SOILS FORMATION, EROSION, AND CONSERVATION

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SOILS FORMATION, EROSION, AND CONSERVATION Miller Chapter 10

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SOILS FORMATION, EROSION, AND CONSERVATION. Miller Chapter 10. I. Soil: Formation Erosion, and Conservation. What is Soil ? complex mixture of eroded rock, minerals, decaying organic matter, water, air, and living organisms. Ratios Differ among various soil types… Average Ratios: - PowerPoint PPT Presentation

Transcript of SOILS FORMATION, EROSION, AND CONSERVATION

Page 1: SOILS FORMATION, EROSION, AND CONSERVATION

SOILSFORMATION, EROSION, AND

CONSERVATION

Miller Chapter 10

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I. Soil: Formation Erosion, and Conservation

A. What is Soil?complex mixture of eroded rock,

minerals, decaying organic matter, water, air, and living organisms.

Ratios Differ among various soil types…

Average Ratios:45% Minerals25% Water25% Air5% Humus

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B. How Soil is Produced

-Weathering of rock -Depositing of sediment -Decomposition of matter

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C. Soil Zones (MATURE)-Soil is arranged into

zones called… SOIL HORIZONS-A cross-section of soil

horizons is called… SOIL PROFILE-Most mature soils have

at least three of the possible horizons

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LAYERS/HORIZONS

O Horizon – Top layer/Surface Liter Layer

-Characterized by debris and animal waste

-Brown/black in color

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A Horizon – • Top Soil Layer -Consists of porous mixture of

partially decomposed organic matter called…

• HUMUS • Inorganic minerals -Most plant roots and organic

matter found here.

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B Horizon – Subsoil Layer andC Horizon – Parent Material

• Contain most of soil’s inorganic matter and varying mixtures of sand, silt,clay, and gravel

• C Horizon lies on BEDROCK

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Soils: zones

O horizonLeaf litterA horizonTopsoil

B horizonSubsoilC horizonParent

material

Mature soil

Young soil

Regolith

Immature soil

Bedrock

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D. Soil Properties*Soils vary in content of … Clay Silt Sand Gravel-Relative amounts of different size and types determines SOIL TEXTURE-LOAMS – soils of equal mixture

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100%clay

Increasingpercentage silt

Increasingpercentage clay

0

20

40

60

80

80

60

40

20

0100%sand 80 60 40 20 100%silt

Increasing percentage sand

CLAY

SILTSAND

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1. Infiltration: Water moving through

the soil layers

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2. Leaching: Soil components from upper layers being carried to lower layers

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3. Porosity:

the measure of the volume of pores and distance of pores per volume of soil

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4. Permeability:the rate at which water and air can move through soilWater Water

High permeability Low permeability

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5. Soil Structure: The way in which soil particles

are organized and clumped together Texture Nutrient Infiltration Water-Holding Aeration Tilth

Capacity Capacity

Clay Good Poor Good Poor Poor

Silt Medium Medium Medium Medium Medium

Sand Poor Good Poor Good Good

Loam Medium Medium Medium Medium Medium

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6. Soil pHA measure

of the acidity of the soil

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II. Soil Erosion1. The movement of soil components, especially surface litter and topsoil, from one place to another*Two main agents are…

-Flowing water -Wind

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2. Types Of Water ErosionA. Sheet – Moving of water in wide flow

B. Rill – Fast moving water that cuts small channels

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C. Gully – • Ditches and gulley’s are

caused by fast moving water over steep, exposed soil

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Areas of serious concern

Areas of some concern

Stable or nonvegetative areas

Global Soil Erosion

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3. U.S. Soil Erosion -1/3 of the original top soil has been washed or blown away.

-USDA states that soil is eroding 16x faster than it can form.

-USDA estimated loss of $30 billion dollars from erosion in 1997

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A.Desertification- The productive potential of

arid or semiarid land falls by 10% or more due to…

Human activities Climate changesMUST REDUCE…Overgrazing & deforestation

4. Other Problems Associated With Soil

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Moderate Severe Very Severe

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B. Salinization-• The accumulation of salts in soil

• Often associated with irrigation

• Effects:• Stunts crop growth• Lowers crop yields• Kills plants

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Severe Salinization

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C. Water logging- An over abundance of

water within the soilEvaporation

TranspirationEvaporation

Waterlogging

Less permeableclay layer

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III. Soil Conservation1. Reducing soil erosion and restoring soil fertility.

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2. Farming Techniques A. Conventional-tillage

farming*Tilling in the fall

B. Conservation-tillage farming

1. Minimum Tillage Farming

2. No Till Farming

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3. Terracing – • Creation of broad, nearly level terraces that run across the contour of the lands

-Mostly used on very steep gradients.

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4. Contour Farming- • Plowing/planting crops in rows across the sloped contour of the land.

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5. Strip Cropping- • Alternating rows of crops with low, ground hugging vegetation.

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6. Alley Cropping/Agroforestry-

• several crops planted together in strips or alleys between trees or shrubs

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7. Windbreaks/Shelterbelts- Rows of trees to reduce wind erosion.

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Conservation During Urban Development

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IV. Soil Restoration-Fertility can be returned by using one of two major types of fertilizer… A. Organic B. Inorganic

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-Animal manure-Green manure

Organic fertilizer

-Compost

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Commercial inorganic fertilizer

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Extreme Erosion