Intro to Soil Science
Alkaline soils are soils that have a pH level greater than 7, indicating a higher concentration of basic ions, such as calcium and magnesium. These soils often result from the accumulation of carbonates, bicarbonates, or other alkaline substances, which can influence nutrient availability and microbial activity. Understanding the characteristics of alkaline soils is crucial for managing soil health and optimizing agricultural productivity.
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