Waterlogging (agriculture)

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Crop yield (Y) and depth of water table (X in dm). At shallow depth the yield reduces. R-3VAR1.JPG
Crop yield (Y) and depth of water table (X in dm). At shallow depth the yield reduces.
Antique Dutch windmills used to pump water into the embanked river to prevent waterlogging of the lowlands (polders) behind them. KinderdijkMolens02.jpg
Antique Dutch windmills used to pump water into the embanked river to prevent waterlogging of the lowlands (polders) behind them.

Waterlogging water is the saturation of soil with water. [1] Soil may be regarded as waterlogged when it is nearly saturated with water much of the time such that its air phase is restricted and anaerobic conditions prevail. In extreme cases of prolonged waterlogging, anaerobiosis occurs, the roots of mesophytes suffer, and the subsurface reducing atmosphere leads to such processes as denitrification, methanogenesis, and the reduction of iron and manganese oxides. [2]

Contents

All plants, including crop, require air (specifically, oxygen) to respire, produce energy, and keep their cells alive. In agriculture, waterlogging typically blocks air from getting to the roots. [3] With the exception of rice (Oryza sativa), [4] [5] most crops like maize and potato, [6] [7] [8] are therefore highly intolerant to waterlogging. Plant cells use a variety of signals such the oxygen concentration, [9] plant hormones like ethylene, [10] [11] energy and sugar status [12] [13] to acclimate to waterlogging-induced oxygen deprivation. Roots can survive waterlogging by forming aerenchyma, inducing anaerobic metabolism, and changing root system architecture. [14]

In irrigated agricultural land, waterlogging is often accompanied by soil salinity as waterlogged soils prevent leaching of the salts imported by the irrigation water.

From a gardening point of view, waterlogging is the process whereby the soil hardens to the point where neither air nor water can soak through.

See also

Related Research Articles

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<span class="mw-page-title-main">Root</span> Basal organ of a vascular plant

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<span class="mw-page-title-main">Ethylene (plant hormone)</span> Alkene gas naturally regulating the plant growth

Ethylene (CH
2
=CH
2
) is an unsaturated hydrocarbon gas (alkene) acting as a naturally occurring plant hormone. It is the simplest alkene gas and is the first gas known to act as hormone. It acts at trace levels throughout the life of the plant by stimulating or regulating the ripening of fruit, the opening of flowers, the abscission (or shedding) of leaves and, in aquatic and semi-aquatic species, promoting the 'escape' from submergence by means of rapid elongation of stems or leaves. This escape response is particularly important in rice farming. Commercial fruit-ripening rooms use "catalytic generators" to make ethylene gas from a liquid supply of ethanol. Typically, a gassing level of 500 to 2,000 ppm is used, for 24 to 48 hours. Care must be taken to control carbon dioxide levels in ripening rooms when gassing, as high temperature ripening (20 °C; 68 °F) has been seen to produce CO2 levels of 10% in 24 hours.

Malcolm Bennett, a Fellow of the Royal Society, is Professor of Plant Science at the University of Nottingham.

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References

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