Laterite soil is infertile due to its high iron oxide content, low nutrient levels, and poor water retention capacity. The soil is highly leached, meaning essential nutrients are washed away, leaving behind a nutrient-poor substrate that is not conducive for plant growth. Additionally, the soil's acidic nature further hinders the availability of nutrients to plants.
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 type of soil described is called laterite.
Laterite soil
Laterite soil is found in Tamil Nadu and Orissa.
what is texture of literate soil
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
the laterite soil is used for the plantaion some crops
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.