Showing posts with label Bihar. Show all posts
Showing posts with label Bihar. Show all posts

Monday, July 13, 2015

Is Bihar State of India prepared for the disaster?



The state of Bihar has been facing floods since for a long time.

By
Dr. Nitish Priyadarshi

Bihar is India's most flood-prone State, with 76% of the population in the north Bihar living under the recurring threat of flood devastation. According to some historical data, 16.5% of the total flood affected area in India is located in Bihar while 22.1% of the flood affected population in India lives in Bihar. About 68,800 square kilometres (26,600 sq mi) out of total geographical area of 94,160 square kilometres (36,360 sq mi) comprising 73.06% is flood affected.

Geographically Nepal is a mountainous region. When heavy rains occur in the mountains of central and eastern Nepal the water flows into the major drainages of Narayani, Bagmati, and Koshi rivers. As these rivers cross into India they flow into the plains and lowlands of Bihar and break their banks.

Bihar is surrounded by Nepal in the north, West Bengal in the east, Uttar Pradesh in the west and  Jharkhand towards the south. There are several rivers that run through the state: Ganga, Sone, Punpun, Falgu, Karmanasa, Durgavati, Kosi, Gandak and the Ghaghara, to name a few. Nearly 85% of the state’s land is under cultivation. Bihar also receives heavy rainfall all through June to October.

The state of Bihar has been facing floods since for a long time. It accounts for almost half of India’s average annual flood losses. In the year 1914, Bengal and Bihar faced floods. In the year 1934, Bihar was shaken by an earthquake which was again followed by floods.

The state has been facing floods ever since, but the frequency of floods has become high in recent years. There have been floods almost every year from 1979 which have caused extensive damage. Lakhs of people have lost their lives and their homes. The state has faced infrastructural losses worth crores of rupees.

The state government has built about 3000 kms of embankments, but the flow of the river has grown 2.5 times resulting in the failure of embankments in every flood.

So the big question is: is the state of Bihar prepared? The Disaster Management Department, Government of Bihar has come out with a number of schemes.
  • Procurement of motor boats and other necessary accessories like life jackets, mahajals, tents, etc. for 28 flood-prone districts.
  • To improve the response mechanism and tackle the impact of natural disasters effectively, a State Disaster Response Force (SDRF) is to be established on the similar pattern of National Disaster Response Force (NDRF).
  • A number of warehouses will be constructed to store the relief and rescue materials and to keep them safe and secure.
  • Establishment of Emergency Operation Centres (EOC) in all the districts to carry out rescue and relief work effectively.
  • Since the communication system often becomes dysfunctional, procurement and proper maintenance of communication systems has been taken into account. Satellite phones, GPS instruments, hand packs, walkie – talkies will be procured.
  • An Early Disaster Warning System is to be established.
  • A plan has been prepared to generate awareness among the masses about the ways and means of mitigating the risk of disaster.
The budget for the above scheme crosses 5000 crores.

What more can be done?

A number of structural measures can be taken up in the state:
  • Detention Basins: The state area has a number of depressions locally called chaurs which act as detention basins. These chaurs absorb a considerable amount of water of the first flood of the season. No man made detention basins or improvements in natural chaurs has been done.
  • Embankments: All the rivers have been embanked in the state. River Kosi is embanked on both the sides. But there are few gaps in these embankments which reduce its effectiveness. The maintenance and repair of these embankments must be taken into account.
  • Afforestation in the catchment area for absorption of rain water.
  • Channel improvement works increasing the discharge capacity of the river.

Waste Management in Bihar.

 

Waste management is the process of treating solid wastes and offers variety of solutions for recycling items that don’t belong to trash. It is about how garbage can be used as a valuable resource. Waste management is something that each and every household and business owner in the world needs.

Methods of Waste Disposal which can be adopted in Bihar.

Landfill

The Landfill is the most popularly used method of waste disposal used today. This process of waste disposal focuses attention on burying the waste in the land. Landfills are found in all areas. There is a process used that eliminates the odors and dangers of waste before it is placed into the ground.

Incineration/Combustion

Incineration or combustion is a type disposal method in which municipal solid wastes are burned at high temperatures so as as to convert them into residue and gaseous products. The biggest advantage of this type of method is that it can reduce the volume of solid waste to 20 to 30 percent of the original volume, decreases the space they take up and reduce the stress on landfills.

Recovery and Recycling

Resource recovery is the process of taking useful discarded items for a specific next use. These discarded items are then processed to extract or recover materials and resources or convert them to energy in the form of useable heat, electricity or fuel.

Composting

Composting is a easy and natural bio-degradation process that takes organic wastes i.e. remains of plants and garden and kitchen waste and turns into nutrient rich food for your plants. Composting, normally used for organic farming, occurs by allowing organic materials to sit in one place for months until microbes decompose it. Composting is one of the best method of waste disposal as it can turn unsafe organic products into safe compost. On the other side, it is slow process and takes lot of space.
Hospital Wastes Management.
Hospital wastes have always been considered as potentially hazardous in view of the inherent potential for dissemination of infection. The major identified hazard was that of infection, because over millennia communicable diseases had been the most common cause of morbidity and mortality in the community and majority of persons receiving treatment in the hospitals were suffering from communicable diseases. Disinfecting right at source and disposal by incineration, which completely destroys micro-organism of all types, has been the time tested and most widely advocated method for safe management of hospital waste.


Solid Waste Mismanagement in Patna

1. Prohibit littering on the streets by ensuring storage of waste at source in two bins; one for biodegradable waste and another for recyclable material.
2. Primary collection of biodegradable and non-biodegradable waste from the doorstep, (including slums and squatter areas) at pre-informed timings on a day-to-day basis using containerized tricycle/handcarts/pick up vans.
3. Street sweeping covering all the residential and commercial areas on all the days of the year irrespective of Sundays and public holidays. Abolition of open waste storage depots, and provision of covered containers or closed body waste storage depots.
5. Transportation of waste in covered vehicles on a day to day basis.
6. Treatment of biodegradable waste using composting or waste to energy technologies meeting the standards laid down.
7. Minimize the waste going to the land fill and dispose of only rejects from the treatment plants and inert material at the landfills as per the standards laid down in the rules.

