CONTENTS
Major Biomes in The World
Population Studies
Facors Affecting Population and Ecological Factors
Major Biomes of the World
Zones of different biomes occur from the equator to the Arctic and to the Antarctic due to differences in climate. In the equatorial and tropical areas where temperature and rainfall are high all year round, tropical forests occur, while in the cold arctic regions, treeless plains called tundra are found. Climates change with distance from the equator and also with height above sea level, as such zones of different biomes occur from the equator to the poles and on a mountainside.
Examples of Major Biomes of the World
- Tropical rainforests: These consist of dense forests with many types of trees, epiphytes, and climbers. Rainfall is abundant throughout the year, and an average temperature of 27ºc is recorded throughout the year. Located around the equator e.g,. around the coasts of West Africa, the Amazon basin of South Africa, etc.
- Temperate forests: These consist of broad-leaved deciduous trees that shed their leaves during winter. A lot of different plants grow at many levels from the ground as the trees are not densely packed as in the tropical forest. It has a moderately wet climate and a dry or cold season. Examples are found in North America, the lowlands of North–West Europe (e.g. France), and Britain.
- Coniferous forest: These consist of needle-leaved, evergreen conifers e.g. pines, firs, and spruces. Only a few types of trees are found in these forests. Other plants such as shrubs, ferns, and mosses are also present. The temperature is cool, and the rainfall is light. There is also light snow. Examples are found in Eurasia and North America.
- Temperate shrubland: Consists of drought-resistant shrubs, aromatic plants, and dwarf trees. The temperature is very high (over 30ºc), rainfall is low, the summers are hot and dry, and the winters are mild and rainy. Examples are found in North-Eastern Brazil, Australia, and close to the Sahara in West Africa.
- Savanna :These are tropical grasslands with few scattered trees. It has a moderately dry climate, a warm dry season, and a hot rainy season. Examples are found in Central America, the Interior of Brazil, West Africa, East Africa, and Southeast Asia.
- Temperate grassland: Consist of large stretches of perennial grasses growing on very fertile soil. Examples are the steppes, prairies, plains, pampas and veld. The climate is moderately dry with a cold winter and hot summer. Examples are Found in the interior continents in Asia, North America, South America, (Argentina), South Africa and Australia.
- Desert: Consist of very sparse vegetation which are mainly succulent perennials with deep root systems and annuals which exist mainly as seeds, germinate and grow rapidly, flower and produce seeds during brief periods of rain. Rainfall is very low and temperature is very high. E.g. Sahara desert (North Africa), Arabian Desert (Arabia), e.t.c.
- Tundra:Consists of treeless marshy vegetation composed mainly of dwarf shrubs, grasses, sedges, lichen and moss. The climate is clod with long icy winters and very short summers. The average temperature is 10ºc. Examples are the coastal strip of Greenland, Northern Canada and Alaska, Arctic seaboard of Eurasia.
- Mountain vegetation:Consist of evergreen rain forest occurring on the slopes of mountains. The forests are less luxuriant than the tropical rainforest. The Afro-alpine vegetation occurs at altitudes above 3000m on mountains. The vegetation consist mainly of heaths, grasses, and sedges. In Africa, it is found in Cameroon mountain, Kenya highland and Kilimanjaro. Temperature decreases with altitude. Rainfall is heavy on the windward side and less on the leeward side of the mountains.
EVALUATION
- List six biomes of the world
- Briefly discuss two biomes of the world.
Population Studies
A population is defined as the total number of organisms of the same species living together in a given area at a particular time. In any ecosystem, the community is made up of many populations of different species.
To study a habitat’s populations, the following are usually investigated.
- The type of organisms in the habitat: This involves listing all the different types of populations found in that particular habitat. This helps to determine the relationships that exist between the different organisms in the habitat.
- The dominant species: This refers to the species of organisms in a community that exert a great influence on the habitat and on the other populations. Dominance may be expressed in terms of their number, size, the portion of space occupied, and contribution to the energy flow of the habitat.
