Agriculture Notes

Receipts

Issues

Commodity/Item

Quantity

Issued to

Quantity

Balance in Stock

Francis

4 years ago

Form 1 Agriculture Notes

Form 2 Agriculture Notes

Form 3 Agriculture Notes

Form 4 Agriculture Notes

FORM ONE AGRICULTURE NOTES

INTRODUCTION TO AGRICULTURE
The word Agriculture is derived from two Latin words Ager which means field and cultura that means cultivation. Therefore agriculture can be defined as field cultivation.
Livestock are all the domesticated animals.
Definition of agriculture:
Agriculture is defined as the art and science of crop and livestock production.
As an art
Involves use of learned skills and performing them manually (by hand). E.g.

Tilling of land.
Construction of farm structures.
Measuring distances.
Machine operations.
Harvesting of crops.
Feeding and handling animals.
Marketing of Agricultural produce.

As a science
It involves experimentation and application of scientific knowledge e.g. in areas such as:

Soil science (pedology) —study of soil.
Crop pathology—Study of crop diseases.
Entomology— Study of insects and their control.
Agricultural Engineering— soil and water conservation and farm power.
Genetics—Plant and animal breeding.

Production — Are activities that increase the quality and quantity of something.
Crop production activities include: land preparation, planting, fertilizer and manure application, weeding, pest control, disease control and harvesting.
Livestock production activities include:

Selection and breeding.
Feeding.
Rearing the young stock.
Parasite and disease control.
Housing.
Obtaining products from animals.

Branches of agriculture

Crop production: e.g. Field crop farming, pomology, Floriculture, olericulture.etc.
Livestock production: e.g. Apiculture, Poultry keeping, aquaculture.etc.
Soil science.
Agricultural Economics.
Agricultural Engineering.

Crop farming or Arable farming: Is the cultivation of crops on cultivated land. E.g. In pure stands (monocropping) or mixed stands (intercropping).
Include:

Field crops: Are crops grown on large areas of land. Are either Annual crops like cereals and pulses or perennial crops e.g. coffee, tea, sisal, cane etc.
Horticultural crops: Are perishable crops and are exported to earn foreign exchange. Include:
Floriculture: Growing of flowers e.g. tuber rose, roses, and carnations.
Olericulture: Growing of vegetables e.g. French beans, cabbages, tomatoes.etc..
Pomology: Growing of fruits e.g. avocado, mangoes and citrus.

Livestock farming: Include:

Pastoralism (mammalian livestock farming). Is the rearing of farm animals on pastures. E.g. cattle, goats, pigs, sheep, camels and rabbits.
Fish farming (Aquaculture); Is the rearing of fish in fish ponds. Fish is a cheap source of proteins.
Bee keeping: ( Apiculture); Is the rearing of bees in bee hives. Bees provide ; Honey and Wax, income, Medicine, pollination of flowers.etc.
Poultry keeping; Is the rearing of birds for meat and eggs, manure, income. Etc. Include classes of birds such as chicken ( most common), Ducks, geese, Ostrich, pigeon and Turkeys etc.

Agricultural Economics: Deals with utilization of scarce resources i.e. of land, labour, capital and management. It aims at maximizing output while minimizing costs.
Agricultural Engineering; Deals with use and maintenance of farm tools and equipment, farm machinery and farm structures.

FARMING SYSTEMS
A farming system is an organization of the farm and all the enterprises in relation to each other.
It can be extensive or intensive.
Extensive system
Characteristics

Large tracts of land.
Low capital investment per unit area.
Low labour per unit area.
Low yields per unit area.

Intensive system
Characteristics

Small tracts of land.
High capital per unit area.
High labour investment per unit area.
High yields per unit area.

Extensive or intensive farming can be carried out on small or large scale of land.
The scale of production depends on:

Level of technology.
Land availability.
Capital availability.
Skilled labour available.
Large Scale Farming

Characteristics

Large tracts of land.
Heavy capital investment.
Skilled labour and qualified man power.
High level of management.
It’s for commercial purpose.
Low operation costs per unit of production since it makes use of economies of scale.
Depends on efficient transport.
Requires good market system.
Most of the work is mechanized.
Provides more employment.

It includes plantation farming and Ranching.

Plantation farming.

Characteristics

Large tracts of land.
Production of only one crop.e.g. Tea plantations in Kiambu and Kericho, Coffee in Kiambu, Sugarcane in Muhoroni, Sisal in Mombasa, Pineapple in Thika.
Ranching : Is the keeping of livestock ( beef animals) in marginal range areas.

It is an improved pastoral-nomadism because:

Animals are enclosed in an area.
Diseases are controlled.
Pastures are improved.
Supplementary feeds and water are provided.
Pests and parasites are controlled.
There is provision of extension staff.

N.B The livestock carrying capacity is low because of limited pasture.
Ranching is becoming more and more common in Kenya because of:

High meat demand.
High population pressure on high potential areas.
Arable farming is becoming smaller.
Small Scale Farming

Characteristics

Small piece of land.
Use of improved technology.
Production of crops and livestock is spread throughout the year.
Goods are produced for subsistence or commercial purpose I,e sale of surplus goods..
Does not require heavy capital investment.

Advantages

Little capital is required.
Source of livelihood to small scale farmers.

Methods of Farming

Mixed Farming
This is the growing of crops and rearing of animals on the same farm.

Advantages

It is a method of diversification whereby should one enterprise fail, the farmer can benefit from the other.
There is mutual benefit between the crops and livestock where crops provide feed for livestock and animals provide them with farm yard manure.
There is maximum utilization of resources.

Disadvantages

Labour intensive.
High initial capital required.
Farmer’s attention is divided.
Nomadic Pastoralism

Pastoralism: This is the practice of rearing livestock on natural pastures.
Nomadism: This is the practice of moving from one place to another.

