The gradient between pre‐dawn rhizoplane and bulk soil matric potentials, and its relation to the pre‐dawn root and leaf water potentials of four species

Abstract

ABSTRACTUptake of soil water by plants may result in significant gradients between bulk soil and soil in the vicinity of roots. Few experimental studies of water potential gradients in close proximity to roots, and no studies on the relationship of water potential gradients to the root and leaf water potentials, have been conducted. The occurrence and importance of pre‐dawn gradients in the soil and their relation to the pre‐dawn root and leaf water potentials were investigated with seedlings of four species. Pre‐germinated seeds were grown without watering for 7 and lid in a silt loam soil with initial soil matric potentials of ‐0.02, ‐0.1 and ‐0.22 MPa. Significant gradients, independent of the species, were observed only at pre‐dawn soil matric potentials lower than ‐0.25 MPa; the initial soil matric potentials were ‐0.1 MPa. At an initial bulk soil matric potential of ‐0.22 MPa, a steep gradient between bulk and rhizoplane soil was observed after 7 d for maize (Zea mays L. cv. Issa) and sunflower (Helianthus annuus L. cv. Nanus), in contrast to barley (Hordeum vulgare L. cv. Athos) and wheat (Triticum aestivum L. cv. Kolibri). Pre‐dawn root water potentials were usually about the same as the bulk soil matric potential and were higher than the rhizoplane soil matric potential. Pre‐dawn root and leaf water potentials tended to be much higher than rhizoplane soil matric potentials when the latter were lower than ‐0.5 MPa. It is concluded that plants tend to become equilibrated overnight with the wetter bulk soil or with wetter zones in the bulk soil. Plants can thus circumvent negative effects of localized steep pre‐dawn soil matric potential gradients. This may be of considerable importance for water uptake and growth in drying soil.