Geography

POULTRY FARMING and SILVER REVOLUTION IN INDIA

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POULTRY FARMING (SILVER REVOLUTION) IN INDIA

  • practice of raising poultry, such as chickens, turkeys, ducks, geese, as a subcategory of animal husbandry, for the purpose of farming meat or eggs for food.
  • requires small capital and provides additional income and job opportunities to a large number of rural population in the shortest possible time.
  • The vast majority of poultry are farmed using factory farming techniques.
  • The contrasting method of poultry farming in free range and friction between the two main methods, has led to long term issues of ethical consumerism.
  • Opponents of the factory farming argue that it harms the environment and creates health risks, as well as abuses animals.
  • In contrast, proponents of factory farming highlight its increased productivity, stating that the animals are looked after in state-of-the art confinement facilities and are happy; that it is needed to feed the growing global human population; and that it protects the environment.

 

Poultry Farming in India

  • Poultry farming in India is quite old.
  • At present, more than three million people are directly or indirectly employed in poultry farming.
  • Further, landless labourers derive more than 50 per cent of their income from livestock, especially poultry.
  • Uninterrupted supplies of feed as well as avian influenza are critical for the continued robust growth of the poultry sector.
  • The first outbreak of avian influenza occurred in India in the state of Maharashtra in the Nandurbar district on 18th Feb. 2006.
  • The Central Poultry Development Organisation has been playing a pivotal role in the implementation of the policies of the Government with respect to poultry as a tool for alleviating nutritional hunger and palliating the impecuniosity’s of the resource-poor farmers, especially the women.
  • The mandate of the Central Poultry Development Organisation has been specifically revised, by restructuring all poultry units of this Department to focus on improved indigenous birds, which lay on an average 180-200 eggs per annum and have a vastly improved FCR ratio in terms of feed consumption and weight gain.
  • The Central Poultry Development Organisations have been entrusted with the responsibility of producing excellent germplasm in the form of day-old chicks and hatching eggs of these varieties like Nierbheek, Hitkari, Vanaraja, Shyama, Cari, Chabro, etc.
  • Besides, these organisations are also playing a crucial role in analysing feed samples.
  • A new Centrally-sponsored scheme called Assistance to State Poultry, is being implemented during the Tenth Plan where one time assistance is provided to suitably strengthen the farms in terms of hatching, brooding, and rearing of birds with provision for feed mill and their quality monitoring and in-house disease diagnostic facilities.
  • A new scheme, Dairy/Poultry Venture Capital Fund, has been launched during the 2004-05, wherein there is a provision to grant subsidy on interest payment.
  • The nodal agency for the implementation of this scheme is NABARD through nationalized commercial bank.

 

Greenhouse effect

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The greenhouse effect is a natural process that warms the Earth’s surface. When the Sun’s energy reaches the Earth’s atmosphere, some of it is reflected back to space and the rest is absorbed and re-radiated by greenhouse gases. It is the process by which radiation from a planet’s atmosphere warms the planet’s surface to a temperature above what it would be without its atmosphere. If a planet’s atmosphere contains radioactively active gases (i.e., greenhouse gases) the atmosphere will radiate energy in all directions.

The greenhouse effect comes from molecules that are more complex and much less common. Water vapour is the most important greenhouse gas, and carbon dioxide (CO2) is the second-most important one. Methane, nitrous oxide, ozone and several other gases present in the atmosphere in small amounts also contribute to the greenhouse effect. In the humid equatorial regions, where there is so much water vapour in the air that the greenhouse effect is very large, adding a small additional amount of CO2 or water vapour has only a small direct impact on downward infrared radiation. However, in the cold, dry polar regions, the effect of a small increase in CO2 or water vapour is much greater. The same is true for the cold, dry upper atmosphere where a small increase in water vapour has a greater influence on the greenhouse effect than the same change in water vapour would have near the surface.

Green house effects changes are due to:-

  • Energy;
  •  Industry;
  •  Agriculture;
  •  Waste; and
  • Land Use Land Use Change

SERICULTURE IN INDIA

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SERICULTURE IN INDIA

Production

  • Silkworm larvae are fed on mulberry leaves and after the fourth molt, they climb a twig placed near them and spin their silken cocoons.
  • The silk is a continuous-filament fibre consisting of fibroin protein, secreted from two salivary glands in the head of each larva, and a gum called sericin, which cements the two filament together.
  • The sericin is removed by placing the cocoons in hot water, which frees silk filaments and readies them for reeling.
  • The immersion of cocoons in hot water also kills the silkworm larvae.
  • In India, silk worms thrive on the leaves of mulberry, mahua, sal, ber, and kusum trees. India ranks third among the silk producing countries of the world.
  • Silk production is mainly confined to areas between 15° and 34° N latitudes.
  • The state of Karnataka is the largest producer of raw silk (65°/o) followed by Andhra Pradesh (17%) West Bengal (8°/o), Tamil Nadu (5°/o), and Assam (3%).

 

 Insolation,heat budget of the earth

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The ultimate source of atmospheric energy is in fact heat and light received through space from the Sun. This energy is known as solar insolation. The Earth receives only a tiny fraction of the total amount of Sun’s radiations. Only two billionths or two units of energy out of 1,00,00,00,000 units of energy radiated by the sun reaches the earth’s surface due to its small size and great distance from the Sun. The unit of measurements of this energy is Langley (Ly). On an average the earth receives 1.94 calories per sq. cm per minute (2 Langley) at the top of its atmosphere.

Incoming solar radiation through short waves is termed as insolation. The amount of insolation received on the earth’s surface is far less than that is radiated from the sun because of the small size of the earth and its distance from the sun. Moreover water vapour, dust particles, ozone and other gases present in the atmosphere absorb a small amount of insolation.

The amount of insolation received on the earth’s surface is not uniform everywhere. It varies from place to place and from time to time. The tropical zone receive the maximum annual insolation. It gradually decreases towards the poles. Insolation is more in summers and less in winters.
The following factors influence the amount of insolation received.
(i) The angle of incidence:-The angle formed by the sun’s ray with the tangent of the earth’s circle at a point is called
angle of incidence. It influences the insolation in two ways. First, when the sun is almost overhead, the rays of the sun are vertical. The angle of incidence is large hence, they are concentrated in a smaller area, giving more amount of insolation at that place. If the sun’s rays are oblique, angle of incidence is small and sun’s rays have to heat up a greater area, resulting in less amount of insolation received there. Secondly, the sun’s rays with small angle, traverse more of the atmosphere, than rays striking at a large angle. Longer the path of sun’s rays, greater is the amount of reflection and absorption of heat by atmosphere. As a result the intensity of insolation at a place is less.
(ii) Duration of the day. (daily sunlight period) :-The duration of day is controlled partly by latitude and partly by the season of the year. The amount of insolation has close relationship with the length of the day. It is because insolation is received only during the day. Other conditions remaining the same, the longer the days the greater is the amount of insolation. In summers, the days being longer the amount of insolation received is also more. As against this in winter the days are shorter the insolation received is also less. On account of the inclination of the earth on its axis at an angle of 23 ½ , rotation and revolution, the duration of the day is not same everywhere on the earth. At the equator there is 12 hours day and night each throughout the year. As one moves towards poles duration of the days keeps on increasing or decreasing. It is why the maximum insolation is received in equatorial areas.

