Classification of Eco-system

 

  1. Natural Ecosystem-

Terrestrial- Forests, Grasslands, Deserts

Aquatic- Fresh Waters, Saline Waters, Marine Waters

Ecotone :- a zone of junction between two or more diverse ecosystems. For e.g. the mangrove forests represent an ecotone between marine and terrestrial ecosystem.

Characteristics of Ecotone

It may be very narrow or quite wide. It has the conditions intermediate to the adjacent ecosystems. Hence it is a zone of tension.

It is linear as it shows progressive increase in species composition of one in coming community and a simultaneous decrease in species of the other out going adjoining community.

A well developed ecotones contain some organisms which are entirely different from that of the adjoining communities.

Sometimes the number of species and the population density of some of the species is much greater in this zone than either community. This is called edge effect For example the density of birds is greater in the mixed habitat of the ecotone between the forest and the desert.

Arunachal Pradesh Geographical Location

 

The state is located in the extreme Northeastern corner of the country. It is situated between latitude 26° 30′ N and 29° 30 ‘ N and longitude 91° 30′ E and 97° 30’ E. It shares its border with the neighboring countries of Bhutan in the West, China (Tibet) in the North and Northeast, Myanmar in the East and Southeast and the Indian states of Assam and Nagaland in the South.  Arunachal Pradesh is generally a hilly region.

The elevation of the hills ranges from 60 meters to over 7300 meters (GORICHEN peak in West Kameng). The territory falls in the outer Himalayas and Patkoi Ranges. It is endowed with wide topographical variations, vegetations and wild life along the greater part of the length of the territory the characteristics Siwalik type formation of Himalayan Mountains is native.

The definition of Siwalik ranges loses its typical character at the point of the valley head and is replaced by series of low hills with easier slopes. These hills gradually merge into the Patkoi hill ranges which separate India & Burma. The general tendency of the hills is found sloping towards the plains of Assam. These hill ridges of Arunachal Pradesh are situated in a very haphazard manner.

As soon as one ridge ends, the other starts either in opposite direction or parallel. At these intervals the wide and narrow valleys come into existence. Because of these hill ridges and the valleys, the surface of Arunachal Pradesh is found variegated almost everywhere which also results into numerous geographical isolation of places caused by various rivers and streams traversing the region and depositing the flowing detritus enroute in valley and again at the foothills

Topography

Topography wise Arunachal Pradesh has been divided into 4 distinct physiographical divisions:

  1. The Himalayan Ranges
  2. The Mishmi Hills
  3. The Naga-Patkoi Ranges and
  4. The Brahmaputra Plains

Arunachal Pradesh is the eastern stretch of the Himalayas and all the 3 sections of the Himalayas are represented here . Every division has a different geology and tectonic history

From the Brahmaputra Plains at an average elevation of 100m, the Himalayas attain an elevation of 7089m. The Himalayas can be further sub-divided into physio-tectonic Zones:

(i) The sub-Himalayan zone rising abruptly from the Brahmaputra Plains along a tectonic plane-the Foot Hill Fault. It is about 10 -20 km wide but narrows down to 1 -2 km in the Dibang valley.

(ii) The lesser or Lower Himalayas: Elevation 2500-4000 m and 80-90 km wide. Take a syntaxial bend towards SE to abut against Mishmi Hills. Its southern limit is defined by the Main Boundary Fault/Thrust.

(iii) The Greater or Higher Himalayas. A zone of very high relief with heights greater than 6000m having precipitous slopes and deep gorges. This zone is generally devoid of vegetation. Its southern limits are defined by the Main Central Thrust.

(iv) Trans-Himalayan Tibetan or the Thethyan zone: It is the northernmost zone which is about 30-40 km wide and of low relief (Elevation 3000 – 6000m). All important Passes are located in this zone .

The Eastern Himalayas that cover 18,518 sq. km area of East and West Siang districts is almost wholly a rugged mountainous terrain extending over the central region of Arunachal Pradesh. The region has been described as ‘an intricate labyrinth of precipitous, rocky and high hills and mountains, with beautiful green valley’s drained by innumerable rivulets and mighty rivers cascading down from upper elevations. The tangle of hills and mountains throwing a series of spurs and towering to majestic heights of eternal snow is the most imposing topographic feature of Siang.