- The characteristics of the population: This refers to;
(a) Population size: The total number of individuals of the same species in the habitat (the total numbers of individuals in a population). A large population stands a better chance of surviving unfavourable conditions such as fires, diseases, harsh climate changes, while a small population can be easily wiped out. A large population also has the advantage of increasing its vigour through breeding which invariably increases its ability to withstand adverse conditions.
(b) Population density: This is defined as the number of individual organisms per unit area or volume of the habitat.
Mathematically represented as; Population density=Total population or Population / size of the area of habitat |
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Example: If an area of land of 100m² has an elephant grass population of 1000 plants, the density of elephant grasses will be;
Total number of individualsTotal area=1000100m2 elephant grasses=10∅∅1∅∅m2 elephant grasses=10 elephant grasses/m2
(c) Population frequency: This refers to how often the species occurs at different sites in its habitat. It is recorded as the number of times the organism is sited (seen).
(d) Population growth rate: This refers to the total and final effect of birthrate and death rate of organisms in the habitat.
(e) Percentage cover: This is the area of ground or space covered (or occupied) by a given species its habitat. It is expressed in percentage.
(f) Distribution: This refers to the way in which individuals of a particular population are arranged in a given habitat. The individuals may live in clumps, they may be evenly spaced or randomly spaced.
Example: If the western half of the habitat contained ¾ of the elephant grasses, then,
Density =34×1000=75Ø5Ø=15 grasses/m^2
Methods of Studying Populations
To conduct population studies the following procedure is used;
- Choose the habitat to be studied
- Choose a sampling method
- Identify the species in the habitat
- Collect, count and record the different types of organisms present.
- Repeat the population studies at different periods.
The following methods can be used to study specific populations:
- Collection of plants: In a small area plants are easy to count and their distribution can be recorded on a map or scale diagram of the area, however for larger areas quadrats or transects are used.
(a) Quadrat Sampling: A quadrat is made of a square or rectangular piece of wire, plastic, wood or metal frame with predetermined area. E.g. the area of a quadrat may be 25cm². A quadrat is used to sample the number of plant species in a habitat. It is not suitable for sampling animals because they move around so much. A quadrat is used by throwing it over the shoulder at random several times and on each landing, the area covered/enclosed by it is observed. The type of plant species and their number within the quadrat are recorded. From the results, the average number of plant per m² is calculated. If the area of the habitat is known, the total number of plants it contains can be estimated.
Permanent quadrats, with mapping grids attached, can be made to study seasonal variations of plants. These quadrats are sturdier, larger and remain permanently fixed on a marked area.
(b) Transect method: A marked tape is used in this method. The tape is marked at convenient intervals and then stretched across the area to be studied. The plants encountered at the interval marks are counted and recorded. This procedure is repeated a few times. In this way, a fairly accurate estimate of the number and types of plants in the habitat are obtained. Plants are usually collected in plastic bags and then pressed and dried in a plant press. The dried plants are mounted on stiff paper, fixed in position with masking tape/cellotape and labeled with both the scientific and common names.
- Collection of Animals: Animals are more difficult to collect than plants; however their presence can be inferred by looking for signs of their presence such as nests, eggs, feaces, tracks, feathers, etc and by studying the vegetation with which they are associated. To study animals different types of nets and traps are used in capturing them. The following methods can be used.
(a) Capture – Recapture method: In this method, animals of one type in a particular area are caught, counted, and marked with ink and released. Their number is recorded as A1. The following day, another set is captured and the number is recorded as A2.This second batch may include animals that had been caught and marked the previous day; their number is recorded as A3. The population of animals present in the area is found using the formula;
Population in area A1×A2A3
This method is based on the assumptions that;
- Individuals do not move out of or into the ecosystem
- The marked individuals are randomly distributed in the population.
- The marked individuals are a random sample.
- The initial capture and markings do not influence recapture.
- That none of the marks have worn off during the interval between the two catches.
NB: The results obtained by this method are approximations.
(b) Collection of soil animals with quadrats: The soil animals in an area can be studied by collecting samples of soil from several sites chosen by tossing a quadrat randomly. A 25% sodium chloride solution is added to each soil sample and the animals are collected as they float in the solution.
