Environment Unit 1
Environment Unit 1
DEFINITION
The term environment refers to one’s surroundings. The physical and
biological factors along with their chemical interactions that affect an
organism or a group of organisms. The environment is the biotic and abiotic
surrounding of an organism or population, and consequently includes the
factors that have an influence in their survival, development and evolution.
The environment can vary in scale from microscopic to global in extent.
Examples include the marine environment, the atmospheric environment
and the terrestrial environment. The sum total of all surroundings of a living
organism, including natural forces and other living things, which provide
conditions for development and growth as well as of danger and damage.
Types of Environments
There are two different types of environments:
Natural Environment
Man-made/Anthropogenic Environment
Natural Environment
It consists of all components provided by nature and hence can be called as
the natural environment. It is also referred to as the physical environment as
it pertains to the physical requirements of life. These physical or geographic
conditions are not dependent on the existence of humans. Sometimes,
humans have no control over the physical conditions of the environment.
Man-Made Environment
ENVIRONMENTAL SEGMENTS
The environment consists of various segments such as atmosphere,
hydrosphere, lithosphere and biosphere
Atmosphere
The following points highlight the vital role played by atmosphere in the
survival of life in this planet
• It absorbs IR radiations emitted by the sun and reemitted from the earth
and thus controls the temperature of the earth.
•It acts as a source for CO2 for plant photosynthesis and O2 for respiration.
• It acts as a source for nitrogen for nitrogen fixing bacteria and ammonia
producing plants.
•The atmosphere transports water from ocean to land.
Troposphere
Though the sunlight reaches the Earth’s surface from top to bottom, the
troposphere is primarily heated at the bottom. The Earth’s surface is much
better at absorbing a wide range of solar radiation than the air. When the
parcel of warm air moves upwards, it expands, and when air expands, it
cools. Due to this reason, the base of the troposphere is warmer than its
base because the air on the surface of the Earth absorbs the sun’s energy,
gets heated up, and moves upward, which cools down.
Stratosphere
The Stratosphere lies above the troposphere and extends up to a height of
50 km. This layer is free of clouds and devoid of any weather-related
phenomenon. Due to this, aeroplanes fly in the Stratosphere for a smooth
ride. The Stratosphere also houses the ozone layer that protects us from
the harmful effect of the sun’s rays.
Mesosphere
The temperature in the mesosphere grows colder with the altitude.
T his is
because there are few gas molecules in the mesosphere to absorb the Sun’s
radiation. The only heat source is the stratosphere below. The mesosphere is
extremely cold, especially at the top, dropping to a temperature as low as -
90°C.
Thermosphere
The density of molecules in the thermosphere is very low. One m gas olecule
can go about a distance of 1 km without colliding with another molecule.
Because so little energy is transferred, the air feels freezing. Satellites are
found orbiting in the upper part of the thermosphere.
Exosphere
The exosphere is the final frontier of the Earth’s gaseous envelope. There is
no clear- cut distinction between the Earth’s atmosphere layers and outer
space. The air in the exosphere is constantly but gradually leaking out of the
Earth’s atmos phere into outer space.
Hydrosphere
The hydrosphere is a collective term given to all different forms of water.
It includes all types of water resources such as oceans, seas, rivers, lakes,
streams, reservoirs, glaciers and ground waters.
On Earth, liquid water exists on the surface in the form of oceans, lakes and
rivers. It also exists below ground—as groundwater, in wells and aquifers.
Water vapor is most visible as clouds and fog.
The frozen part of Earth's hydrosphere is made of ice: glaciers, ice caps and
icebergs. The frozen part of the hydrosphere has its own name, the
cryosphere.
Lithosphere
The lithosphere is the solid, outer part of the Earth. The lithosphere includes
the brittle upper portion of the mantle and the crust, the outermost layers of
Earth’s structure. It is bounded by the atmosphere above and the
asthenosphere (another part of the upper mantle) below. The lithosphere is
the most rigid of Earth’s layers. Although the rocks of the lithosphere are still
considered elastic, they are not viscous. The asthenosphere is viscous, and
the lithosphere asthenosphere boundary (LAB) is the point where geologists
and rheologists—scientists who study the
flow of matter—mark the difference in ductility between the two layers of
the upper mantle. Ductility measures a solid material’s ability to deform or
stretch under stress. The lithosphere is far less ductile than the
asthenosphere. The elasticity and ductility of the lithosphere depends on
temperature, stress, and the curvature of the Earth itself.
The lithosphere is also the coolest of Earth’s layers. In fact, some definitions
of the lithosphere stress its ability to conduct heat associated with the
convection taking place in the plastic mantle below the lithosphere.
