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Soil

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Can lead to salinization due to high evaporation rates. Soil & Plants. Nutrient-Holding Capacity ... Sheet. Gully. Wind. Desert pavement. Causing and Correcting ... – PowerPoint PPT presentation

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Title: Soil


1
Soil
  • Its Ecosystem
  • Chapter 8

2
Objectives
  • Understand basic properties of soil and their
    characteristics
  • Describe a typical soil profile.
  • What are the 4 common soil groups.
  • Why is soil degradation so important?
  • Describe problems that develop from poor
    management.

3
What is soil?
  • A complex natural material derived from
    disintegrated and decomposed rocks and organic
    materials, which provides nutrients, moisture and
    anchorage for land plants.

4
Four Principal components of soil.
  • 1. Mineral
  • 2. Air
  • 3. Water
  • 4.Organic Material

5
How soil are formed
  • 1- Parent material, material from which soils
    were formed.
  • 2- Climate, temperature and moisture.
  • 3- Living organisms, microscopic and macroscopic
    plants and animals.
  • 4- Topography, shape and position of land
    surfaces.
  • 5- Time, period during which parent materials
    have been subjected to soil formation.

6
Plants and Soil
  • Nutrients are released by decomposers
  • Productive soil is a dynamic process
  • Nutrient cycling is key to understanding

7
Soil characteristics
  • Soil Profile
  • Organized into horizons
  • O-Organic
  • A-Topsoil
  • B-Subsoil
  • C-Parent material

8
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9
Soil Texture
  • Clay is the smallest
  • Silt
  • Sand the largest
  • Loam a mixture

10
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11
Soil Structure 4 types of aggregates.
  • 1. Granular (organic matter content is high)
  • 2. Prismatic (found in subsoils and common in
    arid semiarid regions)
  • 3. Blocky (most common in subsoils, particularly
    those in humid regions)
  • 4. Platy (can occur in any part of the profile)

12
Soil Classes
  • Mollisols-Very fertile dark soild found in
    temperate grassland biomes. Deep A horizon.
  • Oxisols-Soils of the tropical and subtropics
    regions. Have thin layer of iron and Al oxides
    in B horizons. Limited fertility.

13
Soil Classes
  • Alfisols-Widespread weathered forest soils. Not
    deep they have well developed O,A,B,C can be
    farmed.
  • Aridisols-found in drylands and deserts, lack
    vegetation and precipitation. Thin light
    colored. Can lead to salinization due to high
    evaporation rates.

14
Soil Plants
  • Nutrient-Holding Capacity
  • Water Holding Capacity (permeability)
  • Aeration ( porosity)
  • pH

15
Soil as an Ecosystem
  • Soil organisms support food web
  • Residue from decomposition is Humus
  • Structure arrangement
  • Plants protect topsoil, roots support structure

16
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17
Soil Degradation
18
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19
Erosion and Desertification
  • Splash
  • Sheet
  • Gully
  • Wind
  • Desert pavement

20
Causing and Correcting Erosion
  • Over cultivation
  • Overgrazing
  • Deforestation
  • Sedimentation

21
Addressing Soil Degradation
  • SAREP
  • LISA
  • BIOS
  • BIFFS
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