For earthworms, the sites chosen with the quadrat are irrigated with 25% formalin solution, and the earthworms are collected as they move to the surface of the soil.
EVALUATION
- What are the major investigations carried out when studying a habitat?
- A pond with an area of 200m² has a duckweed population of 1,500 plants. Find
(a) The population density
- Explain what a Tullgren’s funnel is and what it is used for.
- Make a list of traps used for capturing animals for study, and describe how captured animals are kept or preserved.
Factors Affect Populations
Populations in a habitat may show changes in size or distribution. These changes may be due to;
- Natality (birth rate): Increase in birth rates especially during breeding periods, lead to increase in population size while a decrease in birth rate results in a decrease in the population.
- Mortality (death rate): This refers to the rate at which organisms die. An increase in the death rate leads to a decrease in the population and vice versa.
- Immigration:This is the movement of organisms from different habitats into a particular habitat. This increases the population size of the habitat being moved into.
- Emigration:It is the movement of organisms out of a habitat ant it leads to a decrease in the population. Emigration may be caused by scarcity of food, unfavourable conditions, seasonal climate changes or breeding purposes.
- Availability of food:An abundance of food in a habitat tends to lead to an increase in the population of organisms due to increase in birth rate (reproduction) and influx of organism from other areas and vice versa.
- Seasonal climate changes:Adverse climate changes may lead to a decrease in number of organisms due to death or emigration. Favourable conditions leads to an increase in population.
- Natural disastersg. fire; flood, drought etc. may lead to a decrease in population due to death and emigration.
(others include availability of water, availability of space, war)
Ecological Factors
These are factors in the environment that influence life in the ecosystem. These factors affect the living organisms or cause changes in the habitat (aquatic or terrestrial).
These factors are grouped into two
- Biotic factors
- Abiotic factors
- Biotic factors
The biotic factors are those concerned with the effects of plants and animals on one another in a given habitat e.g., competition, predation, parasitism, etc.
- Abiotic factors
Abiotic factors include climate topographic (or physiographic) and edaptic (soil factors). Variations in the ecological factors bring about changes in the habitat. Abiotic factors also determine the type of biotic community found in a habitat.
Ecological Factors Affecting Terrestrial Habitats
A. Topographic Factors: These factors are associated with the structure of the habitats e.g. effects of hills, valleys, plains, mountains, and rivers. These factors bring about variation in the vegetation and types of animals in an area.
Topographic factors include:
(a) Altitude (elevation): This refers to height of the land above sea level. This affects the growth of plants and the level of erosion in an area. As altitude increases, temperature falls by approximately 1ºc per 150metres, as a result of this, mountain tops are generally cold places cold air causes clouds to condense and fall as rain, thus the annual rainfall on mountains is high especially on the windward side. As one ascends a mountain, the air become less dense, there is less of it to filter the sun’s rays, so organisms at the top of mountains are exposed to intense solar radiation.
(b) Slope: Water flows faster on a steep slope than on a gentle slope as such, run-off is greater and less water sinks into the soil on steep slopes. Also, erosion tends to be more. Gentle slopes are more favourable to plant growth.
(c) Exposure: This refers to the extent to which living things are not protected from climatic factors such as rainfall, sunshine and wind. Exposure is usually high on mountains and low within a forest. Winds tend to be stronger in exposed habitats and relative humidity is lower than in sheltered habitats. Low degree of exposure ensures the availability of nutrients to plants.
B. Edaphic Factors: These are factors related to the nature of soil particles. The word edaptic refers to the influence of soils on plants and animals. Differences in the soil of a locality usually produce difference in vegetation since plants are dependent on the soil and the type of plants determine the type of animals that will be found in the habitat. Edaphic factors include:
(a) Soil Types: this could be sand, loam or clay. The type of soil determines the fertility of the soil, its porosity and water retaining capacity.
(b) Soil Texture: The amount of sand, silt and clay in a soil affects its water retaining capacity. Soil texture refers to the degree of fineness or coarseness of soil particles. It also affects leaching and erosion.
(c) Soil structure: This refers to the arrangement of the various soil particles in soil. This affects the level of soil aeration and percolation and the type and level of soil organisms in the soil.
