Abstract

In wheat, genotypic variability in grain protein content may be affected not only by physiological traits but also by N supply in the soil. The relative importance of these factors was studied for two years, in field experiments with eleven recent spring wheat genotypes and four N regimes. Genotypic differences in grain N content were found only at low early N supply. The extent of genotypic variability in grain N content was generally more strongly related to N uptake than to N translocation. This was ascribed to the high nitrogen harvest index (NHI) of 0.80 to 0.86. Under high early N supply, genotypic variation in N uptake decreased between anthesis and maturity, resulting in non-significant differences in N uptake and, concomitantly, in grain N content at maturity. This feature, also reflected in a negative correlation between pre- and post-floral N uptake, suggests an effect of N supply. Mineral N content in the soil to a depth of 100 cm showed that at flowering and without N application at heading, the soil contained between 22 and 33 kg mineral N per ha. Under each N regime, nitrogen from current N mineralization or from deeper soil layers contributed to post-floral N uptake. It was concluded that the extent of genotypic variation in N uptake and grain N content may be severely restricted by spatial and temporal availability of nitrogen.

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