Osmotic Adjustment in Sorghum: II. Relationship to Gas Exchange Rates.

Lowering of the solute potential by osmotic adjustment (OA) has been proposed to allow maintenance of leaf turgor potential (Psi(p)), stomatal conductance (g), and photosynthesis (A) at low leaf water potential. However, literature concerning the role of OA in the maintenance of g and A under water stress is limited and often contradictory. The objective of this experiment was to examine the association of OA with g and A in grain sorghum (Sorghum bicolor L. Moench). A single sorghum hybrid (cv ATx623 x RTx430) was studied under field conditions using four different water supplies. Diurnal and midday water potential, solute potential, Psi(p), OA, g, and A were measured during preflowering and grain-filling growth stages. A second experiment was conducted under greenhouse conditions. Two sorghum genotypes (BTx623 and BTx378) differing in their g and A responses to plant water stress were compared for their OA capacity during a water deficit cycle imposed from the beginning of panicle initiation through flowering. Under both field and greenhouse conditions, g and A rapidly declined with increased water stress despite the occurrence of OA. Under greenhouse conditions, BTx623 maintained significantly higher g and A than BTx378 during the water stress cycle. However, no significant differences in OA or Psi(p) existed between the two genotypes, indicating that OA was not associated with differences observed in g and A between these genotypes. We conclude that the response of g and A to water stress was not directly associated with OA and certainly was not maintained by OA.