Techniques of compartmental (efflux) and kinetic influx analyses with the radiotracer 13 NH 4 ؉ were used to examine the adaptation to hypoxia (15, 35, and 50% O 2 saturation) of root N uptake and metabolism in 3-week-old hydroponically grown rice (Oryza sativa L., cv IR72) seedlings. A time-dependence study of NH 4 ؉ influx into rice roots after onset of hypoxia (15% O 2 ) revealed an initial increase in the first 1 to 2.5 h after treatment imposition, followed by a decline to less than 50% of influx in control plants by 4 d. Efflux analyses conducted 0, 1, 3, and 5 d after the treatment confirmed this adaptation pattern of NH 4 ؉ uptake. Half-lives for NH 4 ؉ exchange with subcellular compartments, cytoplasmic NH 4 ؉ concentrations, and efflux (as percentage of influx) were unaffected by hypoxia. However, significant differences were observed in the relative amounts of N allocated to NH 4 ؉ assimilation and the vacuole versus translocation to the shoot. Kinetic experiments conducted at 100, 50, 35, and 15% O 2 saturation showed no significant change in the K m value for NH 4 ؉ uptake with varying O 2 supply. However, V max was 42% higher than controls at 50% O 2 saturation, unchanged at 35%, and 10% lower than controls at 15% O 2 . The significance of these flux adaptations is discussed.More than 70% of the worldЈs rice (Oryza sativa L.) is produced in intensively cultivated, irrigated lowland systems in Asia (International Rice Research Institute, 1997). In these systems N is generally the main factor limiting the realization of yield potentials (Kropf et al., 1993; Cassman et al., 1997). As a consequence, large amounts of mineral N fertilizers are used. According to one estimate, 7 ϫ 10 6 metric tons of N is applied each year to the 74 ϫ 10 6 ha of irrigated rice in Asia (Cassman and Pingali, 1995). However, unless the application of N fertilizer is timed precisely to match plant demand (Cassman et al., 1998), less than 50% of fertilizer N is usually recovered by the crop, because of high rates of loss through ammonia volatilization and denitrification (Craswell and Vlek, 1979; Vlek and Byrnes, 1986;Cassman et al., 1993). Clearly, the capacity of the root system to capture N in competition with these processes is critical. Mathematical modeling of the uptake process (Kirk and Solivas, 1997) shows that, under typical field conditions and following the initial flush of available N after fertilization, N absorption from the soil is rate limiting.In flooded lowland rice soils, where the bulk of the soil is hypoxic to anaerobic, the main form of plant-available N is NH 4 ϩ (Sasakawa and Yamamoto, 1978; Yu, 1985). This is in marked contrast to most (aerobic) agricultural soils, where NO 3 Ϫ is the predominant inorganic N species (Kronzucker et al., 1995b). There have been reports that NH 4 ϩ is the preferred N species taken up by rice (Bonner, 1946; Fried et al., 1965; Shen, 1969; Dijkshoorn and Ismunadji, 1972a, 1972b; Yoneyama and Kumazawa, 1974, 1975; Sasakawa and Yamamoto, 1978; Ancheng et al., ...