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Extensive experimentation shows a very small scatter of the estimated conductivity values.
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Open image in new window Fig. 4 Correlations of the estimated conductivity with the measured values.
Estimated hydraulic conductivity values were employed in determining the aquifer transmissivity which ranged from 11.28 to 812.00 m2/day, fractional porosities ranged from 0.0351 to 0.0598.
For both BC, the estimated conductivities converge to the true values with grid refinement, and the solution is accurate and stable when a sufficient number of the observation data is used.
Given error-free measurements, the estimated conductivities and specific storages are accurate within 10% of the true values.
These diffusivity values were used to estimate hydraulic conductivity values of around 4.0 294 × 104 m/day although they may be lower if the aquifer thickness is greater than the estimated 10 m.
The results exhibit good agreement between the simulated and estimated riverbed hydraulic conductivity values.
TDS refers to the total dissolved solids present in the water and is estimated empirically from electrical conductivity values.
Based on these thermal conductivity values, we also estimated the grain boundary conductance, 14.43±1.21×1010Wm−2K−1, and the thermal conductivity for single crystal tBLG, 1510±103Wm−1K−1.
These uncertainties are taken into account in a simulation model with the aim to estimate the distribution of thermal conductivity values at different scales.
They observed that deviation of experimental values from estimated values of thermal conductivity of Al2O3/water nanofluids is considerably high but the experimental values of Al2O3/EG nanofluids are nearly similar to those of the model calculation as seen in Figure 13.
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