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The Nature Of Soil Ms. Scerra
Section I The Nature Of Soil Ms. Scerra
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Formation of soil can take thousands of years
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Soil is a mixture of weathered rock, decayed organic matter, mineral fragments, water, and air
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Formation is influenced by climate, slope, type of rock, types of vegetation, and length of time that the rock has been weathering
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Composition of soil The ingredients that make up soil
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1. Clay, silt, and sand are small particles of sediment
2. Decaying, dark-colored plant and animal material is called humus 3. Small spaces between soil particles may be filled with air or water
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Soil profile Made up of different layers of soil
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Horizon O Top layer of vegetation and organic matter
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1. Horizon A – Top layer of soil
May be covered with organic litter that may turn into humus Fertile layer with more humus and less rock and mineral particles than other soil horizons
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2. Horizon B – middle soil layer
Contains less humus and is lighter in color than A horizon
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Minerals travel from horizon A to B horizon in a process called leaching
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Horizon C – bottom soil layer
Has very little organic matter and is not strongly affected by leaching
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Contains rock – the parent material from the soil
Glaciers can deposit soil that did not form from the bedrock beneath it
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Soil types differ in different places
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Different regions have different climates that affect soil development
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Parent rock affects soil formation and type of vegetation that grows in a region
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Time affects soil development because the longer the weathering has occurred, the less the soil resembles parent rock
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Soil on steep slopes develops poorly
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Section II : Soil Erosion
By: Ms. Scerra
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Soil erosion or loss is important because plants do not grow as well when topsoil is lost.
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Causes and Effects of Soil Erosion:
Many human activities disturb the natural balance between soil production and soil erosion.
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Agricultural Cultivation
Increased farming removes the plant cover, leaving soils open to wind and water erosion.
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Forest Harvesting Removes forest vegetation which increases erosion and particularly damages tropical rain forest soil
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1984 2004
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Overgrazing Results when animals graze until almost all ground cover disappears
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Excess Sediment Can damage the environment when soil erosion is severe
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Preventing Soil Erosion
Soil must be protected / conserved
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Manage Crops Farmers plant shelter belts of trees to break the force of the wind
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Bare soil can be covered with decaying plants to hold soil in place
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Farmers can graze animals on vegetation instead of plowing it under
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With no-till farming, plant stalks are left in the field to provide cover for soil
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Reduce Erosion On Slopes
Contour farming reduces soil erosion by planting along the contours of slopes
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Terracing creates steep-sided flat areas for crops on the sides of hills and mountains
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Reduce erosion of exposed soil
Water sprayed onto bare soil to reduce wind erosion
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Topsoil is replaced and trees are planted
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Water flow can be controlled in strip mines
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After mining, the land can be reclaimed
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