Abstract:
Fifty two vertical electrical sounding (VES) data and six subsurface soil samples were collected at Ondo State Industrial
Layout, Akure, south-western Nigeria in order to determine the subsurface corrosivity. The VES results delineated 3 to 5
geoelectric layers across the area, which correspond to topsoil, weathered layer, weathered basement, weathered/fractured
basement and the presumed fresh bedrock. The layer resistivity values range from 22 to 602 ohm-m, 7 to 2468 ohm-m, 17 to
436 ohm-m, 25 to 39 ohm-m and 203 to 10023 ohm-m in the topsoil, weathered layer, weathered basement,
weathered/fractured basement and the presumed fresh bedrock respectively. The iso-resistivity maps at depth slices of 1 and
2 m show that the northeastern, southeastern and the upper central part of the area are non-corrosive (above 350 ohm-m) to
slightly corrosive (250 - 350 ohm-m), while the lower central, northwestern and southwestern parts of the area are
moderately (150 - 250 ohm-m) to strongly corrosive (60 - 150 ohm-m). Soil sample analysis shows liquid limit results that
vary from 37.6 to 59.7, while the plasticity limit results vary from 29.3 to 42.5 and all the plasticity index plots were below
the A line indicating presence of non-plastic clay. The natural moisture content values vary from 21.4 to 35.5 %. The 2 m
depth slice isoresistivity map and clay plasticity factor were synthesized using additive model to generate subsurface CR-
index corrosivity model map which indicates that the northwestern, north-eastern and southern parts of the area are
moderately (0.4 - 0.6) to strongly corrosive (0.6 - 0.8), while the upper central area and the flanks are slightly corrosive. The
moderately and strongly corrosive zones correspond to the low elevation and water logged zones of the study area. The
corrosivity model map was validated by the pH and corrosivity data.
