What describes soil structure?

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Soil structure refers to how individual soil particles, such as sand, silt, and clay, are arranged and combined to form aggregates or clusters. This arrangement is crucial because it affects various soil properties, including water movement, root penetration, and aeration.

A well-developed soil structure can enhance porosity and permeability, leading to better drainage and root growth. Conversely, poor structure can lead to compaction, reducing air and water movement within the soil, which ultimately impacts plant health.

The other aspects mentioned, such as color, particle size, and pH level, provide important information about soil characteristics but do not specifically define how the particles are organized or grouped, which is the essence of soil structure. Understanding soil structure is important for optimum plant growth and soil management practices.

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