(iii) Transparency of the atmosphere.Transparency of the atmosphere: Transparency of the atmosphere also determines the amount of insolation reaching the earth’s surface. The transparency depends upon cloud cover, its thickness, dust particles and water vapour, as they reflect, absorb or transmit insolation. Thick clouds hinder the insolation to reach the earth while clear sky helps it to reach the surface. Water vapour absorb insolation, resulting in less amount of insolation reaching the surface.

Heat Budget

Energy emitted by the Earth’s climate system tends to maintain a balance with solar energy coming into the system. This balance, known as the radiation budget, allows the Earth to maintain the moderate temperature range essential for life as we know it.
There is positive radiation balance between 35°S and 40°N, which drives the weather systems. Ocean currents even out the difference
When incoming short-wave solar radiation (Figure 3), known as insolation, enters the Earth’s climate system, a portion of it is absorbed at the Earth’s surface, causing the surface to heat up. Some of the absorbed energy is then radiated outward in the form of long-wave infrared radiation. Cloud layers trap some of the radiation from the Earth’s surface, and then emit long-wave radiation, both outward and back to the surface. The temperature of the Earth’s surface is about 33°C higher due to long-wave radiation contribution from the atmosphere .
The amount of radiation emitted by the Earth’s surface that makes it back to space is the result of many interrelated influences, such as the amount of cloud cover, cloud heights, characteristics of cloud droplets, amount and distribution of water vapor and other greenhouse gases, land features, surface temperature, and the transparency of the atmosphere. In the warm tropical areas, low values of outgoing longwave radiation (OLR) correspond to large amounts of high, cold clouds while high values of OLR correspond to relatively clear areas or cloudy areas with low, warm clouds. In the extra-tropics OLR values typically decrease with decreasing temperature.

Let us suppose that the total heat (incoming solar radiation) received at the top of the atmosphere is 100 units (see fig. 10.2) Roughly 35 units of it are reflected back into space even before reaching the surface of the earth. Out of these 35 units, 6 units are reflected back to space from the top of the atmosphere, 27 units reflected by clouds and 2 units from the snow and ice covered surfaces.
Out of the remaining 65 units (100-35), only 51 units reach the earth’s surface and 14 units are absorbed by the various gases, dust particles and water vapour of the atmosphere.
The earth in turn radiates back 51 units in the form of terrestrial radiation. Out of these 51 units of terrestrial radiation, 34 units are absorbed by the atmosphere and the remaining 17 units directly go to space. The atmosphere also radiates 48 units (14 units of incoming radiation and 34 units of outgoing radiation absorbed by it) back to space. Thus 65 units of solar radiation entering the atmosphere are reflected back into the space. This account of incoming and outgoing radiation always maintains the balance of heat on the surface of the earth.

Various National Missions and Programmes:-

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  1. MNREGA
  2. Jan Dhan Yojna
  3. Atal Pension Yojna
  4. Skill India Mission
  5. Deen Dayal Upadhyaya Gram Jyoti Yojana
  6. Pradhan Mantri Suraksha Bima Yojana
  7. Pradhan Mantri Jeevan Jyoti Bima Yojana
  8. Sukanya Samridhi Yojana
  9. Pradhan Mantri  Garib Kalyan Yojana
  10. Jan Aushadhi Yojana (JAY)
  11. Nai Manzil Scheme for minority students
  12. The Pradhan Mantri Awas Yojana (PMAY) or Housing for all by 2022
  13. AMRUT Mission
  14. Smart City Mission
  15. National Food Security Act-2013

 

Evolution and characteristics of landforms in the Fluvial, Glacial, Arid and Karst regions  

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Landform

Each landform has its unique physical shape, size, materials and is a result of the action of certain geomorphic processes and agent(s). Every landform has a beginning. Landforms once formed may change in their shape, size and nature slowly or fast due to continued action of geomorphic processes and agents. Due to changes in climatic conditions and vertical or horizontal movements of landmasses, either the intensity of processes or the processes themselves might change leading to new modifications in the landforms.

Evolution

It implies stages of transformation of either a part of the earth’s surface from one landform into another or transformation of individual landforms after they are once formed. That means, each and every landform has a history of development and changes through time. A landmass passes through stages of development somewhat comparable to the stages of life — youth, mature and old age.

Geomorphic Agents

Changes on the surface of the earth owe mostly to erosion by various geomorphic agents. Running water, ground-water, glaciers, wind and waves are powerful    erosional and depositional agents shaping and changing the surface of the earth aided by weathering and mass wasting processes. These geomorphic agents acting over long periods of time produce systematic changes leading to sequential development of landforms.

Fluvial landforms

The landforms created as a result of degradational action (erosion) or aggradation work (deposition) of running water is called fluvial landforms.

These landforms result from the action of surface flow/run-off or stream flow (water flowing through a channel under the influence of gravity). The creative work of fluvial processes may be divided into three physical phases—erosion, transportation and deposition.

The landforms created by a stream can be studied under erosional and depositional categories.

Erosional category

Valleys, gorge and Canyon

The extended depression on ground through which a stream flows throughout its course is called a river valley. A gorge is a deep valley with very steep to straight sides. A canyon is characterized by steep step-like side slopes and may be as deep as a gorge.

At a young stage, The profile of valley  is typically ‘V’ shaped. As the cycle attains maturity, the lateral erosion becomes prominent and the valley floor flattens out. The valley profile now becomes typically ‘U’ shaped with a broad base and a concave slope.

Potholes, Plunge pools

Potholes are more or less circular depressions over the rocky beds of hills streams.Once a small and shallow depression forms, pebbles and boulders get collected in those depressions and get rotated by flowing water. Consequently, the depressions grow in dimensions to form potholes.Plunge pools are nothing but large, deep potholes commonly found at the foot of a waterfall. They are formed because of the sheer impact of water and rotation of boulders.

