What is Soil Science?
Definition: Soil science is the study of soil as a natural resource, including its formation, classification, mapping, and properties (physical, chemical, biological, and fertility) in relation to crop production.
Concept: Soil science is a multidisciplinary field that draws upon knowledge from geology, biology, chemistry, physics, and other sciences to understand the complex nature of soil.
- Characterize soils: Identify and classify different soil types based on their properties.
- Understand soil formation: Investigate the processes that create and shape soils over time.
- Assess soil quality: Evaluate the suitability of soils for various uses, such as agriculture, forestry, and construction.
- Develop sustainable soil management practices: Promote practices that maintain and improve soil health and productivity.
What is Soil?
Definition: Soil is a dynamic natural body composed of mineral and organic matter, water, and air.
Concepts of soil :
Soil is more than just dirt.
Scientists/Researchers ; who Contributed to Soil or Soil Science
- Vasily Dokuchaev (1846-1903): Considered the "father of soil science," he developed the concept of soil as a natural body influenced by climate, organisms, topography, parent material, and time (the five soil-forming factors).

Fig 1: Vasily V. Dokuchaev (1846-1903) - Eugene W. Hilgard (1833-1916):
A pioneer in American soil science, he conducted extensive research on soil classification and mapping. - Curtis F. Marbut (1863-1935):
A leading figure in soil survey and classification, he developed the first comprehensive soil classification system for the United States. - Hans Jenny (1904-1998): A renowned soil scientist who formulated the "State Factor Equation," a mathematical model that describes soil formation.
- Pedology: The study of soil formation, classification, and mapping.
- Edaphology: The study of how soils interact with living things, especially plants.
- Soil physics: The study of the physical properties of soil, such as texture, structure, water-holding capacity, and aeration.
- Soil chemistry: The study of the chemical composition and reactions of soil, including nutrient availability and pollution.
- Soil biology: The study of the living organisms in soil, such as microorganisms, insects, and plant roots.
- Soil fertility: The study of soil's ability to supply nutrients for plant growth.
- Soil conservation: The study of methods to protect soil from erosion and degradation.
Functions of Soil
- Supports plant growth: Provides essential nutrients, water, and physical support for plant roots.
- Filters water: Removes pollutants and impurities from water as it percolates through the soil.
- Stores carbon: Acts as a significant carbon sink, helping to regulate the Earth's climate.
- Provides habitat: Supports a diverse range of organisms, including microorganisms, insects, and small animals.
- Recycles nutrients: Breaks down organic matter and releases nutrients back into the ecosystem.
- Food production.
- Grazing land.
- Forest products.
- Infrastructure support.
- Cleansing and repository functions.
Components of Soil
• Mineral Matter (45%): Derived from rocks and minerals.
• Organic Matter (5%): Decomposed plant and animal residues.
Pore Space (50%)
• Water (25%): Acts as a nutrient carrier.
• Air (25%): Essential for root and microbial respiration.
Soil Profile and Horizons
Soil profiles consist of distinct layers (horizons) with specific characteristics:
O-Horizon: Organic layer.
A-Horizon: Topsoil with humified organic matter.
E-Horizon: Zone of leaching.
B-Horizon: Zone of accumulation.
C-Horizon: Parent material.
R-Layer: Bedrock.
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| Fig 3: Soil Profile (Horizon) |
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