Environmental Chemistry Class 11 Notes Chemistry Chapter 14

By going through these CBSE Class 11 Chemistry Notes Chapter 14 Environmental Chemistry, students can recall all the concepts quickly.

Environmental Chemistry Notes Class 11 Chemistry Chapter 14

→ Environmental Pollution: Atmospheric, Tropospheric & stratospheric.

→ Water Pollution: Causes of water pollution & International standards of drinking water.

→ Soil Pollution: Pesticides-Intecticides & Herbecides & Fungicides

→ Industrial wastes: Recycling of wastes

→ Strategies to Control Environmental Pollution: Waste management.

→ Green Chemistry: Green Chemistry in day to day life.

→ Environmental Pollution: Environmental pollution is the effect of undesirable changes in the surrounding that have harmful effects on animals & plants & human beings.

→ Atmospheric pollution: Tropospheric & stratospheric.

→ Global warming: About 75 % of solar energy reaching the earth is absorbed by the earth’s surface, which increases its temperature. The rest of the heat radiates back to the atmosphere. Some of the heat is trapped by gases such as CO2, CH4 & O3 & C.F.Cs. & water vapours in the atmosphere. Thus they add to the heating of the atmosphere. This causes Global Warming.

→ Green House Effect: Atmosphere traps the sun’s heat near the earth’s surface & keeps it warm. This is called the Greenhouse effect because this makes the earth perfect for life.

→ Acid Rain: When the pH of rainwater drops below 5.6, it becomes acidic. Acid rain is caused by the presence of oxides of N & O in the atmosphere.

Acid rain is harmful to agriculture, trees & plants & washes away nutrients needed for their growth,

→ Classical Smog: It is a mixture of smoke, fog & SO2 chemically it is a reducing mixture & so it is called reducing smog.

→ Photochemical smog: The main components of the photochemical smog result from the action of sunlight on unsaturated hydrocarbons & nitrogen oxides produced by automobiles & factories. Photochemical smog has a high concentration of oxidizing agents & is, therefore, called oxidizing smog.

→ Ozone hole: In October 1979, A zone of lowered ozone concentration was detected over Antarctica which occurs mainly during September-October & gets replenished during November-December. This is called the ozone hole.

→ B.O.D.: Biochemical oxygen demand.

→ C.O.D.: Chemical oxygen demand.

→ Green Chemistry: It involves processes & products that reduce or eliminate the use or the generation of hazardous substances.

Chapter In Brief:
Environment Pollution:
It is defined as the effect of undesirable changes in our surroundings due to natural sources or human activity that have harmful effects on plants, animals and human beings. A.substance, which causes pollution to one or more components of the ecosystem are called pollutants. Pollutants can be solid, liquid, or gas.

Pollutants are of two types.
1. Non-Biodegradable Pollutants: The materials which do not undergo degradation or degrade very slowly in the environment like DDT, plastic materials, heavy metals, many chemicals, nuclear wastes etc.

2. Biodegradable Pollutants: The materials which are easily decomposed by the micro-organisms either by nature or by suitable treatment are called biodegradable pollutants. Examples; Domestic waste like discarded vegetables, cow dung etc.

→ Atmospheric Pollution: The lowest region of the atmosphere in which human beings along with other organisms live is called the troposphere. It extends up to the height of- 10 km from sea level. Above the troposphere between 10-15 km above sea level lies the stratosphere. Atmospheric pollution is generally studied as tropospheric and stratospheric pollution.

→ Tropospheric Pollution: It occurs due to the presence of undesirable solid or gaseous particles in the air.
1. Gaseous air pollutants: These are oxides of sulphur, nitrogen and carbon, hydrogen sulphide, hydrocarbons, ozone etc.

2. Particulate pollutants: These are dust, mist, fumes, smoke and smog”.
1. Gaseous air pollutants
(a) Oxides of sulphur are produced when sulphur-containing fossil fuel is burnt. SO2 is poisonous to both animals and plants. Particulate matter present in polluted air catalyses the oxidation of SO2 to SO3.
2SO2(g) + O2(g) → 2 SO3(g)

The reaction can also be promoted by ozone and hydrogen peroxide.
SO2(g) + O3(g) → SO3(g) + O2(g)
SO2(g) + H2O2 → H2SO4

(b) Oxides of Nitrogen: At high altitudes when lightning strike’s N2 and O2 present in the air combine to form nitric oxide.
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Rate of formation of NO2 Then NO reacts with O3 is faster.
NO(g) + O3(g) → NO(g) + O2(g)
The irritant red haze in the traffic and congested places is due to oxides of nitrogen. NO2 is a lung irritant.

(c) Hydrocarbons are formed by incomplete combustion of fuel used in automobiles. They are carcinogenic.

(d) Oxides of carbon
1. Carbon monoxide (CO) is one of the most serious air
pollutants. It is highly toxic. It blocks the delivery of oxygen to the organs and tissues. It is produced as a result of incomplete combustion of carbon
C(s) + \(\frac{1}{2}\)O2(g) → CO(g)
Insufficient quantity

It binds to haemoglobin for which it has 200-300 times more affinity than oxygen and forms carboxy-haemoglobin thus the oxygen-carrying capacity of blood is greatly reduced.

2. Carbon dioxide (CO2): It is released into the atmosphere by respiration and burning of fossil fuels. It is also emitted during volcanic eruptions and limestone burning to produce lime for cement plants. Normally a percentage of CO2 in the atmosphere is only 0.03 by volume. The increased amount of CO2 in the air is mainly responsible for global warming.

Global Warming and Greenhouse Effect:
Some of the heat from solar energy is trapped by gases such as carbon dioxide, methane (CH4), ozone, chlorofluorocarbons compounds (CFCs) and water vapours in the atmosphere. They add to the heating of the atmosphere. This causes global warming.

The natural greenhouse where there is an ecological balance of CO2, water vapours which are continuously being converted to carbohydrates and a fresh supply of oxygen during photosynthesis by a lot of green plants, flowers, vegetables makes the earth perfect for life. Sun’s warmth is retained on the earth giving sufficient heat to the soil and plants which emit infrared radiations.

