How is soil texture determined?

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Soil texture is determined by measuring the relative percentages of primary soil particles, which consist of sand, silt, and clay. These particles have different sizes and properties, and their distribution within the soil greatly influences its physical characteristics, such as drainage, aeration, and nutrient retention. The texture of the soil is crucial for understanding how it will behave in various environmental conditions and how it can support plant growth.

In practice, soil texture is typically assessed using techniques like the feel method or laboratory analysis, which will classify the soil into categories such as sandy, loam, or clay. This classification affects water movement, root penetration, and the soil's ability to hold nutrients, making it a foundational aspect of soil science.

Other options like evaluating organic matter content, assessing nutrient retention, or analyzing pH levels relate to other properties of soil but do not define its texture. Each of those factors may be important for different aspects of soil health and management, but they do not directly determine the texture of the soil itself.

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