Biosphere
• The biosphere refers to the realm of living organisms and their interactions
with the environment (VIZ: atmosphere, hydrosphere and lithosphere)
• The biosphere is very large and complex and is divided into smaller units
called ecosystems.
1. The plants obtain the energy directly from the sun, and, in case of animals and
microorganisms, energy is taken from other organisms through feeding on plants, predation,
parasitism and/or decomposition.
2. The terrestrial plants obtain water mainly from soil, while animals get it from free standing
water in the environment or from their food.
3. The plants obtain most of their nutrients from the soil or water, while animals get nutrients
from plants or other organisms. Microorganisms are the most versatile, obtaining nutrients
from soil, water, food, or other organisms.
As a result, the organisms interact with one another and with their environment in
a number of ways. These fundamental interactions among organisms and their
non-living/physico-chemical environment constitute an interrelating and
interdependent ever-changing system known as an ecological system or
ecosystem. The ecosystem has been considered as the basic functional unit of
ecology and ecology as study of ecosystems
ECOSYSTEM STRUCTURE
The ecosystem is largely divided into two components - Abiotic and Biotic
components. Ecosystem structure is created due to interaction between abiotic and
biotic components, varying over space and time.
1. Abiotic Components
The abiotic components of an ecosystem refer to the physical environment or the
non-living factors. The organisms cannot live or survive without their abiotic
components. They mainly include i) inorganic substances required by organisms
such as carbon dioxide, water, nitrogen, calcium, phosphorus, etc. that are involved
in material cycles. The amount of these inorganic substances present at any given
time in ecosystem is called as standing state or standing quality of ecosystem. ii)
organic compounds like proteins, carbohydrates, amino acids, lipids, humic
substances and others are synthesized by the biotic counterpart of an ecosystem.
They make biochemical structure of ecosystem. iii) climatic factors including mainly
rain, light, temperature, humidity, wind and air and iv) edaphic and other factors
such as minerals, soil, topography, pH, etc. greatly determine the functions,
distribution, structure, behavior and inter- relationship of organisms in a habitat.
2. Biotic Components
The biotic components of the ecosystems are the living organisms including plants,
animals and microorganisms. Based on their nutritional requirement, i.e. how they
get their food, they are categorized into three groups –
i) Producers are mainly the green plants with chlorophyll which gives them the ability to use
solar energy
to manufacture their own food using simple inorganic abiotic substances, through
the process of
photosynthesis. They are also called as photoautotrophs (photolight, auto-self,
troph-nutrition). This group is mainly constituted by green plants, herbs, shrubs,
trees, phytoplanktons, algae, mosses, etc. There are some chemosynthetic bacteria
(sulphur bacteria) deap beneath in the ocean which can synthesize their food in
absence of sunlight, thus known as chemoautotrophs (chemo-chemical, auto-self,
troph-nutrition).
ii) Consumers lack chlorophyll, so they depend on producers for food. They are also
known as
heterotrophs. They mainly include herbivorous (feed on plants), carnivorous (feed
on other animals),
omnivorous (feed on both plants and animals) and detritivores organisms (feed on
dead parts, waste, remains, etc. of plants and animals,).
iii) Decomposers (saprotrophs) are the microorganisms, bacteria and fungi, which break down
complex dead organic matter into simple inorganic forms, absorb some of the decomposition
products, and release inorganic nutrients that are reused by the producers. All ecosystems
have their own set of producers,
consumers and decomposers which are specific to that ecosystem. The nutritional
relationship among
different biotic components of an ecosystem is shown.
Nutritional relationship among different biotic components of an ecosyste
Types of Ecosystem
Based on the kind of habitat, there are essentially two types of ecosystems:
Aquatic and Terrestrial
Ecosystem . Any other sub-ecosystem falls under one of these two types-
1. Terrestrial Ecosystem
The ecosystems on land are called as terrestrial ecosystems. They are broadly classed
into:
a) Forest Ecosystem:
They are the ecosystems with an abundance of flora, or plants in relatively small
space. A wide diversity of fauna can also be seen. A small change in this ecosystem
could affect the whole balance and effectively bring down the whole ecosystem.
They are further divided into:
Tropical rainforest: These contain more diverse biodiversity than ecosystems in any
other region on earth. They receive a mean rainfall of 80 cm for every 400 inches
annually. In these, warm, moisture-laden environments, dense evergreen vegetation
comprising tall trees at different heights are present, with fauna species inhabiting the
forest floor all the way up to canopy.