(d) Soil pH: The pH of soil also affects the type of plants in the habitat e.g. some plants grow best in acid soils while others prefer alkaline conditions.
C. Atmospheric factors (Relative Humility): This is a measure of the amount of moisture in the air. It affects the rate of transpiration from plants and evaporation from animals. As relative humidity falls, evaporation and transpiration rise as such organisms that live in areas where humidity is low must prevent water loss from their body surfaces. E.g. in deserts, the leaves of plants like the cactus are reduced to spines to prevent loss of water.
Ecological Factors That Affect Aquatic Habitats
- Salinity: This refers to the concentration of salts in the water. Salinity affects the movement of water and salts across the body tissues of aquatic organisms. Salinity is low in fresh water, high in sea water and moderate in brackish water. Aquatic organisms have to maintain the osmotic balance between their body fluids and their aquatic surroundings in order to survive. Those living in fresh water have adaptive features which enable them get rid of excess water that enters their bodies; those living in sea water have body fluids with almost the same salt concentration as the sea water while those living in brackish water have body tissues that can tolerate wide and sudden fluctuations in salt concentration of their body fluids.
- Depth Of Water: As a body of water becomes deeper, the amount of light and dissolved oxygen become less, so at the bottom of deep lakes and oceans, there may be too little light for photosynthesis as such no green plants can grow there. Shallow bodies of water such as ponds are usually well supplied with oxygen and light and support a lot of plants and animals. However, these habitats are subject to evaporation and drying up in the dry seasons, the plants and animals therefore have to develop adaptation to survive such conditions. E.g. formation of cysts by some protozoans.
- Turbidity: This refers to cloudiness of water. It is caused as a result of suspended materials in water. Light penetration is low in cloudy or muddy water and this hinders green plants from growing at some depths.
- Dissolved Gases: This refers to dissolved oxygen. Oxygen concentration of water decreases with depth. Oxygen is required by most aquatic organisms for respiration as such organisms which live in stagnant or very deep water have to be able to tolerate low levels of oxygen concentration. Organisms that require high oxygen concentration, usually live near the surface of deep water or in fast-flowing rivers and streams e.g. the simulium larva lives in fast flowing streams.
- Tides and Wave Action:Tidal movement refers to the regular rise and fall in the level of the sea. Organisms which live in the intertidal zone of a seashore have to be able to tolerate being alternately covered by sea-water and then exposed to air twice daily.
Wave action is also important both in the intertidal and splash zones of the seashore. Most organisms in these areas are attached to the substratum or live in burrows. Some attach themselves firmly to rocks and other immovable objects, while some others have hard body covering to prevent evaporation of water from their bodies. Waves cause the aeration of the surface waters of the open sea, thus enabling aquatic organisms to have sufficient supply of dissolved gases for their needs.
- Speed of Flow (currents):Plants and animals are affected by the rate at which the water flow. Some organism’s e.g. spirogyra prefer to live in slow moving stagnant water while others e.g. Tilapia, prefer fast-flowing water. Many organisms which live in fast-flowing rivers and streams have adaptations which serve to prevent them from being swept away from their support by currents in water. Water currents increase aeration and the turbidity of the water. Currents also carry warm water to colder regions and this affects the distribution of organisms.
- Density: Density of water varies with the type of habitat. The density of fresh water is about 1.00 while that of sea water is 1.028 at atmospheric pressure and 0ºc. It is easier to move through air than water because water is more dense, as such aquatic organisms have a streamlined shape to help them move easily through water. Some organisms that float on the surface are sensitive to changes in density e.g. eggs of aquatic organisms sink to different depths depending on the density of the water.
Ecological Factors Common To All Habitats
The ecological factors that affect both the terrestrial and aquatic habitats are mainly climatic e.g. temperature, rainfall, relative humidity, wind, high intensity hydrogen ion concentration (pH) and pressure. Of these factors temperature and rainfall determine the type of vegetation in a region.