Monday, December 20, 2010

Geochemistry of Iodine with special reference to Bihar state of India.

Iodine deficiency is an important global health problem.
8 person out of every hundred, suffer from goiter in India.
by
Dr. Nitish Priyadarshi

Halogens are present and are volatile trace elements in most geological samples. Among them, iodine has the lowest abundance; less than 0.1 ppm in igneous rocks and less than several ppm in sedimentary rocks.

Iodine is least abundant of the halogens and is lithophile element. It is typically a dispersed element and is never concentrated enough in rocks or sediments to form independent minerals. The content of iodine is higher in air masses of marine origin than in those over the continents (Rankama and Sahama, 1950). The content of iodine seems to have some relationship to the salinity of the sea water as it is found to increase to the rise in salinity. Iodine is carried away from the atmosphere partly by rainwater and partly by direct adsorption into the soil and into plants. High solubility of iodine makes it enriched in soil and its highest concentration is noted in cultivated soil. According to most comprehensive observation by Goldschmidt(1954), the concentration of iodine in different media is as follows:

Igneous rock- 0.3 gm/tonne.
Cultivated soil- 2.0 gm/tonne.
Air- 0.0005 gm/tonne.
Rain water- 0.001-0.003 gm/tonne.
Sea water- 0.05 gm/tonne.

Konovalov (1959) found that rivers draining Tertiary marine sediment have higher iodine content than rivers draining other areas and this was considered to be due to iodine being easily leached from the marine sediments.

There is very marked increase in the iodine content of soils as compared to the rocks from which they derive. Many authors have suggested that much of the iodine in soils is derived from atmospheric sources, while another major source of soil iodine is that supplied by plant remains. Silty and clay soils appear to be enriched in iodine. It was found that clay fractions of soil fix iodide, a feature which is most marked for illite.

It has been generally accepted that the oceans are a major source of atmospheric origin; other sources are volcanic gases and rotting bio-materials. It has also been observed that some iodine in urban atmosphere may be derived from combustion of fossil fuels.

Iodine is a micro constituent in all plants and animals. Its influence on plant life is unknown and it may only be ballast element (Rankama and Sahama, 1950). Average content of iodine in marine life (from both plant and animal) is more than the fresh water and inland life (Cauer, 1938). In higher animals like mammals it plays a very important role, when it is present in the thyroid gland in the form of amino acid-thyroxin that controls the rate of metabolism.

Aside from tungsten, iodine is the heaviest element to be essential in living organisms, and iodine is the heaviest element thought to be needed by higher animals. About 19,000 tons are produced annually from natural sources.

A case study of Bihar State in India:

Iodine deficiency is an important global health problem with an estimated 200 million people affected by iodine related problems (Moynahan,1979). Indian Coalition for Control of Iodine Deficiency Disorders (ICCIDD) reveals that 79 million or 8 person out of every hundred, suffer from goiter in India (Hindustan Times, New Delhi, 25-11-2001).

The human body contains very little iodine (0.00004% or 0.4 ppm), yet it is essentially required to be maintained through food and water. Any disruption in iodine content jeopardizes the human metabolism. Thyroxin, a hormone secreted by the thyroid gland located on both side of the trachea contains about 65% iodine. In the absence of optimal quantity of iodine, the gland increases in size to compensate the deficiency of iodine and adversely affects the human metabolism. Water with iodine concentration less than 5-10 µg/l produces goiter.

The Gandak basin in Bihar is also known to be goiter prone since long. A detail research was carried out by Prof. N.C. Ghose (2003) of Department of Geology, Patna University on distribution of iodine in soil-water system in the Gandak Basin in Bihar.

According to Prof. Ghose, the vast tract in Gandak basin in north Bihar is known iodine deficient area and the population is prone to dreaded and endemic disease like goiter. Surface water of this area, iodine content ranges from 1.56 µg/l to 5.52 µg/l, while in groundwater which is the only source for drinking, it varies from 2.1 µg/l to 4.56 µg/l. In soil, the iodine content ranges between 3.65 µg/gm to 12.59 µg/gm. Season wise, there is considerable variation in iodine content both in surface and groundwater. During monsoon it reduces considerably in surface water due to dilution and in groundwater it reduces owing to heavy recharge of the aquifer system through infiltration. In soil, there is no definite pattern in seasonal variation in iodine content. In major part of the study area, the iodine content is deficient and ranges between 3 and 4 µg/l. The cause of low iodine is attributed to repeated floods and erosion of top soil which is the main source of iodine to the groundwater system.

The spatial variation of iodine in both surface and groundwater reveals a striking feature. It is observed that the abundance of iodine both in surface and groundwater decreases downstream from West Champaran to Vaishali. However, in surface water, the profile of iodine content of river Gandak increases again near Hajipur, where it rises to 5.52 µg/l. the high incidence of iodine at the confluence of Ganga and Gandak near Patna is due to mixing of the two river waters.

Low iodine content in water (1-4 µg/l) in the vast tract of land in East and West Champaran, Muzaffarpur and Vaishali districts of North Bihar plain makes the people vulnerable to goiter.

Reference:

Rankama, K. and Sahama, Th. G. (1950) Geochemistry, Univ. Chicago Press, Chicago,912p.

Goldschmidt, V.M. (1954) Geochemistry, Clarendon Press, Oxford,730p.

Cauer, H. (1938) Chemisch-bioklimatogische Studien in der Bretagne. II. Mitteilung: Beeinflussung de mitteleuropaischen Jodmilieus durch die Breton ische Jodindustrie auf dem Wege der Luft. Biochen, Z. 299, p.69.

Moynahan, E.J. (1979) Trace elements in man. Phil. Trans. Roy. Soc. London, B-288, pp.65-79.