Pastoral –nomadism is therefore the moving of animals from one place to another in search of pasture and water.
This is common in the arid and semi-arid areas.
Shifting Cultivation
Farming on a piece of land continuously until it is exhausted after which the farmer moves to a new more fertile land.
It is applicable where;
- Land is abundant
- Population is sparse
- Number of livestock per unit area is low.
- Land is communally owned.

Advantages of shifting cultivation

It has low capital requirement
There is no pests and diseases build-up
Soil structure is maintained
No land disputes as land ownership is not individualized.

Disadvantages of shifting cultivation

Total yields per unit are is low
Farmers have no incentive to develop land and conserve water and soil
A lot of time is wasted when the farmer is shifting and building structures.
Not applicable in areas of high population density or where there is high population increase.

iv) Agroforestry
Agroforestry – Involves growing of trees and crops and keeping of animals on the same piece of land at the same time.
Suitable tree species for agroforestry

Leucaena leucocephala
Gravillea robusta
Calliandra catothrysus
Mangifera indica
Sesbania sesban
Lantana camara
Cajanus cajan

Advantages of Agroforestry

Saves labour since some operations can be done at once for both plants and trees
Gives higher combined yield
Provide wide variety of agricultural produce
Reduces the risks of total failure
Crops benefit from nitrogen fixing trees.
Trees help in holding the soil firmly
Some trees act as livestock fodder.
Provides a wider variety of agricultural produce.

Disadvantages of Agroforestry

Mechanization is difficult.
Use of pesticides and fertilizer may be difficult.
Productivity may suffer because the skills for managing the different trees

FACTORS INFLUENCING AGRICULTURE

HUMAN FACTORS.

They are factors in human beings or the way human beings do things.
The following is a list of human factors that influence agricultural production.

Levels of education and technology
This is translated as the ability of a producer who is a farmer to apply appropriate methods and techniques in production using available resources for example, Farmer weighing livestock food to ensure efficiency
Good education level makes a farmer able to understand and translate technical language in farming.
Health of the farmers
A healthy nation is a productive nation
The following are some of the diseases that contribute to lowering agricultural productivity
- Malaria,
- Tuberculosis,
- Typhoid,
- Pneumonia and HIV/AIDS

Effects of HIV/AIDS on farming

- Loss of skilled labour
- Time spent caring for the infected
- Money spent on treatment
State of economic development
The capital earned from economic activities such as farming is used to raise economic growth in the country.
Transport and communication network
Good and efficient infrastructure is important for the smooth flow of farm produce from the farm to the consumer.
The improvement of technology in communication has improved farmers access to important information from the research stations and other fellow farmers
Government policy on agricultural input and produce taxation
The government of Kenya, through different ministries formulates guidelines to be followed by producers of different products. After the guidelines and proposals are legislated they become policies
Availability of storage facilities
Cultural and religious beliefs.
Local and International market forces

Human Factors which improve production

Good health of the farmer
Availability of money
High taxation on imported agricultural produce
Availability of ready market for agricultural produce
Availability of storage facilities
Liberalized market

Human Factors which lower production

Restrictive cultural and religious beliefs
Poor road network
BIOTIC FACTORS.
These are living organisms that affect agricultural production.
Biotic factors influencing agriculture can be divided into the following classes.
- Crop pests: stalk borer damaging maize in the field
- Decomposers: Cause rotting of organic matter there by releasing nutrients for crop growth.

They help in improving soil structure through incorporating organic matter into the soil.

- Nitrogen fixing Bacteria: Nitrogen fixing bacteria are found in root nodules of leguminous plants. Improve crop production through increasing soil nitrogen content which crops require for proper growth.
- Livestock parasites: suck blood and transmit diseases to animals
- Pollinators: Bee pollinating maize flower. Pollination in crop production increases yields and viability of seeds.
- Predators: Eagles can eat chicken, rabbits among other livestock. Eagle can also eat insects and pests for example rats, moles and birds which destroy crops.
- Pathogens: Causes diseases in livestock and crops thereby lowering quality of produce. Increase cost of production when control measures are implemented. Introduce toxic substances into agricultural products thereby lowering the quality of the produce. Can cause death to crops and animals.

Effects of Biotic Factors on Agricultural Production
1. Pests

Feed on crops thereby lowering quantity of agricultural produce.
Feed on grains thereby affecting viability of the seeds
Act as disease vectors
Lower palatability of crop produce
Increase cost of production when control methods are applied
Create entry points for disease causing organisms

2. Parasites

Irritate livestock
Causes anemia in livestock
Some block alimentary canal
Lower rate of production in livestock
Increase cost of production when controlled
Some lower quality of hides and skins
Some absorb food meant for the livestock thereby lowering the level of production.
Some for example ticks transmit disease causing organisms.
CLIMATIC FACTORS.

Climatic factors include:

Rainfall
Poor rainfall distribution results to wilting of crops
Excess rainfall can cause soil erosion
Excess rainfall can result to crop failure due to flooding.

The four aspects of rainfall which affect agricultural production include:-

Rainfall Amount

Rainfall amount refers to quantity of rainfall received in a given area for a period of one year. Rainfall amount is measured using a rain gauge in millimeters per annum. The amount of rainfall determines the crops grown in an area.

Rainfall distribution

This refers to the spread of rainfall over the year. Rainfall distribution is very poor in Kenya and therefore irrigation is necessary to supplement the short supply.

Rainfall reliability

This refers to the certainty with which a given amount of rain is expected in a given place in the year.

Rainfall Intensity

This refers to the strength with which rain falls; it is therefore measured in terms of amount per hour.
Rainfall of low intensity is preferred as it improves water infiltration into the soil and causes less soil erosion.

Temperature
Temperature is the coldness or hotness of a place.
Temperature is measured in degrees Celsius using a thermometer.
Temperature is influenced by altitude and topography.
Temperature decreases with increase in altitude, such that for every 300 meters rise in altitude above sea level temperature decreases by1.7-2.2 degrees Celsius.
Each crop has a temperature range within which it can grow referred to as the cardinal range of temperature.
For crops to grow well and produce high yields, they require a narrow temperature range within the cardinal range referred to as optimum range of temperature

Effects of temperature on agriculture
Low temperature

Slow growth rate.
High incidences of disease such as CDB in coffee.
Improvement of quality in crops such as tea and pyrethrum.

