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The lateritic topsoil is fairly compacted with moderate resistivity values.
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The fourth layer, dominated by fine-medium grained sandstone (saturated), underlies the impervious shale unit with moderate resistivity (121 364 Ωm) values and thicknesses (5.5 12.0 m).
The inferred degree or state of leachate contamination for profiles 1 3 is presented in Tables 1 and 2. At depth of 0 3 m, profile 1 revealed extreme to moderate contamination with resistivity values of 6 36 Ω m.
Figure 2e shows contact resistivity values of each metal for different PtSe2 channel widths, where the contact resistance values were normalized to channel width for direct comparison.
Earlier electrical resistance tomography (ERT) surveys conducted on the Semlach-Eisner and Kreuztratte sites yielded resistivity values for the slag deposits that were two to three times higher than the surrounding soil (Walach, 2007).
However deeper than 5 7 m, the ERT profiles reveal several zones of moderate resistivity (around 900 Ω.m).
The n-type semiconducting behaviour dominates the resistivity values.
The more compact films exhibited lower and more stable resistivity values than the more porous ones.
When comparing the contact resistivity values of the PtSe2 TLM devices with two different contact metals, Ti and Ni, it was found that Ni forms a better electrical contact to the PtSe2 channel.
This is evident from the near smooth reflection pattern (weathered layer) and anomalous low resistivity values shown (Figs. 5, 6) whereas the other traverse set (Figs. 7, 8) displays subsurface layers with low hydraulic conductivity evident by planar reflections/moderate resistivity values (lateritic topsoil) and chaotic reflections/high resistivity values (basement).
Although both beds exhibit high resistivity, the upper bed is characterized by higher resistivity values.
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