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Air Filled Porosity
Air-filled porosity describes the percentage of pore space occupied by air after drainage. It represents the amount of oxygen available to roots and soil micro…
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Bulk Density
Bulk density describes the mass of dry soil or substrate per unit volume, including pore space. It is typically expressed as: - g/cm³ - kg/m³ Bulk density refl…
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CEC
CEC is the ability of a soil or substrate to hold and exchange positively charged ions (cations). It represents the nutrient buffering capacity of the root zon…
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Compaction Dynamics
Compaction is the progressive reduction of pore space caused by pressure, settling, and structural collapse. It affects both soils and substrates. - Repeated t…
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Crop Sensitivity
Crop sensitivity notes highlight how different crops respond to: - Salinity - Sodium and chloride - pH extremes - Nutrient imbalance - Root-zone stress This in…
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Decomposition & C:N ratio
Decomposition is driven by microbes consuming: - Carbon as an energy source - Nitrogen to build proteins If a material is carbon-rich, microbes may temporarily…
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EC & TDS
EC measures the total concentration of dissolved salts (ions) in the root zone. It does not identify which ions are present—only the overall ionic strength. -…
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Field Vs Container Capacity
Field capacity describes the water content of a soil after excess water has drained freely under gravity in an open field. It reflects: - Soil texture - Struct…
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Irrigation Pulse Design
Pulse irrigation applies water in short, controlled events rather than long continuous applications. The aim is to: - Re-wet the root zone - Restore water avai…
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Media Ageing Curves
Media ageing describes how substrates change physically and chemically over time. Ageing is driven by: - Decomposition - Settling - Irrigation cycles - Root gr…
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Mulder
Mulder’s Chart describes nutrient interactions through: - Synergism: one nutrient enhances uptake or function of another - Antagonism: one nutrient suppresses…
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Nitrogen Cycle
The nitrogen cycle describes how nitrogen moves between the atmosphere, soil or substrate, microorganisms, plants, and water. Nitrogen is unique among nutrient…
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Osmotic Stress
Osmotic stress occurs when dissolved salts reduce the plant’s ability to take up water, even when moisture is present. Water moves from low salt concentration…
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Oxygen Vs Temperature
Root respiration is temperature-dependent. As temperature rises, roots consume oxygen faster. This means oxygen stress can occur even when air-filled porosity…
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Phosphorus Cycle
The phosphorus cycle describes the movement of phosphorus between minerals, organic matter, soil solution, plants, and microorganisms. Unlike nitrogen: - Phosp…
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Ratios
Uptake is governed by ion competition, CEC occupancy and root transport. A nutrient can be adequate in absolute terms but poorly available because another nutr…
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Root Respiration Curves
Root respiration is the metabolic process by which roots consume oxygen to generate energy. Respiration rate varies with: - Temperature - Root age - Oxygen ava…
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Root Zone Oxygen Diffusion
Oxygen diffusion is the movement of oxygen from the atmosphere into the root zone and toward respiring roots. It occurs primarily through air-filled pores, not…
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Sodium Adsorption Ratio (SAR)
SAR describes the relative proportion of sodium (Na⁺) to calcium (Ca²⁺) and magnesium (Mg²⁺) in water or soil solution. It is calculated as: SAR = Na⁺ / √((Ca²…
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Soil Texture Classes
Soil texture describes the relative proportion of: - Sand - Silt - Clay Texture strongly influences water, air, and nutrient behaviour. - Very low WHC - Rapid…
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Soil Types
- Low bulk density - Low WHC - High drainage - Low nutrient buffering - Rapid nutrient leaching - Balanced particle size - Moderate WHC - Good structure - High…
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Substrates
- Moderate CEC, often K-dominant - Responds quickly to fertigation chemistry - High K can suppress Ca and Mg uptake - Requires deliberate Ca and Mg supplementa…
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Sulphur Cycle
The sulphur cycle links atmospheric deposition, organic matter, soil minerals, and plant uptake. Sulphur behaves similarly to nitrogen in some respects but is…
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Water
Hard water contains higher concentrations of dissolved calcium (Ca²⁺) and magnesium (Mg²⁺), commonly associated with bicarbonate (HCO₃⁻). Key characteristics:…
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Water Holding Capacity
Water holding capacity describes the amount of water a soil or substrate can retain against gravity after drainage. It is usually expressed as: - % by volume -…
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Wetted Weight
Wetted weight (or wet bulk density) describes the mass of soil or substrate after water has filled its pore space. It reflects: - Water holding capacity - Pore…
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pH
pH is a measure of acidity or alkalinity in the root zone, defined as the negative logarithm (base 10) of hydrogen ion activity: pH = −log₁₀(aH⁺) Because pH is…