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Chapter 5 5.2 Soils
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Characteristics of Soil
Soil is part of regolith (loose materials that cover Earth) that supports the growth of plants There are three important characteristics to soil Composition Texture Structure
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Characteristics of Soil- Composition
Soil has four major components: Organic matter, or humus, which is the decayed remains of organisms Mineral matter, or broken-down rock Water (in pore spaces) Air(in pore spaces)
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Characteristics of Soil- Composition
In pore spaces between soil particles is air and water
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Characteristics of Soil Organic Matter
Organic matter is an important source of: plant nutrients and increases soil’s ability to hold water
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Characteristics of Soil Mineral Part
Soil Texture – refers to the proportions of the 3 different particle sizes: 1. Sand (large size) 2. Silt (medium size) 3. Clay (small size)
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Soil Texture What type of soil consists of 10% clay, 60% silt, and 30% sand? Silty Loam Loam soil is the best for growing plants. Why? A loam soil contains equal parts sand, silt, and clay
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Soil Formation Time Climate
The longer the soil has been forming, the thicker it becomes Climate Greatest effect on soil formation Variations in temp and precipitation influence the rate, depth, & type of weathering
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Soil Formation Organisms
Plants are the main source of organic matter in soil Microorganisms, including fungi, bacteria, and single-celled protozoans, play an active role in decomposing dead plants and animals Burrowing animals mix the mineral and organic matter in soil
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Soil Formation Slope On steep slopes, erosion is accelerated
Little water can soak in, so the soil generally holds too little moisture for plant growth As a result, soils are usually ______ or __________. thin nonexistent
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Soil Formation Flat areas often have very thick soil
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The Soil Profile Soil horizons are zones or layers of soil
A soil profile is a vertical section through all the soil horizons
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Soil Profile
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Soil Profile 1. A horizon Commonly known as “topsoil” 2. B horizon
Its upper part is made mostly of loose leaves and dead plants 2. B horizon Commonly known as “subsoil” Contains fine clay particles
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Soil Profile C Horizon Contains partially weathered parent material
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What is Soil Erosion? Movement of topsoil down slope by the force of running water Erosion can also be caused by blowing of soil particles by wind, like on a beach
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Soil Erosion Humans accelerate erosion by removing natural vegetation from land: Examples – 1. farming 2. logging 3. construction logging construction
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Decreasing Soil Erosion
Hillside Terracing
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Decreasing Soil Erosion
Plowing along the contours of a hillside
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Decreasing Soil Erosion
Planting rows of trees called windbreaks
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