Tropical deciduous forest: In these ecosystems, shrubs and dense bushes are found
along with a broad selection of trees. The trees are mainly which shed their leaves
during dry season. The type of forest is found in quite a few parts of the world while a
large variety of fauna and flora are found there.
Temperate evergreen forest: Those have a few numbers of trees as mosses and
ferns make up for them. Trees have developed needle shaped leaves in order to
minimize transpiration.
Temperate deciduous forest: The forest is located in the moist temperate places
that have sufficient rainfall. Summers and winters are clearly defined and the trees
shed the leaves during the winter.
Taiga: found just before the arctic regions, the taiga is defined by evergreen conifers.
As the temperature is below zero for almost half a year, the remainder of the months, it
buzzes with migratory birds and insects.
b) Desert Ecosystems:
Desert ecosystems are located in regions that receive low precipitation, generally
less than 25 cm per year. They occupy about 17 percent of land on earth. Some
deserts contain sand dunes, while others feature mostly rock. Due to the extremely
high temperature, low water availability and intense sunlight, vegetation is scarce
or poorly developed, and any animal species, such as insects, reptiles and birds,
must be highly adapted to the dry conditions. The vegetation is mainly shrubs,
bushes, fewgrasses and rare trees. The stems and leaves of the plants are modified
in order to conserve water as much as possible, for example, succulents such as
the spiny leaved cacti.
c) Grassland Ecosystems:
Grassland Ecosystems are typically found in both tropical and temperate regions of
the world. They share the common climactic characteristic of semi-aridity. The area
mainly comprises grasses with a little number of trees and shrubs. A lot of grazing
animals, insectivores and herbivores inhabit the grasslands. The two main types of
grasslands ecosystems are
Savanna: The tropical grasslands are dry seasonally and have few individual trees.
They support a large number of predators and grazers.
d) Mountain Ecosystem:
Mountain land provides a scattered and diverse array of habitats where a large
number of animals and plants are found. At the higher altitudes, under harsh
environment, only the treeless alpine vegetation can survive. The animals have
thick fur coats for prevention from cold and hibernation in the winter months.
Lower slopes are commonly covered with coniferous forests.
2. Aquatic Ecosystems:
Aquatic ecosystem is the ecosystem found in a body of water. It encompasses
aquatic flora, fauna and water properties, as well. There are two main types of
aquatic ecosystem – Marine and Freshwater Ecosystem.
a) Marine Ecosystem
Marine ecosystems are the biggest ecosystems, which cover around 71% of earth’s
surface and contain 97% of out planet’s water. Water in marine ecosystems
contains high amounts of dissolved minerals and salts. Various marine ecosystems
include oceanic (a relatively shallow part of oceans which lies on the continental
shelf), profundal (deep or bottom water), benthic bottom substrates, inter-tidal (the
place between low and high tides), estuaries, coral reefs, salt marshes,
hydrothermal vents where chemosynthetic bacteria make up the food base. Many
kinds of organisms live in marine ecosystems: the brown algae, corals,
cephalopods, echinoderms, dinoflagellates, sharks, etc.
b) Freshwater Ecosystem
Contrary to the Marine ecosystems, the freshwater ecosystem covers only 0.8% of
Earth's surface and contains 0.009% of the total water. Three basic kinds of
freshwater ecosystems exist.
iii) Wetlands - places in which the soil is inundated or saturated for some lengthy period of time.
Food Webs
In nature, the food chains never exist as isolated linear sequence; rather they are
interconnected to form a
network called food web. Therefore, a food web can be defined as a network
of food chains
interconnected to each other so that a number of options of eating and being eaten
are available at each trophic level. It was Charles Elton who presented the notion of
food web what he referred to as food cycle (Krebs 2009). In 1927, he recognized
that the length of these food chains was mostly limited to 4 or 5 links and the food
chains were not isolated, but hooked together into food webs. Food web is the real
depiction and illustration of the feeding relationships amongst species in a
community.
It offers an important tool for investigating the ecological interactions that define
energy flows and
predator-prey relationship (Cain et al. 2008). Fig. 5.4 shows a simplified food web in a
desert ecosystem.
this food web, grasshoppers feed on plants; scorpions feed on grasshoppers; kit
foxes prey on scorpions. In addition, the predators of a scorpion in a desert
ecosystem might be a golden eagle, an owl, a roadrunner, or a fox. The analysis of
food web is important to understand ecosystem dynamics.
These ecosystems exhibit resourceful energy and material cycling. It also displays
interconnectedness amid primary producers and predators.
Similarly, the living or the biotic features are the plants which are the primary
producers, and herbivores are the primary consumers. Then, comes the secondary
consumers which are carnivores and omnivores. Further, there are detritivores
which consume the decaying organic matter.