Konovalov, G.S. (1959) Removal of microelements by the main rivers of the U.S.S.R. Dokl. Acad. Sci. S.S.S.R. 129, p912.

Ghose, N.C., Das, K. and Saha, D. (2003) Distribution of Iodine in Soil-Water system in the Gandak Basin, Bihar, Journal of Geol. Soc. of India, pp 91-98.

Tuesday, June 22, 2010

Problems of Urban growth.

Ranchi the capital city of Jharkhand State in India is expanding both vertical and horizontal resulting in lots of problem.
by
Dr. Nitish Priyadarshi

As more and more people leave villages and farms to live in cities, urban growth results. Urbanization occurs naturally from individual and corporate efforts to reduce time and expense in commuting and transportation while improving opportunities for jobs, education, housing, and transportation. Living in cities permits individuals and families to take advantage of the opportunities of proximity, diversity, and marketplace competition.
People move into cities to seek economic opportunities. In rural areas, often on small family farms, it is difficult to improve one's standard of living beyond basic sustenance. Farm living is dependent on unpredictable environmental conditions, and in times of drought, flood or pestilence, survival becomes extremely problematic.
Cities, in contrast, are known to be places where money, services and wealth are centralized. Cities are where fortunes are made and where social mobility is possible. Businesses, which generate jobs and capital, are usually located in urban areas. Whether the source is trade or tourism, it is also through the cities that foreign money flows into a country. It is easy to see why someone living on a farm might wish to take their chance moving to the city and trying to make enough money to send back home to their struggling family.
There are better basic services as well as other specialist services that aren't found in rural areas. There are more job opportunities and a greater variety of jobs. Health is another major factor. People, especially the elderly are often forced to move to cities where there are doctors and hospitals that can cater for their health needs. Other factors include a greater variety of entertainment (restaurants, movie theaters, theme parks, etc) and a better quality of education, namely universities. Due to their high populations, urban areas can also have much more diverse social communities allowing others to find people like them when they might not be able to in rural areas.

Clearly, urban settlements differ greatly in size, as mentioned by their populations. Is there a Theoretical maximum and an optimum size? Criffith Taylor and others believe that the ultimate size may be fixed by the increasing difficulty of obtaining enough water to supply unduly large numbers concentrated in a small area, while Lewis Mumford and similar authors think that the continued growth of very large cities not only produces more administrative problems than benefits. This also paralyses rather than furthers social relationships and phenomenally raises central land values, so much that land ceases to be adaptable to new needs.

Views on the optimum size of a city have altered with the march of history. Plato believed that most desirable size was 5,000, a figure which would allow everybody to hear the voice of an orator and so participate in active political life and develop varied social relations. Late nineteenth – century garden city enthusiasts in Britain thought that towns of 30,000 to 50,000 would be large enough supply all necessary human needs, whether medical, educational, social, economic or cultural.

Towns could not come into being until the surrounding countryside was capable of providing a food surplus in the past. Due to modern transport and large surpluses in many parts of the world, towns generally have little difficulty in obtaining food, even from far distant lands. Developing countries may lack the capital to give all their town folk an adequate diet, and even in developed countries there are sporadic temporary shortages, owing to failures in economic planning, poor harvests, dock strikes and traffic hold-ups occasioned by excessive rain, snow, floods, droughts etc.

The problem of water supply is more permanent and applies specifically to cities. It is becoming increasingly serious even in advanced countries which certainly have no problem in paying for the water they consume. The root of the problem lies in the fact that 98% of the earth’s surface water is contained in the salt oceans and in ice-caps. The remainder is unevenly distributed and often polluted. Over half is needed for agriculture, about a third for industry, 10 percent for domestic use.

Many cities, especially in developing countries, lack a clean supply of fresh water. In India, e.g., less than a third of the urban population has access to pure water, and the main reason why water borne diseases are rampant. Even when people are provided with purified water for drinking, they usually wash themselves and their clothing in contaminated supplies.

The demands made on water by urban industries, power stations and homes are growing at a more rapid rate than the growth of population. Many wells do not yield enough water, river pollution, like Ganga, Damodar etc. in India, is a continuing evil, and the remaining water resources- mostly in thinly populated highland areas of abundant rain- are far from many consuming centres.

After being separated from Bihar, Jharkhand state of India is now fast growing in terms of business. Ranchi the capital city is expanding both vertical and horizontal resulting in lots of problem like irregular electric supply, water supply, ground water depletion, air pollution, noise pollution, municipal waste disposal, failure of drainage systems, traffic jams etc. Surface waters are being contaminated. Seasonal diseases have also multiplied. More and more people are concentrating in the city flats which has raised the land values many fold. Ranchi earlier known as the summer capital has now become the heat furnace during summer. It is all due to the unplanned expansion of the city.

The urban heat island has become a growing concern and is increasing over the years. The urban heat island is formed when industrial and urban areas are developed and heat becomes more abundant. In rural areas, a large part of the incoming solar energy is used to evaporate water from vegetation and soil. In cities, where less vegetation and exposed soil exists, the majority of the sun’s energy is absorbed by urban structures and asphalt. Hence, during warm daylight hours, less evaporative cooling in cities allows surface temperatures to rise higher than in rural areas. Additional city heat is given off by vehicles and factories, as well as by industrial and domestic heating and cooling units. This effect causes the city to become 2 to 10 degree F (1 to 6 degree C) warmer than surrounding landscapes. Impacts also include reducing soil moisture and intensification of carbon dioxide emissions.
Owing to population growth, poor levels of hygiene, and increasing urban poverty, the urban environment in many developing countries is rapidly deteriorating. Densely packed housing in shanty towns or slums and inadequate drinking-water supplies, garbage collection services, and surface-water drainage systems combine to create favourable habitats for the proliferation of vectors and reservoirs of communicable diseases. As a consequence, vector-borne diseases such as malaria, lymphatic filariasis and dengue are becoming major public health problems associated with rapid urbanization in many tropical countries

Another change that has occurred after the oil crisis of 1973 is the vertical growth of large cities. People who were living in suburbs found it costly to travel to the city. The open spaces within the city got filled up by the construction of high rise buildings. Large bungalows and old residences were demolished and high rise buildings have come up both as commercial complexes and as residential flats. Many rich families are migrating from the suburbs to flats or apartments near the city centre. The vertical expansion of cities poses further problems in water supply, sewage disposal and traffic congestion on the roads. Traffic causes urban noise, air pollution, stress and strain in an individual.

