"Environment is everything which surrounds an organism and influences its life. It includes biotic and abiotic components."
The materials present in natural environment and useful to living organisms are called natural resources. A resource satisfies human needs. Water, air, sunshine, land, soil, forests, wildlife, fishes, minerals and power resources all are useful to human. All basic needs of food, shelter and clothing are supplied by natural resources on earth. Natural resource includes total natural environment, that is the entire surface of earth, because all parts of earth's surface are of some use to man as they contribute to the production of necessities and comfort to mankind.
Substances used by man in bulk for survival are called resources and since they are found in nature, they are called natural resources. Probably, the earth is the only planet on which life exists. Life exists on earth because it has all the physical conditions necessary for sustaining it. An ambient temperature, water and food are the basic needs of all life forms. These basic needs of the life forms are to be met by the resources available on the earth and the energy from the sun. The resources available on earth include land [Lithosphere], water [Hydrosphere] and Air [Atmosphere]. The outer crust of the earth is called lithosphere. The water present on the earth's surface and underground constitute hydrosphere. About 75% of the earth's surface is covered with water. The air that covers the whole of the earth like a blanket is called atmosphere.
The life sustaining zone of the earth where the lithosphere, the hydrosphere and the atmosphere interact and make life possible is called the biosphere. Living things constitute the biotic component of biosphere. The air, the water and the soil form the abiotic or non-living component of the biosphere.
Air is a mixture of many gases like nitrogen, oxygen, carbon dioxide, water vapour and some others present in the atmosphere. Air is an important inexhaustible natural resource.
Note: Composition of air is the result of life on Earth. In planets such as Venus and Mars, where no life is known to exist, the major component of the atmosphere is found to be carbon dioxide. In fact, carbon dioxide constitutes up to of the of the atmosphere on Venus and Mars.
Earth's atmosphere has a series of layers. Moving upward from ground level, these layers are named the troposphere, stratosphere, mesosphere, thermosphere and exosphere.
(1) Troposphere:
It extends from 0-12 km. Nearly all-weather changes occur in this layer. Most clouds appear here.(2) Stratosphere:
It extends from 12-50 km. It contains ozone layer at the height of 15-30 km. Ozone absorbs most of the UV rays coming from the Sun. Commercial passenger jets fly in the lower stratosphere.(3) Mesosphere:
It extends from . Most meteors burn up in mesosphere.(4) Thermosphere:
It extends from . Many satellites actually orbit Earth within the thermosphere.(5) Exosphere:
Region at about 700 km above the Earth's surface.(i) Role of atmosphere in climate control: The atmosphere acts as a protective blanket for the Earth. Since atmosphere is a bad conductor of heat, it keeps the average temperature of the Earth fairly constant during the day and even during the course of the whole year. The atmosphere prevents the sudden increase in temperature during daylight hours. And during the night, it slows down the escape of heat into outer space. Thus, the Earth receives just the right amount of heat, which helps in climate control and allows living organisms to exist. Note: Moon is about the same distance from the sun that the Earth is. Despite that, on the surface of the moon, with no atmosphere, the temperature ranges from to . (ii) The movement of air-winds: The atmosphere gets heated from the radiation that is reflected back or reradiated by the land or water bodies. As a result of heating, convection currents are set up in the air. Since land gets heated faster than water, the air over land gets heated faster than the air above water bodies.
In coastal regions, during the day, the air above the land gets heated faster and starts rising. So a region of low pressure is created and air over sea moves into this area of low pressure. The movement of air from one region to the other region causes winds. During the day, the direction of wind would be from the sea to the land. At night, both land and sea starts to cool. Since water cools down slower than the land, the air above water would be warmer than the air above land, thus the direction of wind would be from the land to the sea.
Movement of wind due to uneven heating of the air:
Note: Various other factors also influence these winds - the rotation of the Earth and the presence of mountain ranges in the paths of the wind are a couple of these factors.
(iii) Rain:
When water bodies are heated during the day, a large amount of water evaporates and goes into the air. The wind carries the water vapour to various places. The air gets heated and rises up carrying the water vapour with it. This condensation of water is facilitated by if some particles could act as the 'nucleus' for these drops to form around. Normally dust and other suspended particles in the air perform this function.Once the water droplets are formed, they grow bigger by the 'condensation' on these water droplets. When the drops have grown big and heavy, they fall down in the form of rain. Sometimes, when the temperature of air is low enough, precipitation may occur in the form of snow, sleet or hail. Rainfall patterns are decided by the prevailing wind patterns. In large parts of India, rains are mostly brought by the south west or north east monsoons.
