Alluvial soil

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 Alluvial soil is one of the most fertile soil types, widely distributed across river basins and floodplains. It is primarily composed of fine particles like silt, sand, and clay, brought by rivers and streams during their flow. This soil is rich in nutrients, particularly potash, phosphoric acid, and lime, making it highly suitable for agriculture. Alluvial soil is typically light in texture and porous, allowing for good drainage and aeration. It often supports the cultivation of crops such as rice, wheat, sugarcane, and legumes. Found in regions with ample water supply, it plays a crucial role in sustaining agricultural productivity and supporting large populationshttps://soilscientists.org/award-nomination/?ecategory=Awards&rcategory=Awardee

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