- Temperature: This refers to degree of hotness or coldness. Variation in temperature results in hot or cold climate. It affects the terrestrial habitat more than the aquatic habitat. In the terrestrial habitat temperature varies with season, while in the aquatic habitat it decreases with depth. A rise in temperature usually results in a higher rate of transpiration in plants and higher rate of metabolism in most animals (except homoiotherms). Most living organisms are killed by high temperatures and it reduces the performance of some. Low temperatures lead to inactivity or dormancy. In some organisms (e.g. tadpoles, insect larvae and bacteria) a rise in temperature results in faster rate of growth and shorter length of life-cycle. A higher rate of evaporation of water from the soil, ponds and lakes and a lower relative humidity are also observed.
Too high or too low temperature inhibits the growth and life activities of living things. However most organisms have various adaptive features that allow them to live at low or high temperatures e.g. Bears living in the arctic regions have very thick furs.
2. Rainfall: Rain is the main source of water to most organisms. It also supplies water to soil on which land plants depends. It is also the major source of water in rivers, ponds, lakes, oceans etc. The amount of rainfall in an area has a major effect on the type of vegetation found there. Low amount of rainfall usually causes drought on land and drying up of freshwater habitats (which leads to death of animals). Too much rain causes floods and destruction of vegetation through erosion.
Rainfall increases relative humidity and also increases turbidity of streams, rivers and lakes. Rainfall is necessary for seed germination. It helps to dissolve nutrients in the soil thus making them available to plants. It is also necessary for the vegetative growth of most crops e.g. flowering and proper development of groundnut pods.
Rain water may form puddles and small pools which provide temporary habitats for mosquito larvae, algae and tadpoles. It is also necessary for the start of new termite colonies.
3. Light: Light is necessary for photosynthesis in green plants. It affects the productivity of crops and facilitates flowering and fruiting in some plants. Light is the ultimate source of energy for all organisms. Light affects the activities of animals e.g. some animals are active during the day (butterfly) while others are active at night (cockroaches). The ultra-violet rays of the sun enable animals to manufacture vitamin D.
4. Wind: Winds are important because they cause water currents and waves thus mixing water and making food available in aquatic habitat, Winds carry rain bearing clouds. They also determine a season e.g. In Nigeria, the S/W wind is responsible for the rainy season while the N/E wind brings the harmattan. Wind has drying effects (on land) and so it increases the rate of transpiration in plants. In an area exposed to strong winds only xerophytes can grow there. Winds also aid pollination of flowers and dispersal of seeds and fruits. Winds increase the rate of evaporation from the soil and in savanna and desert areas it is a major cause of soil erosion. Winds also play an important role in the establishment of insects in a given area.
5. Pressure: Atmospheric pressure decreases from the depths of the ocean upwards to the higher attitude of the atmosphere. Plants and animals have special adaptations to a particular level of pressure to enable them survive. For instance in the oceans, the pressure increases by 1.03kg/m² every 10m, so organisms found at depths of about 400m live in conditions of enormous pressure but are well adapted to such conditions and will not survive at levels with lower pressure.
6. Hydrogen ion Concentration (pH):This refers to the acidity or alkalinity of the soil or water in a habitat. pH affects the types of plants and animals in a habitat. E.g. some plants grow best in acidic conditions while others can only grow in alkaline conditions. In aquatic habitats pH varies with the salinity of the water. Freshwater is neutral while sea water is fairly alkaline (pH 8.5). Organisms like the freshwater mollusks (Mytilus) are usually absent in water with a pH less than 6 (i.e. acidic water).
Biotic Factors Affecting the Ecosystem
Biotic factors refer to the effects of plants and animals on themselves or one another. The biotic factors include:
- Parasitism:One organism called the parasite lives in or on another organism called the host. The parasite benefits while the host suffers harm or may die.
- Competition:This may occur between organisms of the same species or different species. Competition may be for food, space, mates, etc. One of the organisms will eventually over come the other.
- Commensalism:This involves two organisms living together. One of the organisms (the commensal) benefits from the association while the other organism neither benefits nor is harmed.
- Predation: This involves an organism (called the predator), killing / feeding on another organism (the prey).
- Trampling: Grazing animals trample on plants and invertebrates.
- Pollinationof flowers by insects (this aids continuity and increase).
