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A site's soil characteristics have a major impact on the type and quality of trees produced. In general, soil type is classified by its texture, or size of soil particles, porosity and fertility. Further classification of a soil's quality is determined by measuring its chemical and biological indicators. A soil's infiltration rate and aggregate structure and stability help determine the soil's water-holding capacity, while its organic matter will indicate the soil's overall fertility level. Generally, fine-textured (clay) and medium-textured soils have a greater nutrient content than course or sandy soils. The soil's porosity, or measure of the spaces between particles, and aggregate structure will determine how quickly water drains from the site. Clay soils can hold more water, but absorb the water more slowly because of its low saturation point. Soils with a high percentage of silt have the most favorable texture for moisture absorption and drainage. For more information on soil types and to get your soil tested, contact your county UW-Extension office. Soil maps are available from your local U.S. Natural Resources Conservation Service office.

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13y ago

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