Incised or Entrenched Meanders

They are very deep wide meanders (loop-like channels) found cut in hard rocks.In the course of time, they deepen and widen to form gorges or canyons in hard rock.The difference between a normal meander and an incised/entrenched meander is that the latter found on hard rocks.

River Terraces

They are surfaces marking old valley floor or flood plains.They are basically the result of vertical erosion by the stream. When the terraces are of the same elevation on either side of the river, they are called as paired terraces.When the terraces are seen only on one side with none on the other or one at quite a different elevation on the other side, they are called as unpaired terraces.

Depositional Features

Alluvial Fans

They are found in the middle course of a river at the foot of slope/ mountains.When the stream moves from the higher level break into foot slope plain of low gradient, it loses its energy needed to transport much of its load.Thus, they get dumped and spread as a broad low to the high cone-shaped deposits called an alluvial fan.

Deltas

They are found in the mouth of the river, which is the final location of depositional activity of a river. \The coarser material settle out first and the finer materials like silt and clay are carried out into the sea.

 

 Flood Plains, Natural Levees

Natural levees are found along the banks of large rivers. They are low, linear and parallel ridges of coarse deposits along the banks of a river.The levee deposits are coarser than the deposits spread by flood water away from the river.

 

 Meanders and oxbow lakes

  • They are formed basically because of three reasons: (i) propensity of water flowing over very gentle gradient to work laterally on the banks; (ii) unconsolidated nature of alluvial deposits making up the bank with many irregularities; (iii) Coriolis force acting on fluid water deflecting it like deflecting the wind.
  • The concave bank of a meander is known as cut-off bank and the convex bank is known as a slip-off
  • As meanders grow into deep loops, the same may get cut-off due to erosion at the inflection point and are left as oxbow lakes.

Braided Channels

When selective deposition of coarser materials causes the formation of a central bar, it diverts the flow of river towards the banks, which increases lateral erosion. Similarly, when more and more such central bars are formed, braided channels are formed. Riverine Islands are the result of braided channels.

 

Karst Topography

Any limestone, dolomite or gypsum region showing typical landforms produced by the action of groundwater through the process of solution and deposition is called as Karst Topography (Karst region in the Balkans).

Sinkholes

A sinkhole is an opening more or less circular at the top and funnel-shaped towards the bottom.When as sinkhole is formed solely through the process of solution, it is called as a solution sink.When several sink holes join together to form valley of sinks, they are called as blind valleys.

 

Caves

In the areas where there are alternative beds of rocks (non-soluble) with limestone or dolomite in between or in areas where limestone are dense, massive and occurring as thick beds, cave formation is prominent. Caves normally have an opening through which cave streams are discharged Caves having an opening at both the ends are called tunnels.

Stalactites and stalagmites

They are formed when the calcium carbonates dissolved in groundwater get deposited once the water evaporates.These structures are commonly found in limestone caves.Stalactites are calcium carbonate deposits hanging as icicles while Stalagmites are calcium carbonate deposits which rise up from the floor.When a stalactite and stalagmite happened to join together, it gives rise to pillars or columns of different diameters.

GLACIERS

Masses of ice moving as sheets over the land (continental glacier or piedmont glacier if a vast sheet of ice is spread over the plains at the foot of mountains) or as linear flows down the slopes of mountains in broad trough-like valleys (mountain and valley glaciers) are called glaciers.

EROSIONAL LANDFORMS

Cirque

Cirques are the most common of landforms in glaciated mountains. They are deep, long and wide troughs or basins with very steep concave to vertically dropping high walls at its head as well as sides. A lake of water can be seen quite often within the cirques after the glacier disappears. Such lakes are called cirque or tarn lakes.

Horns and Serrated Ridges

Horns form through head ward erosion of the cirque walls. If three or more radiating glaciers cut headward until their cirques meet, high, sharp pointed and steep sided peaks called horns form.

 

Glacial Valleys/Troughs

Glaciated valleys are trough-like and U-shaped with broad floors and relatively smooth, and steep sides. There may be lakes gouged out of rocky floor or formed by debris within the valleys. There can be hanging valleys at an elevation on one or both sides of the main glacial valley. Very deep glacial troughs filled with sea water and making up shorelines (in high latitudes) are called fjords/fiords.

 

Depositional landforms

 

Moraines

They are long ridges of deposits of glacial till. Terminal moraines are long ridges of debris deposited at the end (toe) of the glaciers. Lateral moraines form along the sides parallel to the glacial valleys. The lateral moraines may join a terminal moraine forming a horse-shoe shaped ridge. deposits varying greatly in thickness and in surface topography are called ground moraines.

 

Eskers

When glaciers melt in summer, the water flows on the surface of the ice or seeps down along the margins or even moves through holes in the ice. These waters accumulate beneath the glacier and flow like streams in a channel beneath the ice. Such streams flow over the ground (not in a valley cut in the ground) with ice forming its banks. Very coarse materials like boulders and blocks along with some minor fractions of rock debris carried into this stream settle in the valley of ice beneath the glacier and after the ice melts can be found as a sinuous ridge called esker.

Outwash Plains

The plains at the foot of the glacial mountains or beyond the limits of continental ice sheets are covered with glacio-fluvial deposits in the form of broad flat alluvial fans which may join to form outwash plains of gravel, silt, sand and clay.

Drumlins

Drumlins are smooth oval shaped ridge-like features composed mainly of glacial till with some masses of gravel and sand. The long axes of drumlins are parallel to the direction of ice movement. They may measure up to 1 km in length and 30 m or so in height.

 

Arid Landforms

Wind is one of the  dominant agents in hot deserts. The wind action creates a number of interesting erosional and depositional features in the deserts.

 

EROSIONAL LANDFORMS

Pediments and Pediplains

. Gently inclined rocky floors close to the mountains at their foot with or without a thin cover of debris, are called pediments. through parallel retreat of slopes, the pediments extend backwards at the expense of mountain front, and gradually, the mountain gets reduced leaving an inselberg which is a remnant of the mountain. That’s how the high relief in desert areas is reduced to low featureless plains called pediplains.

Playas

Plains are by far the most prominent landforms in the deserts. In times of sufficient water, this plain is covered up by a shallow water body. Such types of shallow lakes are called as playas where water is retained only for short duration due to evaporation and quite often the playas contain good deposition of salts.

