The dependence of Ca uptake and translocation by intact roots of Phaseolus vulgaris on concurrent root metabolism was investigated using 'Ca-labeled Hoagland solutions at one-half and one-twentieth strength (2.5 and 0.25 mM Ca'). Adsorbed and absorbed "5Ca fractions in the roots were distinguished on the basis of the time course of exchange with the outer solution. Uptake of '2K, of which the characteristics are better known, was measured for comparison. The absorbed 'Ca fraction showed a markedly nonlinear increase with time in contrast to the near linear increase in 'K. Exposure of roots to cyanide, arsenate, 2,4-dinitrophenol, or low temperatures caused only slight reductions in '5Ca absorption by roots, but significant reductions of 'K. In all treatments involving inhibitors and low temperatures, the translocation to shoots of both 'Ca and 'K was strongly inhibited. The conclusion that much of the absorbed "Ca fraction in the root tissue is taken up by processes which are not rate-limited by metabolism is discussed.The convention of dividing cations bound by roots into two fractions, adsorbed and absorbed, on the basis of the time course of uptake and exchange has proved convenient for the monovalent cations (4,9,24). The adsorbed fraction characteristically reaches equilibrium with the bathing solution within minutes and is independent of metabolic processes. This process is considered to represent a simple nonspecific ion exchange within cell wall surfaces. The absorbed fraction is characterized by a slower rate of increase which continues for many hours. It is not readily exchangeable with the outer solution and is dependent on concurrent metabolism. The absorbed fraction may represent a net increase in ion content of the tissue or, for roots which have reached dynamic equilibrium with the outer solution, may represent tracer influx. It is implicit that the absorbed ions are retained within protoplasts, although precise localization of the two fractions has rarely been attempted.The characterization of uptake and retention of Ca and other divalent cations has shown less uniformity than that for the monovalent cations. Although some studies have indicated a constant rate of absorption of Ca (9,14,19,25) Measurements of uptake of Ca and other divalent cations by plant tissues is often complicated by the relatively large fraction held on adsorption-exchange sites in cell walls (5,8,9,36). In experiments with labeled ions the usual procedure for displaying this has been to immerse the root tissue at the end of a 'Ca uptake period in an excess of unlabeled solution for 30 min to remove the fraction designated as adsorbed; the amount retained by the root has been considered metabolically absorbed by the root cells (8, 9). For the sake of comparing the present results with previous studies the above terminology and methods have been retained.In this paper we present observations on the uptake of 45Ca by intact bean plants under conditions similar to those used to display, by microautoradiography, the lo...