TOPIC: ENVIRONMENTAL CONSERVATION

Environmental conservation is the process of preserving natural resources from loss, waste or exploitation in order to ensure continuous availability.

Environmental conservation methods include the following:

Afforestation

Re-afforestation

Cover-cropping

Improved farming techniques

Environmental education

Recycling

Legislation against environmental degradation.

EVALUATION:

Define environmental conservation.

Mention some of the methods of environmental conservation.

SOIL

Soil is defined as the thin surface of the uppermost layer of the earth crust on which plants grow.

Composition or Components of Soil

Soil is made up of five components which are (i) inorganic or mineral matter (ii) organic matter (iii) soil water (iv) soil air (v) living organisms

Mineral or Inorganic matter, organic matter, water and air are collectively referred to as physical components of the soil while living organisms are referred to as biological components of the soil.

(1) Mineral or Inorganic Matter

The mineral matter represents small rock fragments of the soil. It forms the bulk of about 45% of total volume of the soil. It consists of gravel, stones, sand, silt and clay.

Importance / Effects of Mineral Matter on Agriculture

It forms the solid part of the soil which provides support for plants.

Mineral matter is the main source of plant nutrients such as nitrogen, calcium, magnesium iron etc.

It represents the home or habitat of all soil living organisms.

It holds water and air for both plants and animal activities.

Mineral matter has moderating effects on soil temperature.

It also affects soil porosity.

(2) Organic Matter

The organic matter represents the remains of the decomposition of plants and animals. It is about 5% of the total volume of the soil. Leaves, roots of plants, the residue of crops, animal dung, etc. when they are deposited on the soil, they decay to form a dark colour on the upper part of the soil. This becomes organic matter which is also called humus.

Importance / Effects of Organic Matter on Agriculture

It is very rich in plant nutrient.

It is the habitat of many soil micro-organisms.

It prevents leaching in soil where it is present in adequate amount.

It also prevents soil erosion and evaporation of soil water.

It allows for good drainage and holds water in the soil for plant use.

It improves the structure of the soil by binding particles together.

It increases water-holding capacity of the soil.

It moderates the soil temperature.

It has moderating effect on PH value.

(3) Soil Water

Soil water refers to the water in the soil which is usually obtained either from rain or irrigation. Water represents 25% of the total volume of the soil. It is usually found in the pore spaces of the soil. When water is too much in a soil (covering the soil surface), the soil is said to be Waterlogged. A waterlogged soil can however be improved by drainage to make such soil more productive. On the other hand, when there is complete lack of water in the soil for a very long time such that plants cannot absorb water even when supplied again, this results in a condition called permanent wilting point. The plant at this stage can die.

Importance / Effects of Soil Water in Agriculture

Water is an important agent of weathering of rocks in the soil.

It helps to dissolve plant nutrients into solution form.

Water is an essential raw material for photosynthesis.

Hydrolysis of many food nutrients and enzymatic activities.

Loss of water from plant through transpiration helps in the cooling of the plant.

Presence of water aids easy tillage of the soil and also improves the soil structure.

It also promotes the activities of soil organisms.

It is needed for the germination of seeds.

(4) Soil Air

This refers to the gases present in the soil pore spaces found between the soil particles. Theamount of soil air varies, depending on the amount of soil water, the size of the porespaces, the type of soil and the amount of living organisms in the soil. The percentage of air is about 25% of the total volume of the soil. The ability of air to circulate freely in the soil is called aeration.

Importance / Effects of Soil Air on Agriculture

Oxygen is necessary for the growth and development of plants.

Oxygen in the soil promotes easy germination of seed.

Soil organisms require oxygen for respiration.

Excess of carbon dioxide in the soil, when combined with water can cause acidity and aid weathering of rocks.

Air is needed in soil reaction particularly carbon and nitrogen cycles.

(5) Living Organisms

This refers to plants and animals which inhabit the soil. They range from microscopic organisms to bigger organisms. Some are beneficial while others are harmful to crops and livestock. The most commonly found groups of soil organisms include bacteria, fungi, virus nematodes, insects e.g termites, soldier ants, millipede, centipede, earthworm, snails, reptile, mammals, (e.g rats and rodents).

Importance / Effects of Living Organisms on Agriculture

They help to improve the aeration of the soil.

They help to decompose organic materials in the soil to form humus.

They aid percolation of water.

They improve the structure of soil.

Some organisms like bacteria help to fix nutrients in to the soil.

Some are pests and parasites while some cause diseases of crops.

Some soil micro-organisms produce acidic materials which help to break down rocks.

EVALUATION QUESTIONS

Mention the components of soil.

Outline four importance of organic matter to soil.

Types of Soil and their Properties

There are three main types of soil. These are: (i) sandy soil (ii) clay soil (iii) loamy soil

(1) Sandy Soil

A soil is said to be sandy if the proportion of sand particles in a sample of soil is very high.

