In this study, we quantified the spatial distributions of inorganic ions and
sugars contributing to osmotic adjustment and their net deposition rates in
the elongating and mature zones of leaf 4 of the main stem of spring wheat
(Triticum aestivum L. cv. Lona) during its linear growth
phase under saline soil conditions. Plants were grown in growth chambers in
soil irrigated/treated with nutrient solution containing either no added
or 120 mM NaCl. The sampling was conducted on the 3rd day after emergence of
leaf 4 at 3 and 13 h into the 16 h photoperiod. The patterns of spatial
distributions of total osmoticum, cation, anion and sugar contents (mmol
kg-1 H2O) were distinct and were
affected by salinity. The total osmoticum content in the region between 0 and
60 mm above the leaf base differed between the two harvests at 120 mM NaCl.
Net deposition rates of total osmotica, cations, anions, and sugars (mmol
kg-1 H2O
h-1) in both treatments increased from the base of the
leaf to the most actively elongating location and then decreased near the end
of the elongation zone. Contributions of cations, anions, and sugars to
osmotic adjustment varied with distance from the leaf base, and were about
21–30, 15–21, and 13%, respectively, in the elongation
zone. We suggest that the accumulation of solutes under saline conditions
occurs both by increasing the net deposition rate of osmotica and by reducing
growth.