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. 2020 Jun 28;126(4):789–806. doi: 10.1093/aob/mcaa120

Fig. 1.

Fig. 1.

Simulated root systems (3-D architture) from CRootBox of upland rice grown on a P-deficient soil with three P treatments in the topsoil [no P amendment (NoP), a sub-optimal rate (SubP) and a non-limiting rate (PlusP)] and two water regimes (field capacity (FC) and drying periods (DP)]. The colour of the root represents the P uptake rate of the root, while the colour on the discs represents the soil P sink. The transition between topsoil and sub-soil (at 20 cm depth) can be observed by the shift in P uptake rate in SubP and PlusP.