
Describe any five main characteristics of alluvial soil in India.
Answer
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Hint: In india we have different types of soils. Majorly there are 6 deposits in india. Alluvium is one of them. Alluvium is made up of silt, sand, clay, and gravel, and it also contains organic matter.
Complete answer:
The formation of alluvial soil is the product of the deposition of these sediments. Rivers erode the rocks as they pass across mountains. These sediments and silt are then deposited on riverbanks and flood-prone land.
On the basis of age, alluvial soil can be divided into two categories: khadar and bhangar. The former has a bright color and is composed of younger deposits. The above is the older alluvium, which is made up of lime nodules or kanker and has a clayey composition.
Alluvial soil has the following major characteristics:
1. It is formed by the accumulation of river load as it flows from its upper to lower course.
2. It is light and porous, making it easy to till.
3. It is a fertile soil because it is mineral-rich, especially in potash and lime.
4. It can be used to cultivate a wide range of Rabi and kharif crops.
5. Soils in drier areas have a higher alkalinity.
6. They are loamy in texture.
Note: The majority of alluvial soils come from sand accumulated by the Ganga in the Indo–Gangetic plain, which stretches from Punjab in the west to West Bengal and Assam in the east, as well as the coastal areas of northern Gujarat, the Narmada, and Tapi valleys, which are created by sea waves.
Crops like rice, wheat, sugarcane, cotton, jute, potato and vegetables are grown in alluvial soil.
The alluvial soils range in color from light grey to ash grey. Its hues are determined by the extent of deposition, the texture of the materials, and the length of time it takes to mature. The cultivation of alluvial soils is extensive.
Complete answer:
The formation of alluvial soil is the product of the deposition of these sediments. Rivers erode the rocks as they pass across mountains. These sediments and silt are then deposited on riverbanks and flood-prone land.
On the basis of age, alluvial soil can be divided into two categories: khadar and bhangar. The former has a bright color and is composed of younger deposits. The above is the older alluvium, which is made up of lime nodules or kanker and has a clayey composition.
Alluvial soil has the following major characteristics:
1. It is formed by the accumulation of river load as it flows from its upper to lower course.
2. It is light and porous, making it easy to till.
3. It is a fertile soil because it is mineral-rich, especially in potash and lime.
4. It can be used to cultivate a wide range of Rabi and kharif crops.
5. Soils in drier areas have a higher alkalinity.
6. They are loamy in texture.
Note: The majority of alluvial soils come from sand accumulated by the Ganga in the Indo–Gangetic plain, which stretches from Punjab in the west to West Bengal and Assam in the east, as well as the coastal areas of northern Gujarat, the Narmada, and Tapi valleys, which are created by sea waves.
Crops like rice, wheat, sugarcane, cotton, jute, potato and vegetables are grown in alluvial soil.
The alluvial soils range in color from light grey to ash grey. Its hues are determined by the extent of deposition, the texture of the materials, and the length of time it takes to mature. The cultivation of alluvial soils is extensive.
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