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Essential Question: How does soil form, and what purposes does it serve? Objectives: 1. Describe the functions of soil 2. Describe the factors of soil formation
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Upper layer of Earth in which plants grow. Formed by weathering, erosion, and the combining of those rock particles with air, water, and organic material It can take 100 to 600 years or more for nature to make one inch of topsoil
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Parent Material Climate Organisms Topography Time
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Provides support and anchorage for vegetation Medium for plant growth and crop production Primary cleansing and recycling medium Sustains biological activity, diversity and production Stores and cycles nutrients and other elements Allows gas exchange
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Organic matter Water Air Nutrients/minerals
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Consists of the remains of plants and animals With favorable temperature and moisture, animals and fungi break down organic matter to humus and soluble nutrients accessible to growing plants Types of plants growing in the soil, management practices, temperature, and drainage determine the amount of organic matter
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From precipitation entering soil cracks, holes, and openings between soil particles Used by plants Lost to evaporation and run-off Moves deep within the ground, inaccessible to plants
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Air in the soil contains less oxygen and more carbon dioxide than air above the soil surface Air is pushed out of the soil as water enters Plant roots take up oxygen for respiration Roots die if air is unavailable for long periods of time
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18 elements essential for plant growth Nitrogen - most important, nitrogen-fixing bacteria Carbon, Hydrogen and Oxygen - from air and water Iron, calcium, phosphorus, potassium, copper, sulfur, magnesium, manganese, zinc, boron, chlorine, cobalt, nickel, and molybdenum - from soil
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Permeability Water holding capacity Porosity
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The rate at which water moves through soil Affected by the amount, size, and arrangement of pores. Macropores, such as sand, can increase permeability
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The ability of a soil’s micropores to hold water for plant use Affected by the amount, size and arrangement of pores
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Soil texture Soil structure Compaction Organic matter
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The relative proportions of sand, silt and clay
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Sand - particles of 2 to.05 mm diameter Silt - particles.05 to.0002 mm diameter Clay - <.0002 mm diameter Loam - contains soils whose properties consist almost equally of clay, silt, and sand separates
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The nature of the arrangement of primary particles into naturally formed secondary particles called aggregates Profound influence on porosity and balance between large and small pores Types Granular Blocky Platy Columnar/Prismatic
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Individual particles of sand, silt, and clay grouped together in small, nearly spherical grains Water easily circulates Common in surface soils with high organic matter content
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Soil particles that cling together in nearly square or angular blocks having more or less sharp edges Resists penetration and movement of water Common in subsoils, especially in humid regions
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Made up of soil particles aggregated in thin plates or sheets piled horizontally on one another Plates often overlap, greatly impairing water circulation Common with puddling or ponding of soils
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Soil particles that have formed into vertical columns or pillars separated by miniature, but definite vertical cracks Water circulation and drainage is poor Common in subsoils in arid and semi-arid regions
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Destroys soil quality Reduces pore size Less space for air and water Difficult for plants to grow roots
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Add organic matter Reduce trips across the area Practice reduced-till or no till systems Harvest when soils are not wet
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What do you think the soil profile is? Why is it important to know about the soil profile?
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Essential Question: What are the horizons of the soil profile, and what do they contain? Objectives: 1. Describe the horizons of the soil profile. 2. Identify individual horizons of the soil profile based on their components. 3. Describe why the soil profile is important to understand.
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6 layers O:Organic A: Topsoil E: Eluviated B:Subsoil C: Parent Material R: Bedrock
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Organic Top layer of soil Made of fresh to partially decomposed organic matter Color varies from brown to black
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Top Soil 2 nd layer Top portion made of highly decomposed organic matter Color ranges from brown to gray
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Eluviated 3 rd layer Made of mostly sand and silt Has lost most of its minerals
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Sub soil 4 th layer More clay and bigger bedrock Reddish brown or tan in color
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Parent Material 5 th layer Weathered bedrock Cracked and broken surface of the bedrock
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Bedrock Last layer Made of unweathered rocks
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