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Multiresponse modeling of variably saturated flow and isotope tracer transport for a hillslope experiment at the Landscape Evolution Observatory.

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Academic year: 2021

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Figure

Figure 1. Hydrological response to the tracer experiment at the LEO-1 hillslope. From top: measured rain input pulses Q r (the
Figure 2. The 3-D numerical grid for the LEO landscape. Points a, b, c, and d are the locations where samples were extracted during the experiment for subsequent laboratory analysis.
Figure 3. Sink term q and correction source term f c over depth z
Figure 4. Results for the six simulations of the integrated flow re- re-sponse analysis (see Table 2)
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