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Excised roots of barley (Hordeum vulgare, var. Campana) were incubated for 24 hr in solutions containing constant total concentrations of KCl and NaCl but in which the mole fractions of K and Na were varied in replacement series. In solutions containing 1, 10, or 50 mm concentrations of K(+) plus Na(+), total cation accumulation was dependent upon the total salt concentration but was relatively independent of the mole fractions of K(+) and Na(+). These results imply that accumulation of K(+) and Na(+) was limited by a common factor. In solutions containing 0.01 mm K(+) plus Na(+) there was a strong preference for K(+) over Na(+) and the sum of K(+) and Na(+) accumulation increased with increasing K(+) concentration.In the replacement series utilizing 0.1 mm K(+) plus Na(+), K(+) accumulation reached a peak at solution concentrations of 0.04 mm K(+) and 0.06 mm Na(+). Potassium accumulation then decreased as Na(+) was further replaced by K(+) to concentrations of 0.06 mm K(+) and 0.04 mm Na(+). Potassium accumulation again increased with additional replacement of Na(+) by K(+).
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A. J. Hiatt (1969) studied this question.
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