The particles are mainly quartz (SiO2).

They have the size of 2.0mm in diameter.

Sandy soil is not very good for farming because it is poor in plant nutrients.

Properties of Sandy Soil

Sandy soil is coarse, grainy and gritty.

It is loose with large pore spaces.

It is well aerated and cannot hold water.

Percolation is high but capillarity is low.

It is not sticky when wet.

(2) Clay Soil

A soil is said to be clayey if the proportion of clay in a sample of soil is very high.

The relative size is less than 0.002mm in diameter.

It is a heavy soil because it is very difficult to work on or cultivate.

Properties of Clay Soils

Clay soil is fine grained and smooth.

Particles are tightly packed with little pore spaces.

It is poorly aerated and can hold water.

Percolation is low but capillarity is high.

It is sticky when wet and hard when dry.

(3) Loamy Soil

Loamy soil is a mixture of sand, clay with high proportion of organic matter.

Loamy soil is the most fertile and the best soil for farming.

Properties of Loamy Soil

Loamy soil is moist and loose.

It contains lots of organic matter (humus).

It does not support erosion and water logging.

It is well aerated and can hold water.

Characteristics of Soil

Certain features or characteristics are used to identify or describe a soil sample. These are:

Soil colour 2) Soil texture

Soil structure 4) Permeability

Porosity 6) Soil PH

EVALUATION QUESTIONS:

Describe a sandy soil.

State the properties of loamy soil.

Define soil.

Mention three types of soil.

Mention two characteristics of each of this soil type.

PROCESSES OF SOIL FORMATION

The following are the processes of soil formation:

Weathering of parent materials.

Action of Chemicals.

Further Disintegration.

Appearance of biological activities.

Formation of humus.

Final soil formation.

EVALUATION

State the processes of soil formation.

Explain the factors that determine soil formation.

SOIL PROFILE

Soil profile is defined as the vertical section through the soil to the underlying rocks, showing

series of horizontal layers. These horizontal layers are called horizons.

A Typical soil profile has three layers or horizons which are A, B and C horizons.

A- HORIZON

A horizon is also called top soil.

It represents the surface layer of the soil profile.

It contains more humus or organic matter.

It is the zone of elluviation where minerals are leached down the profile.

It has maximum biological activities of plant and soil micro-organisms.

B – HORIZON

B horizon is also called sub soil.

It is the zone of illuviation where soil minerals accumulate, especially those leached from the A-horizon.

It contains lot of mineral matter.

There is the conversion of organic matter from A – horizon into inorganic matter.

This zone contains leached materials.

C- HORIZON

C horizon is also called zone of parent materials.

It contains weathered parent rocks.

It represents materials from which top and sub-soil are formed.

Beneath the C Horizon is the bedrock.

Importance of Soil Profile

It determines the level of fertility of the soil e.g. a tick top soil represents high level of soil fertility.

It helps the farmer to know the type of crop to grow.

It determines the level of root penetration, drainage and aeration.

It determines the rate of percolation of water and the level or degree of soil erosion.

Importance of Soil

Agriculture: It provides the only medium through which agriculture is practised to provide food for man.

Building: All buildings are sited and erected on soils.

Construction: Various forms of construction like roads, railway, industries etc are constructed on soil.

Vegetation: All vegetation types form their basis on soil. Without soil, plants cannot get support and nutrient for growth.

Storage of nutrient: Soil provides plants and crop with all nutrients for their continuous existence.

Habitat of organisms: Soil provides the habitat for most organisms, especially bacteria, earthworms, termites and rodents.

Reservoir for water and air: Soil also acts as reservoir for air and water needed by living organism to survive.

Provision of minerals: soil is the source of all minerals used by man.

Evaluation Questions:

How does time affect soil formation?

Mention five importance of soil.

GENERAL EVALUATION QUESTIONS:

What is soil?

State factors affecting soil formation.

Mention five processes of soil formation.

Differentiate between rotation and revolution.

Describe a Great Circle.

Reading Assignment

Essential Geography, pgs 103-108.

Weekend Assignment

The type of water that is tightly held by the soil particles such that it is never available to the plant is known as (a) Capillary water (b) Hygroscopic water (c) Gravitational water (d) Field capacity.

Which of the following soils is made up of mainly quartz particles?(a) Clay soil (b) Sandy soil (c) Loamy soil (d) Humus soil

The best soil for agricultural activities is (a) Loamy soil (b) Sandy soil (c) Clay soil (d) Compost soil

The remains of the decomposition of plants and animals in soil constitute…….. (a) mineral matter (b) organic matter (c) soil water (d) living organisms

The smallest soil particle is __________ (a) Silt (b) Sand (c) Gravel (d) Clay

Theory

Draw and label a typical soil profile.

Describe any two zones of the soil profile.

Revisions

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