GROWTH OF SUGARCANE UNDER HIGH INPUT CONDITIONS IN TROPICAL AUSTRALIA.3. ACCUMULATION, PARTITIONING AND USE OF NITROGEN

Citation
Aw. Wood et al., GROWTH OF SUGARCANE UNDER HIGH INPUT CONDITIONS IN TROPICAL AUSTRALIA.3. ACCUMULATION, PARTITIONING AND USE OF NITROGEN, Field crops research, 48(2-3), 1996, pp. 223-233
Citations number
17
Categorie Soggetti
Agriculture
Journal title
ISSN journal
03784290
Volume
48
Issue
2-3
Year of publication
1996
Pages
223 - 233
Database
ISI
SICI code
0378-4290(1996)48:2-3<223:GOSUHI>2.0.ZU;2-Q
Abstract
Leaf nitrogen (g N m(-2) leaf) is an important determinant of crop rad iation-use efficiency. It is not known to what extent sugarcane can ma intain high leaf N over its long growth duration. This study analyses the accumulation of N in two contrasting cultivars of sugarcane (Q117, Q138) under plant and ratoon crop conditions, and the partitioning of N to the various plant components, including the leaf. The crops were grown for 15 months under irrigated conditions in the same season and received 34.4 g N m(-2) as fertiliser over the first 100-120 days of the season. Higher early N accumulation by the ratoon crop was associa ted with higher early biomass production. However, maximum N accumulat ion was unrelated to maximum biomass accumulation, with the plant crop (25.9 g N m(-2)) accumulating more than the ratoon crop (21.3 g N m(- 2)), which resulted in widely varying values for biomass/N ratio. N ac cumulation ceased later in the plant (200 days) than in the ratoon (15 0 days) crop, and this occurred 100-140 days before maximum biomass. M ore work is needed to determine if this is due to exhaustion of soil N supply, reduced root activity, or a lowered crop N requirement. Leaf N was maintained above 1.2 g N m(-2) for 300 days of the 450 day seaso n. Decline in leaf N below 1.2 g N m(-2) at the end of the season was associated with loss in leaf and total crop N accumulation, and appare ntly unrelated to the timing of cessation in biomass accumulation. Thr oughout the season, leaf N was higher in the plant than the ratoon cro p (averaged over cultivars), and Q117 versus Q138 (averaged over crop classes), however these differences could not explain crop-class diffe rences in RUE. Cultivar differences in leaf N were due to higher N acc umulation because specific leaf area and partitioning of biomass and N to leaf were unaffected by crop class or cultivar. The biomass/N rati o varied with cultivar and crop class, and increased with crop age.