. Deflation Hollows and Caves

Weathered mantle from over the rocks or bare soil, gets blown out by persistent movement of wind currents in one direction. This process may create shallow depressions called deflation hollows. Deflation also creates numerous small pits or cavities over rock surfaces. The rock faces suffer impact and abrasion of wind-borne sand and first shallow depressions called blow outs are created, and some of the blow outs become deeper and wider fit to be called caves.

Mushroom, Table and Pedestal Rocks

Many rock-outcrops in the deserts easily susceptible to wind deflation and abrasion are worn out quickly leaving some remnants of resistant rocks polished beautifully in the shape of mushroom with a slender stalk and a broad and rounded pear shaped cap above. Sometimes, the top surface is broad like a table top and quite often, the remnants stand out like pedestals.

Depositional Landforms

When the wind slows or begins to die down, depending upon sizes of grains and their critical velocities, the grains will begin to settle.

Sand Dunes

Dry hot deserts are good places for sand dune formation. Obstacles to initiate dune formation are equally important. There can be a great variety of dune forms Crescent shaped dunes called barchans with the points or wings directed away from wind .Parabolic dunes form when sandy surfaces are partially covered with vegetation. That means parabolic dunes are reversed barchans with wind direction being the same.

Seif is similar to barchan with a small difference. Seif has only one wing or point. Longitudinal dunes form when supply of sand is poor and wind direction is constant. They appear as long ridges of considerable length but low in height. Transverse dunes are aligned perpendicular to wind direction. These dunes form when the wind direction is constant and the source of sand is an elongated feature at right angles to the wind direction.

 

 Air masses and fronts

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Airmasses

 

An airmass is a large body of air with relatively uniform thermal and moisture characteristics. Airmasses cover large regions of the earth, typically several hundred thousand square kilometers. Airmasses can be as deep as the depth of the troposphere or as shallow as 1 to 2 km.
Airmasses form when air remains over a relatively flat region of the earth* with homogeneous surface characteristics for an extended period of time. ( Canadian and Siberian plains, cool oceanic regions such as the North Atlantic and Pacific, deserts, such as the Sahara and the American southwest, and tropical oceanic regions including the equatorial Atlantic and Pacific, and smaller water bodies such as the Caribbean Sea and the Gulf of Mexico).

Polar air masses, containing little moisture and low temperatures move downward from the poles.  Air masses that form over water are generally moist, and those that form over the tropical oceans are both moist and warm. Because of the Coriolis effect due to the Earth’s rotation, air masses generally move across North America from west to east.  But, because of the differences in moisture and heat, the collision of these air masses can cause instability in the atmosphere.

Polar air mass is cold and tropical air mass is warm. When cold air mass and warm air mass blow against each other, the boundary line of convergence separating the two air masses is termed as front. When the warm air mass, moves upward over the cold air mass the front formed in such a situation is called warm front. On the contrary, when the cold air mass advances faster and undercuts the warm air mass and forces the warm air upwards, the front so formed is called cold front. The frontal surface of cold front is steeper than that of a warm front . A prevailing air mass in any region – polar, tropical, maritime or continental largely controls the regions general weather.

Different air masses are:-

  1. Maritime tropical (mT)
    ii. Continental tropical (cT)
    iii. Maritime polar (mP)
    iv. Continental polar (cP)
    v. Continental arctic (cA).

Where ‘m’ stands for Maritime; ‘c’ stands for continental; ‘T’ stands for tropical; ‘P’ stands for polar and ‘A’ stands for arctic region.

Fronts

An important properties of air is that it is a poor conductor of energy. This means that when two different bodies of air come together, they do not readily mix. Rather, each body of air will retain its individual properties, and a boundary forms between them. When two large air masses meet, the boundary that separates them is called a front. Fronts represent fairly abrupt transitions between two large air masses. The warm, moist air might dominate an area hundreds of miles across, while in another part of the continent a cold, dry air mass holds sway over an equally large region. However, where the two air masses meet, the transition layer between them may be only a few tens of miles across, clearly a sharp transition between two massive bodies of air.

Fronts are recognized by the following properties:-

  • Sharp temperature changes over a relatively short distance. Sometimes change of 10 to 20 C may be observed.
  • Change in moisture content
  • Rapid shifts in wind direction
  • Pressure changes
  • Clouds and precipitation patterns

Types of Fronts:-

Warm Fronts: A warm front occurs when a warm air mass advances and replaces a cold air mass. On a weather map, a warm front is depicted as a red arc, with red semicircles pointing in the direction of the advancing warm air.

Cold Fronts :-A cold front occurs when a mass of cold air advances into a region of warmer air.

Stationary Fronts:- A stationary front forms when a cold front or warm front stops moving. This happens when two masses of air are pushing against each other but neither is powerful enough to move the other. Winds blowing parallel to the front instead of perpendicular can help it stay in place.

Occluded Fronts:- Sometimes a cold front follows right behind a warm front. A warm air mass pushes into a colder air mass (the warm front) and then another cold air mass pushes into the warm air mass (the cold front). Because cold fronts move faster, the cold front is likely to overtake the warm front. This is known as an occluded front

 

 

Wegner’s Continental Drift Theory

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Alfred Wegner was a German Meteorologist in the early 1900s who studied ancient climates. Like most people, the jigsaw puzzle appearance of the Atlantic continental margins caught his attention. He put together the evidence of ancient glaciations and the distribution of fossil to formulate a theory that the continents have moved over the surface of the Earth, sometimes forming large supercontinents and other times forming separate continental masses. He proposed that prior to about 200 million years ago all of the continents formed one large land mass that he called Pangea .

According to Alfred Wegener, the entire landmass of the globe was together about 280 million years ago. It was termed as Pangea, a super continent. The huge water body surrounding the Pangea was known as Panthalasa. From 80 to 150 million years ago, Pangea was broken latitudinally into northern and southern parts known as Laurasia (Angaraland) and Gondwanaland, respectively. Both of them drifted away and in between a shallow sea emerged by filling up the water from Panthalasa. It was known as Tethys sea. Later on Laurasia and Gondwanaland rifted and finally drifted to form the present day distribution of land and water on the earth .

 

Wegener’s explanation of continental drift in 1912 was that drifting occurred because of the earth’s rotation. Fossil records from separate continents, particularly on the outskirts of continents show the same species.