If the amount of CO2 crosses the delicate 0.03% the natural greenhouse balance is disturbed. It is a major contributor to global warming. CFCs are damaging the ozone layer. Other contributors to global warming are CH4, N2O, and ozone. Cutting down forests and trees, burning fossil fuels, production of fertilizers, man-made industrial chemicals etc. add to global warming.

Acid Rain:
Due to the presence of CO2 in the atmosphere, the pH of rainwater is 5.6.
H2O(l) + CO2(g) ⇌ H2CO3(aq)
H2CO3(aq) ⇌ H+(aq) + HCO3 (aq)

When the pH of rainwater falls below 5.6, it is called Acid Rain Various human activities release oxides of Nitrogen and Sulphur in the atmosphere. SO2 and NO2 are thus major contributors to acid rain.
2SO2(g) + O2(g) + 2H2O(l) → 2H2SO4 (aq)
4NO2(g) + O2(g) + 2H2O(g) → 4HNO3(aq)

Acid rain is harmful:

  1. For plants, trees and agriculture as it washes away nutrients needed for their growth.
  2. For human beings and animals as it causes respiratory ailments.
  3. An aquatic ecosystem is disturbed when this add rain reaches water objects like rivers, lakes etc.
  4. It corrodes water pipes resulting in the leaching of heavy metals such as iron, lead and copper into drinking water.
  5. Acid rain damages buildings and other structures made of stone or metal. The Taj Mahal is being corroded by acid rain.
    CaCO3 + H2SO4 → CaSO4 + H2O + CO2

As a result, the beautiful white marble of which the Taj Mahal was built centuries ago is rendered lusterless and is being slowly eaten away.

Particulate Pollutants:
They are of two types.
1. The Viable Particulates: They are bacteria, fungi, moulds, algae etc. which are minute living organisms that are dispersed in the atmosphere. They cause allergy to human beings and bring disease to plants.

2. Non-Viable Particulates: They are classified according to their nature and size as follows:
(a) Smoke particulates are solid or a mixture of solid and liquid particles formed during combustion of organic matter,
(b) Dust particles. Over 1 mm in diameter produced during the crushing, grinding and attribution of solid materials, sawdust, sand and cement particles, fly ash, dust storm etc. are the typical examples of this type of particulate emission.
(c) Mists are produced by particles of spray liquids and by condensation of vapours in air, Examples are H2S04 mist, herbicides and insecticides.
(d) Fumes coming out from chemical plants, sublimation, distillation, generally organic solvents, metals and metal oxides form fume particles.

The effect of particulate pollutants are largely dependent on particle size, They are all dangerous to human health.

Smogs:
The word smog is derived from smoke and fog. This is the major cause of air pollution.

Smogs are of two types:
(a) Classical Smog
(b) Photochemical Smog

(a) Classical Smog: It occurs in a cool humid climate. It is a mixture of smoke, fog, and SO2. Because of its reducing nature, it is also called Reducing Smog.

(b) Photochemical Smog: It occurs in a warm, dry and sunny climate. The main components result from the action of sunlight on unsaturated hydrocarbons and oxides of nitrogen. Since it has a high concentration of oxidizing agents, it is called Oxidizing Smog.

Formation of Photo Chemical Smog:
When both unsaturated hydrocarbons (unburnt fuels) and nitric oxide (NO) build-up to sufficiently high levels, a chain reaction occurs in the presence of sunlight.
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Ozone is a toxic gas. Both NO2 and O3 are oxidising agents.
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They further produce chemicals like acrolein (CH2 = CH CHO) and peroxyacetyl nitrate (CH3 CO3 NO2) or PAN

→ Effects of Photochemical Smog: Photochemical smog causes serious health problems. Both O3 and PAN present in photochemical smog cause extreme irritation to the eyes. O3 and NO irritate nose and throat and their high concentration causes a headache, chest pain, dryness of throat, cough and difficulty in breathing. It causes extensive damage to plant life, causes corrosion of metals, building materials, cracking of rubber etc.

→ Control: Photochemical smog can be controlled by controlling—the production of oxides, of nitrogen, controlling the burning of fossil fuels, using catalytic converters in automobiles etc. Certain plants also metabolise NO and therefore their plantation can help.

Stratospheric Pollution
Formation and Breakdown of Ozone: A large amount of ozone (O2) is present in the stratosphere. O3 protects us from the harmful UV rays coming from the sun.

→ Reactions occurring in the stratosphere: The main reactions occurring in the stratosphere. In this region ozone is formed in two steps: In the first step ultraviolet radiation coming from the sun have sufficient: energy to split dioxygen into two oxygen atoms. In the second step, the oxygen atoms react with more dioxygen to form ozone.
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This ozone absorbs ultraviolet radiation and breaks down into dioxygen and an oxygen atom. Heat is given off, which warms up the stratosphere. Thus there is a dynamic equilibrium between the production and decomposition of ozone molecules.
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This ozone layer is acting like a protective layer for the life on the earth. The following reactions take place in this context:
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Freons are introduced in the atmosphere from aerosol sprays in which they function as propellants and from refrigerant equipment in which they act as coolants:
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This is reactive chlorine destroys the ozone through the following reactions:
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The Ozone Hole:
The depletion of the ozone layer by two major compounds [NO2 and CH4] is called the ozone hole.

In the summer season, NO2 and CH4 react with chlorine monoxide (CIO2) and chlorine atoms (Cl) forming chlorine sinks, preventing much ozone depletion.
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Whereas in winter, a special type of clouds, called polar stratospheric clouds are formed over Antarctica. On the surface of these clouds, chlorine nitrate (CIONO2) formed gets Hydrolysed to form hypochlorous acid. It reacts also with HCl (above) to give Cl2
CIONO2(g) + H2O(g) → HOCl(g) + HNO3(g)
CIONO2(g) + HCl(g) → Cl2(g) + HNO3(g)

When sunlight returns to Antarctica in the spring, the sum’s warmth breaks up the clouds and HOCl and Cl2 are photolysed to gaseous chlorine atoms.
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The chlorine-free radicals thus formed, initiate the chain reaction for ozone depletion. One CFC molecule destroys one lac molecules of O3.