It is an undesirable change in the physical, chemical or biological characteristics of the air. It is caused due to an increase in the content of harmful substances (air pollutants) in air such as oxides of nitrogen and sulphur, etc. The major sources of air pollution are burning of fossil fuels like coal and petroleum, automobiles, thermal power plants and industries.
(i) Air pollution affects the respiratory system causing breathing difficulties and diseases such as bronchitis, asthma, lung cancer, tuberculosis and pneumonia. (ii) Burning of fossil fuels like coal and petroleum release oxides of nitrogen and sulphur inhalation of these gases is dangerous. These gases also dissolve in rain to give rise to acid rain. (iii) The combustion of fossil fuel also increases the amount of suspended particles in air. These suspended particles could be unburnt carbon particles or substances called hydrocarbons. The presence of high levels of all these pollutants, reduce visibility in cold weather where water also condenses out of air forming smog. Smog is an indication of air pollution. (iv) Regular breathing in the polluted air increases the incidence of allergies, cancer and heart diseases.
(i) The oceans, rivers, streams, lakes, ponds, pools, polar ice caps, water vapour, etc. collectively form the hydrosphere, the main component of which is water. Major part of water is found in seas and oceans and is saline. (ii) Water is the most essential component of life. (iii) Fresh water is found in icecaps at the two poles and on snow
(i) All cellular processes take place in water medium. (ii) All reactions that take place within our body and within the cells occur between substances that are dissolved in water. (iii) Substances are also transported from one part of the body to the other in a dissolved form. (iv) Organisms need to maintain the level of water within their bodies in order to survive. (v) Terrestrial life forms require fresh water because their bodies cannot tolerate or cannot get rid of the high amount of dissolved salts in saline water. (vi) Water regulates the Earth's temperature. It also regulates the temperature of the human body, carries nutrients and oxygen to cells, cushions joints, protects organs and tissues and removes waste. (vii) The availability of water is the major resource which determines the diversity of life on land. (viii) Thus, water is essential for sustenance of life.
Note: Availability of water is not the only factor that decides the sustainability of life in a region. other factors like the temperature and nature of soil also matter. But water is one of the major resources which determine life on lands.
Water pollution:
It is contamination of water of rivers and lakes with unwanted and harmful substances. Water is said to be polluted when there is any physical, biological or chemical change in its quality that adversely affects living organisms and makes it unfit for use. Ways by which water is polluted: (i) Agricultural substances such as fertilisers and pesticides are used to increase crop yield and some percentage of these is washed into the water bodies that pollutes the water. (ii) Sewage from homes and wastes from factories are dumped into rivers or lakes. (iii) Hot and cold water discharge from industries make a change in temperature which is harmful for aquatic organisms. (iv) All these affects the balance among various organisms that are found in water bodies.Thus, water pollution refers to: (i) Addition of undesirable substances to water bodies: The substances like fertilisers and pesticides used in farming, mercury salts used by paper industries could be poisonous. There could also be disease-causing organisms like the bacteria which causes-cholera. (ii) Removal of desirable substances from water bodies: Industrial or household waste reduces the dissolved oxygen in water bodies, thereby affecting the aquatic life. (iii) A change in temperature: Aquatic organisms can stay alive in a certain range of temperature. Sudden change in temperature of water bodies is dangerous for aquatic organisms and affects their breeding. The eggs and larvae of many animals are particularly susceptible to temperature changes.
It forms the upper surface of the land and supports plant growth. Soil is the layer of unconsolidated particles derived from weathered rock, organic matter (humus), water and air. Soil is an important resource that decides the diversity of life in an area. The outermost layer of our Earth is called the crust and the minerals found in this layer supply a variety of nutrients to life forms. Formation of soil: The formation of soil depends on the parent rock material, the climate and topography of the area, the organisms present in the soil and the time over which the soil has been developing. Over long periods of time, thousands and millions of years, the rocks near the surface of the Earth are broken down by various physical, chemical and some biological processes. The end product of this breaking down is the fine particles of soil.
