Apical segments of roots of corn (Zea mays, L.) were excised and mounted in experimental salt solutions containing "RbCl and CaCl2.Xylem exudates were collected hourly beginning at the 21st hour. At the 24th hour, experimental solutions were replaced with solutions of other chlorides (nonlabeled) of Ca2' ± some monovalent cation.Following replacement of the labeled solutions, the rate of MRb+ release to the exudates from root segments declined by about the same proportional amount regardless of the initial steady-state output rate or the kinds of salts used to replace the RbCl. The content of 5*Rb+ in the roots also declined with time, but to a relatively less degree. Loss of accumulated 86Rb+ to the various external solutions following replacement was hss than 6% in 6 hours. It is concluded that movement of accumulated Rb+ to the exudate is dependent on the concentration of Rb+ in the root but is largely independent of exchange between accumulated ions and other ions in transit across the root.The release of mobile mineral elements from cells in which they had been accumulated occurs naturally, and it can also be induced under some experimental conditions (4,8,12,16,19). What is not settled, however, is whether the release to the xylem of accumulated ions in the root can be influenced by exchange with other ions in transit across the cortex to the xylem. Although some reports indicate that such exchange is minimal or nonsignificant (5, 10), others suggest that it occurs at significant rates (3, 9). Some workers assume that this exchange routinely occurs, and such an assumption prompted criticism (1) of an earlier paper (18). The present work was undertaken to determine whether such exchange does in fact occur at detectable rates in exuding roots maintained under experimental conditions similar to those described previously (18).In the present experiments, excised, mounted root segments of corn were permitted to attain steady-state exudation in a solution containing MRb+ after which the labeled salt was replaced with various nonlabeled salts. Volumes of exudate produced subsequent to the replacement of radioactive solution were influenced by the kinds of salts in the replacement solutions, but the '*Rb+ contained in those exudates would necessarily be ions which had been accumulated within the root segments prior to the solution replacement. Between the sampling times evaporation of the exudate was minimized by covering each collar with a small inverted polyethylene stopper (hollow) which was partially stuffed with a wad of Kimwipe kept wet with distilled H20.
MATERIALS AND METHODS
SeedlingsEach experimental vessel held 480 ml of solution which was constantly aerated and stirred by a stream of air bubbles rising through a glass jacket. The experimental solution was composed of 0.1 mm RbCl and 0.5 mm CaCl2, with enough added 'Rb+ to give 0.04 yCi 'Rb ,mol-1 Rb. In one case, the first experiment described below, 0.01 mm RbCl was also used. All experimental solutions were replaced once every 8 hr with fresh...