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Consequently, the CPD values reported in the paper could likely be erroneous.
The 22 estimated CPD values of the study area range from 11.5 to 21.9 km.
Accordingly, the estimated CPD values and ensuing geothermal gradients and heat flows by Abraham et al. ([2014]) could be erroneous.
Table 1 and Figure 6 shows the CPD values and CPD map of the study area, respectively.
Intraobserver and interobserver variability of the CPD and VI quantitation was low (r = 0.99 and 0.97, respectively, for intraobserver and interobserver variability of the CPD values).
The map in Figure 6 shows the CPD for the Ikogosi Warm Spring area, determined by applying a minimum curvature algorithm to the CPD values in Table 1.
Similar(48)
Finally, the computed and measured Cp values were compared using statistical indices, demonstrating that the CFD-designed model could accurately compute the Cp values.
The CFD-computed Cp values closely corresponded to the measured Cp values when the first cell height was 1.5 × 10−4 m.
Table 2 shows the Cp values that represent the average of at least three measurements.
Cp values versus log (number of cells) of five oral bacterial species.
Cp values (crossing point) are shown in Table 2.
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