Effects of Depletion of Ozone Layer:

  1. The most serious effect is the development of an ozone hole which will allow UV radiations from the sun to pass through the stratosphere and reach the earth causing among other ailments skin cancer.
  2. UV rays cause; damage to the cornea and lens of the eye and may cause cataract or even blindness. ,
  3. It affects plants chlorophyll, proteins, and causes harmful mutation.
  4. O3 depletion will affect the climate badly. It will upset the heat balance of the earth.
  5. It will lead to ecological imbalance which will adversely affect both man and animal.

Water Pollution: Major Water Pollutants

Water Pollutants Sources
1.. Plant nutrients. 1. Chemical fertilizer
2. Sediments. 2. Erosion of soil agriculture and strip mining.
3. Microorganisms. 3. Domestic sewage.
4. Toxic heavy metals. 4. Industries and chemical tãctories.
5. Organic wastes. 5. Domestic sewage, animal waste, decaying animals and plants and discharge from food processing factories.
6. Pesticides. 6. Chemicals used for killing insects, fungi, and weeds.
7. Radioactive substances. 7. Mining of Uranium containing minerals.
8. Heat 8. Water used for cooling in industries.

Causes of Water Pollution:
1. Pathogens: They are disease-causing agents. They include bacteria and other organisms that enter the water from domestic sewage and animal excreta. Human excreta contain bacteria that cause gastrointestinal diseases.

2. Organic Wastes: The other major water pollutant is organic matter such as leaves, grass, trash etc. Excessive phytoplankton growth within the water is also a cause of water pollution. These are biodegradable. Decomposition of organic matter by bacteria in water causes depletion of dissolved oxygen in the water which is very essential for aquatic life.

3. Chemical Pollutants: Water-soluble inorganic chemicals like cadmium, nickel and nickel salts are an important class of water pollutants. They are dangerous to human life because our body cannot excrete them. Slowly and slowly they damage kidneys, central nervous system, liver etc. Petroleum products like oil spills in oceans, polychlorinated biphenyls (PCBs), though biodegradable are another source of organic chemicals that pollute water.

International Standards For Drinking Water:

  1. Fluoride: A deficiency of fluoride in water for drinking is harmful to man and causes tooth decay. Soluble fluoride is added to drinking water to bring its concentration to 1 ppm. Its concentration in water is more than 2 ppm and has harmful effects on teeth, bones.
  2. Lead: The upper prescribed limit for the presence of lead in water is 50 ppb. Lead damages the kidney, liver and reproductive system.
  3. Sulphate: Excessive sulphate (> 500 ppm) in drinking water causes a laxative effect. At moderate levels it is harmless.
  4. Nitrate: The maximum limit of nitrate in drinking water is 50 ppm. Excessive presence can cause disease such as methemoglobinemia (blue baby syndrome)
  5. Other metals: The maximum concentration of some common metals recommended in drinking water are given below:

Maximum Prescribed Concentration of Some Metals in Drinking Water:

Metal Maximum Concentration (ppm or mg dm-3)
Fe 0.2
Mn 0.05
Al 0.2
Cu 3.0
Zn 5.0
Cd 0.005

Soil Pollution
Insecticides, pesticides and herbicides used for the protection of crop cause soil pollution.

Pesticides
Commonly used pesticides which are toxic substances are DDT, Aldrin, and Dieldrin. When their concentration increases beyond a limit, they cause serious metabolic and physiological disorders in higher animals. They are water-insoluble and non—biodegradable. With the passage of time, insects & pests have become immune to these pesticides and insecticides. More potent and biodegradable products like organophosphates and carbonates have beef put to use.

These chemical are extremely harmful to humans and agriculture felid work who spray them.

Nowadays, the pesticide industry is using Herbicides such as sodium chlorate (NaCIO3), sodium arsenite (Na3AsO3) and many others. But all of them are not environmental friendly. Most herbicides are toxic to mammals,

Industrial Waste:
Industrial solid wastes are sorted out as biodegradable and non- Biodegradable wastes. The former is generated by cotton mills, food processing units, paper mills and textile factories, whereas the latter is generated by thermal power plants, iron and steel plants, industries producing Al, Zn and Cu.

The disposal of non-degradable industrial solid waste should be done suitably, otherwise, it may cause a serious threat to the environment. There should be proper management of both domestic and industrial wastes.

Green Chemistry:
Green chemistry as an alternative tool for reducing pollution: One way to protect our environment from chemical effluents and waste is to use green chemistry. By green chemistry, we mean producing the chemicals of our daily needs using such reactions and chemical process which neither use toxic chemicals nor emit such chemicals into the atmosphere. Although it is a very challenging task.

Green chemistry does not employ toxic reagents and severe conditions but uses mild and environmentally friendly reagents, such as sunlight, microwaves, sound waves and enzymes. The use of sunlight and ultraviolet radiation is very useful to produce some useful products which cannot be obtained by simple chemical reactions microwaves and sound waves are used for chemical reactions giving extraordinary results which are not possible by simple chemical reactions.

Enzymes are environmentally friendly reagents. These work in aqueous solutions and at ambient temperatures. These methods are used for preparing medicines and certain antibiotics. For examples, semi-synthetic penicillins such as ampicillin, and Amoxycillin, have been prepared by using this technique.

By using these methods, green chemistry will help us to keep our environment pollution-free.

Green Chemistry in Day-to-Day Life:
1. Dry cleaning of clothes: In places of tetrachloroethene (C12C = CC12) which was earlier used for dry-cleaning nowadays liquefied carbon dioxide along with a suitable detergent is used. It will cause less harm to groundwater. Hydrogen peroxide (H2O2) is also nowadays used for bleaching clothes which gives better results.

2. Bleaching of paper: Cl2 gas which was earlier used for bleaching paper-has been replaced by hydrogen peroxide (H2O2) with a suitable catalyst.

3. Synthesising chemicals: Acetaldehyde (CH3CHO) is now prepared by one-step oxidation of ethylene (H2C = CH2) in the presence of an anionic catalyst in an aqueous medium with a yield of 90% on a commercial scale.

