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. 2017 Sep 18;114(40):10572–10577. doi: 10.1073/pnas.1712381114

Fig. 1.

Fig. 1.

Schematic of soil water profiles along a drainage gradient, wetted from above by rain infiltration and from below by groundwater capillary rise, with a dry gap that diminishes downslope. Along this gradient, plant rooting depths vary systematically (see text). SI Appendix, Fig. S3 gives examples of published root images at different drainage positions.