning of the Ghardimaou multilayered aquifer, a potential target for water supply in the Mejerda basin (Tunisia).
Conclusively, the combined interpretation of the electrical logs and the gamma log reveal that there is no clear indication of existence of any zone in this borehole favorable for hydro-fracturing neither within the Togo-sequence nor within the underlying Dahomeyan formation.
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