Soil Physics, Chemistry & Structure

Beneath every productive field lies a complex interplay of physical, chemical, and structural properties that determine how soil holds water, releases nutrients, and supports root growth. Texture, porosity, aggregation, pH, cation exchange capacity, and mineral composition all shape what a soil can do — and how it responds to management. Understanding these fundamentals is essential for diagnosing problems, predicting behaviour, and making sound agronomic decisions. The Soil Physics, Chemistry & Structure session gathers soil scientists and field practitioners to unpack the mechanisms that govern soil function, from the molecular reactions controlling nutrient availability to the architecture of aggregates that lets air and water move through the profile.

Why do some soils compact easily while others drain freely? How do chemical reactions at the particle surface dictate fertility? These are the questions explored through current research and applied diagnostics presented here. Anyone attending this Agriculture Conference can expect a deeper grasp of how physical and chemical processes interact, and how that knowledge translates into better tillage, irrigation, and amendment choices. By treating soil structure and soil chemistry as connected rather than separate disciplines, the session equips growers, advisors, and researchers to read their soils more accurately and manage them with greater precision.

The Science Behind Soil Behaviour

Soil Physical Properties

  • Texture, porosity and bulk density
  • Water-holding capacity and drainage

Soil Chemical Properties

  • pH, buffering and nutrient availability
  • Cation exchange and mineral reactions

Soil Structure and Aggregation

  • How aggregates form and stabilise
  • Pore networks for air and water movement

Compaction and Degradation

  • Causes and indicators of compaction
  • Restoring structure in damaged soils

Soil–Water Interactions

  • Infiltration, retention and movement
  • Managing waterlogging and drought stress

Diagnosing Soil Constraints

  • Field and laboratory assessment methods
  • Linking measurements to management

From Soil Science to Field Decisions

Smarter Tillage and Cultivation

See how knowledge of structure and compaction guides decisions that protect porosity and keep soils workable.

More Precise Nutrient Management

Understand how chemistry — pH, exchange capacity, mineralogy — shapes fertiliser choices and nutrient efficiency.

Better Water and Irrigation Planning

Connect physical properties to infiltration and retention so irrigation matches what the soil can actually hold.

Accurate Problem Diagnosis

Learn to interpret soil tests and field signs to identify the real cause of underperformance, not just the symptoms.

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