- Aeration of the soilby some animals e.g. earthworms, termites, etc.
- Support provided to climbing plantsby trees or bigger plants.
- Shade provided by trees, etc.
EVALUATION
- State five ecological factors that (a) affect terrestrial habitats (b) affect aquatic habitats (c) are common to both habitats
- Discuss two of each set of factors mentioned above.
Simple Measurement of Ecological Factors
- Temperature: This is measured using a mercury thermometer read in degree celcius (ºc). At least two readings are taken in a particular area of the habitat being studied to ensure accuracy. A soil thermometer is used for soil temperature, a maximum-minimum thermometer for recording the highest and lowest temperature of the day, and a waxed bulb thermometer for temperature of water at different depths in a pond, stream, etc. The waxed bulb thermometer is usually tied to a string knotted at regular intervals to indicate depth.
- Rainfall: This is measured with a rain gauge. This can be made from a tin can, a plastic funnel and a 50ml measuring cylinder. The amount of rainfall is calculated in millimeters, with the formuladD2×h= rainfall for a period where;d = diameter of mouth of funnelh = height of rainwater in the cylinderD = diameter of collecting cylinder
Usually, the height of the water in the cylinder indicates the amount of rainfall after every storm
- Relative Humidity: This is measured using a wet and dry bulb hygrometer, or a pocket hygrometer. The pocket hygrometer is exposed to air and the reading taken after the lever arm has stabilized. The wet and dry bulb hygrometer is swung in air for 30seconds and the reading on the thermometers taken and converted to relative humidity units using a table of conversion. The hygrometer may also be kept in a Stevenson’s screen.
- Wind:Wind has both speed and direction. Wind direction is measured / indicated by a wind vane while wind speed is measured with an anemometer (recorded in ms־¹).
- Light Intensity: Is measured by a light meter or photometer. The readings on the meter are expressed in lux units. The greater the intensity of light, the higher the readings on the meter and vice-versa.
- Pressure: Atmospheric pressure is measured with a barometer. It is measured in millibars (or millimeters of mercury, mmHg). The readings are taken directly from a scale.
Picture: Modern Aneroid barometer
- Water Depth: Is measured with a meter rule or a marked and weighted line knotted at one meter intervals. The meter rule is attached to a weighted line to ensure that it is vertical in water.
- Water Flow: To measure the speed of flow of a water body, the distance (m) covered per unit times by a float is taken. The float may be a weight tube and the distance covered has to be pre-determined. Speed of the current is calculated in meters per second. A simple water-speed meter can be used to compare the speed of water flow at different positions in a stream
- Turbidity: Is measured by slowly sinking a weighted white disc called a secchi disc into the water, noting the depth at which it just cannot be seen anymore. This is not a real measurement of turbidity but a useful method of comparing the turbidity of different aquatic habitats, different sites of the same habitats, or at different times.
- Slope: Is measured with a simple slope gauge constructed with a meter rule to which a protractor is attached. The angle readings on the protractor are read and recorded. Small angles indicate a steep slope.
- Height: The height of objects like tall trees is measured using the principle of similar triangles.
Relationship between Soil Types and Water Holding Effects of Soil on Vegetation
Soil is the uppermost layer of the earth’s crust which provides support and nutrient for plants growth and habitat for some animals. The soil is a complete mixture of mineral matter, humus, air and living organisms. Soil is classified on the basis of the size of the particles present in it. Soil particles vary in size and chemical composition, depending on the types of rock from which they were formed and how they were weathered. Those soils with a high proportion of sand are known as sandy soils; those with a high proportion of clay and silt are called clayey soils and those with nearly equal amount of sand, clay and silt are known as loamy soils. The proportions of these particles in the soil have an important effect on their properties and on the types of plants found on them.
Types of Soil
- Sandy Soil: This contains 80% sand and gravel and 20% of the other types of particles taken together. Large coarse particles of sand and gravel predominate.
- Clay Soil: This contains more fine clay (60%) and silt particles.
- Loamy Soil:This contains a mixture of both clay and sand with some humus in roughly equal proportion. Loamy soils are the most fertile and the humus in it gives it a mellow tilth i.e. the size of the soil particles and the air spaces between the particles are the most suitable for cultivation.
