Abstract
Water absorption by and seedling emergence of barley (Hordeum vulgare) seeds was studied in a two layer drying out system. Seeds were placed 3 cm below surface in sandy loam (Typic Ustochrept) soil having 4 or 7g.100g−1 water underlain by wet (10g.100g−1) layer 2, 4 or 6cm below seed. The study was carried out at 18°, 23°, 28° and 33°C with and without a thin liquid-flow barrier placed on top of the wet layer.
Water absorption by seed and coefficient of rate of emergence showed parabalic relation with temperature and strong soil-water × temperature interactions. Liquid-flow barrier considerably reduced the seed water absorption, percent emergence and coefficient of rate of emergence showing thereby that liquid flow was the principal mode of upward water transport from the wet soil to the seed. Influence of both the wet soil and the liquid-flow barrier was detectable up to about 8 cm; shorter the distance greater the effect. It is concluded that in a drying out seed-zone, in addition to wetness of the soil surrounding the seed the wetness of the soil several cm below the seed is also crucial for seedling emergence. Also indicated that the optimum temperatures in drying out seed-zones are different from those in the absence of evaporation.
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Gill, K.S., Prihar, S.S. Seedling emergence at four temperatures from drying-out seed-zones underlain by wet soil. Plant Soil 112, 267–272 (1988). https://doi.org/10.1007/BF02140005
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DOI: https://doi.org/10.1007/BF02140005