“…In sharp contrast to most agricultural soils, where nitrate (NO $ − ) is the predominant N species (Kronzucker et al, 1998), hypoxic conditions in the paddy environment largely preclude the microbial formation of NO $ − through nitrification (Bouldin, 1986 ;Arth et al, 1998) and, consequently, ammonium (NH % + ) is the main form of N available to rice in the field (Shen, 1969 ;Wang et al, 1993 ;Arth et al, 1998 ;Kronzucker et al, 1998). It is therefore not surprising that NH % + nutrition, as opposed to NO $ − nutrition, has received almost exclusive attention in rice (Bonner, 1946 ;Fried et al, 1965 ;Shen, 1969 ;Wang et al, 1993). However, some reports have indicated that rice does possess some capacity for root NO $ − absorption (Ismunadji & Dijkshoorn, 1971 ;Sasakawa & Yamamoto, 1978 ;Youngdahl et al, 1982 ;Raman et al, 1995) and for the reduction of NO $ − in leaves (Tang & Wu, 1957).…”