One solution for both lateral expansion and vertical growth of a city is to develop satellite towns at a distance of 40 to 50 km from the city. The satellite town will not be a mere residential town to accommodate commuters. Such a satellite town will be both a place of work and a place of living.

Tuesday, December 29, 2009

Arsenic alarm in Bihar and Jharkhand Villages of India.

Bihar and Jharkhand is facing one of the gravest natural disasters in the form of arsenic contamination of ground water.
by
Dr. Nitish Priyadarshi

Thousands of people living in over hundreds of villages in different district of Bihar and Sahebganj district of Jharkhand state in India are facing serious threat to their health due to alarmingly high quantity of arsenic present in the underground water.

Bihar is facing one of the gravest natural disasters in the form of arsenic contamination of ground water. In the first detailed study of ground water quality, the Department of Environment and Water Management, A.N.College, Patna, has already submitted Interim Reports to PHED and UNICEF about the alarming findings on arsenic poisoning cases in the districts of Patna, Bhojpur, Vaishali and Bhagalpur. The study was conducted from April 2004 to May 2006, the study area being confined to 10 kms. wide belt along the Ganga river as per the instructions of PHED and UNICEF.

According to Dr.Ashok Ghosh, Principal Investigator of Project Arsenic, Dept. Of EWM, A.N.College, these findings are just the tip of the iceberg, as more contaminated aquifers are waiting to be detected in the remaining parts of the state. The water quality testing was done initially by Field Test Kits and then confirmed by AAS or UV Spectrophotometric tests. Epidemiological studies indicate that drinking water having more than permissible arsenic levels of 10 ppb. increases the mortality rates as arsenic is a bio-accumulative toxin.

Persons suffering from arsenicosis have not yet responded to known treatment procedures. The high the intake of arsenic, along with under nourishment and lack of medical help have worsened the lives of the population in the arsenic affected rural areas. Arsenic can also contaminate standing food crops if it is present in the soil and soil water. As Bihar Plains are highly fertile and its crops are marketed to many distant places, apart from being locally consumed, it becomes imperative to test the levels of arsenic in the food chain too. What is worrisome is that arsenic contaminated ground water tables have abrupt occurrences both over time and space. This explains why a public hand pump in village Ramnager in Maner tested 30 ppb. in the post monsoon period and more than 60 ppb. in the month of May. Also arsenic manifestation exists at different levels in different areas. In north-west Maner, arsenic contaminated hand pumps have a shallow depth of between 60 to 80 feet in the diara belt.

In Bhojpur, the depth of contaminated aquifers goes down to 150 feet away from new diara land, while in Vaishali, arsenic is found in the shallow and middle aquifers at an average distance of 5 km. away from the river bank. Regular monitoring of drinking water from hand pumps is immediately required as a part of the mitigation strategy. Patna, the first district to be covered, revealed pockets of high arsenic contamination, above the acceptable limit of 10 ppb., in 171 villages in Maner, Danapur, Sampatchak, Barh, Bakhtiarpur, , Fatuha, Khusrupur, Phulwari, Mokama, Pandarak and Patna City.

1060 village hand pumps were arsenic contaminated The highest AAS reading of arsenic level in government hand pump water is 724 ppb. in village Naikatola in Maner, 450 ppb. in Kasimchak village in Danapur, 553 ppb. in Ghiaspur Mahazi and 538 ppb. in Kala Diara, Bakhtiarpur,, and 484 ppb. in Malahi Banda village in Barh. Sampatchak Block has low contamination levels of below 50 ppb. over a larger area in most of the villages. In Bhojpur, the highest AAS test readings are 1861 ppb. and 1064 ppb. in Pandey tola, Barhara Block, a situation far more serious than the one represented by the much-touted village Ojhapatti of Shahpur Block. Out of the 6292 hand pumps tested, 47.70 % were arsenic contaminated hand pumps. In Barhara, 62.84%, in Udwantnagar 59.39%, in Shahpur 40.41%, in Behea 37.17%, in Koilwar, 29.20%, and in Ara 25.88% of Block level hand pumps were arsenic contaminated. In Vaishali, all the Blocks covered within 10 km. along the Ganga banks, has low level arsenic contamination at present.
In Bhagalpur district most affected areas are Kahalgaon, Pirpainti, Sabaur and Sultanganj. A detailed study has been presented on groundwater metal contents of Sahebgunj district in the state of Jharkhand, with special reference to arsenic. Both tubewell and well waters have been studied separately with greater emphasis on tubewell waters. Groundwaters of all the nine blocks of Sahebgunj district have been surveyed for iron, manganese, calcium, magnesium, copper and zinc in addition to arsenic. Groundwaters of three blocks of Sahebgunj, namely, Sahebgunj, Rajmahal and Udhawa have been found to be alarmingly contaminated with arsenic present at or above 10 ppb.
Rivers flowing through the coal fields of Jharkhand have been reported to carry arsenic responsible for arsenic poisoning in downstream areas of West Bengal. The coal fields of Bachara and Piprawar areas of Jharkhand have contaminated the waters of the Damodar and its tributary, the Safi. According to author, arsenic contamination arises mainly due to the dumping of waste from the coal mines along the river bed. Coals of the area mentioned contains sufficient amount of arsenic.
Arsenic upto 608 parts per billion (ppb) was detected against the permissible limit of 10 ppb in some villages of Kahalgaon block in Bhagalpur district in 2005. Work was carried out by Dr. Sunil Chaudhary of TM Bhagalpur University.
A detailed work was carried out by Dr. Ashok Ghosh, Professor-in-charge, department of environment and water management, A.N. College Patna, in the arsenic affected areas of Bihar State. He found that out of 27,061 hand pumps, 7,218 pumps tested had arsenic contaminated water greater than 10 ppb (26.67%). Highest arsenic value recorded was 1861 ppb. Study also revealed that 87% of the Trivalent arsenic was found in the groundwater of Bihar State.
The study by Bihar's Public Health and Engineering Department (PHED) reveals that the average arsenic content in drinking water in the 12 districts is 500 parts per billion (ppb). The state capital, Patna, is among the affected areas.
According to Dr. Ghosh, a total of 16 Bihar districts (57 blocks) are affected by high level of arsenic in the groundwater. Worst-affected districts are Bhojpur, Buxar, Vaishali, Bhagalpur, Samstipur, Khagaria, Katihar, Chapra, Munger and Dharbanga.
A very alarming recent finding by the research group is the detection of high arsenic content (more than 50 ppb) in the water of River Jaminia – flowing parallel to River Ganga in Bhagalpur district of Bihar.This river merges with Ganga and water from this river is being supplied to urban Bhagalpur without any treatment, alarmed Dr. Ghosh.
Alarmed by the severity of arsenic’s impact on human body in these villages, the team also collected samples of hair and nail of affected persons for detail medical examination to ascertain the level of damage, said Principal Investigators Dr. Ashok Kumar Ghosh and Nupur Bose of A.N. College Patna. The findings indicated that a wider area, including the fertile irrigational lands, was under the grip of arsenic.
According to another research report done by Mr. Dipanka Chakraborti in Semria Ojha Patti village in the Middle Ganga Plain, Bihar, where tube wells replaced dug wells about 20 years ago, analyses of the arsenic content of 206 tube wells (95% of the total) showed that 56.8% exceeded arsenic concentrations of 50 micro g/L, with 19.9% greater than 300 micro g/L, the concentration predicting overt arsenical skin lesions.