 

subsidies, MSP, PDS, FOOD SECURITY

yojna managing inflation aug 2010 here read FOOD INFLATION IN INDIA: CAUSES AND REMEDIES
https://docs.google.com/file/d/0B_FR6Jkv0z2cNDFuTDdBRnA5YkE/edit?usp=sharing 

 krukshetra tribal development nov 2010here read sucsess stories how farmer get a better prise
https://docs.google.com/file/d/0B_FR6Jkv0z2cU3diSVlkVmNKOTA/edit?usp=sharing 

 yojna monsoon july 2012 here read monsoon and fool inflation
https://docs.google.com/file/d/0B_FR6Jkv0z2cZENhRERWMkJhdHc/edit?usp=sharing

rest there are certain article reports and no doubt ignou booklets there links are
  FOOD SECURITY- TPDS
https://docs.google.com/file/d/0B_FR6Jkv0z2cSTlVcXQ3dDVEV0k/edit?usp=sharing 


Chandrayaan-1

Launch: October 22, 2008             Site: Satish Dhavan Space Centre, Sriharikota

The objectives of the programme were:

  1. To develop and orbit a spacecraft around moon using an Indian-made launch vehicle.
  2. To prepare a three-dimensional atlas of both the near and the far side of the moon.
  3. Chemical and mineralogical mapping of the entire lunar surface.
  4. To study the impact of Moon Impact Probe on the surface of the moon as a fore-runner to future soft landing missions.

NASA’s Moon Mineralogy Mapper (M3) had on Chandrayaan-1 had detected water on the surface of moon. The mission was expected to last two years. However, the communication with the satellite was lost on 29 August 2009 and the mission was declared over. It lasted for 312 days and achieved 95 percent of its objectives.

Chandrayaan-1 was selected by the American Institute of Aeronautics and Astronautics (AIAA) as one of the recipients of its annual AIAA SPACE 2009 awards for contributions to space science and technology.

Read moreChandrayaan-1

Climate Change

 

  • National Environmental Appraisal and Monitoring Authority has been setup

 

 

India UK

UK-India Business Climate Leaders Group has been constituted. Comprising of leading CEOs the group will work on synergystic business for carbon reduction and joint work to evolve national emission reduction strategies.

FDI could be streamlined into low carbon initiatives.

Read moreClimate Change

ESTUARY ECOSYSTEM

 

  • located where river meets the sea.
  • the most productive water bodies in the world
  • The complete salinity range from 0-35 ppt is seen from the head (river end) to the mouth (sea end) of an estuary
  • Coastal lakes which have their connection with the sea through small openings are better known as lagoons or backwaters acting as a natural water filter

 

Estuary Formation:

grouped into four geomorphic categories based on the physical processes responsible for their formation:

1) rising sea level; (2) movement of sand and sandbars; (3) glacial processes; and (4) tectonic processes.

India Estuarine Ecosystem

The Country has 14 major, 44 medium and 162 minor rivers drains into the sea through various estuaries.

Major estuaries occur in the Bay of Bengal.

Most of the India’s major estuaries occur on the east coast. In contrast, the estuaries on the west coast are smaller.

agriculture

the syllabus states that -mazor crops,cropping patterns in various parts of the country,different types of irrigation system,storage,transport and marketing of agricultural product,and issues related to constraints,e-tec hnology in the aid of farmers….
the link for yojna January  2011 for agriculture is for dowloading dere would be a link as  
download pdf

also ncert geography land use and agriculture is
https://docs.google.com/file/d/0B_FR6Jkv0z2ceE8wX05oUUN1b0k/edit?usp=sharing

for e-tec hnology in the aid of farmers.there is great krukshetra its link is


 krukshetra agriculture productivity dec 2011 link 
 krukshetra  climate change and suistainable agriculture march 2011 link
 krukshetra soil rejuvenation  nov 2011 link
and most imp krukshetra june 2013…sorry no pdf copy yet released…
and
yojna budget march 2011
yojna celebration 60 years jan 2010 
yojna north eas dec 2011

