The very significant yield increases obtained by adding NH 4 to N0 3supplying hydroponic cultures have, for unknown reaso1~s, not been duplicated in soil systems. This research was conducted tu consolidate and extend our knowledge of the effects of added NH. on plant processes, and to define the plant and culture characteristics requisi1te to optimal utilization of mixed N sources. Wheat (Triticum aestivum L. cv. Anza) and tomato (Lycopersicon esculentum Mill. cv. 6718 VF) were grown in solution cultures providing variables of N source (N0 3 , NH 4 , and NH 4 N0 3 ), culture buffering, and concentration of NH 4 and NH 3 (aq). Treatment effects on plant growth and composition were evaluated. Wheat grew best in NH 4 N0 3 culture, equally well in ]110 3 or NH 4 cultures buffered at pH 6, and poorest in unbuffered NH 4 cultures. Growth enhancement with NH 4 N0 3 was accompanied by increased N intake and synthesis of protein. Lowered yields in unbuffered NH 4 cultures were associated with H + injury to the roots and reduced intake of N and nutrient cations. Toxic effects of NH 4 pel' se occurred when culture concentrations exceeded 16 mmol L -• for nots. Severity or toxicity was associated with abnormally high root and shoot amide concentrations, and tissue levels of unassimilated NH 4 exceeding 50 mmol kg-'. In alkaline cultures, NH 3 (aq) concentrations greater than 0.028 mmol L·' for tomato and 0.15 mmol L·' for wheat reduced top growth, and destroyed the structure and functioning of roots. These detrimental effects of NH 3 (aq) were related to its concentration in the culture, not to tissue NH 4 • Y IELDS OF SEVERAL CROPS have been increased by 40 to 70% by adding NH 4 to NOrsupplying hydroponic cultures (Weissman, 1964;Cox and Reisenauer, 1973;Blacquiere et al., 1988; Herberer and Below, 1989). In contrast, enhanced NH 4 supply in greenhouse soil cultures has increased crop yield an average of only 11% (Malhi et al., 1988;Camberato and Bock, 1990;Hagin et al., 1990), and in field experiments with corn (Zea mays L.) summarized by Hoeft (1984) by a mere 7%. The reasons for this wide discrepancy in data from hydroponic and soil systems are not immediately apparent. Both N0 3 and NH 4 are readily absorbed by plants and their N utilized as a constituent of identical organic compounds. They differ in that their absorption and metabolism require different ionic equilibria in which both organic and inorganic cations and anions have a part (I