Resources
Everything in our environment which can be used to satisfy our needs and is technologically accessible, economically feasible and culturally acceptable is termed as ‘Resource’. Human beings themselves are essential components of resources. They transform material available in the environment into resources and use them.
Interdependent relationship between
nature, technology and institutions:-
The process of transformation of things
available in our environment involves an interactive relationship between
nature, technology and institutions .Human beings interact with nature through
technology and create institutions.
Classification of
Resources
Resources
can be classified in the following ways:
(a)
On the basis of origin – biotic and abiotic
(b)
On the basis of exhaustibility – renewable and non-renewable
(c)
On the basis of ownership – individual, community, national and international
(d)
On the basis of the status of development – potential, developed stock and
reserves
(a) On the Basis of Origin – Biotic and
Abiotic
Biotic Resources are obtained from the
biosphere and have life.
Eg:
Human beings, flora and fauna, fisheries, livestock etc.
Abiotic Resources: All those things
which are composed of non-living things are called abiotic resources.
Eg:
rocks and metals.
(b) On the Basis of Exhaustibility –
Renewable and Non-Renewable
The
resources which can be renewed or reproduced by physical, chemical or
mechanical processes are known as Renewable or Replenishable Resources.
The renewable resource may further be
divided into continuous or flow.
Eg:
Solar and wind energy, water, forests and wildlife, etc.
Non-Renewable Resources occur over a
very long geological time. These resources take millions of years in their
formation. Some of the resources like metals are recyclable and some like
fossil fuels cannot be recycled and get exhausted with their use.
Eg:
Minerals and fossil fuels.
(c) On the Basis of Ownership – Individual,
Community, National and International
Individual Resources are owned privately by individuals. In
villages people own lands whereas in urban areas people own plots, houses and
other properties.
Eg:
Plantation, pasture lands, ponds, water in wells etc.
Community Owned Resources are accessible
to all the members of the community.
Eg:
Grazing grounds, burial grounds, public parks, picnic spots, playgrounds etc.
National
Resources are
owned by a nation or country. All the minerals, water resources, forests,
wildlife, land within the political boundaries and oceanic area up to 12
nautical miles (22.2 km) from the coast termed as territorial water and
resources therein belong to the nation.
Eg:
Roads, canals, railways etc.
International Resources are regulated by international
institutions. The oceanic resources beyond 200 nautical miles of the Exclusive
Economic Zone belong to open ocean and no individual country can
utilise these without the concurrence of international institutions.
(d) On the Basis of
the Status of Development – Potential, Developed Stock and Reserves
Potential
Resources are
the resources which are found in a region but have not been utilised. Eg:
Rajasthan and Gujarat have enormous potential for the development of wind and
solar energy, but so far these have not been developed properly.
Developed
Resources:
Resources
which are surveyed and their quality and quantity have been determined for
utilisation. The development of resources depends on technology and level of
their feasibility. Eg:-Wood Using technology for its
development.
Materials
in the environment which have the potential to satisfy human needs but human
beings do not have the appropriate technology to access these, are called Stock.
Eg:
Hydrogen can be used as a rich source of energy. But we do not have advanced
technology to use it.
Reserves are the subset of the
stock, which can be put into use with the help of existing technical ‘know-how’
but their use has not been started. These can be used for meeting future
requirements.
Eg:
Water in the dams, forests etc. is a reserve which can be used in the future.
Development of
Resources
It
was believed that resources are free gift of nature. As a result human beings
indiscriminately and this has led to the following major problems.
- Depletion
of resources for satisfying the greed of a few individuals.
- Accumulation
of resources in a few hands, which, in turn, divided the society into two
segments i.e rich and poor.
- It has
led to global ecological crises such as global warming, ozone layer
depletion, environmental pollution and land degradation.
Resource
planning is essential for the sustainable existence of all forms of life.
Sustainable
Economic Development means “development should take place without damaging
the environment, and development in the present should not compromise with the
needs of future generations.”
Rio de Janeiro Earth Summit, 1992- 100 countries met Rio
de Janeiro in Brazil. The summit was convened for addressing urgent problems of
environment protection and socio economic development. Rio adopted Agenda 21
for achieving Sustainable Development.
Agenda 21- Agenda 21 was the
declaration signed by world leaders in 1992 at the United Nations conference on
Environment and Development (UNCED), which aimed at achieving global
cooperation on common interests, mutual needs and shared responsibilities.
