Several species of grasses which have different ratings for seedling vigor were examined for rapidity of germination, seedling growth rates in the dark, and the ultimate length of dark grown seedlings. These are attributes which could be of importance in seedling vigor during the early, nonphotosynthetic stage of seedling growth.Extreme rapidity of germination largely accounts for the high seedling vigor of Schismus arabicus. In three species and strains of Phalaris, there were indications that rapidity of germination and mean seedling growth rates paralleled their rating for seedling vigor. No relation appeared to exist between total seedling length adjusted to a common seed weight and rating for seedling vigor.
Seed germination is regulated by multiple environmental cues and understanding their relationships is critical to planning seed drilling and subsequent seedling management. We develop a new framework by viewing the metabolic reactions associated with seed germination as a moving event in a physiological dimension to simulate seed germination. Fluctuations in environmental cues and genetic heterogeneity of seed lot make the metabolic reactions in each seed uncertain, and we use an average germination rate to describe the average metabolic reactions and a dispersion coefficient to describe the genetic heterogeneity. We apply the model to winter wheat seeds drilled at different dates in plots under different soil water contents and prove that the model accurately reproduces the time course of germination in all treatments. We found the average germination rate increases nonlinearly with temperature in the base-suboptimal temperature range, and there is an optimal soil water content where the germination rate peaks due to soil anaerobicity. Our model can be fitted to field data using temperature and soil water content to describe the trade-off impact of soil water on soil anaerobicity and imbibition, whereas the difficulty of obtaining accurate water potential and oxygen measurements makes this difficult with the hydrothermal time models.
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