Short-and long-term responses of inorganic N pools and plant-atmosphere NH 3 exchange to changes in external N supply were investigated in 11-week-old plants of two grass species, Lolium perenne and Bromus erectus, characteristic of N-rich and N-poor grassland ecosystems, respectively. A switch of root N source from NO 3 Ϫ to NH 4 ϩ caused within 3 h a 3-to 6-fold increase in leaf apoplastic NH 4 ϩ concentration and a simultaneous decrease in apoplastic pH of about 0.4 pH units in both species. The concentration of total extractable leaf tissue NH 4 ϩ also increased two to three times within 3 h after the switch. Removal of exogenous NH 4 ϩ caused the apoplastic NH 4 ϩ concentration to decline back to the original level within 24 h, whereas the leaf tissue NH 4 ϩ concentration decreased more slowly and did not reach the original level in 48 h. After growing for 5 weeks with a steady-state supply of NO 3 Ϫ or NH 4 ϩ , L. perenne were in all cases larger, contained more N, and utilized the absorbed N more efficiently for growth than B. erectus, whereas the two species behaved oppositely with respect to tissue concentrations of NO 3 Ϫ , NH 4 ϩ , and total N. Ammonia compensation points were higher for B. erectus than for L. perenne and were in both species higher for NH 4 ϩ -than for NO 3 Ϫ -grown plants. Steady-state levels of apoplastic NH 4 ϩ , tissue NH 4 ϩ , and NH 3 emission were significantly correlated. It is concluded that leaf apoplastic NH 4 ϩ is a highly dynamic pool, closely reflecting changes in the external N supply. This rapid response may constitute a signaling system coordinating leaf N metabolism with the actual N uptake by the roots and the external N availability.Grasses growing in terrestrial ecosystems receive the major part of their N as NH 4 ϩ derived from mineralization of soil organic matter (Whitehead, 1995). However, some nitrification occurs even in grassland soils and may lead to significant supply of nitrate to the roots (Hatch et al., 2000). Once in the root, nitrate can be stored, assimilated, or transported to the shoot. Ammonium absorbed by the roots has previously been assumed to be almost completely assimilated in the roots, but recent studies have shown that significant amounts of NH 4 ϩ can be transported in the xylem (Mattsson and Schjoerring, 1996; Finnemann and Schjoerring, 1999) and that plants can contain substantial concentrations of NH 4 ϩ in their tissues (Wang et al., 1993;Kronzucker et al., 1995). These NH 4 ϩ pools in leaf tissue and apoplast are important for regulating N utilization, including the exchange of gaseous NH 3 between plant leaves and the atmosphere.Because plants can act as both a source of and a sink for atmospheric NH 3 , it is important to know the physiological mechanisms that are involved in determining their NH 3 compensation point, i.e. the NH 3 concentration in the air within the sub-stomatal cavities at which no net exchange with the atmosphere takes place (Farquhar et al., 1980). The NH 3 compensation point varies with the level of N nutr...