The evidence which gave rise to the theory of continental drift includes the following:

  • The coasts of the continents surrounding the Atlantic ocean could, if the continents were moved closer, fit together like a jigsaw puzzle.
  • Living animals in widely separated lands are similar. For example India and Madagascar have similar mammals, which are quite different from those in Africa, even though it is now near to Madagascar.
  • Fossil plants in India, South Africa, Australia, Antarctica and South America are similar to each other. This so-called Glossopteris flora is quite different from plants found in other parts of the world at the same time.
  • There are numerous geological similarities between eastern South America and western Africa.
  • Apparent Polar Wandering: Paleomagnetism tells us how far from the poles rocks were when they formed, by looking at the angle of their magnetic field. The story told by different continents is contradictory, and can only be explained if we assume the continents have moved over time.There are ridges in the floors of the main oceans.Paleomagnetism shows that the sea floor has spread away from these ridges. Distinct patterns of stripes can be seen in the magnetism of rocks on either side of the ridges.

Indian Agriculture- Current Status, Issues & initiatives.

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Indian Agriculture

  • Mainstay of Indian Economy
  • Since independence, undergone a change from being the sector contributing the highest share to the GDP to one contributing the lowest share.
  • Agriculture is a state subject.
  • GDP contribution (Agriculture and allied sector)
    • 5 pc in 1950-51
    • 7 pc in 2008-09 and 14.6 pc in 2009-10. It was 19 pc in 2004-05. (2004-05 prices)
    • Agricultural GDP grew by 0.4 pc in 2009-10 and -0.1 pc in 2008-09.
  • Employment
    • 9 pc in 1961
    • 9 pc in 1999-2000
    • 2 pc in 2008-09
    • 1999-2000: Number at 237.8 million
  • GCF
    • Share in total GCF 2009-10: 7.7 pc (2004-05 prices)
    • GCF as % of agricultural GDP: 2007-08 – 16.3, 2008-09(P) – 19.67, 2009-10(QE) – 20.3
    • GCF as % of total GDP: 2007-08 – 2.69, 2008-09P – 3.09, 2009-10QE – 2.97
  • Contributes to agricultural growth and industrial demand
  • Contributed 10.59 pc of total exports in 2009-10.
  • Due to the large number of workforce in this sector, the growth of agriculture is a necessary condition for inclusive growth.
  • Food grains production
    • Highest in 2008-09: 234. 47 mn t
    • 2009-10: 218.11 mn t

Agriculture and Industry

  • Agriculture as
    • Supplier of wage goods to the industrial sector
    • Provider of raw materials
    • Consumer of agricultural capital goods produced by industry
  • Stagnation in agriculture
    • Get data on CAGR

Land Reforms

  • Great scarcity and uneven distribution of land
  • Focus of agricultural policies in the initial years was on institutional changes through land reforms
  • Two objectives of land reforms in India
    • To remove the impediments to agriculture that arise due to the character of agrarian structure in rural areas
    • To reduce or eliminate the exploitation of tenants/small farmers
  • Four main areas of land reforms in India
    • Abolition of intermediaries (zamindars)
    • Tenancy reforms
    • Land ceilings
    • Consolidation of disparate land holdings
  • Economic arguments for land reforms
    • Equity
    • Small farms tend to be more productive than large farms
    • Owner cultivated plots of land tend to be more productive that those under sharecropped tenancy
  • Abolition of zamindari was successful while the other three areas of land reforms met with limited success
  • Operation Bargha. Also, LR in Kerala
  • Regional trends in LR
  • Effect of land reforms
    • On tenants
      • Absentee landlordism declined
      • Tenancy declined. In some cases, tenants were evacuated from the land.
      • In some cases there was a drift of tenants into landless
      • Where tenants had not been evicted, tenancy was pushed underground
    • On equity
    • On productivity
    • On agrarian power relations
  • The National Commission on Farmers has placed the unfinished agenda in land reform first in its list of five factors central overcome an agrarian crisis
  • Way forwards
    • Land reforms that make tenancy legal and give well defined rights to tenants, including women, are now necessary

Technology and Green Revolution

  • In the early 60s India faced several crises
    • It had to fight two wars: Pakistan and China
    • Severe drought in 1965 and 1966
    • US was using PL-480 food supply as a means to twist India’s arms to meet US interests
  • This called for an overhaul of the agricultural strategy and the need to be self-sufficient in food production
  • Three phases of green revolution
    • 1966-1972
    • 1973-1980
    • 1981-1990
  • 1966-1972
    • C Subramaniam and MSS
    • 1965: Agricultural Prices Commission and Food Corporation of India set up
    • Introduction of HYV seed of wheat from Mexico created by CIMMYT
    • Under the new agricultural policy, the spread of HYVs was supported by public investments in fertilisers, power, irrigation and credit
    • Food grain production shot up
      • 1966-67: 74 mt
      • 1971-72: 105 mt
    • India became nearly self-sufficient in food grains
    • What led to the increased production?
      • Favourable pricing policy led to adequate incentives
      • National research system proceeded to indigenise the new seeds to tackle their shortcomings
      • Availability of inputs including canal water, fertilisers, power and credit
      • Subsidies
      • Role of credit began to be important after 1969
    • 1973-1980
      • This phase saw many challenges
      • Consecutive droughts in 1972-73
      • Oil shock
      • Production fell. Imports began again.
      • Thereafter, government increased fertiliser subsidies
      • Groundwater irrigation increased in  importance
      • HYV technology extended from wheat to rice
    • 1981-1990
      • 1986
        • Rice prod: 63.8 mt (1964: 37)
        • Wheat prod: 47 mt (1964: 12 mt)
      • Even when the ‘worst drought of the century’ struck in 1987, food needs could be adequately met due to buffer stocks
      • HYV technology spread eastward to states like West Bengal and Bihar
      • The impact of HYV technology had started to plateau however
      • Input subsidies kept on increasing
      • 1991: Input subsidy was 7.2 pc of agricultural GDP
    • What was the impact of highly regulated policies on agriculture?
      • There were barriers on pricing, movement and private trading of agricultural produce
      • The external sector was burdened with various tariff and non-tariff barriers to agricultural trade flows
      • The overvalued rupee produced an anti-export environment for agriculture
      • High protection to industry produced high industrial prices and adverse terms of trade for agriculture, reducing the relative profitability of the primary sector
    • What was the aim of agricultural pricing in pre-reform era?
      • Ensure inexpensive food for consumers
      • Protect farmers’ incomes from price fluctuations
      • Keep the balance of payments in check
    • Agriculture in post-reform era
      • Impact: 1. Growth in PCI led to an increase in food demand and also diversification. Terms of trade between agricultural and industrial prices improved in favour of agriculture
      • Increased profitability has led to increase in private investments which are now double the public investment in agriculture.
      • Growth rates
        • 1980s: 3 pc
        • 1990s:
        • 2000s:
        • Tenth Plan: 2.47 pc (as against 7.77 pc of overall economic growth)
      • This has however not translated into reduction of poverty
      • There has been an increase in both urban and rural inequality
    • Deceleration in agricultural growth
      • Declined during 90s
      • Deceleration in the growth of area, production and yield
      • Food production of Rabi crops has off late equalled the Kharif crops. This has to an extent reduced the over dependence on monsoon and imparted some stability to agricultural production
      • Area-wise, the deceleration was more in case of the Indo-Gangetic region
    • The instability in agricultural growth is more in states with high percentage of rain-fed areas
    • Acreage: declining trend in most crops during the period 1995-96 to 2004-05
    • Productivity: sharp decline (1995-2005). Healthy performance of cotton and maize though

