Soil formation and classification
Soil formation, or pedogenesis, pedology being the branch of soil science focused on soil formation, is a process influenced by the five factors of soil formation: parent material, climate, topography, biology, and time (Jenny, 1954). These factors interact to produce a diverse range of soil types with distinct properties and functions. They are represented by the Twelve Soil Orders of the World. The classification of soils is often based on these properties and the soil horizons (layers) that develop over time, with each having similar characteristics and potentially similar behaviour.
There are several soil classification systems:
Physical and chemical properties
Soil physical properties include texture, structure, and density, which affect water infiltration, root growth, and soil stability. The soil texture triangle, as detailed in "The Nature and Properties of Soils" (Brady and Weil, 2016), helps in understanding the relative proportions of sand, silt, and clay in soil and how this informs a soil's biogeochemical characteristics. Chemical properties, including pH, cation exchange capacity, and mineral content, determine soil fertility and its ability to support plant growth. "Soil Chemistry" by Daniel G. Strawn, et al. (2022), offers an in-depth look at these chemical interactions and their implications for soil management.
Biological properties
Soil is also a living entity, teeming with microorganisms, fungi, and macrofauna that play critical roles in nutrient cycling, organic matter decomposition, and soil health. "Biological Diversity and Function in Soils" by Richard Bardget et al., (2005), is a seminal collection in soil biology.
Further reading