In a nutshell, Green chemistry is a cost-effective approach, which involves

  1. Reduction in cost
  2. Reduction in energy consumption
  3. Reduction in waste production.

Domestication Of Plants

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Domestication Of Plants

Domestication is the process of bringing a plant species under the control of humans and gradually changing it through careful selection, genetic alteration and handling so that it is more useful to people. The domesticated species are renewable sources that have provided food and other benefis to human.

The possible changes in the plant species due to domestication are listed below;

  • Adaptation to a greater diversity of environments and a wider geographical range.
  • Simultaneous / uniform flwering and fruiting.
  • Lack of shattering or scattering of seeds.
  • Increased size of fruits and seeds.
  • Change from a perennial to annual habit.
  • Change in breeding system.
  • Increased yield.
  • Increased resistance for disease and pest.
  • Developing seedless parthenocarpic fruit.
  • Enhancing colour, appearance, palatability and nutritional composition.

Relationship Between Human and Plants

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Relationship Between Human and Plants

From the very early times, human beings have co-existed with plants which played a vital role in their survival. Though a long process of trial and error, our ancestors have selected hundreds of wild plants from the various parts of the world for their specific use. The knowledge of the plants and its applications have led to the development of the humans and their civilization in many ways.

People depend on plants for food, clean air, water, fuel, clothing, and shelter. Nearly all food webs begin with plants, the primary producers. During photosynthesis, green plants use sunlight to change carbon dioxide from the air and water into simple sugars made of carbon, hydrogen, and oxygen.

Plants such as trees, on the other hand, can take in this carbon dioxide, which is unusable for humans, and use it to produce their own energy. In a way, they are a cycle – plants help humans breathe by providing us with oxygen, and humans help plants “breathe” by providing them with carbon dioxide.

There are numerous examples of symbiosis in agriculture. Agriculture in a broad sense involves a symbiotic relationship between humans and plants or animals. Humans plant, fertilize, control weeds and pests, and protect crops. Humans also nurture, feed, and protect livestock.

Humans, of course, benefit greatly from their mutualisms with agricultural plants, through the provision of crops of food, fiber, and other products. Similarly, agricultural animals live in a symbiotic mutualism with humans. Even the keeping of animals as pets represents a type of mutualism.

An exploration of the relationship between plants and people from early agriculture to modern-day applications of biotechnology in crop production. Plants and People: Origin and Development of Human-Plant Science Relationships covers the development of agricultural sciences from Roman times through the development of agricultural experiment stations in the United States.

To the rise of agri-business. It underscores the symbiotic relationship and mutuality that define the intertwined histories of plants and people. It does not merely present the latest science but puts the sciences themselves in the context of history.

The book provides the science, chronology, and history that undergird the relationships between humans and plants. It discusses plant anatomy, physiology, and reproduction; evolution of plants and people; early uses of plants; the rise of agriculture in both Old and New Worlds; creation of land grant universities and agricultural experiment stations; the Green Revolution; plant biotechnology; and the future of plant sciences in feeding the growing human population.

The agricultural sciences were not a product of the nineteenth century but of the careful observation and advice of Roman writers who lived some 2000 years ago. This book reveals the malleability of the sciences, the people who practice them, and the plants that are the focus of scientific research.

The author is careful to distinguish between basic and applied science while recognizing that the agricultural sciences pursue both. He also challenges the traditional notion that basic research necessarily yields practical results. The book demonstrates how plants and the agricultural sciences have shaped the everyday world we inhabit.

Carbon Capture And Storage (CCS)

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Carbon Capture And Storage (CCS)

Carbon capture and storage is a technology of capturing carbondioxide and injects it deep into the underground rocks to a depth of 1 km or more and it is an approach to mitigate global warming by capturing CO2 from large point sources such as industries and power plants and subsequently storing it instead of releasing it into the atmosphere.

Various safe sites have been selected for permanent storage in various deep geological formations, liquid storage in the Ocean and solid storage by reduction of CO2 with metal oxide to produce stable carbonates. It is also known as Geological sequestration which involves injecting CO2 directly into the underground geological formations (such as declining oil fields, gas fields saline aquifers and unmineable coal have been suggested as storage sites).

Carbon Sequestration

Carbon sequestration is the process of capturing and storing CO2 which reduces the amount of CO2 in the atmosphere with a goal of reducing global climate change. Carbon sequestration occurs naturally by plants and in ocean. Terrestrial sequestration is typically accomplished through forest and soil conservation
practices that enhance the storage carbon.

As an example microalgae such as species of Chlorella, Scenedesmus, Chroococcus and Chlamydomonas are used globally for CO2 sequestration. Trees like Eugenia caryophyllata, Tecoma stans, Cinnamomum verum have high capacity and noted to sequester carbon. Macroalgae and marine grasses and mangroves are also have ability to mitigate carbon-di-oxide.

Carbon Foot Print (CFP)

Every human activity leaves a mark just like our footprint. This Carbon foot print is the total amount of green house gases produced by human activities such as agriculture, industries, deforestation, waste disposal, buring fossil fuels directly or indirectly. It can be measured for an individual, family, organisation like industries, state level or national level. It is usually estimated and expressed in equivalent tons of CO2 per year. The burning of fossil fuels releases CO2 and other green house gases.

In turn these emissions trap solar energy and thus increase the global temperature resulting in ice melting, submerging of low lying areas and inbalance in nature like cyclones, tsunamis and extreme weather conditions. To reduce the carbon foot print we can follow some practices like

  1. Eating indigenous fruits and products
  2. Reducing use of electronic devices
  3. Reduce travelling
  4. Avoid buying fast and preserved, processed, packed foods.
  5. Plant a garden
  6. Reducing consumption of meat and sea food. Poultry requires little space, nutrients and less pollution compared cattle farming.
  7. Reducing use of Laptops (when used for 8 hours, it releases nearly 2 kg. of CO2 annually)
  8. Line drying clothes. (Example: If you buy imported fruit like kiwi, indirectly it increases CFP. How? The fruit has travelled a long distance in shipping or airliner thus emitting tons of CO2)
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Biochar

Biochar is another long term method to store carbon. To increase plants ability to store more carbon, plants are partly burnt such as crop waste, waste woods to become carbon rich slow decomposing substances of material called Biochar.

