Alkaline soil


  • Shallow alkaline topsoil

Alkali soil
Alkali soil (wikipedia.org)

Description

Alkali, or Alkaline, soils are clay soils with high pH (greater than 8.5), a poor soil structure and a low infiltration capacity. Often they have a hard calcareous layer at 0.5 to 1 metre depth. Alkali soils owe their unfavorable physico-chemical properties mainly to the dominating presence of sodium carbonate, which causes the soil to swell and difficult to clarify/settle. They derive their name from the alkali metal group of elements, to which sodium belongs, and which can induce basicity. Sometimes these soils are also referred to as alkaline sodic soils. Alkaline soils are basic, but not all basic soils are alkaline.
Source: Wikipedia

Incidence

Alkaline soils are widely distributed in the drier areas of the world. A great deal of foodstuff is produced on soils where salts may be a problem. In regions of low rainfall, salts accumulate where drainage is poor. The tolerance of various plants to soluble salts in soils differs greatly. Among the less tolerant agricultural crops are beans, peas, clover, vetch, oats and peaches. The presence of high concentrations of salts limits the intake of water by plant roots. Yields are reduced approximately in proportion to the osmotic pressure of the nutrient solution. Concentrations of more than 0.2% of salts in a soil will harm crop yields. Alkaline salts are toxic at even lower concentrations. Many irrigation projects have failed because the soil has become alkaline through lack of proper drainage facilities or failure to use enough water to move excess salts down and out of the soil. Others have failed because of the high concentration of sodium in the irrigation water.


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