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Base saturation percentage (BSP) is an important soil chemical property that has implications both for soil taxonomic classification and soil fertility. BSP is defined as the sum of four basic cations (Ca, Mg, K, and Na) relative to total soil cation exchange capacity (CEC) at pH 7.0 or 8.2. Furthermore, BSP is a dynamic soil property affected by climatic, geochemical, and environmental conditions. Increases in BSP can elevate plant availability of Ca+2, Mg+2, and K+. Contrariwise, nutrient deficiencies, soil acidification, changes in soil biota, and general degradation of soil health are common consequences of low base saturation. As aforementioned, BSP is important in the characterization of soil types and their pedogenesis.