Major factors affecting growth potential

  • Lack of long term policy perspective
    • No long term strategy for agricultural development
    • National Agricultural Policy was announced only in the year 2000
    • Sectoral priority to industry from the second FYP
    • Weaknesses of policies followed for agricultural development
      • Policies provided little incentives for the farmers as the prices were depressed and the sector was disprotected vis a vis other sectors of the economy
      • Inward-looking policies
      • Excessive price based focus than non-price factors like water, infrastructure, R&D, extension services etc
    • Investment in Agriculture and Subsidies
      • There have been cutbacks in agricultural investment and extension, but not in subsidies
      • Agricultural subsidy as pc of GDP:
      • Public investment in agriculture declined from 4 pc of agriculture GDP in 1976-1980 to
      • Subsidies on fertiliser, power and irrigation have contributed to soil degradation
      • It is important to reduce subsidies and increase public investment in crucial areas such as soil amelioration, watershed development, groundwater recharge, surface irrigation and other infrastructure
      • Public Sector GCF in agriculture stood at less than Rs 50 bn at 1993-94 prices
      • It is imperative to reduce these subsidies for stepping up public investment in agriculture
      • After 2003, the investments have started to increase. In  2006-07 public sector GCF was 3.7 pc of agricultural GDP and  total GCF was 12.5 pc of agricultural GDP
      • Three areas should get priority in public investments
        • Rural roads
        • Electricity
        • Irrigation projects
        • <all three of them are under Bharat Nirman project>
      • Complimentarity between public and private sector capital formation in agricultural sector. Public sector can create infrastructure while the private investment is essential for short term asset building mainly in the areas of mechanisation, ground levelling, private irrigation etc
    • Lagging research and development efforts
      • After the green revolution, there has been no major breakthrough in agricultural research. GM is a promising area but its safety has not yet been conclusively established.
      • Poor productivity in India compared to other countries and even compared to world average
      • India, however, has the largest public agricultural research establishment in the world. ICAR and agricultural universities
      • India spends only 0.3 pc of agricultural GDP for research as compared to 0.7 pc in other developing countries and 2-3 pc in case of developed countries.
      • There is hardly any scope for expansion of area. Hence, productivity must increase to keep up with the increasing demand. R&D has a lot of role to play here
      • New varieties of seeds need to be developed suited to different regions of the country
      • The research system should be responsive to the changing needs and circumstances
    • Technology generation and dissemination
      • Fixed land. Hence technology
      • Focus on yield as well as sustainable use of land
      • Focus should be on specific requirements of each agro-climatic region
      • Ned to develop much stronger linkages between extension and farmers
    • Rising soil degradation and over-exploitation of groundwater
      • Around 40 pc of Indian’s total geographical area are officially estimated as degraded
      • Soil health is deteriorating in Punjab and Haryana
    • Degradation of natural resources
    • Subsidies vis-a-vis investments and farm support systems
    • Agriculture’s terms of trade and farm price volatility
      • Ensure rapid development of backward farm linkages
    • Summary: Need to correct the policy bias against agriculture, make higher investments, develop new varieties of seeds, conserve natural resources like land and water and provide incentives to the farmers to adopt modernisation

 

Some Issues in Indian Agriculture

  • Low public investment
  • Halt in the modernization of agriculture
  • Agricultural indebtedness
  • Farmer suicides
  • Agricultural imports and future markets

Subsidies

  • Talk about bringing urea under the Nutrient Based Subsidy (NBS) system and decontrolling its prices
  • Downsides
    • Fertilizer subsidy touched almost 1 lakh crore in 2008-09
    • Promotes overuse of fertiliser and thereby catalysing soil degradation
    • As a result, agricultural production in the bread baskets of the country has stagnated, posing a threat to the food security of the country
    • Drylands do not receive the benefit of crores of subsidy given in fertilizers

Government Intitiatives

  • Green Revolution
  • National Policy on Agriculture, 2002
  • National Policy for Farmers, 2007
    • Major policy provisions include provisions for asset reforms, water use efficiency, use of technology, inputs and services like soil health, good quality seeds, credit, support for women etc
    • Focus on millets as well

Agriculture during the 11th plan

  • Flagship schemes
    • Rashtriya Krishi Vikas Yojana
    • National Food Security Mission
    • National Horticulture Mission (2005-06)
    • Integrated Scheme of Pulses, Oilseeds and Maize
    • Technology Mission for Integrated Development of Horticulture in North-east and Himalayan States (2001-02)
    • National Mission for Sustainable Agriculture
    • National Mission on Micro Irrigation was launched in 2010 in addition to the earlier Micro Irrigation Scheme launched in 2006
    • National Bamboo Mission
  • Avg growth of 2.03 pc against the Plan target of 4 pc per annum.
  • For sustainable and inclusive growth
    • Must focus on the small and marginal farmers as well as female farmers
    • Group approach should be adopted so that they can reap economies of scale
    • Bring technology to farmers
    • Improving efficiency of investments
    • Diversifying while also protecting food security concerns
    • Fostering inclusiveness through a group approach
  • Irrigation
    • Envisages creation of an additional potential of 16 mn ha
    • Bharat Nirman aims to bring an additional 1 crore ha of land under irrigation by 2012
    • Accelerated Irrigation Benefits Programme still on

Irrigation

  • 45 pc of nearly 175 mn ha of cropped area is irrigated
  • Trends
    • Nearly trebled from 24 mn ha in 1953-64 to 75 mn ha in 1998-99
    • It accounts for the largest part of total investments in the agricultural sector
    • Importance of ground water as an irrigation source has also increased considerably
  • Uneven access
    • Inter-regional variance
    • Inequality in access within the farming population
  • Areas of concern
    • Depletion of ground water
    • Environmental concerns
    • Costs
  • Steps to take
    • Improving water use efficiency
    • Water governance
    • Economic incentives for efficient use
  • Govt Schemes
    • Accelerated Irrigation Benefits Programme was started during 1996-97. It extends assistance for the completion of incomplete irrigation schemes
  • In 11th FYP – refer previous section

