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Duration of hypoxia (days)
Figure 6.12 Effect of hypoxia on influx of NH 4 + into rice roots. Seedlings were culti-
vated in nutrient solutions containing 100 µ MNH 4 , aerated for 3 weeks then at 15% O 2
for indicated times (Kronzucker et al ., 1998a). Reproduced by permission of the American
Society of Plant Biologists
Table 6.2 Effect of hypoxia on Michaelis-Menten parame-
ters for NH 4 + absorption by rice. Plants were grown in nutrient
solutions containing 100 µ MNH 4 , aerated for 21 days and
then exposed to hypoxia for 7 days
O 2 pressure
(% of air-saturated)
V max
( µ mol g 1 fresh wt h 1 )
K m
( µ M )
100
5.22
31.8
50
8.21
38.9
35
5.41
32.6
15
4.69
46.9
Source : Kronzucker et al . (1998a).
compounds to neutralize acidity, and the subsequent down-regulation of influx
is as a result of restrictions in ATP supply. Though they did not measure the
changes in root morphology in response to hypoxia, other work shows that
within 7 days aerenchyma formation and other changes would have occurred
(Kronzucker, unpublished). But since influx was at steady state after 4 days at
about 50% of the pre-hypoxia level this had no very dramatic effect on the
capacity for NH 4 + absorption.
Ammonium versus Nitrate Absorption
Kronzucker et al . (1999, 2000) have found that lowland rice (cv IR72) grown
hydroponically is exceptionally efficient in absorbing NO 3 , raising the possi-
bility that rice growing in flooded soil may absorb significant amounts of NO 3
formed by nitrification of NH 4 + in the rhizosphere. This is important because
(a) this NO 3 is otherwise lost through denitrification in the soil bulk (Reddy
 
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