Course Content
Concept, scope and importance of soil physics in agriculture
0/4
Introduction
Importance of soil physics
Structure of Water
Physical Properties of Water
Soil Water Energy Concept and soil moisture characteristics curve
0/15
Introduction
Factors affecting the potential energy of water
Soil Water Potential (SWP)
Water Movement Based on Soil Moisture Levels
Gravitational Potential (yg)
Matric Potential (ym)
Osmotic Potential (yo)
Submergence Potential (ys)
Soil Moisture Content
Soil Moisture Measurement
Soil moisture characteristics curve (SMCC), moisture extraction/retention curves or Soil water potential curve
Factors Affecting Soil Moisture Characteristic Curve
Hysteresis
Quantitative Description of Soil Wetness or Classification of Soil Water
Plant Water Availability
Soil water movement under saturated and unsaturated conditions
0/7
Introduction
Poiseuille’s Law
Darcy’s Law
Saturated Water Flow in Vertical Column of Soil
Saturated Hydraulic Conductivity and  Unsaturated Water Flow in Soil
Key differences between saturated and unsaturated water flow in soil
Relationship between k and ym
Air and heat movement in soil and infiltration characteristics in soil
0/7
Water Vapor Movement in Soils
Heat movement in soil
Factors affecting soil thermal regime
Modes of thermal energy transfer
Conduction of heat in soil
Latent heat transfer (LHT)
Soil temperature management
Surface sealing, its effect on soil and crop growth and its management
0/4
Surface sealing
Soil crusting
Renewal of soil air
Impact of poor aeration
Structural management of arable soil
0/4
Introduction
Soil management
Factors involved in genesis and stability of soil aggregate
Aggregate stability
Soil profile development
0/2
Soil Profile
Horizon boundaries and horizon continuity in pedon
Surface and subsurface soil horizons
0/3
Introduction
Diagnostic surface horizons (Epipedons)
Diagnostic Subsurface Horizons
Soil moisture and temperature regimes
0/2
Soil Moisture Regime
Soil Temperature Regime
Soil classification on the basis of USDA soil taxonomy
0/8
Introduction
Soil taxonomy (USDA Soil Taxonomy)
Bases for Soil Classification in Soil Taxonomy
Major Soil orders of Nepal according to USDA taxonomy
Baldwin and Associate’s Genetic Approach
Orders of Genetic Approach
Limitations in Genetic Systems of Soil Classification
New Comprehensive System of Soil Classification (USDA Soil Taxonomy)
The FAO-UNESCO soil classification system
0/1
Introduction
Concept and development of land capability classification
0/2
Introduction
The USDA Land Capability Classification System
Learn Soil Physics, Genesis and Classification with Rahul

Osmotic Potential (yo)

  • Osmotic potential (Ψₒ) results from dissolved solutes (salts, organic compounds) in soil water.
  • Negative Value: Ψₒ is always negative because solutes reduce water’s free energy and restrict movement.
  • Solute Concentration Effect: Higher solute concentration = lower (more negative) Ψₒ.
  • Water Movement: Water moves from low solute concentration (less negative Ψₒ) to high solute concentration (more negative Ψₒ).
  • Limited Role in Bulk Soil Flow: Since soils lack semi-permeable membranes, Ψₒ has minimal direct impact on mass water movement.
  • Plant Water Uptake: Critical for roots—semi-permeable membranes allow osmosis; high salinity (very negative Ψₒ) makes water uptake harder.
  • Vapor Pressure Impact: Solutes reduce soil water’s vapor pressure, slowing evaporation.
  • Salinity Stress: Excess salts lower Ψₒ, causing “physiological drought” (water exists but plants can’t absorb it easily).
  • Irrigation Concerns: Saline irrigation water increases osmotic stress, requiring management like leaching or salt-tolerant crops.
  • Total Soil Water Potential: Ψₒ combines with matric (Ψₘ) and gravitational (Ψ₉) potentials to determine overall water movement (Ψₜ = Ψₘ + Ψₒ + Ψ₉).
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