Way Forward

  • Second green revolution (?)
  • Relook at all the issues offering forward and backward linkages in the agricultural production cycle
  • Focus on oilseeds, pulses and coarse cereals
  • Coarse cereals: high nutrition, can be grown in dry areas, enhance fertility of soil in rotation
  • PDS should be reformed: coarse cereals should also be provided through PDS
  • Timely availability of credit at affordable costs
  • Wider extension of insurance facilities to the farm sector
  • Water and irrigation infrastructure
  • Drip irrigation
  • Organic manures should be popularized and their commercial production encouraged
  • Educate farmers about technology and agricultural techniques

Food Security

  • Food security should also incorporate nutritional security. This requires emphasising the increase in production of pulses, fruits, vegetables, poultry and meat.
  • Interpreted broadly
  • Includes nutritional security which particularly incorporates maternal health and infant health due to the involvement of the nutritional aspect
  • Also covers employment security (?)
  • Affordability, accessibility and availability
  • Food security seeks to address all the three dimensions of hunger: chronic, hidden and transient
  • It also is the first step towards inclusive development

Public Distribution System

  • High procurement prices

Irrigation

  • The total irrigation potential in the country has increased from 81.1 mn hectares in 1991-92 to 108.2 mn hectares in March 2010.
  • 1996-97: Accelerated Irrigation Benefit Programme initiated
  • Reservoir Storage Capacity: 151.77 billion cubic metres

Agricultural Pricing

  • To ensure
    • Remunerative prices to growers
    • Encouraging higher investment and production
    • Safeguard the interest of consumers by making sure that adequate supplies are available
  • It also seeks to evolve a balanced and integrated price structure in the perspective of the overall needs of the economy

 

Investment in Agriculture

  • FAO estimates that global agricultural production needs to grow 70 pc by 2050 in order to meet projected food demand
  • Hence investment should grow by a whopping 50 pc
  • In India, public investment in agriculture has witnessed a steady decline from the 6th FYP onwards
  • Share of investment in agriculture has been between 8-10 pc
  • Most of this has gone into current expenditure in the form of increased output and input subsidies
  • Though private sector investment has been increasing, it has not proved to be enough
  • Decreased public spending in creation of supporting infrastructure in rural areas has discouraged private investment in this sector
  • Some of the measures could be
    • Investment in general service like R&D, education, marketing and rural infrastructure
    • Increased investment in rainfed areas
    • Private sector participation
    • Increased investment for sustainable development

 

WTO and Agriculture

 

  • Uruguay Round multilateral trade negotiations were concluded after 7 years of negotiation in December 1993
  • The WTO Agreement on Agriculture was one of the main agreements which was negotiated
  • Agreement on Agriculture contains provisions in three broad areas of agriculture
    • Market Access
    • Domestic Support
    • Export Subsidies
  • Market Access
    • This is the most important aspect of the negotiation because all countries restrict market access while only few have export subsidies and domestic support
    • This includes tariffication, tariff reduction and access opportunities
    • Tariffication means that all NTTBs should be withdrawn (such as quotas, minimum export prices etc)
    • Adopts a single approach using a tiered formula
    • Single approach: everyone except LDCs have to contribute by improving market access for all products
    • Sensitive products: All countries can list some sensitive products and are allowed flexibility in the way these products are treated, although even sensitive products have to see ‘substantial improvements’ in market access.
    • Special and differential treatment
      • Purpose: for rural development, food security and livelihood security
      • Specifically, special treatment is to be given to developing countries in ‘all elements of the negotiation’, including ‘lesser’ commitments in the formula and long implementation period
      • Special products: developing countries will be given additional flexibility for products that are specially important for their food security, livelihood security and rural development.
      • Special Safeguard Mechanisms: is intended to provide contingent protection to poor farmers in developing countries from negative shocks to import prices or from surges in imports. [Safeguards are contingency restrictions on imports taken temporarily to deal with special circumstances such as a sudden surge in imports. AoA has special provisions on safeguards. In agriculture safeguards, (unlike normal safeguards) can be triggered automatically when import volumes rise above a certain level or if prices fall below a certain level; and it is not necessary to demonstrate that serious injury is being caused to the domestic industry]
    • AoA requires (from 1995)
      • 36% average reduction by developed countries, with a minimum per tariff line reduction of 15% over six years
      • 24% average reduction by developing countries with a minimum per tariff line reduction of 10% over ten years
    • Domestic Support (subsidies)
      • AoA structures domestic support into three categories
        • Green Box
        • Amber Box
        • Blue Box
      • Green Box
        • Non (or minimal) trade distorting subsidies
        • They have to be government funded and must not involve price support
        • They tend to be programmes that are not targeted at particular products and include direct income supports for farmers that are not related to current production levels or prices. They also include environmental protection and regional developmental programmes. These subsidies are therefore allowed without limits
      • Amber Box
        • All domestic support measures considered production and trade fall into the amber box
        • These include measures to support prices, or subsidies directly related to production quantities
        • These supports are subject to limits which are allowed: 5% of total production for developed countries, 10% for developing countries
        • Reduction commitments are expressed in terms of a “Total Aggregate Measurement of Support” (Total AMS)
      • Blue Box
        • This is the “amber box with conditions” – conditions designed to reduce distortion
        • Any support that would normally be in the amber box, is placed in the blue box if the support also required farmers to limit production
        • At present there are no limits on spending on blue box subsidies.
      • Export subsidies
        • Developed countries are required to reduce their export subsidy by 36% (by value) or 21% (by volume) over the six years
        • For developing countries the % cuts are 24% (by value) or 14% (by volume) over 10 years
      • India’s commitment
        • As India was maintaining QRs due to balance of payments reasons (which is a GATT consistent measure), it did not have to undertake any commitments in regard to market access
      • In India, exporters of agricultural commodities do not get any direct subsidy. Indirect subsidies are given

 

 

Food Processing

  • Food processing is a large sector that covers activities such as agriculture, horticulture, plantation, animal husbandry and fisheries
  • Ministry of Food Processing indicated the following segments within the Food Processing industry:
    • Dairy, fruits and vegetable processing
    • Grain processing
    • Meat and poultry processing
    • Fisheries
    • Consumer foods including packaged foods, beverages and packaged drinking water
  • Industry is large and has grown after 1991. However, of the country’s total agriculture and food produce, only 2 per cent is processed.
  • FP has 9% share in manufacturing
  • Structure
    • 42 pc: Unorganised
    • 33 pc: SSI
    • 25 pc: Organised

