Focus: Basic concepts in soil chemistry and its relevance to soil fertility.
Key Topics Covered:
Basic chemistry concepts: atoms, compounds, ions, and chemical reactions.
Essential soil nutrients for plant growth.
Nutrient uptake processes, including Cation Exchange Capacity (CEC) and base saturation.
Soil pH and effects on nutrient availability.
Basic chemistry concepts pertaining to soil chemistry and nutrient uptake processes.
Principles of cation exchange and its importance in soil fertility.
Understanding of soil pH and its impact on nutrient availability.
Overview of plant nutrients, their cycles, and deficiency symptoms.
Building foundational knowledge to support practical organic farming skills.
Lectures: 2 sessions (1.5-2 hours each) to discuss soil chemistry and nutrient cycling.
Demonstrations: 5 suggested demonstrations to enhance learning through visual representation.
Assessment: Questions to reinforce key concepts, encouraging comprehension and application.
Gershuny, Grace. Start With the Soil. Key chapters covering basic soil chemistry.
Brady, Nyle C., and Ray R. Weil. The Nature and Properties of Soils. Selected chapters for theoretical backing.
Atoms and Elements
Elements: Basic units of matter (e.g., O, Fe).
Atoms: Smallest part of an element not broken by chemical means.
Components: Protons (positive), neutrons (neutral), electrons (negative).
Compounds and Molecules
Compounds: Formed when different elements combine (e.g., H2O).
Bonds: Atoms join by sharing electrons, forming ionic or covalent bonds.
Ions
Formed by imbalances of protons and electrons. Types include cations (positive) and anions (negative).
Plant Nutrients
Sources: Carbon, hydrogen and oxygen from air and water; essential nutrients from soil (e.g. N, P, K).
Soil Colloids
Tiny particles (0.1 to 0.001 µm) that stay suspended in solution; critical for cation exchange.
Soil Solution
Water carrying dissolved nutrients and colloidal matter essential for plant uptake.
Cation Exchange Capacity (CEC)
Indicates soil's ability to retain and exchange cations; influenced by clay and organic matter content.
Base Saturation
The percentage of CEC sites occupied by bases. High saturation indicates higher fertility.
Root Interception
Roots grow into nutrient-rich areas, enhancing uptake.
Mass Flow
Nutrients dissolved in soil water are drawn into roots via transpiration.
Diffusion
Movement from areas of high concentration to low; significant for nutrients like P and K.
Plants need a balance of macronutrients and micronutrients for optimal growth.
Macronutrients: N, P, K (needed in large quantities).
Micronutrients: B, Cu, Fe, Mn, Mo, Zn (required in trace amounts, but critical).
Fixation: Conversion of N2 gas into usable forms by bacteria.
Ammonification & Nitrification: Process converting organic N to usable forms.
Denitrification: Loss of N under anaerobic conditions, which can pollute groundwater.
Necessary for DNA and energy transfer, usually bound tightly to soil particles, making losses minimal except through erosion.
Vital for photosynthesis and growth, mobile in soil, but may be trapped in clay particles; sources include wood ash and granite dust.
Iron: Important for chlorophyll synthesis, deficiency causes yellowing.
Manganese: Important for metabolism and photosynthesis; symptoms include grey specks.
Zinc: Key for enzyme activation, symptoms include stunted growth and mottled leaves.
Recycled organic matter, various amendments, and careful management of soil to maintain nutrient levels.