High temperature

High evaporation rate hence wilting in crops.
Hasten the rate of maturity due to increased growth rate.
Improvement of quality in crops such as pineapples and oranges.
Increase incidences of diseases such as leaf rust in coffee.
Increased incidences of pest infestation such as aphids in vegetables.

Effects of altitude on agriculture

Kenya is divided into three ecological zones which include;
Low altitude zone o – 1500 meters above sea level
Medium altitude zone 1500 – 2500 meters above sea level
High altitude zone above 2500 meters above sea level

Crops perform differently when grown in each of these ecological zones and therefore each crop has its most suitable zone for maximum performance as illustrated below.

Wind

Wind refers to air in motion.

Below is a list of effects of strong wind on agricultural production.
Blowing and bringing rain bearing clouds
Destruction of farm structures
Strong wind may course lodging in weak plants.
Wind erosion on bare land
Increases rate of moisture evaporation
Increase spread of pests and diseases
Agent of dispersal.
Pollination in crops.
Light
- Light is the source of energy which plants require for photosynthesis.
- During photosynthesis, plants manufacture food using water and carbon dioxide in the presence of sunlight and chlorophyll.

Aspects of light that influence agriculture
i). Light intensity.

This is the strength with which light hits the surface of the earth.

ii) Light duration

This is the period of time the plants are exposed to light recorded using a Campbell sunshine recorder

Photoperiodism

This is the response of plants toward light duration.

Long day plants

These are plants which require more than 12 hours of lighting to flower and produce fruits or seeds e.g. some wheat varieties

Short day plants

These are plants which require less than 12 hours of lighting to flower and produce e.g Maize

Day neutral plants

These are plants which produce flowers regardless of the duration of lighting they have been exposed to e.g Tobacco.

iii) Light wavelength:

This refers to the type or quality of light. A wavelength is the distance between two corresponding points of a light wave.
Chlorophyll absorbs certain wavelengths of light which are not present in artificial light unless it is ultra violet or infra red.

NB/ Green houses can be used to control the temperature, relative humidity and light duration and intensity.

Relative Humidity.
This is the amount of water vapour held by air at a given temperature.
At high humidity the rate of evaporation is low and vice versa.
EDAPHIC/SOIL FACTORS
Soil is a mixture of weathered rock and decayed organic matter.
It supports plant growth by providing anchorage nutrients and water.
Topsoil covers most of the earth and it contains minerals, organic matter, air, water and living organisms.

Soil Formation

Soil is formed through the process of weathering.
Weathering is the breakdown and alteration of the parent rock near the earth’s surface.
Parent rock is first broken into smaller fragments and eventually into individual constituent minerals.
The individual minerals combine to form the soil.
Weathering is a continuous process and it takes hundreds of years to form a centimeter of the soil.
Weathering involves breakdown (disintegration) and building up (synthesis).
Weathering process is influenced by the following factors.
Climate.
Parent material.
Topography.
Living organisms.
Time.

Agents of The Weathering Process.

Physical agents.
In this case no chemical changes are involved.
These include wind, water, moving ice and temperature.
Strong winds carry materials which hit against each other and break into smaller fragments.
Raindrops hit the ground with some force causing soil erosion.
Moving ice causes rocks to disintegrate.
High temperatures in the arid areas cause the rocks to at different rates. During the night, temperatures drop making the rock to contract. The rock surface contracts faster than the inside. This unequal contraction causes the rocks to disintegrate.
In places with very low temperature, water gets into the cracks, freezes and becomes ice. As water turns into ice, it increases in volume pushing the rock apart hence disintegration.
Biological agents.
This involves living organisms.
Large animals like elephants and cattle exert pressure on rocks as they move causing them to break.
Mans activities such as mining, quarrying, road construction and earth moving breaks rocks into smaller fragments.
Bacteria and fungi help in the breakdown of plant and animal tissues (decomposition). These materials are incorporated into the soil.
Termites and moles bring to the surface large quantities of fine materials. This promotes weathering by aerating lower layers of the rocks.
Roots of plants force their way through rocks making them to disintegrate. They also produce acids during respiration which dissolves rock minerals. Decayed roots may mix with water forming organic acids which dissolves rock minerals.
Chemical agents.
This is the decay or decomposition of the rocks. It involves the following processes.
Carbonation.
As the rain falls through the atmosphere, it dissolves some Co2 forming weak carbonic acid.

Over time this acid reacts with the rock minerals particularly calcium carbonate causing decomposition.

The calcium bicarbonate formed in this reaction is soluble in water causing water to eventually dissolve the entire rock.
Oxidation.
Oxygen reacts with many elements found in rocks causing them to disintegrate.
Solution.
Hydrolysis.
Hydration.

Factors Influencing Soil Formation

Parent rock material
This influences the physical and chemical properties of the soil such as
The texture of the soil e.g. granite gives coarse grained soil.
Mineral composition of the soil e.g. rocks containing calcite, feldspar and ferro-magnesium minerals produce deep heavy soils rich in nutrients.
The rate of soil formation e.g. limestone is easily weathered in warm humid regions and the carbonates are easily soluble.
Since the parent material influences the physical and chemical properties of the soil, it therefore controls the type of vegetation in an area.
Climate
High temperature speed up the rate of chemical reactions.
Wind acts as a transport agent and carries the weathered materials from one place to another. Where a lot of weathered materials are deposited, the soils are deep and rich in nutrients.
Rainfall provides water which is an important reagent during the weathering process. A lot of rain may cause rocks to break hastening the weathering process.
Topography(Relief)
This is the shape of the land in relation to the underlying rock of the earth’s surface.
It may quicken or slow the weathering process.
The slope affects the depth of the soil and kind of vegetation growing in an area.
Soils found in flat land and low lying areas tend to be more fertile than those found on higher slopes. Such areas have deeper soils.
On a steep slope, erosion is high and such areas have shallow soils.
Living organisms(Biotic factors)
The presence of the various agents of biological weathering speeds up the process of soil formation.
Time.
The process of soil formation is very slow and takes a lot of time.
Deep mature soils are found where soil forming processes have taken place over a long period.
If the parent material is resistant to weathering agents, more time is required for the soil to mature.
Areas with severe soil erosion have a poorly differentiated soil profile.