Wars and Treaties

War Year Treaty Gov General Battles et al
Anglo Marathas
First 1775-82 Began: Treaty of Surat

End: Treaty of Salbai

Warren Hastings Battle of Wadgaon
Second 1803-05 Began: treaty of Bassein Lord Wellesley Battle of Assaye
Third 1816-19 Treaty of Gwalior Marquess  of Hastings Battle of Pindari

End of Peshwa rule

Anglo French
First 1746-48 Treaty of Aix-la-Chepelle Reason: Austrian succession in Europe 1746: Battle of Adyar/San Thome
Second 1749-54 War of succession between Nasir Jung (English) and Muzaffar Jung (French) after death of Nizam 1749: Battle of Ambur

 

Rise of Robert Clive

Third 1758-63 Treaty of Paris Reason: 7 years war in Europe 1760: Battle of Wandiwash (French defeat)
Anglo Mysore
First 1766-69
Second 1780-1784 Treaty of Mangalore Warren Hastings After death of Hyder Ali in 1782 Tipu led the war
Third 1789-92 Treaty of Seringapatnam Cornwallis Defeat of Tipu
Fourth 1799 Wellesley Battle of Seringapatnam. Death of Tipu.
Anglo Sikh War
First 1845-46 Treaty of Lahore Hardinge
Second 1848-49 Dalhousie Final Subjugation of the Sikhs

Read moreWars and Treaties

Kyoto Protocol

The Kyoto Protocol has put in place three flexibility mechanisms to reduce emission of Green House Gases. Although the Protocol places maximum responsibility of reducing emissions on the developed countries by committing them to specific emission targets, the three mechanisms are based on the premise that reduction of emissions in any part of the globe will have the same desired effect on the atmosphere, and also that some developed countries might find it easier and more cost effective to support emissions reductions in other developed or developing countries rather than at home. These mechanisms thus provide flexibility to the Annexure I countries, helping them to meet their emission reduction obligations. Let us take a look at what these mechanisms are.

What are the three flexibility mechanisms put in place of the Kyoto Protocol for reducing GHG emission?

  • The three mechanisms are joint implementation. Emissions Trading and Clean Development

What is Joint Implementation?

  • Through the Joint Implementation, any Annex I country can invest in emission reduction projects (referred to as joint Implementation Project) in any other Annex I country as an alternative to reducing emissions domestically.
  • Two early examples are change from a wet to a dry process at a Ukraine cement works, reducing energy consumption by 53 percent by 2008-2012; and rehabilitation of a Bulgarian hydropower project, with a 267,000 ton reduction of C02 equivalent during 2008-2012.

What is Clean Development Mechanism?

  • The Clean Development Mechanism (CDM) allows-‘l developed country with an emission reduction or emission-limitation commitment under the Kyoto Protocol to implement an emission reduction project in developing countries as an alternative to more expensive emission reductions in their own countries. In exchange for the amount of reduction In emission thus achieved, the investing gets carbon credits which it can offset against its Kyoto targets. The developing country gains a Step towards sustainable development.
  • To get a CDM project registered and implemented, the investing country’ has to first take approval from the designated national authority in the host country, establish “Additionally”, define baselines and get the project validated by a third party agency, called a Designated Operational Entity (DOE). The Executive Body of CDM registers the project and issues credits, called Certified Emission Reductions (CERs), or carbon credits, where each unit is equivalent to the reduction of one metric tonne of. C02 or its equivalent. There are more than 4200 CDM projects in the pipeline as on 14.3.2010. The expected CERs till the end of2012 is 2,900,000,000

What is “Additionality” in a CDM project ?

  • The feature of “additionality” is a crucial element of a CDM project it means that the industrialized country that is seeking to establish the CDM project in the developing country and earns carbon credits from it has to establish that the planned carbon reductions would not have occurred on its own, in the absence of the CDM project. They have to establish a baseline of the project. Which is the emission level that would have been there in the absence of the project. The difference between this baseline level and the (lower) emission level achieved as a result of the project is the carbon credit due to the investing country

What are some of the concerns regarding CDM ?

  • The risk of “false Credits” is a cause for concern with regard to CDM projects. If a project does not actually offer an additionally and the reduction in emission would have happened anyway Even without the project.

 

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