Waterlogging (agriculture)

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
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.

Waterlogging refers to 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]

In agriculture, various crops need air (specifically, oxygen) to a greater or lesser depth in the soil. Waterlogging of the soil stops air getting in. How near the water table must be to the surface for the ground to be classed as waterlogged, varies with the purpose in view. A crop's demand for freedom from waterlogging may vary between seasons of the year, as with the growing of rice (Oryza sativa).

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 blocks off all water and is so hard it stops air getting in and it stops oxygen from getting in.

See also[edit]

References[edit]

  1. ^ "waterlog - definition of waterlog in English | Oxford Dictionaries". Oxford Dictionaries | English. Retrieved 2017-03-10. 
  2. ^ Hillel, Daniel (2004). Introduction to Environmental Soil Physics. United States of America: Elsevier Academic Press. p. 441. ISBN 0-12-348655-6. 

External links[edit]