SOIL PROFILE

This is the vertical arrangement of the soil horizons (layers).
The horizons show soil layers at different stages of development.
Soil forming processes are continuous and the soil develops in depth resulting in the formation of the distinct sequence of soil layers.
The layers differ from each other in terms of colour, organic matter content, chemical composition, porosity, depth and the arrangement of soil particles.

The horizons are;

Superficial layer.
It’s a thin layer consisting of dead decaying and decayed organic matter covering the soil.
Top soil (Horizon A).
It lies beneath the superficial layer.
It contains a lot of humus hence it’s darker than the other layers.
It’s well aerated and contains active living organisms.
It’s well drained and rich in plant nutrients.
Most of the roots are found here.
Sub soil (Horizon B).
Found beneath the top soil.
More compacted and less aerated than top soil.
May contain an impermeable layer called the hard pan which may prevent drainage and root penetration.
Minerals leached from top soil accumulate here hence this layer is referred to as the layer of accumulation.
It has clay deposits.
Substratum/weathered rock (Horizon C).
Made up of partly weathered rocks.
Has no humus.
Hard and impermeable to water.
Roots of big trees may reach this layer and draw water from it during the dry season.
Parent rock/Bed rock (Horizon D).
It’s found beneath the weathered rock. Soil is formed from this rock. It may contain ponds of water.

NB/ . Between any two bordering soil layers, there is a transitional zone whereby one layer gradually merges into the next one in the series.
The soil profile influences agriculture in the following ways.

Topsoil contains most of the soil nutrients, well aerated and has soil microorganisms.
A well developed profile holds more moisture for plant use than a shallow one.
Loosely packed subsoil allows easy root penetration, drainage and aeration.
Nature and composition of the bedrock determines the mineral components of the whole soil.

SOIL CONSTITUENTS

Mineral matter.
The mineral composition of the parent rock determines the mineral constituents of the soil.
The mineral matter makes the framework of the soil.
It holds the roots firmly in the soil giving anchorage to plants.
Between the particles are spaces which are filled with water and air.

Diagram

Organic matter.
When the dead materials rot, they are decomposed by bacteria and fungi to form the soil organic matter.
Humus is dead organic matter which is in the state of continuous chemical decomposition, transformation and construction.
Humus in the soil improves the soil structure.
Humus contains plant nutrients such as sulphates, nitrates, phosphates, calcium, magnesium, potassium etc.
Air.
The soil contains all the gases such as nitrogen, oxygen, Co2 and the rare gases.
Availability of air in the soil is influenced by the type of the soil and amount of water in the soil.
Oxygen is needed by plants during respiration. It is also required by microorganisms in the soil during decomposition and nitrogen fixation.
Excess Co2 in the soil is poisonous to plants and microorganisms.
For best crop performance, a balance of soil water and soil air has to be maintained.
Water.
Soil contains water. Soil water exists in three forms;
Superfluous water.
This is water occupying large air spaces (macro pores).
This water is loosely held by the soil and therefore easily lost.
The water is readily available to plants but not useful because excess water in the soil brings about poor aeration.
A lot of water in the soil causes leaching of nutrients.
Capillary water.
This is water occupying small pores (microspores).
It is held with grater force by soil particles.
It is available to plants and acts as a solvent for plant nutrients.
It is also referred to as available water.
It leaves most of the macro pores empty allowing aeration of the soil.
Hygroscopic water.
This is water that forms a thin film around the soil particles.
It is firmly held by soil particles making it not available to plants.
Clay particles have a lot of hygroscopic water but sandy soils contain very little hygroscopic water because sandy particles have weaker forces.

Importance of water to plants

A solvent for plant nutrients.
Raw materials for photosynthesis.
During transpiration plants lose a lot of water hence a cooling effect on them.
Water makes plant cells turgid hence support.
Living organisms (biotic factors)
They are important in the soil in the process of decomposition.
They are divided into ;
Soil microorganisms
They include bacteria, fungi and protozoa. They help in decomposition process.
Some bacteria e.g. Rhizobium spp helps in nitrogen fixation in legumes.
Some microorganisms are harmful because they cause diseases.
Soil macro organisms
They are larger organisms found in the soil such as moles, earthworms, termites, ants and plant roots.
They burrow in the soil aerating the soil and making it loose..

PHYSICAL PROPERTIES OF THE SOIL

Soil structure
This refers to the physical appearance of soil according to how the individual soil particles are arranged, packed or aggregated.
The soil structure type is determined by the general shape of the aggregates.
Soil structure class is determined by the size of the aggregates.
The soil structure grade is determined by the stability or cohesiveness of the aggregates.

Types of soil structures

Single grained structure.
There is no aggregation at all.
Particles are not cemented together. The particles are non-porous and spherical.
Mostly found in the top soil of sandy soils, arid climates and alkaline soils.
Crumby soil structure.
The aggregates are small, soft and porous irregular in shape.
Aggregates are not closely fitted together.
Granular soil structure.
The aggregates have irregular shape called granules.
Soil is very porous when wet.
Structure is found in the topsoil of cultivated soils and in the subsoil of soils under grass or bush.
Prismatic soil structure.
Aggregate are arranged vertically.
The vertical axis of each aggregate is longer than the horizontal axis.
When the tops are rounded, they are said to be columnar and when they have flat ends they are prismatic.
Platy soil structure.
The aggregates are arranged on top of one another in thin horizontal plates.
The structure has poor permeability, drainage and root penetration.
Structure is mostly found in top horizon of soils in the forest and in clay soils.
Blocky soil structure.
Aggregates are arranged in rectangular blocks.
Aggregates easily fit together along vertical edges.

