MEV 013: Unit 07 - Soil Chemistry
UNIT 7: SOIL
CHEMISTRY
7.0 Introduction
Soil is the thin
outer layer of the Earth's crust that supports plant life and forms a key
component of terrestrial ecosystems. It is a dynamic system composed of
minerals, organic matter, water, air, and living organisms. Soil chemistry
deals with the chemical composition, reactions, and properties of soil in
relation to its fertility, structure, and environmental interactions.
7.1 Objectives
After studying
this unit, you will be able to:
- Understand
the origin, nature, and composition of soil.
- Explain the
processes of soil formation and the factors involved.
- Describe the
chemical properties of soil including pH, ion exchange, and nutrients.
- Differentiate
between soil macronutrients and micronutrients.
- Understand
soil fertility and the importance of maintaining soil health.
7.2 Origin and Nature of Soil
Soil originates
from the weathering of rocks and the decomposition of organic materials over
time. It acts as a medium for plant growth, a reservoir for nutrients and
water, and a habitat for organisms.
7.2.1 Soil Composition
Soil is composed
of:
- Mineral
Matter (45%): Sand, silt, clay derived from parent rock.
- Organic
Matter (5%): Decomposed plant and animal material (humus).
- Water (25%): Held in pores, essential for chemical reactions and plant uptake.
- Air (25%): Occupies the remaining pore space, supports microbial activity.
7.3 Soil Formation
Soil formation,
or pedogenesis, is a slow, continuous process influenced by several
environmental factors.
7.3.1 Soil Forming Processes
- Weathering: Physical, chemical, and biological breakdown of rocks.
- Leaching: Downward movement of dissolved substances.
- Humification: Formation of humus from organic matter.
- Mineralization: Conversion of organic nutrients into inorganic forms.
- Aggregation: Binding of soil particles into clusters.
Five Factors of
Soil Formation:
- Parent
material
- Climate
- Topography
- Biological
activity
- Time
7.4 Soil Chemical Properties
Soil chemistry
influences nutrient availability, soil fertility, and crop productivity.
7.4.1 Soil Acidity
- Soil pH: Indicates hydrogen ion concentration.
- Acidic
(< 7), Neutral (= 7), Alkaline (> 7)
- Sources of
Acidity:
- Leaching of
bases
- Decomposition
of organic matter
- Use of
ammonium-based fertilizers
- Importance: Affects nutrient solubility and microbial activity.
7.4.2 Ion Exchange and Cation Exchange Capacity (CEC)
- Ion Exchange: Reversible exchange of ions between soil colloids and soil solution.
- Cation
Exchange Capacity (CEC):
- A measure
of soil’s ability to hold positively charged ions (cations).
- Units:
meq/100g of soil
- High CEC
indicates high fertility potential.
Common
exchangeable cations: Ca²⁺, Mg²⁺, K⁺, Na⁺, H⁺, Al³⁺
7.5 Macro and Micronutrients in Soil
Plants require essential
nutrients for growth, broadly divided into:
7.5.1 Soil Macronutrients
Required in large
amounts:
- Primary
Macronutrients: Nitrogen (N), Phosphorus (P), Potassium (K)
- Secondary
Macronutrients: Calcium (Ca), Magnesium (Mg), Sulfur (S)
Functions:
- Nitrogen:
Protein synthesis
- Phosphorus:
Energy transfer (ATP)
- Potassium:
Enzyme activation and water balance
7.5.2 Soil Micronutrients
Required in trace
amounts:
- Examples: Iron (Fe), Zinc (Zn), Copper (Cu), Manganese (Mn), Boron (B),
Molybdenum (Mo), Chlorine (Cl), Nickel (Ni)
Functions:
- Fe:
Chlorophyll synthesis
- Zn: Enzyme
cofactor
- B: Cell wall
strength
Deficiency or
excess of these nutrients affects plant growth, yield, and quality.
7.6 Soil Fertility
Soil fertility is the ability
of soil to supply nutrients in adequate amounts and proportions for plant
growth.
Factors affecting
fertility:
- Nutrient
availability
- Soil pH
- Organic
matter content
- Microbial
activity
- Water
retention and drainage
Improvement of
Soil Fertility:
- Organic
amendments (compost, manure)
- Crop
rotation and green manuring
- Balanced
fertilization
- pH
correction using lime or gypsum
7.7 Let Us Sum Up
This unit
introduced the foundational aspects of soil chemistry, focusing on the nature,
formation, and chemical behavior of soil. We covered important properties like
pH, cation exchange capacity, and the distinction between macro- and
micronutrients. A comprehensive understanding of these factors is essential for
managing soil fertility and ensuring sustainable agricultural practices.
7.8 Key Words
- ·
Pedogenesis-The process of soil
formation.
- ·
Soil Profile-Vertical section showing
different soil horizons.
- ·
Cation Exchange Capacity (CEC)-The ability of
soil to hold and exchange positively charged ions.
- ·
Macronutrients-Essential elements
required in large amounts by plants (e.g., N, P, K).
- ·
Micronutrients-Essential elements
required in small quantities by plants (e.g., Fe, Zn).
- ·
Soil Acidity-Degree to which soil has
a low pH, often limiting nutrient availability.
- ·
Ion Exchange-Exchange of ions between
soil and soil solution, critical for nutrient dynamics.
- ·
Soil Fertility-Capacity of soil to
support plant growth and yield by providing nutrients.
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