1.1 Postlab Factors of Soil Formation

Influence of Parent Material on Soil Formation

  • Soils formed from different parent materials (residual vs transported) show varying degrees of development.
    • Residual parent material: Formed in place, resulting in:
    • Lower degree of horizon formation due to lack of environmental influences.
    • Fewer distinct horizons (A, E, B).
    • Transported parent material: Influenced by environmental factors (wind, water, ice, gravity) leading to:
    • Higher degree of development evident from a greater number of horizons observed.

Influence of Climate on Soil Formation

  • Soils from regions with varying rainfall intensities were studied.
    • Higher rainfall intensity results in:
    • Deeper horizons with a characteristic "k" layer (indicative of leaching).
    • Significant leaching processes that affect mineral content and soil composition.

Influence of Vegetation on Soil Formation

  • Comparison of soils formed under grassland vs forest vegetation.
    • Grassland soils:
    • Thicker, dark surface layer due to abundant root masses.
    • Contributes substantial organic matter (OM) upon decay, resulting in darker colors.
    • Forest soils:
    • Dark color attributed to humus but generally less OM contribution than grasslands.

Influence of Topography on Soil Formation

  • Various landscape positions of soils examined.
    • Waterlogged soils (gleyed):
    • Characterized by the presence of the letter "g" indicating poor drainage.
    • Formation leads to anaerobic conditions causing the reduction of iron (Fe).
    • Appearance: Typically gray color due to reduced Fe.
    • Mottled soils:
    • Presence of spots or blotches of color (grey/orange) due to wetness conditions.

Influence of Time on Soil Formation

  • Comparison of soil profiles of varying ages.
    • Oxisols and Ultisols:
    • Red/rust color indicative of high oxidation states of iron.
    • Both types are common in humid tropical areas and are characterized by:
      • High acidity and low fertility.
      • Oxisols are the most weathered soils, while Ultisols are strongly leached.
    • Younger soils:
    • Generally exhibit higher fertility, as older soils lose nutrients through leaching and weathering.
    • Inceptisols:
    • Newly formed soils showing minimal horizon development.
    • Alfisols:
    • Forest soils characterized by higher fertility and better development over time.