Effect of soil type on nitrogen balance at maturity in wheat characterized using N-labelled NH NO -fertilizer and sink–source modifications at flowering
Wheat plants were grown in a greenhouse in containers filled with chalky or loamy soil. Single-labelled ammonium nitrate fertilizer NH 4 15 NO 3 or 15 NH 4 NO 3 (5 atom% 15 N) was applied in a split-dose after the third leaf-stage. Initial soil nitrate levels were lower in chalky soil. At maturity,...
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Veröffentlicht in: | Functional plant biology : FPB 1998, Vol.25 (4), p.475-480 |
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Sprache: | eng |
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Zusammenfassung: | Wheat plants were grown in a greenhouse in containers filled with chalky or loamy soil. Single-labelled ammonium nitrate fertilizer NH 4 15 NO 3 or 15 NH 4 NO 3 (5 atom% 15 N) was applied in a split-dose after the third leaf-stage. Initial soil nitrate levels were lower in chalky soil. At maturity, the amount of N recovered in shoots was lower in chalky plants (CP) than in loamy plants (LP) but N fertilizer recovery was higher in CP than in LP. There was a greater 15 NO 3 recovery, in CP: 15 NO 3 / 15 NH 4 being 1 in LP and 1.3 in CP seeds. This was explained by efficient N mobilization enriched in 15 NO 3 in CP. Leaf excision or shoot shading at flowering changed the seed 15 NO 3 / 15 NH 4 ratio; it increased in CP and decreased in LP for plants with excised leaves whereas it was not modified in CP but decreased in LP for shaded plants. This indicated that grain filling was predominantly via mobilization in CP, whereas a late assimilation was involved in LP. The flag leaf in CP was the site for early and transient storage of NO 3 - and later a main source of assimilated N for seeds. Benefits previously observed in vegetative wheat plants grown on chalky soils compared to loamy soils with respect to enhanced NO 3 utilisation, are also manifest at grain-filling and maturity. Keywords: Triticum aestivum L, chalky soil, loamy soil, ammonium nitrate, 15 N seed filling, sink– source modifications. Australian Journal of Plant Physiology 25(4) 475 - 480 Full text doi:10.1071/PP97044 © CSIRO 1998 |
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ISSN: | 1445-4416 |
DOI: | 10.1071/PP97044 |