| Abstract: | A technique is described for precisely measuring the drop inwater potential,   , between the soil and the leaf xylem of wheatseedlings. The technique was used to explore the relation betweentranspiration rate and at various times during the monotonicdrying of the soil in which the plants were growing. When thesoil was wet, the relation was linear, but, as the soil dried,nonlinearities appeared which were, in the main, explicablein terms of simple soil physical models describing the flowof water through the soil to the roots. There was no sign ofthe major hydraulic resistance at the root: soil interface thatother people have recently found. |