Importance of Soil Structure on Crop Production
Soil structure influences:

Soil aeration.
Soil drainage and water holding capacity.
Plants root penetrability and anchorage.
Microbial activities in the soil.
Circulation of gases in the soil.

The following farming practices improve the soil structure

Application of inorganic manure into the soil.
Tilling the land at the right moisture content.
Crop rotation.
Minimum tillage.
Cover cropping.
Mulching.

Soil texture

It refers to the relative proportion of the various sizes of the mineral particles of soil.
Also defined as the coarseness or fineness of the soil when felt between the fingers.
Different soil particles have different sizes as shown below.

Particle	Size (Diameter) in mm
Stones (Gravel)	Above 2.00 mm
Coarse sand	Between 0.20 – 2.00 mm
Fine sand	Between 0.02 – 0.20 mm
Silt	Between 0.002 – 0.02mm
Clay	Below 0.002 mm

Determination of Soil Texture
This can be done through;

Mechanical analysis.
Chemical analysis.

Mechanical analysis
Apparatus
Garden soil, sieves of different measured mesh diameter, containers and weighing balance.
Procedure

Put a known amount of soil sample into a container.
Crush the soil lumps without breaking the particles.
Pass the soil through the sieve with the largest mesh diameter (2.00 mm) and shake vigorously.
Weigh the soil that remains on the sieve and record.
Repeat the process using other sieves with mesh diameters of 0.2mm, 0.02mm and 0.002mm always using the soil that passes through the previous sieve.

Observation

Soil particles left on first sieve of mesh diameter 2.00mm are called gravel.
From the second sieve of 0.20mm; coarse sand particles.
From the third sieve (0.02 mm); fine sand particles.
From the fourth sieve (0.002 mm); silt particles.
All the particles that pass through the fourth sieve are clay particles.

Importance of soil texture on crop production

Influences soil fertility.
Affects the organic matter content.
Influences the drainage of the soil.
Influences soil aeration.
Influences water holding capacity

Influences the capillarity or movement of water in the soil.

NB/ Based on texture, soil can be classified as;

Sandy soil. (50-80% sand, 20-50% silt and clay and 0.1-3% organic matter).
Are made up of largely sand particles (coarse textured).
Have large air spaces hence poor in water retention.
Easy to till (light soils)
Low fertility due to leaching of minerals.
Easily eroded.
Free draining.
These soils can be improved by addition of organic matter and fertilizers.
Silty loam (20-30% sand, 70-80% silt and clay and 0.1-4% organic matter).
Fine textured
Well drained
Good water holding capacity.
Moderately fertile and aerated.
Area acidic to moderate pH.
Clayey loam soils. (20-50% sand, 20-60% silt and clay and 0.1 – 6% organic matter).
Poorly drained and aerated
Fine textured
High capillarity and water holding capacity.
Slightly acidic to slightly alkaline.
Rich in plant nutrients.
Difficult to work on when dry or wet.
Are suitable for flood irrigation of crops like rice.
Clayey soils. ( > 40% clay content)
Made up of largely clay particles.
Have small pore spaces hence good in moisture retention.
Difficult to till (heavy soils)
Poorly drained.
Expand when wet, crack when dry.
High capillarity.
Rich in plant nutrients.
Are suitable for flood irrigation.
They can be improved by drainage.
Loamy soils. (30-50% sand, 50-70% silt and clay and 0.1 – 4% organic matter).
Moderately textured and drained.
Slightly acidic.
Do not erode easily.
Easy to work on.
Have a good water holding capacity.
They are the most suitable for crop production since they contain good amounts of plant nutrients and organic matter.
They can be improved further by planting cover crops to maintain fertility and by adding manures and fertilizers.

Soil Colour

This depends on the mineral composition of the rock and the organic matter content.
Soils containing a lot of iron are brownish, yellowish or reddish in colour.
Soils with a lot of silica are white.
Soils with a lot of humus are dark or grey.
Soil colour influences the soil temperature.
Dark soils absorb and retain more heat than light coloured soils.
Relatively high temperatures in the soil enhance microbial activity.

Soil pH

This refers to the acidity or alkalinity of the soil solution.
It is determined by the concentration of hydrogen ions (H+) or the hydroxyl ions (H-) in the soils solution.
pH is measured using the pH scale which ranges from 1-14.
A pH of less than 7 means that the soil solution is acidic.
A pH of more than 7 means that the soil is alkaline.
pH of 7 is neutral.
As the hydroxyl ions in the soil increase, the soil becomes more alkaline and vice versa.

Influence of Soil pH on Crop Growth

Determines the type of crop to grown in a particular area.
Affects the type of fertilizer to be used.
Affects the availability of some nutrients e.g. at low pH phosphorous and molybdenum are less available while high pH makes manganese, potassium, iron, boron and zinc less available.
Very acidic or very alkaline conditions affect activities of soil microorganisms.

Modifying Soil pH
The following are applied to the soil in order to lower its pH (Increase soil acidity)

Application of sulphur.
Application of acidic fertilizers such as sulphate of ammonia.

In raising its pH (increase alkalinity) the following is done.

Application of lime which is a basic compound which raises the soil pH after some time.
Application of basic fertilizers.

Agricultural Economics

Agricultural economics is defined as an applied science that aims at maximizing output while minimizing costs, by combining the limited resources of land, capital, labour and management to produce goods and services for use by the society over a period of time.

Basic Economic Concepts

Scarcity.
The factors of production such as land, capital, labour and management are scarce or limited.
The farmer therefore must decide on how to allocate the few/scarce resources to the many competing production needs.
Preference and Choice
Since the available resources are limited and production needs are many, a farmer has to make a choice of how to allocate these resources.
A farmer therefore has to choose one or several enterprises from very many.
The choice made is determined by factors such as needs of the society, farmer’s preference and ecological conditions.
Opportunity Cost
Since a choice has to be made from very many competing enterprises, some revenue has to be foregone. For example, a piece of land may be suitable for the production of maize and wheat.
If a farmer chooses o grow maize, the returns that the farmer would have obtained from wheat is foregone.
The foregone returns are called the opportunity cost. Opportunity cost is the revenue foregone from the best alternative.

