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Salt tolerance in Aster tripolium L. III. Na and K fluxes in intact seedlings
Author(s) -
SHENNAN C.
Publication year - 1987
Publication title -
plant, cell and environment
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.646
H-Index - 200
eISSN - 1365-3040
pISSN - 0140-7791
DOI - 10.1111/j.1365-3040.1987.tb02082.x
Subject(s) - salinity , shoot , chemistry , sodium , advanced spaceborne thermal emission and reflection radiometer , halophyte , horticulture , botany , osmotic pressure , zoology , biology , ecology , biochemistry , geology , remote sensing , organic chemistry , digital elevation model
Uptake and transport of Na and K was studied using the radioactive tracers 22 Na and 42 K in intact Aster tripolium L. seedlings grown at two salinities CS 10 and CS 100, (containing 10mol m −1 and 100 mol m −3 Na, respectively, together with other major ions in the proportions found in sea water). At both salinities a much greater proportion of the Na than K taken up by the plant was subsequently transported to the shoot. Most 42 K fluxes were reduced by about 40% in CS 100 plants relative to CS 10 except root accumulation which increased. Experiments involving changing the salinity from CS 10 to CS 100 showed that 42 K fluxes remained constant for at least 40 h, indicating that competition with Na for uptake sites was not the cause of the reduced flux in CS 100 plants. 22 Na fluxes responded immediately to a change in salinity with all fluxes increasing six‐fold when the salinity was raised. When the salinity was lowered, however, root accumulation returned to the level in CS 10 control plants whereas transport to the shoot was inhibited by the previous high salinity treatment, being reduced to only 35% of the rate in CS 10 plants. The time courses of osmotic adjustment and Na accumulation following an increase in salinity were found to be very similar, with sufficient Na being accumulated to account for the observed increase in sap osmotic pressure.