Thus, we see how biotic factors depend on the abiotic factors in order to survive.
Similarly, the plants need particular temperature, soil plus moisture for thriving.
Next, animals depend on these plants for food. Therefore, if there is a change or
alteration of any one feature, the balance in an ecosystem gets disturbed.
Impact of Human Activities on Balance in an Ecosystem
Just like any other animal, humans also depend on a balanced ecosystem for a
healthy life. Unfortunately, the activities being carried out by humans is creating a
negative impact on the balance in an ecosystem.
For instance, when humans pollute the abiotic features like water, soil, air and
more. They are degrading the quality of our environment and disrupting the
balance. Similarly, deforestation, land conversion, overfishing, and more impacts
our balanced ecosystem.
However, several good sustainable human activities can restore the lost balance in
an ecosystem. Some of them are the use of biofuels, reforestation, plastic ban,
prevention of burning of fossil fuels and more. So, we must try to adopt practices
which will help in maintaining the balance of our ecosystem rather than degrading
it.
HUMAN ACTIVITIES
With the development of science and technology, man continued to plunder natural
resources and polluted the environment. The craze of progress in industry,
agriculture and transportation has jeopardized the existence of man himself. Today
man equipped with a variety of skills and superior technology has ruined the
natural environment without understanding the rebounding repercussions even on
his own existence.
Instead of sparkling blue and white jewel, the biosphere now seems dull and dark
swirling with clouds of pollutants. Now numerous issues like ecological imbalance,
ozone hole, acid rain, CFC’S and global warming have been raised. We find
warnings everywhere as air unfit for breathing, water unfit for drinking, vegetables
unfit for eating and so on. Some human activities are as below.
FOOD
The need of increased food production as a result of global population explsion led
to manipulation of land resources causing a stress in the natural environment. The
food production and protection technologies are, however so interwoven and
interdependent that it is impossible to visualise a shoot up in crop production
individually. The use of pesticides helped in the eradication of diseases, pests and
in boosting crop production. But the pesticides endangered our life by acutely
affecting man, animals, plants, soil as well as aquatic biota. In a nutshell, if we
continue to rely upon broad spectrum of pesticides for crop production, the
recovery of natural forms of control wil become almost impossible.
SHELTER
Shelters for human living are increasing exponentially with the increasing
population. A good share of land which once was cropland, wetland, forest or fallow
land has been converted to concrete shelters adversely affecting the ecosystem.
ECONOMIC ASPECT
Man, in his pursuit of economic growth is upsetting the environmental equilibrium
and destroying his own life support system. Development in any region be made in
a holistic manner by optimal use of existing and potential resources in the
biosphere for the ultimate improvement of human well being.
SOCIAL SECURITY
Simple reforms of societies, with limited needs have secure and sustainable life
styles. Rapid changes towards a more consumeristic life style and increase in
various types of wastes makes the human life socially insecure.
AGRICULTURE
Modern agricultural techniques which are geared towards bumper crop production
to meet the evergrowing demands of rapidly increasing population are exploring
new agro-technologies to feed the masses. With the extensive use of
agrochemicals, the world is heading towards a complex array of
Fertilizer enriched soil can not support microbial flora. Hence there remains poor
humus and less nutrients while the soil can readily become eroded by wind and
water. So the question is: Why fertilizers are used to improve the quality of food
stuffs? Do they harm or benefit the soil?
• It is reported that there is a 30% decline in protein and carbohydrate content when
corn, maize, gram and wheat crops were grown on soils fertilized with NPK fertilizers.
• Potassium fertilizers in soil decreases the valuable nutrient ascorbic acid (vitamin C) and
carotene in vegetables and fruits. Fertilized soil produces bigger sized vegetables and fruits
which are more prone to pest, insects and diseases.
•Excessive use of nitrogenous fertilizers, caled' the miracle drug of farming, lead to
accumulation of nitrate in the soil which are transferred to man through plants. Nitrates,
being highly soluble, go into drinking ground water and become toxic when its concentration
exceeds 90 ppm., In human body these nitrates and nitrites are converted to nitrisoamines
and nitroso compounds which are suspected as agents of stomach cancer.
Though some pesticides (DDT) are banned, they still show small doses in foods.
Increasedproductivity of crops leads to greater dependency on agrochemicals
creating new problems to be faced in future.
HOUSING
The increase in population increased the demand for housing and dwelling units.
Due to increased human activities, more and more forest land and agricultural
fields are occupied for constructing houses and factories. .
• Housing degraded the land and shrunk the space for other living creatures.
• Since the land is not available, shallow lakes, ponds and other low lying areas are filled up for
housing.