Farm Records

These are documents kept in the farm showing farm activities over a period of time.
They should be neat, concise and complete showing actual amounts, weights, measurements or dates.

Uses of farm records to a farmer

Help to determine the value of the farm/ determine assets and liabilities.
Provide history of the farm.
Assist in planning and budgeting in various fields.
Helps to detect losses or theft in the farm.
Assists when sharing losses or profits (dividends) for communal owned farms/ partnership.
Help to settle disputes in the farm among heirs.
Help to support insurance claim e.g. against fire and theft.
Provide labour information like terminal benefits, NSSF due, Sacco dues for all employees.
Help to compare the performance of different enterprises within a farm or other farms.
Help in the assessment of income tax to avoid over or under taxation.
Records help to show whether the farm business is making profit or losses. This information helps in obtaining credit.

Types of Farm Records

Production Records
They show the total yield and the yield per unit of each enterprise such as the total number of litres of milk from the whole herd and from each cow.

Name /No. of cow	Days in the month							TOTALS
Name /No. of cow	1		2		3		etc
	AM	P.M	A.M	PM	AM	PM
1
2
3
4
etc
Totals

Inventory records
They show all the assets on the farm e.g. livestock, machinery, buildings, crops etc.
They are divided into two;
Consumable goods such as animal feeds, fertilizers, fuel, pesticides etc.
Permanent goods such as machinery, farm tools and equipment, buildings etc.

Consumable Goods Inventory

Permanent goods Inventory

Date	Commodity/Item	Quantity	Written off	Balance in Stock	Comment

Field Operations Records
They show all the activities being carried in the field such as date of ploughing, planting, fertilizer used etc.
They help to work out the cost of production for each field at the end of the season.
Breeding Records
They are kept to show the breeding activities and programmes for various animals on the farm.
There are different breeding records depending on the animals being reared.
Feeding Records
They show the type and amounts of feeds used to feed the animals.

Daily feeding record for the month of………………………………………………………… Enterprise ……………………………………………………………………………………… Type of feed…………………………………………………………………………………….
Date	No. of Animals	Amount Received (kg)	Amount Used (Kg)	Balance in Stock (Kg)	Remarks

Health Records
They show the health conditions of the animals. They show when actions such as vaccinations and deworming are to be done.
They help in the selection of the breeding stock. They also help in calculating the cost of treatment.

Date	Disease symptom	Animal(s) affected	Drugs used	Cost of treatment	Remarks

Marketing Records
They show the commodity, quantity, amount sold, date, rate per unit of the commodity, total value and where sold.

Commodity……………………………………………………………

Date	Amount sold	Price per unit (kshs)	Total Value (ksh)	Where sold	Remarks

Labour Records
They show the type of labour, date of employment, rate of payment, skilled and unskilled labour.
They are divided into two;
Muster Roll – this checks the number of days worked for and therefore determine how much to be paid to a worker.
This record shows the name of the worker, payroll number, days worked for, rate of payment, the amount of salary and signature.

Muster Roll

Name of Person	Pay Roll No.	Days					Days Worked	Rate of Pay (kshs)	Total Pay (Kshs)	Signature of Workers.
		1	2	3	4	5	Days Worked	Rate of Pay (kshs)	Total Pay (Kshs)	Signature of Workers.
Mr. X	08							25	@100/-	2,500/-
Mr. Y	09							25	@100/-	2,500/-

-Labour Utilisation Analysis. They show how labour is utilized on the farm and helps to determine labour allocation; labour requirement for the purpose of budgeting when labour is in peak demand or when to lay off unproductive labour.

No of hours Worked	Livestock Production	Crop Production	Machinery Maintenance	Date of Working	Remarks




Total cost

CROP PRODUCTION 1
LAND PREPARATION
Land preparation involves all the activities that make land suitable for planting such as

–ploughing/digging
-harrowing
-ridging
-rolling etc

A piece of land that has been prepared for planting is called seedbed. In a seedbed the planting materials germinate and grow to maturity and are harvested from same place.
IMPORTANCE OF LAND PREPARATION

-To kill the weeds.
-Encourage water infiltration into the soil.
-To aerate the soil.
-Incorporate manure and other organic matter into the soil.
-To destroy stages of crop pests such as eggs, larvae, pupa or adults burying them, exposing them to the suns heat or predators and starving them.
-To encourage root penetration into the soil.
-To make subsequent operations possible e.g. planting, fertilizer application, rolling and ridging.

OPERATIONS IN LAND PREPARATIONS
They include;

Land clearing.
Primary cultivation.
Secondary cultivation.
Tertiary operations.
LAND CLEARING

This is the removal of vegetation cover from the surface before tillage. This is done to prepare land for cultivation and as method of land reclamation. Land clearing is necessary under the following conditions.

When opening up a virgin land.
Where a stalk growing crop was previously planted such as maize.
Where land was left fallow for long time.
Where the interval between primary and secondary cultivation is long such that the land has reverted to the original virgin state.

Methods of Land Clearing

Tree felling. Axes, pangas and power saws are used to cut down trees. Bulldozers and root rakers are used in felling trees on a large scale. Removal of stumps and trash later follows.
Burning. The vegetation cover is set ablaze. The method should be discouraged as it destroys the soil organic matter, soil micro organisms and plant nutrients.
Slashing. This is done to cut small bushes and grasses using slashers, pangas or tractor drawn mowers.
Use of chemicals. Chemicals used to kill weeds are called herbicides.
Primary Cultivation

This follows land clearing,

Small scale farmers use jembes or fork jembes during hand digging.
In Large scale framing ploughing is done using mouldboard or disc plough.
Other farmers use ox ploughs.
Primary cultivation should be done before the onset of the rains. This ensures that all other subsequent operations are done in good time.