 

Constraints & Drivers of Growth
Changing lifestyles, food habits, organized food retail and urbanization are the key factors for processed foods in India, these are post-liberalization trends and they give boost to the sector.
There has been a notable change in consumption pattern in India. Unlike earlier, now the share and growth rates for fruits, vegetables, meats and dairy have gone higher compared to cereals and pulses. Such a shift implies a need to diversify the food production base to match the changing consumption preferences.
Also in developed countries it has been observed that there has been a shift from carbohydrate staple to animal sources and sugar. Going by this pattern, in future, there will be demand for prepared meals, snack foods and convenience foods and further on the demand would shift towards functional, organic and diet foods.
Some of the key constraints identified by the food processing industry include:

  • Poor infrastructure in terms of cold storage, warehousing, etc
  • Inadequate quality control and testing infrastructure
  • Inefficient supply chain and involvement of middlemen
  • High transportation and inventory carrying cost
  • Affordability, cultural and regional preference of fresh food
  • High taxation
  • High packaging cost

In terms of policy support, the ministry of food processing has taken the following initiatives:

  • Formulation of the National Food Processing Policy
  • Complete de-licensing, excluding for alcoholic beverages
  • Declared as priority sector for lending in 1999
  • 100% FDI on automatic route
  • Excise duty waived on fruits and vegetables processing from 2000 – 01
  • Income tax holiday for fruits and vegetables processing from 2004 – 05
  • Customs duty reduced on freezer van from 20% to 10% from 2005 – 06
  • Implementation of Fruit Products Order
  • Implementation of Meat Food Products Order
  • Enactment of FSS Bill 2005
  • Food Safety and Standards Bill, 2005
  • Mega Food Parks

Apart from these initiatives, the Centre has requested state Governments to undertake the following reforms:

  • Amendment to the APMC Act
  • Lowering of VAT rates
  • Declaring the industry as seasonal
  • Integrate the promotional structure

 

Plan Schemes

During the 10th Plan, the Ministry implemented Plan schemes for Technology Upgradation/Modernization/Establishment of Food Processing Industries, Infrastructure Development, Human Resource Development, Quality Assurance, R&D and other promotional activities.

In the 11th Plan, it has been proposed to continue assistance to the above schemes with higher levels of assistance. In the 11th Plan, the Ministry proposes to launch a revamped Infrastructure Scheme under which it will promote setting up of Mega Food Parks, cold chain infrastructure, value added centres and packaging centres. The Mega Food Park Scheme will provide backward and forward linkages as well as reliable and sustainable supply chain. The emphasis will be on building strong linkages with agriculture and horticulture, enhancing project implementation capabilities, increased involvement of private sector investments and support for creation of rural infrastructure to ensure a steady supply of good quality agri/horticulture produce. It will provide a mechanism to bring farmers, processors and retailers together and link agricultural production to the market so as to ensure maximization of value addition, minimize wastages and improve farmers’ income. The Mega Food Park would be a well-defined agri/horticultural-processing zone containing state of the art processing facilities with support infrastructure and well established supply chain. The primary objective of the proposed scheme is to facilitate establishment of integrated value chain, with processing at the core and supported by requisite forward and backward linkages. It is envisaged that the implementation of the projects would be assisted by professional Project Management Agencies (PMA) from concept to commissioning. In 11th Plan it is planned to support establishment of thirty (30) Mega Food Parks in various parts of the country.

Vision 2015 on Food Processing Industries

A vision, strategy and action plan has also been finalized for giving boost to growth of food processing sector. The objective is to increase level of processing of perishable food from 6% to 20%, value addition from 20% to 35% and share in global food trade from 1.6% to 3%. The level of processing for fruits and vegetables is envisaged to increase from the present 2.2% to 10% and 15% in 2010 and 2015 respectively. The Cabinet has approved the integrated strategy for promotion of agri-business and vision, strategy and action plan for the Food Processing Sector, based on the recommendations made by the Group of Ministers (GOM).

Integrated Food Law

An Integrated Food Law, i.e. Food Safety and Standards Act, 2006 was notified on 24.8.2006. The Act enables in removing multiplicity of food laws and regulatory agencies and provide single window to food processing sector. Ministry of Health & Family Welfare has been designated as the nodal Ministry for administration and implementation of the Act.

National Institute of Food Technology Entrepreneurship & Management (NIFTEM)

The Ministry has set up a National Institute of Food technology Entrepreneurship & Management (NIFTEM) at Kundli (Haryana). The Institute will function as a knowledge centre in food processing. Certificate of Incorporation of NIFTEM as a section 25 Company under the Companies act 1956 has been obtained.

 

SWOT Analysis of Food–Processing Industry
Strengths

  • Abundant availability of raw material
  • Priority sector status for agro-processing given by the central Government
  • Vast network of manufacturing facilities all over the country
  • Vast domestic market

Weaknesses

  • Low availability of adequate infrastructural facilities
  • Lack of adequate quality control and testing methods as per international standards
  • Inefficient supply chain due to a large number of intermediaries
  • High requirement of working capital.
  • Inadequately developed linkages between R&D labs and industry.
  • Seasonality of raw material

Opportunities

  • Large crop and material base offering a vast potential for agro processing activities
  • Setting of SEZ/AEZ and food parks for providing added incentive to develop greenfield projects
  • Rising income levels and changing consumption patterns
  • Favourable demographic profile and changing lifestyles
  • Integration of development in contemporary technologies such as electronics, material science, bio-technology etc. offer vast scope for rapid improvement and progress
  • Opening of global markets

Threats

  • Affordability and cultural preferences of fresh food
  • High inventory carrying cost
  • High taxation
  • High packaging cost

 

Subsidies

 

Fertilizer Policy:    Urea is the only fertilizer under statutory price control.  Government of India has introduced nutrient based subsidy with effect from 1st April, 2010 in respect of phosphatic and potassic  fertilizers. Under the policy, subsidy is based  on the nutrient (N,P,K and S) content of the  decontrolled P and K fertilizers. Price of Urea has been increased by 10% while price of other subsidized fertilizers are being maintained around current levels. Additional subsidy on micronutrients has been introduced on Boron and Zinc, to begin with.  In order to promote the concept of balanced use of fertilizers and to encourage use of micronutrients, several fertilizers fortifed with Boron and Zinc have been incorporated in the Fertilizer (Control) Order, 1985.

 

 

 

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