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. 2015 May 29;6:370. doi: 10.3389/fpls.2015.00370

Figure 8.

Figure 8

Sums of the standard uptake fraction over soil depth increments of 0.25 cm for (A) the NoSplit root system at t = 32 days solved for different parameterizations of radial and axial root hydraulic conductivities and (B) for the reference parameterization of root hydraulic conductivities for the three different plant architectures. The observed variability for the two split setups was less than shown in subplot (A) and is shown in Supplementary Figure 2.