Nepenthes rajah: A pitcher plant found in Borneo.
Soil: Complex living ecosystem,
A Horizon (Topsoil): Contains decaying organic matter, microbial organisms, and broken-down rock.
B Horizon (Subsoil): Consists of less weathered material.
C Horizon: Composed of rock, also known as 'parent material.'
Distinction: It's "Soil, Not Dirt!"
Root Functionality: Roots acidify soil solution:
Releases CO2 and H+ ions, leading to cation exchange.
Roots absorb cations from soil particles, supported by root hairs.
Cytoplasm and Extracellular Fluid: Interplay of ATP and H+ ions.
Proton pumps create membrane potential and gradients to drive solute transport into cells.
K+ Absorption: Membrane potential assists in absorbing potassium ions into root cells.
Cotransport: A transport protein couples diffusion of H+ with active transport of anions.
Efficient anion accumulation occurs through inward diffusion of H+ via cotransporters.
Topsoil Composition: Rich in humus, which is organic matter from decaying plants and animals.
One teaspoon of topsoil contains about 5 million bacteria.
Functions: Vital in nutrient availability, soil structure, and water retention.
Management Importance: Managing organic components in the soil is crucial for conservation.
Crop Rotations: Ancient technique to maintain soil health.
Green Revolution: High-input agriculture in the 1960s and 70s aimed at food security is viewed as unsustainable.
Plants require essential elements to complete their life cycle.
Early experiments indicated plants grow while leaving soil unchanged, suggesting nourishment from air.
Elements in Plants:
Macronutrients: Needed in large quantities (C, H, O, P, K, N, S, Ca, Mg).
Micronutrients: Needed in smaller quantities (Cl, Mn, B, Zn, Cu, Ni, Mo).
Controlled environments help determine essential elements for plants.
Control Group: Solution containing all minerals.
Experimental Group: Solution lacking potassium.
Macronutrients:
Carbon, Oxygen, Hydrogen: Major components of organic compounds.
Nitrogen: Critical for nucleic acids, proteins, and chlorophyll.
Potassium, Calcium, Magnesium, Phosphorus, and Sulfur: Various roles in cell function and structure.
Micronutrients:
Chlorine, Iron, Manganese, Boron, Zinc, Copper, Nickel, and Molybdenum: Essential in smaller amounts for various cellular functions.
Examples: Healthy plants vs. phosphate, potassium, and nitrogen-deficient plants.
Soybean Root Nodules: Bacteroids form within root nodules, showcasing the interaction of Rhizobium bacteria with plant roots.
Infection thread forms leading to the development of nodules containing vascular tissue.
Atmospheric Nitrogen (N2) is transformed by:
Nitrogen-fixing, Denitrifying, and Ammonifying bacteria.
Soil bacteria are crucial for providing nitrogen to plants.
Ectomycorrhizae: Form protective sheath around roots (present in about 10% of plant families).
Arbuscular mycorrhizae: Fungal hyphae extend inside plant roots, enhancing nutrient uptake.
Epiphytes: Grow on other plants without rooting in soil, derive nutrients from the environment.
Parasitic Plants: Absorb water/minerals directly from hosts; some lack chlorophyll.
Carnivorous Plants: Photosynthetic plants supplement nutrition by digesting small animals, usually found in nitrogen-poor soils.
Major components of soil and their importance.
The necessity for soil conservation practices.
The roles of macro- and micro-nutrients in plants.
Symptoms indicative of mineral deficiencies.
Importance of nitrogen fixation and roles of mycorrhizae.
Adaptations of certain plant types for unique nutritional strategies.