Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan

<div>Optimal estimated heterogeneous <i>α</i> field in the real aquifer (50th observation well used for the inverse model). (a) Optimal estimated heterogeneous <i>α</i> field; (b) uncertainty of <i>α</i> estimation.</div>

Geofluids

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Figure 12

Figure 12: Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan 

Figure 12 | Hydraulic Tomography for Estimating the Diffusivity of Heterogeneous Aquifers Based on Groundwater Response to Tidal Fluctuation in an Artificial Island in Taiwan 