Soil Fertility and Plant Nutrition
HORSS-201 & AGRMI-202
UNIT I
Soil Fertility Concept
Soil fertility refers to a soil’s capacity to sustain plant growth by providing essential nutrients, water, oxygen, and a favourable physical, chemical, and biological environment.
Key characteristics of fertile soil include:
- Nutrient supply: Adequate levels of 17 essential elements (see below) in plant-available forms.
- Absence of toxins: Low concentrations of harmful substances (e.g., excess heavy metals).
- Structure: Good aggregation, porosity, and organic matter (humus) for moisture retention and root penetration.
- pH balance: Optimal range of 5.5–7.5 for nutrient availability and microbial activity.
- Maintains adequate organic matter and biological activity.
- It has good moisture retention and proper drainage.
Soil Fertility vs. Soil Productivity
- Soil Fertility: The nutrient-supplying capacity of the soil.
- Soil Productivity: The ability of the soil to produce crops under a defined set of management practices.
Note: All productive soils are fertile, but all fertile soils may not be productive.
Types of Soil Fertility
- Natural (Inherent) Fertility: Fertility present without human intervention.
- Acquired Fertility: Fertility developed through external inputs like fertilizers, manures, irrigation, etc.
- Apparent Fertility: Temporary fertility based on favorable conditions like good weather or irrigation.
Fertility Evaluation
- Done through soil testing, plant tissue analysis, and crop response studies.
- Parameters like available N, P, K, pH, EC, organic carbon, and micronutrients are analysed.
Factors Affecting Soil Fertility
- Soil texture:
- Loam (balanced clay, sand, silt) is ideal for nutrient retention and root growth.
- Clay soils retain nutrients but may restrict aeration; sandy soils drain quickly.
- Organic matter (humus): Enhances nutrient retention (especially nitrogen and phosphorus), soil structure, and microbial activity.
- Moisture and aeration: Adequate moisture ensures nutrient solubility, while oxygen supports root respiration and aerobic microbes.
- Soil depth: Deeper soils allow extensive root development and water storage.
- Structure: Good structure promotes aeration and root penetration.
- Porosity and Compaction: Affects oxygen supply and water movement.
- Temperature: Influences microbial activity and nutrient availability.
- Soil pH: Affects nutrient solubility (e.g., phosphorus becomes unavailable in acidic soils).
- Cation exchange capacity (CEC): Determines the soil’s ability to hold positively charged ions (e.g., K⁺, Ca²⁺, Mg²⁺).
- Mineral composition: Parent material influences nutrient availability (e.g., potassium in feldspar).
- Soil biota: Microbes (bacteria, fungi) decompose organic matter, fix nitrogen, and solubilize minerals.
- Pathogen balance: Beneficial microbes suppress plant diseases.
- Crop rotation: Prevents nutrient depletion (e.g., legumes fix nitrogen).
- Tillage practices: Over-tillage reduces organic matter and disrupts soil structure.
Essential and Beneficial Elements
Essential Elements
Essential elements are nutrients indispensable for plant growth, development, and reproduction. The deficiency of any essential element cannot be substituted by another element, and it must be directly involved in plant metabolism.
Criteria of Essentiality (Arnon and Stout, 1939)
An element is considered essential if:
- A plant cannot complete its life cycle without it.
- The element is part of a vital plant constituent or metabolite.
- Its function cannot be replaced by another element.
Classification of Essential Elements
A. Based on Quantity Required:
- Macronutrients (Required in large quantities)
- Primary Macronutrients: Nitrogen (N), Phosphorus (P), Potassium (K)
- Secondary Macronutrients: Calcium (Ca), Magnesium (Mg), Sulfur (S)
- Micronutrients (Required in small quantities)
- Iron (Fe), Manganese (Mn), Zinc (Zn), Copper (Cu), Boron (B), Molybdenum (Mo), Chlorine (Cl), Nickel (Ni)
B. Based on Function:
- Structural elements: C, H, O (make up 96% of plant dry matter; obtained from air and water)
- Energy-related elements: N, P, S (involved in proteins, nucleic acids, ATP)
- Charge balance and osmotic potential: K, Ca, Mg
- Enzyme activators or cofactors: Fe, Zn, Mn, Cu, Mo, B, Cl, Ni
17 elements are critical for plant life cycles:
Beneficial Elements
- Improve growth or yield
- Replace essential elements in some metabolic roles
- Be essential for certain lower plants or specialized functions
- Sodium (Na): Beneficial for C4 and CAM plants (e.g., sugar beet) and Enhances osmotic regulation in some crops (e.g., spinach).
- Silicon (Si): Enhances drought/pest/disease resistance, mechanical strength (not essential but very beneficial for grasses and rice)
- Cobalt (Co): Required by nitrogen-fixing bacteria in legumes
- Selenium (Se): Beneficial for some plants, toxic in excess
- Aluminum (Al): Beneficial for tea plant root growth in acidic soils (toxic in most others)
Table: Essential Elements and Their Typical Concentration
Key Interactions
- Law of the Minimum: Plant growth is limited by the scarcest nutrient.
- Nutrient immobilization vs. mineralization: Microbial activity determines nutrient availability.
- pH-dependent solubility: Example: Iron becomes inaccessible in alkaline soils, causing chlorosis.
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