Factors or processes for soil formation
(i) The Sun: The Sun heats up rocks during the day so that they expand. At night, the rocks cool down and contract. The unequal expansion and contraction in different parts of the rock results in the formation of cracks and ultimately rocks break up into smaller pieces. (ii) Water: Water helps in the formation of soil in two ways: Firstly, water could get into the cracks in the rocks formed due to uneven heating by the Sun. If this water freezes, it will widen the cracks.Secondly, fast flowing water carries big and small particles of rock downstream, causing breakdown of rock particles into smaller, finer particles through their abrasive effects. (iii) Wind: Strong winds also erode rocks down. They also carry sand from one place to the other like the water does. (iv) Living organisms also influence the formation of soil. While lichens grow on surface of rocks, they release certain substances that cause the rock surface to powder down and form a thin layer of soil. Small plants like moss and roots of big trees also break the rocks. Components of soil: soil is a mixture. (i) It contains small particles of rocks that vary in size (sand > silt > clay). (ii) It contains bits of decayed living organisms which is called humus. (iii) Soil also contains various forms of microscopic life. (iv) It contains nutrients and availability of which depends on the rocks from which it was formed. (v) It contains air & water.
Top soil
It is the topmost layer of the soil that contains humus and living organisms in addition to the soil particles. Humus is a major factor in deciding the soil structure because it causes the soil to become more porous and allows water and air to penetrate deep under the ground. The quality of the topsoil is an important factor that decides biodiversity in that area.It is the removal of useful components from the soil and addition of other substances, which adversely affect the fertility of the soil and kill the diversity of organisms that live in it. Use of large amounts of fertilizers and pesticides destroy the soil structure by killing soil microorganisms that recycle nutrients in the soil. It also kills the earthworms which are instrumental in making the
Soil pollution rich humus thus affect the fertility of soil.
It is the removal and thinning of the fertile top soil from a region due to climatic and physical processes, such as high rainfall and wind etc. Soil erosion occurs easily where the soil is not covered by vegetation.
Causes of soil erosion
(i) Wind causes soil erosion by carrying away the top soil particles. (ii) Rain causes soil erosion on unprotected top soil by washing it down. (iii) Improper farming or tilling and leaving the field fallow for long time causes soil erosion. (iv) Frequent flooding of rivers causes soil erosion by removing the top soil of the fields near the river banks. (v) Deforestation also leads to soil erosion.Prevention of soil erosion
(i) It can be prevented by intensive cropping. (ii) It can be prevented by providing proper drainage canals around the fields. (iii) Soil erosion in hilly areas can be prevented by practising terrace farming. (iv) It can be prevented by planting trees and sowing grasses. (v) It can be prevented by constructing strong embankments along the river banks.The cyclic flow of nutrients between non-living environment and living organisms is known as biogeochemical cycles. It is the process of transfer and circulation of the essential chemical nutrients such as Carbon, Hydrogen, Oxygen and Nitrogen in a biosphere.
The whole process in which water evaporates and falls on the land as rain into the sea via river is known as water cycle. It is the whole process in which water evaporates and falls on the land as rain and later flows back into the sea via rivers. But all the water that falls on the land does not immediately flow back into the sea. Some water moves inside the soil and reaches the underground water. Some of the underground water comes up to surface through springs or wells. Plants also release water to the atmosphere through transpiration. Water is also released into the atmosphere from soil, rivers and oceans by evaporation. Three important processes in water cycle are evaporation, condensation and precipitation. Evaporation add water as vapour to the atmosphere. The air gets heated and rises up carrying the water vapour with it. As this air rises, it expands and cools causing the water vapour in the air to condense in the form of tiny droplets. The presence of dust and other suspended particles in air also facilitates the process of condensation.
Once the water droplets are formed, they grow bigger by the 'condensation' on these water droplets. When the drops grow big and heavy, they fall down in the form of rain. Water leaves the atmosphere through precipitation. The amount of water, the atmosphere can hold depends on abiotic factors, such as temperature and air pressure. Once the atmosphere becomes saturated with water vapour, precipitation occurs in the form of rain, snow, hail or fog.