It is a kind of charcoal used as a soil amendment. Biochar is a stable solid, rich in carbon and can endure in soil for thousands of years. Like most charcoal, biochar is made from biomass via pyrolysis.

(Heating biomas in low oxygen environment) which arrests wood from complete burning. Biochar thus has the potential to help mitigate climate change via carbon sequestration. Independently, biochar when added to soil can increase soil fertility of acidic soils, increase agricultural productivity, and provide protection against some foliar and soil borne diseases.

It is a good method of preventing waste woods and logs from getting decayed and instead we can convert them into biochar thus converting them to carbon storage material.

Environmental Conservation Issues

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Environmental Conservation Issues

India due to its topography, geology and climate patterns has diverse life forms. Now this huge diversity is under threat due to many environmental issues for this conservation becomes an important tool by which we can reduce many species getting lost from our native land.

By employing conservation management strategies like germplasm conservation, in situ, ex-situ, in-vitro methods, the endemic as well as threatened species can be protected and also have educational and recreational values for the society.
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In-situ conservation:

It means conservation and management of genetic resources in their natural habitats. Here the plant or animal species are protected within the existing habitat. Forest trees, medicinal and aromatic plants under threat are conserved by this method. This is carried out by the community or by the State conservation which include wildlife, National park and Biosphere reserve.

The ecologically unique and biodiversity rich regions are legally protected as wildlife sanctuaries, National parks and Biosphere reserves. Megamalai, Sathyamangalam wildlife, Guindy and Periyar National park, and Western ghats, Nilgiris, Agasthyamalai and Gulf of Mannar are the biosphere reserves of Tamil Nadu.

Sacred groves

These are the patches or grove of cultivated trees which are community protected and are based on strong religious belief systems which usually have a signifiant religious connotation for protecting community. Each grove is an abode of a deity mostly village God Or Goddesses like Aiyanar or Amman.

448 grooves were documented throughout Tamil Nadu, of which 6 groves (Banagudi shola, Thrukurungudi and Udaiyankudikadu, Sittannnavasal, Puthupet and Devadanam) were taken up for detailed floristic and faunistic studies. These groves provide a number of ecosystem services to the neighbourhood like protecting watershed, fodder, medicinal plants and micro climate control.

Ex-situ conservation

It is a method of conservation where species are protected outside their natural environment. This includes establishment of botanical gardens, zoological parks, conservation strategies such as gene, pollen, seed, in-vitro conservation, cryo preservation, seedling, tissue culture and DNA banks. These facilities not only provide housing and care for endangered species, but also have educational and recreational values for the society.

Endemic Centres and Endemic Plants

Endemic species are plants and animals that exist only in one geographic region. Species can be endemic to large or small areas of the earth. Some are endemic to a particular continent, some to a part of a continent and others to a single island. Any species found restricted to a specified geographical area is referred to as ENDEMIC. It may be due to various reasons such as isolation, interspecific interactions, seeds dispersal problems, site specifiity and many other environmental and ecological problems.

There are 3 Megacentres of endemism and 27 microendemic centres in India. Approximately one third of Indian flora have been identified as endemic and found restricted and distributed in three major phytogeographical regions of india, that is Indian Himalayas, Peninsular India and Andaman nicobar islands.

Peninsular India, especially Western Ghats has high concentration of endemic plants. Hardwickia binata and Bentinckia condapanna are good examples for endemic plants. A large percentage of Endemic species are herbs and belong to families such as Poaceae. Apiaceae, Asteraceae and Orchidaceae.
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Majority of endemic species are threatened due to their narrow specifi habitat, reduced seed production, low dispersal rate, less viable nature and human intereferences.. Serious efforts need to be undertaken for their conservation, otherwise these species may become globally extinct.
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Alien Invasive Species | Eichhornia Crassipes | Prosopis Juliflra

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Alien Invasive Species | Eichhornia Crassipes | Prosopis Juliflra

Invasion of alien or introduced species disrupts ecosystem processes, threaten biodiversity, reduce native herbs, thus reducing the ecosystem services (benefis). During eradication of these species, the chemicals used increases greenhouse gases.

Slowly they alter ecosystem, micro climate and nature of soil and make it unsuitable for native species and create human health problems like allergy, thus resulting in local environmental degradation and loss of important local species. According to World Conservation Union invasive alien species are the second most signifiant threat to bio-diversity after habitat loss.

What is invasive species?

A non-native species to the ecosystem or country under consideration that spreads naturally, interferes with the biology and existence of native species, poses a serious threat to the ecosystem and causes economic loss. It is established that a number of invasive species are accidental introduction through ports via air or sea.

Some research organisations import germplasm of wild varieties through which also it gets introduced. Alien species with edible fruits are usually spread by birds. Invasive species are fast growing and are more adapted. They alter the soil system by changing litter quality thereby affecting the soil community, soil fauna and the ecosystem processes.

It has a negative impact on decomposition in the soils by causing stress to the neighbouring native species. Some of the alien species which cause environmental issues are discussed below.

Eichhornia crassipes:

It is an invasive weed native to South America. It was introduced as aquatic ornamental plant, which grows faster throughout the year. Its widespread growth is a major cause of biodiversity loss worldwide. It affects the growth of phytoplanktons and finally changing the aquatic ecosystem.

It also decreases the oxygen content of the waterbodies which leads to eutrophication. It poses a threat to human health because it creates a breeding habitat for disease causing mosquitoes (particularly Anopheles) and snails with its free flating dense roots and semi submerged leaves. It also blocks sunlight entering deep and the waterways hampering agriculture, fiheries, recreation and hydropower.
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Prosopis juliflra

Prosopis juliflra is an invasive species native to Mexico and South America. It was first introduced in Gujarat to counter desertifiation and later on in Andhra Pradesh, Tamil Nadu as a source of firewood. It is an aggressive coloniser and as a consequence the habitats are rapidly covered by this species.

Its invasion reduced the cover of native medicinal herbaceous species. It is used to arrest wind erosion and stabilize sand dunes on coastal and desert areas. It can absorb hazardous chemicals from soil and it is the main source of charcoal.
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An Overview Of Afforestation And Its Acheivements

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An Overview Of Afforestation And Its Acheivements

Afforestation is planting of trees where there was no previous tree coverage and the conversion of non-forested lands into forests by planting suitable trees to retrieve the vegetation. Example: Slopes of dams affrested to reduce water runoff erosion and siltation. It can also provide a range of environmental services including carbon sequestration, water retention.