Reference:

http://ghosh51.tripod.com/id15.html
http://www.biomedexperts.com/Abstract.bme/12842773/Arsenic_groundwater_contamination_in_Middle_Ganga_Plain_Bihar_India_a_future_danger
http://news.bbc.co.uk/2/hi/south_asia/6982031.stm

Wednesday, December 16, 2009

High levels of black carbon likely to impact Tibetan Plateau's temperature.

The Dark Side of Black Carbon
by
Dr. Nitish Priyadarshi
Image Credit: NASA

As interest in Earth's changing climate heats up, a tiny dark particle is stepping into the limelight: black carbon. Commonly known as soot, black carbon enters the air when fossil fuels and biofuels, such as coal, wood, and diesel are burned. Black carbon is found worldwide, but its presence and impact are particularly strong in Asia. Black carbon, a short-lived particle, is in perpetual motion across the globe. The Tibetan Plateau's high levels of black carbon likely impact the region's temperature, clouds and monsoon season.

Black soot deposited on Tibetan glaciers has contributed significantly to the retreat of the world's largest non-polar ice masses, according to new research by scientists from NASA and the Chinese Academy of Sciences. Soot absorbs incoming solar radiation and can speed glacial melting when deposited on snow in sufficient quantities.
Temperatures on the Tibetan Plateau -- sometimes called Earth's "third pole" -- have warmed by 0.3°C (0.5°F) per decade over the past 30 years, about twice the rate of observed global temperature increases. New field research and ongoing quantitative modeling suggests that soot's warming influence on Tibetan glaciers could rival that of greenhouse gases.

Since melt water from Tibetan glaciers replenishes many of Asia's major rivers -- including the Indus, Ganges, Yellow, and Brahmaputra -- such losses could have a profound impact on the billion people who rely on the rivers for fresh water. Areas going to most affected in India would be Uttrakhand, Uttar Pradesh, Bihar, Jharkhand, West Bengal and Assam. While rain and snow would still help replenish Asian rivers in the absence of glaciers, the change could hamper efforts to manage seasonal water resources by altering when fresh water supplies are available in areas already prone to water shortages.
Researchers led by Baiqing Xu of the Chinese Academy drilled and analyzed five ice cores from various locations across the Tibetan Plateau, looking for black carbon (a key component of soot) as well as organic carbon. The cores support the hypothesis that black soot amounts in the Himalayan glaciers correlate with black carbon emissions in Europe and South Asia.
Black carbon or BC is formed through the incomplete combustion of fossil fuel, biofuel, and biomass, and is emitted in both anthropogenic and naturally occurring soot. Black carbon warms the planet by absorbing heat in the atmosphere and by reducing albedo, the ability to reflect sunlight, when deposited on snow and ice. Black carbon stays in the atmosphere for only several days to weeks, whereas CO2 has an atmospheric lifetime of more than 100 years. The term black carbon is also used in soil sciences and geology, referring either to deposited atmospheric BC or to directly incorporated BC from vegetation fires. Especially for the tropics, BC in soils significantly contributes to fertility as it is able to adsorb important plant nutrients .

Black carbon is a potent climate forcing agent, estimated to be the second largest contributor to global warming after carbon dioxide (CO2). Because black carbon remains in the atmosphere only for a few weeks, reducing black carbon emissions may be the fastest means of slowing climate change in the near-term.

Black carbon emissions from northern Eurasia, North America, and Asia have the greatest absolute impact on Arctic warming.

In some regions, such as the Himalayas, the impact of black carbon on melting snowpack and glaciers may be equal to that of CO2.Warmer air resulting from the presence of black carbon in South and East Asia over the Himalayas contributes to a warming of approximately 0.6°C. An “analysis of temperature trends on the Tibetan side of the Himalayas reveals warming in excess of 1°C.

