Plant roots accumulate K+ from micromolar external concentrations. How
ever, the absence of a firm determination of the trans-plasma-membrane
electrochemical gradient for K+ in these conditions has precluded an
assessment of whether K+-accumulation requires energization in additio
n to the driving force provided by the inside-negative membrane electr
ical potential (E(m)). To address this question unequivocally, we meas
ured E(m), and the cytosolic and external K+-activities in root cells
of Arabidopsis thaliana (L.) Heynh. cv. Columbia in conditions in whic
h net K+-accumulation occurs at low external K+ (10 muM). In these con
ditions, net K+-uptake was about 0.1 mumol . (g FW)-1 . h-1, E. varied
between - 153 and - 129 mV and the cytosolic K+-activity, determined
with K+-selective electrodes, was 83+/-4 mM. These values yield an out
wardly-directed driving force on K+ of at least 6.5 kJ . mol-1. Only i
f external potassium is raised to the region of 1 mM does E(m) become
sufficient to drive net K+-accumulation. It is therefore concluded tha
t at micromolar external K+-activities which prevail in most soils, K-uptake cannot be solely energized by E(m) - as exemplified by a chann
el-mediated mechanism. The nature of the energization mechanism is dis
cussed in relation to processes operating in fungal and algal cells.