Soil Microbiology and Formation Quiz
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Questions and Answers

What is soil microbiology concerned with?

Soil-inhabiting microorganisms, their functions, and activities.

Which layer of soil is mainly composed of organic materials?

  • O horizon (correct)
  • B horizon
  • C horizon
  • A horizon
  • Which horizon is known as the zone of accumulation?

  • O horizon
  • A horizon
  • C horizon
  • B horizon (correct)
  • The C horizon is the most influenced by soil-forming processes.

    <p>False</p> Signup and view all the answers

    What is soil texture?

    <p>The proportion of sand, silt, and clay particles that make up soil.</p> Signup and view all the answers

    Which type of soil is considered the poorest for agriculture?

    <p>Sandy soil</p> Signup and view all the answers

    What are the soil particle size ranges for sand?

    <p>0.05 to 2.0 mm</p> Signup and view all the answers

    The soil horizon characterized by light color and more clay than the A horizon is called the ______.

    <p>B horizon</p> Signup and view all the answers

    Match the following types of soil with their characteristics:

    <p>Sandy Soil = Poorest for agriculture, low nutritional value Silt Soil = Smoother, holds water better, more fertile Clay Soil = Composed of smallest particles, retains water Loamy Soil = Combination of sand, silt, and clay</p> Signup and view all the answers

    Study Notes

    Soil Microbiology

    • Soil microbiology is the study of microorganisms within soil, their functions, and their activities.
    • Soil is a key natural resource essential for life on Earth.

    Soil Formation

    • Soil is formed by the interaction of five factors:
      • Topography
      • Organisms
      • Climate
      • Parent material
      • Time

    Soil Profile

    • A soil profile represents a vertical cross-section of soil layers, known as horizons.
    • Each horizon has distinct features.
    • Horizons are labeled: O, A, E, C, B, and R.

    Soil Horizons

    • O Horizon (Topsoil): Composed of organic matter like leaves, grasses, and decomposed material.
    • A Horizon (Topsoil): Mineral horizon with accumulated organic matter, rich in nutrients, darker color, high in sand and lower in clay.
    • B Horizon (Subsoil): Zone of accumulation where substances like iron and aluminum leach from the A horizon. Illuviation occurs here.
    • C Horizon (Parent Soil): Less affected by soil-forming processes, lacks organic matter and microbial activity.
    • R Horizon (Rocky Bed): Underlying bedrock, like limestone or sandstone, found beneath the C horizon.

    Soil Properties

    • Soil texture and structure influence soil behavior:
      • Water holding capacity
      • Nutrient retention and supply
      • Drainage
      • Nutrient leaching
    • Soil texture is determined by the proportion of sand, silt, and clay particles.

    Soil Texture Table

    Particle Type Size Range (mm)
    Sand 0.05 to 2.0
    Silt 0.002 to 0.05
    Clay Less than 0.002

    Soil Texture Impact

    • Soil texture influences plant growth characteristics:
      • Water-holding capacity
      • Permeability
      • Soil workability

    Soil Types

    • Sandy Soil: Large particle size, poor water retention, low nutrient value.
    • Silt Soil: Smaller particles than sand, holds water better than sand, more fertile than other soils.
    • Clay Soil: Smallest particles, densely packed, retains water well, hinders moisture and air penetration.
    • Loamy Soil: Mixture of sand, silt, and clay, combines beneficial properties from each, suitable for plant growth.

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    Description

    Test your knowledge on soil microbiology, formation processes, and the structure of soil profiles. Learn about the different soil horizons and their unique characteristics while exploring the critical roles they play in the ecosystem.

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