Black carbon sources vary by region. For example, the majority of soot emissions in South Asia are due to biofuel cooking, whereas in East Asia, coal combustion for residential and industrial uses plays a larger role.

Black carbon can be controlled in developing countries through the implementation of cleaner fuels, new cooking technologies, and changing crop management practices.

Reference:

http://www.sciencedaily.com/releases/2009/12/091214173658.htm
http://fixtheclimate.com/component-1/the-solutions-new-research/black-carbon/
http://www.nasa.gov/multimedia/imagegallery/image_feature_1546.html
http://en.wikipedia.org/wiki/Black_carbon

Friday, September 25, 2009

The survival of Agriculture in a destabilized climate

With special reference to India and its Jharkhand State.
Crops become toxic in warmer world- says study
by
Dr. Nitish Priyadarshi
Department of Environment and Water Management,
J.N. college, Ranchi University, Ranchi, India.


Climate change has been the norm through out the earth’s history. Ice ages have been interspersed with interglacial periods with warmer temperatures. Although the causes of these previous natural changes are not completely understood, there is a growing consensus that human activities are contributing to the current period of climate change. In 1996, the World Meteorological Office/ United Nations Environmental Program’s Inter- governmental Panel on Climate Change (IPCC) cautiously stated: ‘ The balance of evidence suggests a discernible human influence on global climate. In spite of the nay-sayers, by 2001, new evidence and improved understanding led the IPCC to state unequivocally in its Third Assessment Report that, in its Judgement, ‘most of the warming observed over the last 50 years is attributed to human activities.

Climate change is the outcome of the “Global Warming”. It has now started showing its impacts worldwide. Either it is in the form of floods, heavy rain or in a form of drought.

Climate change induced by increasing greenhouse gases is likely to affect crops differently from region to region. For example, average crop yield is expected to drop down to 50% in Pakistan according to the UKMO scenario whereas corn production in Europe is expected to grow up to 25% in optimum hydrologic conditions.
Crops such as these sunflowers can be affected by severe drought conditions in Australia.
Between 1996 and 2003, grain production has stabilized slightly over 1800 millions of tons. In 2000, 2001, 2002 and 2003, grain stocks have been dropping, resulting in a global grain harvest that was short of consumption by 93 millions of tons in 2003.
The earth's average temperature has been rising since the late 1970s, with nine of the 10 warmest years on record occurring since 1995. In 2002, India and the United States suffered sharp harvest reductions because of record temperatures and drought. In 2003 Europe suffered very low rainfall throughout spring and summer, and a record level of heat damaged most crops from the United Kingdom and France in the Western Europe through Ukraine in the East. Bread prices have been rising in several countries in the region.
The 2001 IPCC Third Assessment Report concluded that the poorest countries would be hardest hit, with reductions in crop yields in most tropical and sub-tropical regions due to decreased water availability, and new or changed insect pest incidence. In Africa and Latin America many rainfed crops are near their maximum temperature tolerance, so that yields are likely to fall sharply for even small climate changes; falls in agricultural productivity of up to 30% over the 21st century are projected.
The impacts of global warming have been truly global and extraordinarily varied. The average rise in global temperatures may seem small- 0.76 degrees C since the Industrial Revolution in roughly the mid-18th century, the earth’s average temperature reaching 14.5 degree C in 2005- but this is only an average. The farther one goes from the equator, in northern latitudes in particular, the rise is much higher than the average.

In this article my emphasis will be more on impact on agriculture due to climate change, with special reference to India and its Jharkhand State. India’s agriculture is more dependent on monsoon from the ancient periods. Any change in monsoon trend drastically affects agriculture. Human interference has certainly made the Indian monsoon fickle. Even the increasing temperature is affecting the Indian agriculture. A recent study by the Indian Agriculture Research Institute found that increase in temperature by about 2 degrees C “reduced potential (wheat) grain yields in most regions”, and that “overall, temperature increases are predicted to reduce rice yields”, the impact on rice yields being most in eastern India. even the IPCC, scarcely alarmist, says 0.5 degree C rise in winter temperature would reduce wheat yield by 0.45 tons per hectare in India. And this when Indian agriculture has already pushed into crisis, and 1.5 lakh farmers have committed suicide since 1995.

There has been a major shift in the pattern of rainfall during the south-west monsoon season (from June to September) in recent years. This is one of the findings of an analysis by scientists at the India Meteorology Department’s National climate Centre at Pune.

Another is that rainfall over Kerala, Chhattisgarh and Jharkhand has been showing a significant decreasing trend, while that over coastal Andhra Pradesh, Rayalaseema, north interior Karnataka, Madhya Maharashtra, Konkan, Goa and Gangetic West Bengal is showing a significant increasing trend. While the contribution of July rainfall to the overall monsoon exhibit a significant increasing trend. The contribution in June and August exhibited a significant increasing trend. The findings are significant in the context of the global phenomenon of climate change. Due to global warming intensity and number of cyclones has increased. In the cyclone seasons of 2006, the number of depressions and cyclonic storms over Bay of Bengal were almost twice the annual average. This is damaging coastal agriculture and livelihoods. Due to global warming there is high influx of water in the Himalayan rivers flowing through Assam, Bihar and West Bengal in eastern India in the form of floods due to melting of Himalayan glaciers associated with heavy rains in the Himalayas. These floods annually destroy millions of tons of crops. This year the world's largest river island Majuli in Assam State of India has been severely hit by flood and erosion. Floodwaters have inundated over 87 villages of the island causing tremendous difficulty to the inhabitants and due to rapid erosion many fertile paddy fields have also been washed away by gushing water.

