A rapid and simple method for the determination of a ferric iron pool in the free space of roots is described. Formation of this pool depended on the source of iron in the nutrient solution. During growth in water culture at pH 5 to 6 with Fe-ethylenediaminetetraacetate, a free space pool of 500 to 1000 nanomoles Fe per gram fresh weight was formed in the roots of bean (Phaselus vullgaris L. var. Prelude), maize (Zea mays L. var. Capella), and chlorophytum (Chlorophytum comosum IThunb. Jacques). No si nt pool (less than 100 nanomoles per gram fresh weight) was formed with ferrioxamine. Upon impending Fe deficiency, bean and chlorophytum were able to mobilize this pool. Fe-deficient bean plants mobilized iron from the free space iron pool of another plant in the same vessel.Iron uptake by plants is fastest when iron is present in the ferrous form (10). In anaerobic soils, high concentrations of ferrous ions may lead to iron toxicity by excessive iron uptake. Plants may limit iron uptake under those conditions by oxidation of ferrous ions with oxygen which is transported from the shoot via aerenchyma (12). Iron in aerobic soils is mainly present as the ferric ion in precipitates (14) or in soluble chelates (22). Dicotyledonous plants may enhance their capacity for iron uptake in response to a developing deficiency, by increasing their ability to reduce ferric chelates at the root surface (10). The uptake of iron by roots is therefore a result of several processes which may occur simultaneously: (a) reduction of ferric chelates in the rhizosphere by excreted reducing compounds (20) Crude Cell Wall Preparations. Root systems were washed in 0.5 mM CaSO4 for 10 to 15 min, frozen in liquid N2, and milled with an iron-free mortar and pestle. The resulting powder was suspended in 0.5 mM CaSO4, and the material precipitating at 500g was collected. This washing procedure was repeated at least three times, after which the final precipitate was suspended in 0.5 mM CaSO4, 10 mM Mes (pH 5.5).Determination of Apoplasmic Iron. A plant was transferred from nutrient solution to a beaker with 0.5 mm CaSO4 under vigorous aeration. After 10 to 15 min, the plant was placed with its root system in a wide 40-ml tube with 21 ml 10 mm Mes, 0.5 mM Ca(NO3)2, 1.5 mM 2,2'-bipyridyl (pH 5.5) at 25°C. Nitrogen was bubbled through the solution and the tube was covered with a cotton plug to prevent entry of oxygen by turbulence. After 5 min under N2, 1 ml 250 mm Na2S204 was added from a syringe.The A520 of the solution (A520 of 1 mM Fe[bipyridyl]3 = 8.650) was followed on 2-ml samples. The first sample was taken just before addition ofdithionite. The reaction was stopped, routinely after 10 min, by transferring the plant to a beaker with 0.5 L vigorously aerated 0.5 mM CaSO4. The plant could then be used for other determinations, or be put back on nutrient solution for further culture.Reducible iron in crude cell wall preparations was determined in the same way as described for intact roots, but samples taken from the incubation suspens...