Types of Alluvial Soil
Bangar and Khaddar are the two primary kinds of alluvial soils:
- Bangar Soil: It is found at higher elevations in river valleys and differs from Khaddar soil in its coarser texture, higher acidity, and lesser fertility. Because of its elevation location, it is frequently found on river terraces and is well-drained. It is, nevertheless, more prone to erosion than Khaddar soil. Bangar soil is ideal for producing crops such as wheat, barley, and millet, which can endure a drier and less fertile climate.
- Khaddar Soil: On the other hand, is found in river valleys’ lower regions and has a finer texture, better fertility, and lower acidity than Bangar soil. It is generated by flood deposits and is commonly found in river floodplains. Khaddar soil is well-irrigated and very productive due to its closeness to the river, making it suitable for producing water-loving crops like rice and sugarcane. Since the riverbanks protect it, khaddar soil is less prone to erosion.
Why does Alluvial Soil Differ in Texture?
Sediments transported by rivers, streams, and other bodies of water are deposited to form alluvial soil. With around 35% of India’s total land area covered by it, it is one of the most productive soils on the entire planet. The Indo-Gangetic plain and river deltas in Northern and Eastern India are covered in alluvial soil.
Although this soil is incredibly productive and capable of supporting a variety of crops, its texture, structure, and composition change depending on the environment.
Contact Us