Resource Planning
In
India, there are some regions which can be considered self-sufficient in terms
of the availability of resources and there are some regions which have acute
shortage of some vital resources. This calls for balanced resource planning at
the national, state, regional and local levels. For example: Chattisgarh and
Madhya Pradesh are rich in Minerals and Coal deposits. Arunachal Pradesh has
abundance of water resource but lack in infrastructural development. The State
of Rajasthan is very well endowed with solar and wind energy but lacks in water
resources. This calls a balanced resources planning at the national, state,
regional and local levels.
Resource Planning in India
Resource
planning is a complex process which involves:
(i)
Identification and inventory of resources across the regions of the country.
This involves surveying, mapping and qualitative and quantitative estimation
and measurement of the resources.
(ii)
Evolving a planning structure endowed with appropriate technology, skill and
institutional set up for implementing resource development plans.
(iii)
Matching the resource development plans with overall national development
plans.
Resources
can contribute to development only when they are accompanied by appropriate
technological development and institutional changes. India has made concerted
efforts towards achieving the goals of resource planning, right from the First
Five Year Plan launched after Independence.
To
overcome irrational consumption and over-utilization of resources, resource conservation at various levels is
important.
Land Resources
Land
is a natural resource of utmost importance. It supports natural vegetation,
wildlife, human life, economic activities, and transport and communication
systems. India has land under a variety of relief features, namely; mountains,
plateaus, plains and islands as shown below:
Land Utilisation
Land
resources are used for the following purposes:
1. Forests
2. Land not available for
cultivation
a) Barren and
wasteland
b) Land put to
non-agricultural uses
3. Fallow lands-
a. Current fallow-
left without cultivation for one or less than one agricultural year). b.Other
uncultivated lands (excluding fallow land)
4. Net sown area
Land Use Pattern in India
The
use of land is determined
1. Physical factors: such as
topography, climate, soil types
2. Human factors: such as
population density, technological capability and culture and traditions etc.
The
data below represents the land use pattern in India.
Waste
land is
the land put to other non-agricultural uses which include rocky, arid and
desert areas, roads, railways, industry etc. Continuous use of land over a long
period of time without taking appropriate measures to conserve and manage it,
has resulted in land degradation.
Land Degradation and Conservation
Measures
Human
activities such as deforestation, overgrazing, mining and quarrying have
contributed significantly to land degradation. Mining sites leave deep scars
and traces of over-burdening the land. In recent years, industrial effluents as
waste have become a major source of land and water pollution in many parts of
the country.
Some
of the ways through which we can solve the problems of land degradation are:
1. Afforestation and
proper management of grazing.
2. Planting of shelter
belts of plants.
3. Stabilization of sand
dunes by growing thorny bushes.
4. Proper management of
waste lands.
5. Control of mining
activities.
6. Proper discharge and
disposal of industrial effluents and wastes after treatment.
Soil as a Resource
Soil
is the most important renewable natural resource. It is the medium of plant
growth and supports different types of living organisms on the earth.
1. It takes millions of
years to form soil upto a few cms in depth. Various forces of nature such as
change in temperature, actions of running water, wind and glaciers, activities
of decomposers etc contribute to the formation of soil.
2. Parent rock or
bedrock, climate, vegetation and other forms of life and time are important
factors in the formation of soil.
3. Chemical and organic
changes which take place in the soil play an important role.
4. Soil also consists of
organic (humus) and inorganic materials.
Classification of
Soils
On
the basis of the factors responsible for soil formation, colour, thickness,
texture, age, chemical and physical properties, the soils of India are
classified in different types as mentioned below.
Alluvial Soils
1. The entire northern
plains are made of alluvial soil.
2. The Alluvial Soil is
deposited by 3 important Himalayan river systems – the Indus, the Ganga and the
Brahmaputra.
3. It is also found in
Rajasthan, Gujarat and eastern coastal plains particularly in the deltas of the
Mahanadi, the Godavari, the Krishna and the Kaveri rivers.
4. The alluvial soil
consists of various proportions of sand, silt and clay. As we move inlands
towards the river valleys, soil particles appear to be bigger in size whereas
in the upper side of the river valley, the soils are coarse.
5. Based on age, Alluvial
soils can be classified as:
6. Old Alluvial (Bangar): The Bangar soil
has a higher concentration of kanker nodules than the Khadar.
7. New Alluvial (Khadar): It has more fine
particles and is more fertile than the Bangar.