In year 2008 more than two million people have been marooned by late monsoon floods in 15 of the country's 64 districts, according to the Bangladesh Water Development Board (BWDB). According to a report by the Department of Agricultural Extension (DAE), crops such as Aman (the mainstay of the country's rice production and a staple component of the population's diet), t-Aman (a locally developed hybrid paddy), Aush (a secondary rice crop whose volume is less than half of Aman), jute and vegetables on more than 100,000 hectares of land in the 15 flood-hit districts were submerged. More than 20,000 hectares of Aman and Aus crops in Companiganj, Golapganj, Jaintapur, Kanaighat, Gowainghat, Fenchuganj and Beanibazar Sub-districts have been destroyed in Sylhet and Sunamganj districts, according to agriculture officials.

Few years ago, there were reports coming in of massive forced migration due to persistent droughts in Bundelkhand area in Central India. large lakes had completely dried, water in wells that people use for their daily needs had run down, rivers and tributaries had dried up, thousands of hand pumps had become useless because the groundwater levels had fallen. People had abandoned their cows and other cattle to a dusty death, as they were unable to provide them fodder and water.

Global warming intensifies drought conditions in regions that already face dry conditions, particularly in [ Sub] continental interiors. The IPCC’s report in 2007 says that “increased continental temperatures are expected to lead to greater evaporation and drying, particularly important in dry regions where surface moisture is limited… drought has become more common, especially in the tropics and subtropics, since the 1970s … more intense and larger drought have been observed.

Drought like situation is also threatening Jharkhand State of India where scanty and late arrival of monsoon this year is affecting crops and depletion of ground water. Drought is a recurrent phenomenon in Jharkhand. It affects the livelihoods of the majority of its people, particularly tribals and dalits living in rural areas. Twelve of the 22 districts of the state, covering 43% of the total land area, are covered under the Drought Prone Areas Programme (DPAP).Hunger and starvation deaths are reported almost every year. Jharkhand is one of the richest states in the country in terms of natural resources. However, the rate of growth in agriculture has been one of the slowest in the country both in terms of production and productivity. Almost 90% of the cultivated area is monocropped. Only 9% of the total cropped area is irrigated. Hence the rural population is very vulnerable to rainfall fluctuations.

Jharkhand receives almost 1200-1300 mm of rainfall every year but from last few years the rains are erratic in many areas. The probability of rainfall failures and coefficient of variations is quite high in the last weeks of June-July and in the last weeks of September-October. Hence, drought in the state primarily occurs at the start or end of the kharif season.

This year there was less rain in the month of July. In July, upland crops grow to maturity and seedlings for transplanted rice are established. If there is deficient rain, the upland crop—mainly paddy and maize, which provides food security in August-September— is affected.

This year most of the vegetables have been destroyed either due to uneven rainfall or due to intense un-seasonal hailstorms that damaged the standing crops and vegetables and led to huge losses to farmers. In year 2007 and 2008 also hailstorms destroyed crops. This year situation worsened as most of the green vegetables vanished from the local markets or was too costly to be purchased by the common and poor people.

Palamau district in Jharkhand State of India is reeling under drought due to scanty rainfall. Crops have been destroyed and the region is facing a famine-like situation. It has not only affected the crops but also depleted the ground water and well water forcing people to drink contaminated water.

The Indian Irrigation Commission described Palamau as the driest and probably the poorest district of the province. The frequent draughts and famines or scarcity conditions that have visited this district within the last century support this observation. The district falls within the retreating range of the south-west monsoon and as such rainfall is wholly dependent upon local conditions and local winds which are seldom favourable to the district.

The rainfall in Palamau is not only scanty but very capricious in its distribution. There are, it is true, a large number of rivers and streams in the district, but in most of them the supply of water diminishes rapidly or fails entirely soon after the end of the scanty rains.

It is not only Palamau but other districts are also under threat of drought like conditions including Ranchi district. It is not only the scanty rain but rise in temperature and short period of winter has also affected the crops and vegetables of the state.

Jharkhand is one of the most food-insecure and malnourished states in the country. NSSO (55th round) data reveal that 10.46% of all households in Jharkhand face seasonal food insecurity. Around 2.5% of households face chronic food shortages. Of the families facing food insecurity, 64% face food shortages for two to three months while as many as 28% do not have sufficient food for four to five months. Almost 6% of the food-deficient
households have to go hungry for more than half the year. The incidence of food insecurity is higher among ST and SC families. Assured food supplies exist for only three to four months of the year, after the harvest in late October-early November. Food supplies tend to run short by the end of winter. The starvation period begins by mid-summer (June) and in many cases, continues till the end of October.

Entire Jharkhand has been now declared drought-hit following scanty rainfall. The decision was taken at the meeting of the Advisory Council of the Governor. Earlier, the Council had announced 11 of the 24 districts as drought-hit. In the face of severe drought, it was decided to distribute grains free of cost to BPL (below poverty line) families, besides setting up of grain godowns at district and block headquarters.


If the same condition prevails in coming years situation will be worse as the state lacks proper irrigation facilities and proper storage facilities for grains.

A dry spell has led the Uttar Pradesh government to declare 20 of the state's 70 districts as "drought-hit". According to weather reports, Uttar Pradesh has received only about 128 cm of rainfall since June 1 as against the expected normal rainfall of about 307 cm. In the 20 drought-hit districts, the recorded rainfall was barely 60 cm.

Scanty rainfall in most parts of Uttar Pradesh, will hit agricultural production leading to a shortage of rice in the state, says a government report. According to the report prepared by the state agriculture department, the worst hit would be paddy yield, which is expected to decline by about 60 percent this year. Maize production is also expected to fall 1.15 million tonnes to 900,000 tonnes.
The districts where rainfall has been lowest include Chitrakoot (81 percent below normal), Etah (84 percent below normal) and Rampur (85 percent below normal).
Twenty six of Bihar’s 38 districts were declared drought-hit this year in view of scanty rainfall that has badly hit transplanting of paddy seedlings and affected millions of farmers.