Importance of Primary Cultivation

To remove weeds.
To bury organic matter for easy decomposition.
To facilitate water infiltration and aeration.
To destroy soil borne pests by exposing them to predators and the sun.
To make planting easy.

Methods of Primary Cultivation

Hand digging. This is done by use of jembes, mattocks and fork jembes to cut and turn the soil slices.
Mechanical cultivation. This is the use of tractor drawn implements such as mouldboard and disc ploughs. Subsoilers, cultivators and chisel ploughs are used to break the hard pan. Subsoiling is the process of cultivating the soil with the purpose of breaking up the hard pan. Hard pans may be formed due to continuous use of heavy machinery on the land.

Importance of subsoiling

Breaking up the hard pan hence improving drainage.
Improving soil aeration.
Bringing to the surface leached minerals.
Improve root penetration.
Use of an oxplough. This is the use of ploughs drawn by oxen, donkeys or camels. The method is faster and more efficient than hand cultivation. It’s common in areas where land is fairly flat.

The following aspects should be considered when carrying out primary cultivation.

Time of Cultivation

Land should be prepared before the onset of the rains so as to;

Give enough time for the weeds to dry up and decompose into organic matter.
To allow CO2 and other gases to diffuse out of the soil while being replaced by oxygen.
Give enough time for subsequent operations to be done hence giving way to early planting.
Depth of Cultivation

This is determined by;

Type of crop to be planted. Shallow rooted crops do not deep cultivation. Deep rooted crops require deep cultivation.
Type of the soil. Heavy soils are hard when dry making jembes and fork-jembes to dig shallowly.
The implements available. Tractor drawn implements give deeper depth than hand operated tools.
Choice of the Correct Implements

This is determined by:

Condition of the land. If the land has a lot of stones and stumps, a disc plough is preferred because it rolls over the obstacles without braking.
Type of the tilth required. Very fine tilth requires different types of implements.
Depth of cultivation. When deep cultivation is required heavy implements are used. Light implements are used when shallow cultivation is needed.
Topography of the land. Tractor drawn implements cannot be used where the slope is very steep.
Implements available. A farmer can only use what is locally available.
Shape of the land. Some land shapes may not allow tractor drawn implements to be used efficiently e.g. where there are acute corners.
Size of the land.
Secondary Cultivation
This follows primary tillage.
This involves the refinement of the seedbed before planting.
It is also referred to as harrowing.
Small scale farmers can use pangas, jembes, fork-jembes, and garden rakes to break the soil clods and pulverize the soil.
Large scale farmers use factors drawn harrows such as disc harrows, spike toothed harrows, spring tine harrows.

IMPORTANCE OF SECONDARY CULTIVATION

To remove any weeds that might have germinated immediately after primary cultivation.
To break the soil clods into small pieces for easy planting.
To level the field so as to obtain the uniform depth of planting.
Incorporate organic matter into the soil in order to encourage decomposition before planting.

Factors determining the number of times secondary cultivation is done.

Size of the planting materials. Small seeds require a fine tilth than large seeds.
Slope of the land. If the land is hilly, less number of secondary cultivations are preferred to discourage soil erosion.
Moisture content of the soil. in dry soils less operations are preferred so as to conserve the soil moisture.
Condition of the land after primary cultivation. If after primary cultivation, a lot of trash is left, more harrowing operations should be carried out so as to incorporate the trash into the soil.
Tertiary Operations
They are carried out to meet the needs of certain crops.
They are conducted after land clearing, primary and secondary cultivations. They include;
Ridging
This is the process of digging soil in a continuous line and heaping it on one side to form a ridge (bund) and a furrow.
These ridges are used in planting crops such as Irish potatoes, cassava, groundnuts etc.
Ridges facilitate tuber expansion and easy harvesting of the root crops.
Furrows are made when planting sugarcane.
They help to conserve soil and water.
Rolling
This is done to compact the soil which is loose or of fine tilth.
This is done to prevent small seeds from being blown away by the wind and to prevent soil erosion.
This also increase seed soil contact.
Heavy rollers are used in large scale.
Leveling
This is making the soil surface flat and uniform to promote easy germination of small seeded crops.
Rolling ensures uniform germination of seeds.

MINIMUM TILLAGE
This is the use of a combination of farming practices that disturb soil the least. These farming practices include;

Application of herbicides in controlling weeds.
Timing cultivation/timely weeding of the previous crop.
Mulching. Mulch prevents weeds from growing.
Restricting cultivation to the area where seeds are to be planted. Weeds in the rest of the field are controlled by slashing.
Establishing a cover crop on the field.
Uprooting or slashing weeds in perennial crops.

Reasons for carrying out minimum tillage

Reduce the cost of cultivation. By reducing the number of operations.
To control soil erosion.
To maintain soil structure.
To conserve soil moisture. Continuous cultivation exposes the soil to sun’s heat hence evaporation of soil moisture.
To prevent root and underground structures disturbance.
To prevent exposure of humus to adverse conditions such as sun’s heat that cause volatilization of nitrogen

Soil Fertility I: (Organic Manures)
Soil Fertility: This is the ability of the soil to provide the crops with the required nutrients in proper proportions for high production.
Characteristics of Fertile Soils

Good Depth: Deep soil gives plants greater volume to obtain nutrients and also provide anchorage.
Good water holding capacity: This ensures that water is retained well for plant use.
Proper drainage: Well drained soils are well aerated facilitating healthy root development.
Correct soil pH. Different crops have different nutrient requirements.
Adequate nutrient supply. It should supply the crops with the nutrients they require in adequate amounts.
Free from excessive infestation of soil borne pests and diseases.