8. Alluvial soils are
very fertile. These soils contain an adequate proportion of potash, phosphoric
acid and lime, which are ideal for the growth of sugarcane, paddy, wheat and
other cereal and pulse crops.
Black Soil
1. This soil is black in
colour and is also known as regur soil. Climatic conditions along
with the parent rock material are the important factors for the formation of
black soil.
2. The soil is ideal for
growing cotton and is also known as black cotton soil.
3. This type of soil is
typical of the Deccan trap (Basalt) region spread over northwest Deccan plateau
and is made up of lava flows.
4. The soil covers the
plateaus of Maharashtra, Saurashtra, Malwa, Madhya Pradesh and Chhattisgarh and
extends in the south-east direction along the Godavari and the Krishna valleys.
5. The black soils are
made up of extremely fine i.e. clayey material and well-known for their
capacity to hold moisture.
6. Black soil is
nutrients rich and contains calcium carbonate, magnesium, potash and lime.
7. The soil is sticky
when wet and difficult to work on unless tilled immediately after the first
shower or during the pre-monsoon period.
1. This type of soil
develops on crystalline igneous rocks in areas of low rainfall in the eastern
and southern parts of the Deccan plateau.
2. These soils develop a
reddish colour due to diffusion of iron in crystalline and metamorphic rocks.
It looks yellow when it occurs in a hydrated form.
3. Found in parts of
Odisha, Chhattisgarh, southern parts of the middle Ganga plain and along the
piedmont zone of the Western Ghats.
Laterite Soil
1. The laterite soil
develops under tropical and subtropical climate with the alternate wet and dry
season.
2. This soil is the
result of intense leaching due to heavy rain.
3. Lateritic soils are
acidic (pH<6.0) in nature and generally deficient in plant nutrients. This
type of soil is found mostly in Southern states, Western Ghats region of
Maharashtra, Odisha, some parts of West Bengal and North-east regions.
4. The soil supports
deciduous and evergreen forests but humus poor.
This soil is very useful
for growing tea and coffee.
Arid Soils
1. Arid soils range from
red to brown in colour.
2. This soil is generally
sandy in texture and saline in nature. In some areas, the salt content is very
high and common salt is obtained by evaporating the water.
3. Arid soil lacks humus
and moisture.
4. The lower horizons of
the soil are occupied by Kankar because of the increasing
calcium content downwards. The Kankar layer formations in the bottom horizons
restrict the infiltration of water.
Forest Soils
1. These soils are found
in the hilly and mountainous areas.
2. The soil texture is
loamy and silty in valley sides and coarse grained in the upper slopes.
3. In the snow covered
areas of Himalayas, these soils experience denudation and are acidic with low
humus content. The soil is fertile on the river terraces and alluvial fans.
Soil Erosion and Soil
Conservation-
·
The
removal of top soil cover due to various reasons like wind, glacier and water
is called soil erosion.
·
The
processes of soil formation and erosion go simultaneously and generally there
is balance between the two. But sometimes, this balance is disturbed due to
human activities.
·
Natural
forces like wind, glacier and water lead to soil erosion. Soil erosion is also
caused due to defective methods of farming.
·
Contour
ploughing, terrace cultivation, shelter belts are some of the measures that
prevent soil erosion.
The denudation of the soil cover and
subsequent washing down is described as soil erosion. The soil erosion is
caused due to human activities like deforestation, over-grazing, construction
and mining etc. Also, there are some natural forces like wind, glacier and
water which lead to soil erosion. Soil erosion is also caused due to defective
methods of farming.
The
running water cuts through the clayey soils and makes deep channels as gullies.
The land becomes unfit for cultivation and is known as bad land.
When water flows as a sheet over large areas down a slope and the topsoil is
washed away, it is known as sheet erosion. Wind blows loose soil
off flat or sloping land known as wind erosion.
Different Ways for
Soil Conservation
1. Ploughing along the
contour lines decelerate the flow of water down the slopes. This is called
Contour Ploughing.
2. Terrace cultivation restricts erosion.
This type of agriculture practice is done in Western and Central Himalayas.
3. When a large field is
divided into strips and strips of grass are left to grow between the crops.
Then, this breaks up the force of the wind. This method is known as Strip
Cropping.
4. Planting lines of
trees to create shelter helps in the stabilisation of sand dunes and in
stabilising the desert in western India. Rows of such trees are called Shelter
Belts.
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