Afforestation Objectives

  • To increase forest cover, planting more trees, increases O2 production and air quality.
  • Rehabilitation of degraded forests to increase carbon fiation and reducing CO2 from atmosphere.
  • Raising bamboo plantations.
  • Mixed plantations of minor forest produce and medicinal plants.
  • Regeneration of indigenous herbs / shrubs.
  • Awareness creation, monitoring and evaluation.
  • To increase the level and availability of water table or ground water and also to reduce nitrogen leaching in soil and nitrogen contamination of drinking water, thus making it pure not polluted with nitrogen.
  • Nature aided artifiial regeneration.

Achievements

  • Degraded forests were restored
  • Community assets like overhead tanks bore-wells, hand pumps, community halls, libraries, etc were established
  • Environmental and ecological stability was maintained.
  • Conserved bio-diversity, wildlife and genetic resources.
  • Involvement of community especially women in forest management.

Environmental Deforestation | Definition, Causes and Effects

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Environmental Deforestation | Definition, Causes and Effects

Deforestation is one of the major contributors to enhance green house effect and global warming. The conversion of forested area into a non-forested area is known as deforestation. Forests provide us many benefits including goods such as timber, paper, medicine and industrial products. The causes are

  • The conversion of forests into agricultural plantation and livestock ranching is a major cause of deforestation.
  • Logging for timber
  • Developmental activities like road construction, electric tower lines and dams.
  • Over population, Industrialisation, urbanisation and increased global needs.

Effects of deforestation

  • Burning of forest wood release stored carbon, a negative impact just opposite of carbon sequestration.
  • Trees and plants bind the soil particles. The removal of forest cover increases soil erosion and decreases soil fertility. Deforestation in dry areas leads to the formation of deserts.
  • The amount of run of water increases soil erosion and also creates flash floding, thus reducing moisture and humidity.
  • The alteration of local precipitation patterns leading to drought conditions in many regions. It triggers adverse climatic conditions and alters water cycle in ecosystem.
  • It decreases the bio-diversity signifiantly as their habitats are disturbed and disruption of natural cycles.
  • Loss of livelihood for forest dwellers and rural people.
  • Increased global warming and account for one-third of total CO2 emission.
  • Loss of life support resources, fuel, medicinal herbs and wild edible fruits.

Environmental Issues On Various Types Of Forestry

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Environmental Issues On Various Types Of Forestry

Agro forestry

Agroforestry is an integration of trees, crops and livestock on the same plot of land. The main objective is on the interaction among them. Example: intercropping of two or more crops between diffrent species of trees and shrubs, which results in higher yielding and reducing the operation costs. This intentional combination of agriculture and forestry has varied benefits including increased bio-diversity and reduced erosion.

Some of the major species cultivated in commercial Agroforestry include Casuarina, Eucalyptus, Malai Vembu, Teak and Kadambu trees which were among the 20 species identified as commercial timber. They are of great importance to wood-based industries.

Benefits of agroforestry

  • It is an answer to the problem of soil and water conservation and also to stabilise the soil (salinity and water table) reduce landslide and water run-of problem.
  • Nutrient cycling between species improves and organic matter is maintained.
  • Trees provide micro climate for crops and maintain O2 – CO2 balanced, atmospheric temperature and relative humidity.
  • Suitable for dry land where rainfall is minimum and hence it is a good system for alternate land use pattern.
  • Multipurpose tree varieties like Acacia are used for wood pulp, tanning, paper and firewood industries.
  • Agro-forestry is recommended for the following purposes. It can be used as Farm Forestry for the extension of forests, mixed forestry, shelter belts and linear strip plantation.

Rehabilitation of degraded forests and recreation forestry

The production of woody plants combined with pasture is referred to silvopasture system. The trees and shrubs may be used primarily to produce fodder for livestock or they may be grown for timber, fuel wood and fruit or to improve the soil. This system is classified into following categories.

(i) Protein Bank:

In this various multipurpose trees are planted in and around farm lands and range lands mainly for fodder production. Example: Acacia nilotica, Albizzia lebbek, Azadirachta indica, Gliricidia sepium, Sesbania grandiflora.

(ii) Livefence of fodder trees and hedges:

Various fodder trees and hedges are planted as live fence to protect the property from stray animals or other biotic inflences. Example: Gliricidia sepium, Sesbania grandiflra, Erythrina spp., Acacia spp.

Social forestry

It refers to the sustainable management of forests by local communities with a goal of climate carbon sequestration, change mitigation, depollution, deforestation, forest restoration and providing indirect employment opportunity for the youth.

Social forestry refers to the management of forests and afforestation on barren lands with the purpose of helping the environmental, social and rural development and benefits. Forestry programme is done for the benefit of people and participation of the people. Trees grown outside forests by government and public organisation reduce the pressure on forests.

In order to encourage tree cultivation outside forests, Tree cultivation in Private Lands was implemented in the state from 2007-08 to 2011-12. It was implemented by carrying out block planting and inter-crop planting with profitable tree species like Teak, Casuarina, Ailanthus, Silver Oak, etc in the farming lands and by a free supply of profiable tree species for planting in the bunds.

The Tank foreshore plantations have been a major source of firewood in Tamil Nadu. The 32 Forestry extension centres provide technical support for tree growing in rural areas in Tamil Nadu. These centres provide quality tree seedlings like thorn / thornless bamboo, casuarinas, teak, neem, Melia dubia, grafted tamarind and nelli, etc in private lands and creating awareness among students by training / camps.

Major activities of forestry extension centres

  • Training on tree growing methods
  • Publicity and propaganda regarding tree growing
  • Formation of demonstration plots
  • Raising and supply of seedlings on subsidy
  • Awareness creation among school children and youth about the importance of forests through training and camps.

