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The effect of different evapotranspiration methods on portraying soil water dynamics and ET partitioning in a semi arid environment in Northwest China

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Academic year: 2020

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Figure

Figure 1. Schematic drawing of the large lysimeter structure.
Table 2. Soil hydraulic (Van Genuchten, 1980) and thermal (De Vries, 1963) properties including saturated (θs) and residual (θr) watercontent; curve-fitting parameters (α and n); saturated hydraulic conductivity (Ks); specific heat capacities of the water (Cw), air (Ca), quartz(Cq), clay (Cc), and organic matter (Co).
Figure 2. The seasonal variation in crop growth parameters used in the simulations: (a) leaf area index (LAI), (b) relative values of LAIcompared to the reference scenario, (c) root depth (Zr), and (d) relative values of root depth compared to the referenc
Figure 3. Comparison of observed and simulated soil volumetricwater content, at selected depths: 20, 40, 60, 80, and 100 cm, with measured precipitation and irrigation (the solid black bar with theright axis of “P + I (mm)”)
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