Laterite soil is rich in iron oxide and aluminum and is derived from a wide variety of rocks through leaching. It is formed in hot and wet tropical areas and is blackish brown to reddish in color.
Laterite soil
Laterite soil is characterized by high levels of iron and aluminum. When it rains, these elements dissolve in the water and are leached downward because they are not retained in the soil due to its low clay content. This leaching process can lead to soil infertility and nutrient depletion in laterite soils.
Paalai soil is called laterite soil in English.
The rate of percolation in laterite soil can vary depending on factors such as soil composition, structure, moisture content, and porosity. Generally, laterite soils have a moderate to high rate of percolation due to their porous nature and ability to drain water quickly.
Laterite soil has good drainage properties, making it suitable for agriculture in areas with heavy rainfall. It is rich in iron and aluminum oxides, which can help crops grow well in acidic conditions. Additionally, laterite soil is porous, allowing roots to penetrate easily and access nutrients.
the laterite soil is used for the plantaion some crops
Laterite soil
Laterite soil is found in Tamil Nadu and Orissa.
what is texture of literate soil
On the basis of morphological features and physico-chemical properties, different types of soil of Kerala have been classified into:Red loamLateriteCoastal alluviumRiverine alluviumOnattukara alluviumBrown HydromorphicSaline HydromorphicKuttanad alluviumBlack soilsForest loam
the crops grown in laterite soil are coconut tea and coffee . it is rich in iron and aluminum hydroxide.
donkey
iron and aluminium
coffee is grown in laterite soil
Laterite soil is characterized by high levels of iron and aluminum. When it rains, these elements dissolve in the water and are leached downward because they are not retained in the soil due to its low clay content. This leaching process can lead to soil infertility and nutrient depletion in laterite soils.
Paalai soil is called laterite soil in English.
The rate of percolation in laterite soil can vary depending on factors such as soil composition, structure, moisture content, and porosity. Generally, laterite soils have a moderate to high rate of percolation due to their porous nature and ability to drain water quickly.