Green House Effect, Ozone Depletion And Its Effects

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Green House Effect, Ozone Depletion And Its Effects

Green House Effect is a process by which radiant heat from the sun is captured by gases in the atmosphere that increase the temperature of the earth ultimately. The gases that capture heat are called Green House Gases which include carbon dioxide (CO2), methane (CH4), Nitrous Oxide (N2O) and a variety of manufactured chemicals like chloroflorocarbon (CFC).

Increase in greenhouse gases lead to irreversible changes in major ecosystems and climate patterns. For example, coral ecosystem is affected by increase in temperature, especially coral bleaching observed in Gulf of Mannar, Tamil Nadu.

Human activities lead to produce the green house effect by:-

  • Burning fossil fuels, which releases CO2 and CH4
  • Way of Agriculture and animal husbandry practices
  • Electrical gadgets like refrigerator and air conditioners release chloro floro carbons
  • The fertilizers used in Agriculture which release N2O
  • The emissions from automobiles.

The increase in mean global temperature (highest in 4000 years) due to increased concentration of green house gases is called global warming. One of the reasons for this is over population which creates growing need for food, fire and fuel and considered to be the major cause of global warming.
Green House Effect, Ozone Depletion img 1

Effects of Global Warming

  • Rise in global temperature which causes sea levels to rise as polar ice caps and glaciers begin to melt causing submergence of many coastal cities in many parts of the world.
  • There will be a drastic change in weather patterns bringing more floods or droughts in some areas.
  • Biological diversity may get modified, some species ranges get redefied. Tropics and sub-tropics may face the problem of decreased food production.

Sources of Green House Gases Emission (Natural and Anthropogenic)

CO2 (Carbon dioxide)

  • Coal based power plants, by the burning of fossil fuels for electricity generation.
  • Combustion of fuels in the engines of automobiles, commercial vehicles and air planes contribute the most of global warming.
  • Agricultural practices like stubble burning result in emission of CO2.
  • Natural from organic matter, volcanoes, warm oceans and sediments.

Methane

Methane is 20 times as effective as CO2 at trapping heat in the atomosphere. Its sources are attributed paddy cultivation, cattle rearing, bacteria in water bodies, fossil fuel production, ocean, non-wetland soils and forest / wild fies.

N2O (Nitrous oxide)

It is naturally produced in Oceans from biological sources of soil and water due to microbial actions and rainforests. Man-made sources include nylon and nitric acid production, use of fertilizers in agriculture, manures cars with catalytic converter and burning of organic matter.

Global Warming Effects on Plants

  • Low agricultural productivity in tropics
  • Frequent heat waves (Weeds, pests, fungi need warmer temperature)
  • Increase of vectors and epidemics
  • Strong stroms and intense flood damage
  • Water crisis and decreased irrigation
  • Change in flowering seasons and pollinators
  • Change in Species distributional ranges
  • Species extinction

Strategies to deal with Global Warming

  • Increasing the vegetation cover, grow more trees
  • Reducing the use of fossil fuels and green house gases
  • Developing alternate renewable sources of energy
  • Minimising uses of nitrogeneous fertilizers, and aerosols.

Ozone depletion

Ozone layer is a region of Earth’s stratosphere that absorbs most of the Sun’s ultra violet radiation. The ozone layer is also called as the ozone shield and it acts as a protective shield, cutting the ultraviolet radiation emitted by the sun. Just above the atmosphere there are two layers namely troposphere (the lower layer) and stratosphere (the upper layer).

The ozone layer of the troposphere is called bad ozone and the ozone layer of stratosphere is known as good ozone because this layer acts as a shield for absorbing the UV radiations coming from the sun which is harmful for living organisms causing DNA damage. The thickness of the ozone column of air from the ground to the top of the atmosphere is measured in terms of Dobson Units.

The ozone shield is being damaged by chemicals released on the Earth’s surface notably the chloroflorocarbons widely used in refrigeration, aerosols, chemicals used as cleaners in many industries. The decline in the thickness of the ozone layer over restricted area is called Ozone hole.

Ozone depletion in the stratosphere results in more UV radiations especially UV B radiations (shortwaves). UV B radiation destroys biomolecules (skin ageing) and damages living tissues. UV – C is the most damaging type of UV radiation, but it is completely filtered by the atmosphere (ozone layer). UV – a contribute 95% of UV radiation which causes tanning burning of skin and enhancing skin cancer. Hence the uniform ozone layer is critical for the wellbeing of life on earth.

During 1970’s research fidings indicated that man-made chloroflorocarbons (CFC) reduce and convert ozone molecules in the atmosphere. The threats associated with reduced ozone pushed the issue to the forefront of global climate issues and gained promotion through organisation such as World Meterological Organisation and the United Nations.

The Vienna Convention was agreed upon at the Vienna conference of 1985 but entered into force in 1988 provided the frameworks necessary to create regulative measures in the form of the Montreal protocol.

The International treaty called the Montreal Protocol (1987) was held in Canada on substances that deplete ozone layer and the main goal of it is gradually eliminating the production and consumption of ozone depleting substances and to limit their damage on the Earth’s ozone layer.

Clean Development Mechanism (CDM) is defied in the Kyoto protocol (2007) which provides project based mechanisms with two objectives to prevent dangerous climate change and to reduce green house gas emissions. CDM projects helps the countries to reduce or limit emission and stimulate sustainable development.

An example for CDM project activity, is replacement of conventional electrifiation projects with solar panels or other energy efficient boilers. Such projects can earn Certified Emission Reduction (CER) with credits / scores, each equivalent to one tonne of CO2, which can be counted towards meeting Kyoto targets.
Green House Effect, Ozone Depletion img 2

Effects of Ozone depletion

The main ozone depletion effects are:

  • Increases the incidence of cataract, throat and lung irritation and aggravation of asthma or emphysema, skin cancer and diminishing the functioning of immune system in human beings.
  • Juvenile mortality of animals.
  • Increased incidence of mutations.
  • In plants, photosynthetic chemicals will be affected and therefore photosynthesis will be inhibited. Decreased photosynthesis will result in increased atmospheric CO2 resulting in global warming and also shortage of food leading to food crisis.
  • Increase in temperature changes the climate and rainfall pattern which may result in flood / drought, sea water rise, imbalance in ecosystems affecting flora and fauna.

