Course Content
Historical development of soil science and soil institutions in Nepal
0/2
Soil as a Natural Body & Its Ecological Functions
0/2
Kinds and distribution of soil flora and fauna
0/2
Learn Fundamentals of Soil Science and Geology with Rahul

Historical development of soil science

A. Early Agricultural Practices (Pre-2500 BC)

  • The cultivation of plants for food marked a shift from nomadic hunting-gathering to settled communities.
  • Early societies recognized the link between soil fertility and crop yield, particularly in river valleys with annual floods.

 

B. Ancient Civilizations and Soil Fertility (2500–1000 BC)

  • Mesopotamian Civilization (2500 BC): Flourished along the Tigris and Euphrates rivers (modern-day Iraq), utilizing nutrient-rich alluvial soils.
  • Nile Civilization (Egypt): Depended on the Nile River’s annual flooding for fertile agricultural lands.
  • Indus Valley Civilization (Pakistan/India): Practiced advanced irrigation and soil management.
  • Hwang Ho River Civilization (China): Recognized the role of silt deposition in maintaining fertility.

 

C. Soil Fertility Before the 18th Century (A.D.)

  1. Pietro de Crescenzi (1230–1307)
  • Known as: Founder of Modern Agronomy
  • Work: Published “Opus Ruralium Commodorum” – a comprehensive guide on agricultural practices.

Key Contribution:

  • Advocated for increased manure application to enhance soil fertility.
  • Recognized the role of organic matter in maintaining soil health and crop productivity.
  • Significance: His work influenced European agricultural practices for centuries.

 

  1. Jan Baptist Van Helmont (1577–1644)
  • Hypothesis: Water is the sole nutrient required for plant growth.
  • Famous Experiment: The Willow Tree Experiment (1620s)
  • Planted a 5-pound willow tree in a 200-pound pot of soil and watered it exclusively for five years.
  • After five years, the tree weighed 169 pounds, while the soil mass remained largely unchanged.

Conclusion: Incorrectly inferred that water alone nourished plants, overlooking the role of air and soil nutrients.

Significance: Sparked interest in plant nutrition and laid the foundation for later discoveries about photosynthesis and mineral uptake.

 

  1. Jethro Tull (1674–1741)
  • Book: “Horse Hoeing Husbandry” (1731)

Innovations:

  • Seed Drill: Revolutionized planting efficiency by depositing seeds uniformly in the soil.
  • Horse-Drawn Hoe: Enhanced soil aeration and weed control, promoting better nutrient uptake.
  • Theory: Believed plants ingested tiny soil particles directly. Though incorrect, it emphasized soil cultivation to improve crop growth.
  • Significance: His mechanical innovations modernized agriculture by increasing efficiency and crop yields.

 

D. Soil Fertility in the 19th Century (Modern Period)

  1. Théodore de Saussure (1804)

Discovery:

  • Plants absorb CO₂ and release O₂ in the presence of light (photosynthesis).
  • Nitrogen (N₂) is essential for plant growth.

Significance:

  • Challenged earlier misconceptions about humus as the sole source of carbon.
  • Pioneered the understanding of gas exchange in plants.

 

  1. Justus von Liebig (1803–1873)
  • Title: Father of Agricultural Chemistry

Contributions:

  • Refuted the Humus Theory—proved that plants obtain carbon from CO₂ in the atmosphere, not from humus.
  • Identified the importance of water (H₂O) as a source of hydrogen (H₂) and oxygen (O₂).
  • Highlighted the need for alkaline metals (Ca, Mg, Na) to neutralize plant-produced acids.
  • Demonstrated the critical role of phosphates (PO₄³⁻) in seed formation.

Key Concept:

  • Liebig’s Law of the Minimum (1862)
  • “Plant growth is limited by the scarcest essential nutrient, rather than by the total amount of nutrients available.”
  • Impact: Revolutionized fertilizer use by advocating for N-P-K fertilizers based on soil nutrient deficiencies.
  1. Vasily V. Dokuchaev (1870)
  • Contribution: Developed the first scientific soil classification system.
  • Formula: Soil = f(Cl, O, R, P, T)

Cl: Climate

O: Organisms

R: Relief (topography)

P: Parent material

T: Time

  • Significance: Recognized soil as a dynamic natural body influenced by environmental factors, laying the groundwork for modern pedology.

 

  1. Hermann Hellriegel & Hermann Wilfarth (1886)
  • Discovery: Established that nitrogen fixation in leguminous plants requires symbiotic bacteria.

Key Findings:

  • Nitrogen-fixing bacteria reside in root nodules of legumes.
  • These bacteria convert atmospheric N₂ into plant-available nitrogen (NH₃).

 

  1. Martinus W. Beijerinck (Late 1880s)

Contribution:

  • Isolated the nitrogen-fixing bacterium responsible for symbiosis with legumes.
  • Named it Bacillus radicicola (later reclassified as Rhizobium).

Impact:

  • Pioneered the field of microbial ecology in soil science.

 

 

E. In 21st century

  • Conservation tillage/ Zero tillage
  • Improved irrigation system (drip, sprinkle)
  • Integrated Pest Management (IPM)
  • Efficient use of fertilizers (slow release fertilizer)
  • Disease and pest resistant crop species
  • Sustainable land use
  • Nutrient deficiency identification by leaf color chart (LCC), chlorophyll meter, pH meter, methods of lime calculation
  • Geographical Information System (GIS) to boost soil fertility status
  • Integrated nutrient management system
  • C sequestration to increase soil fertility status
  • Climate change and its impact on soil.
Scroll to Top