• Migratory birds that visit these ponds are also affected as they lose a major source of food and
shelter.
• Most severe effect of housing is that any river passing by an urban settlement gets badly
polluted.
INDUSTRY
Industrialisation by man brought an overall change in circumstances accompanying
a society's movement, population and resources from farm production to
manufacturing production and associated services.
• Industrial effluents when discharged through sewage system will poison the biological
purification mechanism of sewage treatment causing several soil and water borne diseases.
• Industrial metallic contaminents (e.g., Hg, Pb, Zn, As, Cd) destroy bacteria and beneficial
micro-organisms in the soil.
• Severe agricultural crop damage is caused by high acidity and alkalinity of the soil
coming from chemical industries.
• Products of industries, such as synthetic fibres, plastics and waste paper when
consigned to incineration, their emissions may contaminate with toxic vapours and
particulates causing air pollution. When discarded plastic materials, textile packagings and
toys of polyvinyl chloride are burnt in soil, they emit highly toxic gases SO2 and NO2 etc.
(i) Jaduguda uranium mine, Jharkhand. Exposed local people to radioactive hazards.
(ii) Jharia coal mines, Jharkhand. Underground fire leading to land subsidence and forced
displacement of people.
(iii) Sukinda chromite mines, Orissa. Seepage of Cr (VI) into river. Chromium is
highly toxic and carcinogenic.
(iv) Kudremukh iron ore mine, Karnataka. Causes river pollution and threat to biodiversity.
(v) East coast bauxite mine, Orissa. Land encroachment and issue of rehabilitation unsettled.
(vi) North-eastern coal fields, Assam. Very high sulphur contamination of groundwater.
IMPACTS OF MINING
1. Devegetation of landscape. Soil damage during surface mining is inevitable as it leads
to loss of grazing and fertile land, soil erosion, sedimentation, damage to flora and fauna.
Open cast coal mining alone eroded 2,00,000 hectares of fertile land.
3. Groundwater contamination. Mining disturbs the natural hydrological cycle. Acid mine
drainage from sulphur bearing minerals leaches toxic metals to ground water.
4. Surface water pollution. Cyanide solution from gold mining severely pollute surface water.
5. Air pollution. Smelting results in emission of particulates, NO, SO2, CO, thereby causing
global warming, acid rain and climatic changes.
6. Dust and noise pollution, is caused during loading, crushing and drilling operations.
TRANSPORTATION
Transport is a good consumer of both land and energy. Transport consumes 30% of
world's energy (of which 82% is consumed on roads) and produces CO, NO,
particulates and hydrocarbons.
But there is hope of new cleaner transport in future. Several cars now run on
ethanol/petrol mixture and CNG. Use of leaded petrol has curtailed lead emission
by 87%. Auto-emissions have also been cleaned up.
ENVIRONMENTAL IMPACT ASSESSMENT (EIA)
Objective of EIA:
This Notification was amended on 4th May, 1994 and the amended version
includes a self explanatory note detailing the procedure for obtaining
environmental clearance, technical information, documents required to be
submitted for getting environmental clearance from the Ministry of Environment
and Forests.
• If so, an EIA is undertaken and the Environmental Impact Statement (EIS) is prepared.
4. Reviewer. Individual/Agency/Board.
• Site characteristics.
Importance of ElA
• It is the Government policy that any industrial project has to obtain EIA clearance
from the Ministry of Environment before approval by the Planning Commission.
SUSTAINABLE DEVELOPMENT
The World Commission on Environment and Development (the Brundtland
Commission) in its report to the United Nations in 1987 defined sustainable
development as meeting the needs of the present without compromising the
ability of future generation to meet their own needs.
Agenda 21, adopted during the United Nations Conference on Environ- ment
and Development (UNCED) called Earth Summit held in Rio de Janeiro in
Brazil in 1992 is a blue print on how to make development socially,
economically and environmentally sustainable.
• Conservation of biodiversity.
• Air, water, soil pollution prevention and control.
• Renewable energy resources.
• Renovation, recycling and reuse of wastes.
• Environmental education and awareness at all levels.
Pollution Prevention
Design of Environment
Future challenge is to switch over from the present pollution control policy and
Government regulations to a new more realistic pollution prevention policy
based on source reduction, recycling and reuse of wastes.
Industrial Ecology
Green Chemistry
PEM involves elimination of wastes and pollutants at their source rather than at
the end-of-the pipe stage. The principles of PEM are as follows.
• Prevention ofpollution at source.
• Recycling and treatment in a safe manner.
• Disposal, a last resort, should be done in an environmentally benign manner.