Effects of Soil On Vegetation
Soil factors play an important role in determining the vegetation of a region. Soils account for the variation in type of plants that are found in regions with similar climates. To support a rich growth of plants, soil must have the following characteristic;
(i) A rich humus content
(ii) A rich mineral content
(iii) A good water-holding capacity; this is determined by the amount of humus and clay in it.
(iv) Good soil porosity; determined by the humus, sand content and soil texture.
Sandy soil is low in plant nutrient and so it supports scanty vegetation or grassland. Clay soil has a little more amount of plants nutrients than sandy soils and thus can support light vegetation such as shrubs. Loamy soil is very fertile and can support luxuriant vegetations such as a forest.
Water Holding Capacity of Soil
Water holding capacity of soil refers to the ability of the soil to retain water. The amount of water retained by any soil depends or the size of the particles, the humus content, aeration, temperature and presence of microbes. Clay and humus retain a higher amount of the water than sand. In clay soil, most of the water is held firmly to the surface of the soil particles (hygroscopic water) and this is not usually available to plants. In sandy soil very little amount of water is retained as most of it drains off. Loamy soil is able to retain more water within its particles. This is called capillary water and is available for plants use.
Practical Guide on Soil
- Experiment to Determine The Water Retaining Capacity of Soil Types
Title of experiment: To compare the porosity and water holding capacity of three soil types
Materials required: Three measuring cylinders of 100cm³, cotton wool, three funnels, water, dry sand, dry clay, dry loam, stop clock, balance.
Method: Stand the three funnels in the three measuring cylinders and block the funnels with cotton wool.
- Place an equal weight of dry sand, dry clay and dry loam in the three funnels respectively.
- Pour 50ml of water onto each sample at the same time and allow to drain.
- Allow the set up to stand for an hour or until the water has stopped dripping through each funnel.
- Read the level of water in the measuring cylinder.
Calculations:
(a) Rate of drainage/porosity is calculated from the amount of water collected in the measuring cylinder. The more the water, the more porous the soil sample. Usually porosity is highest in sandy soil because it has large pore spaces and large particle sizes, followed by loamy soil and then clay soil which has the least drainage because of its tiny pore spaces and fine particles .
(b) Water holding/retaining capacity is calculated as follows;
Volume of water added to soil =50ml
Volume of water collected in cylinder =xml
Volume of water retained in the soil =(50−x)ml
The percentage of water retained in each of the soil samples will be
50−x50×100=Y%
Observation: It is observed that water drained out from the sandy soil faster than the loamy soil and finally the clay soil. It was also observed that clayey soil retained more water than loamy soil and least retained by the sandy soil.
Conclusion: Sandy soil is more porous than loam which is more porous than clay. Clayey soil retained more water than the loamy soil and the sandy soil retained the least amount of water.
- Experiment To Compare The Capillary Action Of Soil Types
- Take three wide glass tubes and plug each at one end with cotton wool.
- Nearly fill the tubes with the three soil samples separately.
- Clamp the tubes upright in a trough of water,
- Allow the set-up to remain for 3-6 hours
- Observe every 30mins.
Observation: It will be observed that at the early stage of the rise of water in the three tubes, it was faster in sandy soil than the clay and loamy soil samples, however by the end of the experiment the water had risen to the highest levels in loam, followed by clay but remained at a low level in the sandy soil.
Conclusion: Loamy and clayey soils have greater capillary actions due to their tiny pore spaces. The presence of organic matter in loam also enhanced its capillary. The sandy soil had poor capillary action because of its large pore spaces and large particles.
EVALUATION
- List the three major soil types.
- Discuss the constituents of the soil types mentioned.
- Compare the water holding capacities of the three soil types.
- Describe how the height of a forest tree can be measured?
- In a table outline the properties/characteristics of the three major soil types (at least ten properties)
- Make large well labeled drawings of a maximum and minimum thermometer; a rain gauge, a wind vane, an anemometer, a light meter, a secchi disc, a barometer and a slope gauge.