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+91 98967 93832Texture, or size distribution of mineral particles (or associated pore volume), is one of the most important measures of a soil because individual particles have much greater surface area per unit mass or volume than coarse particles. Thus, a small amount of fine clay and silt will be much more important in chemical reactions, release of nutrient elements, retention of soil moisture, etc., than a large volume of coarse gravel or sand.
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