Figure 8 | Scientific Reports

Figure 8

From: Fiber optics passive monitoring of groundwater temperature reveals three-dimensional structures in heterogeneous aquifers

Figure 8

Images (a–b) show the saturated hydraulic conductivity field resulting from model calibration in sections A-A’ and B-B’, whose position is indicated in image (d). Note that the color scale of the hydraulic conductivity is logarithmic and that elevations are reported in meters above the mean sea level. Image (c) shows the simulated temperature field in section A-A’ at the final simulation time step. (Figure created with FEFLOW v. 7.5, https://www.mikepoweredbydhi.com/products/feflow).

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