Maize kernel moisture, carbon and nitrogen concentrations from silking to physiological maturity

Grain characteristics prior to physiological maturity are important for silage harvest and for grain harvest when grain fill has been prematurely terminated by factors such as hail or early frost. The objective of this study was to investigate changes in grain moisture, C and N concentrations associated with the progression of milk line from silking to physiological maturity for hybrids with maturity ratings between 76 and 95 Minnesota relative maturity days. A field experiment with a total of 15 hybrids was carried out on a well-drained sandy loam soil at Ottawa, Canada, from 1995 to 1997, inclusive. A large number of uniform plants with the same phenology were marked in each plot near tasseling, and ears were sampled from these plants at weekly intervals from R1 to final harvest. It was noted that 50% milk line was associated with a range of kernel moisture concentrations: in 1995, a relatively warm year, kernel moisture was 389 g kg(-1) when 50% milk line occurred; in 1996, a relatively cool year, kernel moisture was over 420 g kg(-1) at 50% milk line. During the course of grain fill, C concentrations remained relatively constant whereas N concentrations were dramatically reduced from as high as 50 g kg(-1) to approximately 15 g kg(-1). Maximum dry matter accumulation was reached at 325 g kg(-1) moisture. In general, later-maturing hybrids appeared to have longer duration from silking to 50% milk line; however, they took less time to reach physiological maturity (faster grain fill and dry down). Although benchmarks of 50% milk line and 0% milk line are commonly used for silage and grain production, there is a range of grain moisture-milk line relationships among genotypes and under different environmental conditions during grain fill.