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Diurnal variation in settling velocity of pollen released from maize and consequences for atmospheric dispersion and cross-pollination

► Measurements show that settling velocity of maize pollen changes during the day. ► Changes are caused by drying of pollen grains and associated with atmospheric VPD. ► Simple models explore consequences for dispersion and cross-pollination. ► Results suggest that drier pollen is transported furthe...

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Published in:Agricultural and forest meteorology 2011-08, Vol.151 (8), p.1055-1065
Main Authors: Chamecki, Marcelo, Gleicher, Simone C., Dufault, Nicholas S., Isard, Scott A.
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Language:English
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description ► Measurements show that settling velocity of maize pollen changes during the day. ► Changes are caused by drying of pollen grains and associated with atmospheric VPD. ► Simple models explore consequences for dispersion and cross-pollination. ► Results suggest that drier pollen is transported further but has decreased viability. ► Current models do not account for these processes and overestimate cross-pollination. Settling velocity of maize ( Zea mays L.) pollen plays an important role in its dispersal and, therefore, cross-pollination. Estimated probability density functions (PDFs) of settling velocity based on experimental measurements show strong variation between early morning and noon. The variation is correlated to the time-integrated vapor pressure deficit (VPDT) and reflects the drying of pollen grains. A model for the decrease in germination rate of pollen grains exposed to atmospheric conditions suggests that the decrease in settling velocity is accompanied by a decrease in pollen viability. A simple dispersion model is used to illustrate the possible consequences of changes in settling velocity and germination rate for pollen dispersal and cross-pollination of maize. Results suggest that current models of pollen dispersal that do not account for these changes overestimate cross-pollination rates.
doi_str_mv 10.1016/j.agrformet.2011.03.009
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Settling velocity of maize ( Zea mays L.) pollen plays an important role in its dispersal and, therefore, cross-pollination. Estimated probability density functions (PDFs) of settling velocity based on experimental measurements show strong variation between early morning and noon. The variation is correlated to the time-integrated vapor pressure deficit (VPDT) and reflects the drying of pollen grains. A model for the decrease in germination rate of pollen grains exposed to atmospheric conditions suggests that the decrease in settling velocity is accompanied by a decrease in pollen viability. A simple dispersion model is used to illustrate the possible consequences of changes in settling velocity and germination rate for pollen dispersal and cross-pollination of maize. 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Settling velocity of maize ( Zea mays L.) pollen plays an important role in its dispersal and, therefore, cross-pollination. Estimated probability density functions (PDFs) of settling velocity based on experimental measurements show strong variation between early morning and noon. The variation is correlated to the time-integrated vapor pressure deficit (VPDT) and reflects the drying of pollen grains. A model for the decrease in germination rate of pollen grains exposed to atmospheric conditions suggests that the decrease in settling velocity is accompanied by a decrease in pollen viability. A simple dispersion model is used to illustrate the possible consequences of changes in settling velocity and germination rate for pollen dispersal and cross-pollination of maize. Results suggest that current models of pollen dispersal that do not account for these changes overestimate cross-pollination rates.</description><subject>Agricultural and forest climatology and meteorology. Irrigation. 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Settling velocity of maize ( Zea mays L.) pollen plays an important role in its dispersal and, therefore, cross-pollination. Estimated probability density functions (PDFs) of settling velocity based on experimental measurements show strong variation between early morning and noon. The variation is correlated to the time-integrated vapor pressure deficit (VPDT) and reflects the drying of pollen grains. A model for the decrease in germination rate of pollen grains exposed to atmospheric conditions suggests that the decrease in settling velocity is accompanied by a decrease in pollen viability. A simple dispersion model is used to illustrate the possible consequences of changes in settling velocity and germination rate for pollen dispersal and cross-pollination of maize. 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ispartof Agricultural and forest meteorology, 2011-08, Vol.151 (8), p.1055-1065
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1873-2240
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subjects Agricultural and forest climatology and meteorology. Irrigation. Drainage
Agronomy. Soil science and plant productions
Atmospherics
Biological and medical sciences
corn
Cross-pollination
Dispersal
Dispersions
diurnal variation
drying
Economic plant physiology
Flowering, floral biology, reproduction patterns
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Germination
Grains
Growth and development
Maize
Maize pollen
Pollen
pollen germination
probability
Probability density functions
Settling
Settling velocity
vapor pressure
Viability
Zea mays
title Diurnal variation in settling velocity of pollen released from maize and consequences for atmospheric dispersion and cross-pollination
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