Water cycle in nature The Nitrogen cycle: The source of nitrogen is atmosphere which contains 78 percent of nitrogen in the form of gas. Nitrogen is thus an essential nutrient for all life forms. Nitrogen-cycle in the biosphere involves the following important steps. (i) Nitrogen fixation: The process is converting atmospheric nitrogen into usable form (nitrates, ammonium ions) which are soluble in water. This is done by various fixing bacteria e.g. Rhizobium, blue green algae and bacterium Azotobacter. Other than these bacteria, the only other manner in which the nitrogen molecule is converted to nitrates and nitrites is by a physical process. During lightning, the high temperature and pressure created in the air convert nitrogen into oxides of nitrogen which dissolve in water to give nitric and nitrous acids and fall on land along with rain which is then utilised. (ii) Ammonification: It is the process of decomposing complex, dead organic matter into ammonia. This is done by microorganisms living in the soil e.g. bacteria and fungi. (iii) Nitrification: It is the process of conversion of ammonia into nitrites and then into nitrates. This is done by nitrifying bacteria e.g. Nitrosomonas and Nitrobacter. (iv) Denitrification: It is the process of reducing nitrates present in the soil to release nitrogen gas back into the atmosphere e.g. Pseudomonas.
Thus, there is a nitrogen cycle in nature in which nitrogen passes from its elemental form in the atmosphere into simple molecules in the soil and water, which gets converted into more complex molecules in living beings and back again to the simple nitrogen molecule in the atmosphere.
The carbon cycle:
Carbon is found in various forms on the Earth. It occurs in the elemental form as diamond and graphite. In abiotic environment, carbon is present in the following forms: (i) As carbon dioxide in the atmosphere. (ii) As carbonate and hydrogen-carbonate salts in various minerals. (iii) As dissolved carbonic acid and bicarbonates in water. (iv) As fossil fuels like coal, petroleum and natural gas.Plants utilise the atmospheric carbon dioxide in photosynthesis to produce carbohydrates which are taken by herbivores and then pass through small and large carnivores. Many marine animals use carbonates dissolved in sea water to make their shells.
The Green house effect:
Greenhouse is a glass enclosure which is used for growing tropical plants in colder climates even in winters. The interior of a greenhouse remains warm because glass allows solar radiations to pass through but prevents their reradiation due to the longer wavelength of the same. Similar principle is used to describe an atmospheric phenomenon known as greenhouse effect. It is an effect occurring in the atmosphere because of the presence of certain gases (greenhouse gases) e.g. , etc., that absorb infrared radiation and prevent the escape of heat from earth thereby increasing the temperature worldwide. Thus, increase in carbon dioxide content in the atmosphere would cause more heat to be retained by the atmosphere leading to global warming.The oxygen cycle:
Oxygen constitutes about 21 percent of the atmospheric gases. It is also present in dissolved form in water bodies and helps in the survival of aquatic life. Oxygen is also present in combined forms such as carbon dioxide and water . In the earth's crust oxygen is found as the oxides of most metals and silicon and also as carbonate, sulphate, nitrate and other minerals. It is also an essential component of most biological molecules like carbohydrates, proteins, nucleic acids and fats.Oxygen cycle maintains the level of oxygen in the atmosphere. Oxygen from the atmosphere is used up in three processes, namely combustion, respiration and in the formation of oxides of nitrogen.
Almost all living organisms, plants, animals and decomposers take oxygen from their surroundings and utilise it for respiration.
Oxygen is returned to the atmosphere in only one major process, i.e., photosynthesis. Green plants are the major source of oxygen in the atmosphere.
Ozone layer:
This is a layer of ozone ( ) present in the stratosphere of atmosphere surrounding the Earth. It is poisonous in nature. It protects the earth from harmful radiations like ultraviolet radiations. (i) When the harmful chemicals like chlorofluorocarbons (CFC) (Carbon compounds having both fluorine and chlorine which are very stable and not degraded by any biological process) are released into the air, it accumulates in the upper atmosphere and reacts with ozone, resulting in reduction of the ozone layer. (ii) Thus, the ozone layer in the atmosphere becomes thinner and gets depleted allowing more ultraviolet rays to pass through the earth. There is a hole in Ozone layer above Antarctica.Satellite picture showing the hole (magenta colour) in the ozone layer over Antarctica
Harmful effect of ozone layer depletion:
Due to ozone depletion living organisms expose to ultraviolet radiations which may cause following effects - (i) Ultraviolet radiation is highly damaging to organisms. It causes skin cancer in human beings. (ii) These cause damage to eyes and also cause increased incidence of cataract disease in eyes.Note:
(Session 2025 - 26)