“…As the soils dried down during water stress (Figure 1), soil water potential decreased from approximately À 0.01 to À 0.6 MPa (moderate drought stress) and root and leaf water potentials further decreased from approximately À 0.4 to À 1.2 and approximately À 1.0 to À 1.6 MPa, respectively, in maize seedlings (Adeoye and Rawlins, 1981). Under field conditions, leaf water potentials in the range of À 0.5 to À 2.5 MPa are commonly seen for crop species (Cary and Wright, 1971). Leaf water potential can change significantly during the day, with maximum values in the morning and minimum values during the afternoon (Cary and Wright, 1971;Acevedo et al, 1979).…”