Ecological Plant Succession – Characteristics, Types and Examples

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Ecological Plant Succession – Characteristics, Types and Examples

We very often see that forests and lands in our areas are drastically affcted by natural calamities (Flood, earthquake) and anthropogenic activities (Fire, over grazing, cutting of trees). Due to these reasons all plants of an area are destroyed and the areas become nude. When we observe this area, over a period of a time we can see that it will be gradually covered by plant community again and become fertile.

Such successive replacement of one type of plant community by the other of the same area / place is known as plant succession. The first invaded plants in a barren area are called pioneers. On the other hand, a series of transitional developments of plant communities one after another in a given area are called seral communities. At the end a final stage and a final plant community gets established which are called as climax and climax community respectively.

Characteristics of ecological succession

  • It is a systematic process which causes changes in specifi structure of plant community.
  • It is resultant of changes of abiotic and biotic factors.
  • It transforms unstable community into a stable community.
  • Gradual progression in species diversity, total biomass, niche specialisation, and humus content of soil takes place.
  • It progresses from simple food chain to complex food web.
  • It modifies the lower and simple life form to the higher life forms.
  • It creates inter-dependence of plants and animals.

Types of succession

The various types of succession have been classified in different ways on the basis of different aspects. These are as follows:

1. Primary succession:

The development of plant community in a barren area where no community existed before is called primary succession. The plants which colonize first in a barren area is called pioneer species or primary community or primary colonies. Generally, Primary succession takes a very long time for the occurrence in any region.
Ecological Plant Succession img 1
Example: Microbes, Lichen, Mosses.

2. Secondary succession:

The development of a plant community in an area where an already developed community has been destroyed by some natural disturbance (Fire, flood, human activity) is known as secondary succession. Generally, This succession takes less time than the time taken for primary succession.
Ecological Plant Succession img 2

Example: The forest destroyed by fire and excessive lumbering may be re-occupied by herbs over a period of times.

3. Allogenic succession

Allogeneic succession occurs as a result of abiotic factors. The replacement of existing community is caused by other external factors (soil erosion, leaching, etc.,) and not by existing organisms. Example: In a forest ecosystem soil erosion and leaching alter the nutrient value of the soil leading to the change of vegetation in that area.
Ecological Plant Succession img 3

Classification of plant succession

Detailed study of Hydrosere and Lithosere are discussed below:
Ecological Plant Succession img 4

Hydrosere

The succession in a freshwater ecosystem is also referred to as hydrosere. Succession in a pond, begins with colonization of the pioneers like phytoplankton and finally ends with the formation of climax community like forest stage. It includes the following stages Fig 7.21.

1. Phytoplankton stage:

It is the first stage of succession consisting of the pioneer community like blue green algae, green algae, diatoms, bacteria, etc., The colonization of these organisms enrich the amount of organic matter and nutrients of pond due to their life activities and death. This favors the development of the next seral stages.

2. Submerged plant stage:

As the result of death and decomposition of planktons, silt brought from land by rain water, lead to a loose mud formation at the bottom of the pond. Hence, the rooted submerged hydrophytes begin to appear on the new substratum. Example: Chara, Utricularia, Vallisneria and Hydrilla etc.

The death and decay of these plants will build up the substratum of pond to become shallow. Therefore, this habitat now replaces another group of plants which are of floating type.

3. Submerged free flating stage:

During sthis stage, the depth of the pond will become almost 2-5 feet. Hence, the rooted hydrophytic plants and with floating large leaves start colonising the pond. Example: Rooted flating plants like Nelumbo, Nymphaea and Trapa.

Some free flating species like Azolla, Lemna, Wolff and Pistia are also present in this stage. By death and decomposition of these plants, further the pond becomes more shallow. Due to this reason, floating plant species is gradually replaced by another species which makes new seral stage.
Ecological Plant Succession img 5

4. Reed-swamp stage:

It is also called an amphibious stage. During this stage, rooted floating plants are replaced by plants which can live successfully in aquatic as well as aerial environment. Example: Typha, Phragmites, Sagittaria and Scirpus etc. At the end of this stage, water level is very much reduced, making it unsuitable for the continuous growth of amphibious plants.

5. Marsh meadow stage:

When the pond becomes swallowed due to decreasing water level, species of Cyperaceae and Poaceae such as Carex, Juncus, Cyperus and Eleocharis colonise the area. They form a mat-like vegetation with the help of their much branched root system. This leads to an absorption and loss of large quantity of water. At the end of this stage, the soil becomes dry and the marshy vegetation disappears gradually and leads to shurb stage.

6. Shrub stage:

As the disappearance of marshy vegetation continues, soil becomes dry. Hence, these areas are now invaded by terrestrial plants like shrubs (Salix and Cornus) and trees (Populus and Alnus). These plants absorb large quantity of water and make the habitat dry. Further, the accumulation of humus with a rich flora of microorganisms produce minerals in the soil, ultimately favouring the arrival of new tree species in the area.

7. Forest stage:

It is the climax community of hydrosere. A variety of trees invade the area and develop any one of the diverse type of vegetation. Example: Temperate mixed forest (Ulmus, Acer and Quercus), Tropical rain forest (Artocarpus and Cinnamomum) and Tropical deciduous forest (Bamboo and Tectona).

In the 7 stages of hydrosere succession, stage1 is occupied by pioneer community, while the stage 7 is occupied by the climax community. The stages 2 to 6 are occupied by seral communities.

Significance of Plant Succession

  • Succession is a dynamic process. Hence an ecologist can access and study the seral stages of a plant community found in a particular area.
  • The knowledge of ecological succession helps to understand the controlled growth of one or more species in a forest.
  • Utilizing the knowledge of succession, even dams can be protected by preventing siltation.
  • It gives information about the techniques to be used during reforestation and affrestation.
  • It helps in the maintenance of pastures.
  • Plant succession helps to maintain species diversity in an ecosystem.
  • Patterns of diversity during succession are inflenced by resource availability and disturbance by various factors.
  • Primary succession involves the colonization of habitat of an area devoid of life.
  • Secondary succession involves the reestablishment of a plant community in disturbed area or habitat.
  • Forests and vegetation that we come across all over the world are the result of plant succession.