How Soil Loses Fertility

Leaching. Soluble minerals are carried to lower horizons beyond the reach of plant roots.
Mono cropping. Growing one type of crop continuously for a long time leads to the exhaustion of certain minerals that the plant uses.
Change of soil pH. Changes in the soil pH affect the activity of the soil microorganisms and the availability of certain soil nutrients.Use of some fertilizers can change the soil pH.
Continuous cropping. Crops take up a lot of nutrients during their growth which are never returned to the soil. This makes the soil deficient of these plant nutrients.
Burning of vegetation cover. This destroys the organic matter hence destruction of the soil structure.
Soil erosion. When the fertile top soil is carried away, the soil loses its fertility.
Accumulation of salts. This is as result of irregular rainfall and insufficient removal of salts from the soil especially in the arid and semi arid areas. Accumulation of salts is called salinisation

Maintenance of Soil Fertility

Control of soil erosion to enhance soil infiltration onto the soil and reduce surface run off.
Weed control to prevent competition for nutrients. Water space and light with crops. It also reduces pests and diseases.
Carrying out crop rotation, this helps to control accumulation of crop pests and diseases on the farm. It also helps to ensure maximum utilization of nutrients.
Use of inorganic fertilizers helps to add nutrients to the soil e.g. CAN, DAP, Urea etc..
Use of organic manure helps to supply organic matter to the soil.
Minimum tillage which helps to maintain soil structure and prevent soil erosion.
Intercropping (Mixed cropping) of leguminous and non- leguminous crops fix nutrients and improve fertility.
Proper drainage by breaking hard pans or creation of water channels this ensures proper aeration.
Control of pH to almost neutral to ensure proper functioning of micro-organisms which help in decomposition of organic matter.

Organic Manures
They are obtained from plant and an animal remains after decomposition.
Role/ Importance of Organic Matter Improves soil structure – aeration, drainage absorption and retention.

Improve water holding capacity of the soil.
Increases soil fertility e.g. carbon nitrogen etc.
It provides food and shelter to soil microorganisms.
Help to keep PH of soil stable (Buffers soil pH).
Reduces toxicity of plant poisons that have build up in the soil as a result of continuous use of pesticides and fungicides etc.
Humus gives soil dark appearance making the soil to absorb heat. This moderates soil temperature.

Problems Associated with the use of Organic Manures

Bulkiness – they have low nutritive value per unit volume hence required in large volumes.
Laborious in application and transportation – this is due to their bulkiness.
They spread diseases, pests and weeds – i.e. if they are made from materials that are contaminated.
Losses of Nutrients – if they are poorly stored, soluble nutrients are easily leached and some become volatilized when exposed to the hot sun.
If used when not fully decomposed the plant does not benefit from them.

Types of Organic Manures
They are of three types:

Green Manure.
Farm Yard Manure (FYM)
Compost Manure.

Green Manure

It is made of green plants which are left to grow until flowering and then are incorporated into the soil through ploughing. The crops used include; cowpeas, groundnuts, Lucerne, beans, sunflower etc.

Characteristics of Plants used as Green Manure

Should be leafy or highly vegetative.
Should have high nitrogen content hence leguminous ones are preferred.
Should have a fast growth.
Must be capable of rotting quickly.
Should be hardy i.e. Capable of growing in poor conditions.

Reasons Why Green Manure is not Commonly Used

Most crops used for green manure are food crops
Takes time for the manure to decompose delaying planting
Most of the nutrients are used up by micro-organisms in the process of decomposing the green manure
Green manure might use most of the soil moisture and leave very little for the next crop

Farm Yard Manure (FYM)

This is mixture of animal waste (urine and dung) and crop remains used as animal beddings.
The quality of Farm Yard Manure is determined by the following factors.
Type of the animal used –
Dung from fattening animals has a high level of nutrients than that from a dairy cow.
Non ruminants such as hens and pigs give very rich dung in terms of nutrients.
Type of food eaten – nutritious feedstuffs give manure with more nutrients.
Type of litter used – wood shavings and sawdust are slow to decompose and contain very little nutrients as compared to leguminous ones which give manure rich in nutrients.
Method of storage – for manure to retain its nutritive status, it must be stored in place with a leak proof roof and a concrete floor.
Age of the farm yard manure –well rotten manure is rich in nutrients and is easy to apply.

Preparation of the farm Yard Manure

Provide materials such as grass or wood shavings in the animal house to serve as bedding.
Animals deposit their droppings and urine on the bedding and mix them by trampling.
After some time Collect the used animal bedding/litter and other rotten plant residues;
Store collected materials under roof/shed to prevent leaching and oxidization of nutrients;
Turnover the materials regularly;
Sprinkle water if dry;
Leave the material to rot completely before use

Compost Manure

This is a type of manure made from decomposed materials such as kitchen refuse, plant and animal remains.
The following factors are considered when selecting the site for making compost manure.
Well drained place – this avoids waterlogging which may cause leaching of nutrients.
Direction the prevailing wind – this aims at preventing bad smells from being blown to the homestead.
Size of the Farm –thesite should be centrally placed on the farm.
Accessibility – this makes transportation of the manure possible.

Preparation of Compost Manure

There are two methods of preparing compost manure;
- Indore Method (pit Method)
- Four Heap System (Stack Method).

Indore Method (pit Method)

A pit 1.2m long by 1.2m wide and 1.2m deep is made.
Te materials to be composted are placed in layers in the following order;
Fibrous materials such as maize stalks form the foundation.
They are followed by a layer of grass, leaves or any kitchen refuse material.
A layer of well rotten manure is then applied to provide nutrients for the microorganisms.
A thin layer of wood ash is applied to improve the level of phosphorous and potassium in the manure.
A layer of top soil is then added to introduce microorganisms that are required to decompose the organic materials..
The above sequence of layers is repeated until the pit is full.
A layer of soil is added to cover the pit.
During the dry season, the materials should be kept moist by adding water.

Term 3 Form 4 Agriculture Exam Paper 1

Term 3 Form 3 Agriculture Exam Paper 1

form 3 biology notes

2019 MOKASA Physics Paper 1

Term 3 Form 2 Agriculture Exam

revision notes biology form 2

revision notes biology form 1

form 3 business studies notes

form 4 history notes

Term 3 Form 4 Agriculture Exam Paper 2