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Published byTimothy Grant Modified over 9 years ago
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Soil 6 th grade Earth Science Howard Middle School
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Soil Soil is defined as the layer of unconsolidated material found at the earth’s surface. Soil thickness varies from a few millimeters (mm) to several meters (m).
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Soil Thinner soils can indicate a very young soil or a place where soil has been removed by water, wind, gravity, or animal activity.
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Composition Weathered mineral particles Dead and living organic matter Dissolved substances
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Composition The type of soil that exists in an area is influenced by five major factors: Local climate Topography Rock types Organisms (especially plants) Amount of time the soil has been developing
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Classifying Soils In general, soils are classified based on the proportion of organic material and the different-sized particles—sand, clay, and silt—that they contain.
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Inorganic and Organic Components The size and type of the inorganic components of a soil are determined mostly by the local rock type and terrain. The type and amount of organic material is influenced mostly by climate (temperature, sunlight, and precipitation).
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Dead and Living Organic Material Dead organic material is particularly important because it contains a readily accessible source of necessary nutrients. Living organic material helps aerate the soil and decompose the dead material.
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