“…The fact seems well established that the time course of cation uptake consists of at least two, easilv distinguished, time phases: 1) an initial non-metabolic process which is presumed by many to be an adsorption, adsorption-exchange, or exchange process (1, 24,26,28,30,32), and 2) a metabolic process, which is dependent on aerobic respiration and in which accumulation may proceed against a concentration gradient (2, 3,4,17,21,28,36). Phase one of the uptake, or loss, is essentially independent of temperature and aeration as shown by isotopic exchange of potassium (5); it corresponds in exchange to relative concentration of two ions as expected by the law of mass action (36); and it shows ion selectivity (13,22).…”