Osmotic adjustment, defined as a lowering of osmotic potential (*In) due to net solute accumulation in response to water stress, has been considered to be a beneficial drought tolerance mechanism in some crop species. The objective of this experiment was to determine the relative contribution of passive versus active mechanisms involved in diurnal 'II changes Loss of water from turgid leaf tissue in response to transpiration results in not only a significant decline in 'I',' but also a decline in 'In, to a lesser extent. As the leaf tissue 'I,, declines even more in response to soil water deficits, 'I' declines accordingly as reported in a large number of crop species (2,(13)(14)(15)(16)19). A decline in measured 'I' can result from a simple passive concentration of solutes due to dehydration or due to net solute accumulation. The lowering of 'n by net solute accumulation is termed OA. OA has been considered a beneficial drought tolerance mechanism in some 'Abbreviations: I', water potential (MPa); 'n, osmotic potential (MPa); Ip, turgor potential (MPa); In°"°, 'n at full hydration (MPa); RWC, relative water content (%); OA, osmotic adjustment (MPa); E, modulus of elasticity (MPa); TW, turgid weight (g); DW, dry weight (g); WC, water content (g).field crop species (6,9,20,22). Processes such as cell expansion are dependent on the influx of water driven by the maintenance of lower T' by net solute increase in the expanding cell. The lowering of Tr, by OA also minimizes the opportunity for significant water loss to occur from leaftissue.Passive concentration of solutes due to dehydration can arise from a decrease in WC per unit DW, reduced leaf tissue volume due to cellular shrinkage, change in leaf tissue elasticity, or relative partitioning of water between the symplastic and apoplastic fractions.