Bihar has recorded a 42 percent rainfall deficit so far this monsoon season. This has hit the transplanting of paddy seedlings.
The state during the period between June 1 and Aug 6 had received just 331.7 mm of rainfall against the average 568.5 mm — a deficiency of 42 percent. It has resulted in 58 percent decline in paddy transplantation. Bihar had targeted sowing of paddy in 8,772,241 acres this year, but the crop could only be planted in only 3,822,967 acres so far.
Uttarakhand State is under drought-like conditions for last six months. 50 per cent of crops damaged in 3216 villages of five districts alone. Rainfall in the months of December, January, February and March has been far below normal, severely affecting winter crops in the hilly areas.

Madhya Pradesh state of central India is going to witness the worst drought of the century due to the scanty rainfall in as many as 37 districts following which it has declared them drought-affected.
Due to scanty rainfall, as many as 37 districts of the state were declared drought-affected. The districts which were declared drought-affected are Alirajpur, Ashok Nagar, Anuppur, Barwani, Bhind, Balaghat, Burhanpur, Chhatarpur, Dewas, Dindori, Datia, Damoh, Guna, Gwalior, Jhabua, Jabalpur, Katni, Khandwa, Morena, Mandla, Narsinghpur, Panna, Ratlam, Raisen, Rewa, Satna, Sidhi, Singrauli, Shahdol, Sagar, Sehore, Shivpuri, Sheopur Kalan, Shajapur, Tikamgarh, Umaria and Vidisha.

Drought like conditions is prevailing in most parts of Northern India. According to William Cline, a senior fellow at the Center for Global Development (CGD) and the Peterson Institute for International Economics, “India is among the most adversely affected with losses of 30-40% (in agriculture productivity) depending upon whether higher carbon dioxide provides a significant fertilization effect.”He noted that in the southern parts of India, damage will be substantial and similar to that in other countries also located close to equator. In these locations, where temperatures are already at high levels, an increase in temperature will surpass crop tolerance levels. In North India, the unusual increase in rainfall combined with higher temperature could result in a higher decline in productivity than one would expect from where it is located relative to equator. Cline finds that agricultural production in developing countries may fall between 10 and 25 percent, and if global warming progresses unabated, India's agricultural capacity could fall as much as 40 percent.
Poverty in South Asia is still largely rural. About 70% of South Asia’s population lives in rural areas, and it accounts for about 75% of the poor. Most of the rural poor depend on agriculture for their livelihood. Agriculture employs about 60% of the labor force in South Asia and contributes 22% of regional GDP. The Green Revolution of 1970s and 1980s substantially increased food grain productivity and increased rural wages. Recent agricultural growth in South Asia, however, is less than 3% and is far below the growth rates of other economic sectors.

Prime Minister of India Manmohan Singh said that the country was facing a drought threat. India's vital monsoon rains have been 29 percent below normal since the beginning of the June-September season, hurting crops such as rice and sugarcane and triggering a sharp rise in food prices. "We are staring at the prospect of an impending drought,".

Since agriculture constitutes a much larger fraction of GDP in developing countries, even a small percentage loss in agricultural productivity would impose a larger proportionate income loss in a developing country than in an industrial country.

A study published in Science suggest that, due to climate change, "southern Africa could lose more than 30% of its main crop, maize, by 2030. In South Asia losses of many regional staples, such as rice, millet and maize could top 10%".

Drought obviously leads to water stress in plants. Heat waves, on the other hand, are acute episodes which, if the temperature is high enough, above 40 degree C for instance, lead to wilting and death, because of structural damage to essential proteins. The problem is that plants react by closing their stomata when subjected to water stress, so shutting down on transpiration and conserving water. But rather as the body would overheat dangerously if it shut its pores to prevent sweating, so in a plant the shutting of the stomata will cause internal temperatures to rise and may well cause permanent damage, if not death. According to a report temperatures above 45 degree C will damage most plants if lasting for half-an-hour or more. High soil temperatures will also damage roots and prevent nutrient uptake.

David Pimental from the college of Agriculture and Life Sciences, Cornell University, points out that each crop has its optimum temperature and length of growing season for maximum yields. Rice generally grows best when temperatures are between 30 degree C and 33 degree C, yet it will still ‘fruit’ and generally produce as long as temperatures do not fall below 18 degree C. Some varieties will tolerate temperatures rising to as high as 40 degree C. In contrast potatoes do badly if temperature rise above 28 degree C and do best when they lie between 15 and 20 degree C. higher soil temperatures will increase the rate of oxidation and hence loss of nutrients and organic matter. Less organic matter means less soil organisms such as earthworms and insects that do so much to improve the ground. Hence global warming and temperature rises could have a deleterious effect on the main cereal crops.

In temperate latitudes crops need at least 250 millimeters of rain a year and in the tropics 500 millimeters. However, it is not just the amount of precipitation, but when the bulk of it occurs that is important. Global warming will undoubtedly play havoc with a crop’s specific needs, both through increasing surface temperatures, which itself will lead to a greater likelihood of water stress on vegetation because of enhanced evaporation from soils and through distorting rainfall patterns. A failure of the monsoon spells disaster for India as does just a small decline in the amount of rain over the semi-arid countries of the Sahel.

Global warming is not only affecting the production of the crops but also making some of the crops toxic. According to an Australian scientist, Staples such as cassava on which millions of people depend become more toxic and produce much smaller yields in a world with higher carbon dioxide levels and more drought.

A team of Monash University in Melbourne tested cassava and sorghum under a series of climate change scenarios, with particular focus on different CO2 levels, to study the effect on plant nutritional quality and yield. Both species belong to a group of plants that produce chemicals called cyanogenic glycosides, which break down to release poisonous cyanide gas if the leaves are crushed or chewed.
Around 10 percent of all plants and 60 percent of crop species produce cyanogenic glycosides.
The team grew cassava and sorghum at three different levels of CO2; just below today's current levels at about 360 parts per million in the atmosphere, at about 550 ppm and about double at 710 pm.
It was found that at double current CO2 levels, the level of toxin was much higher while protein levels fell.
The ability of people and herbivores, such as cattle, to break down the cyanide depends largely on eating sufficient protein.
Anyone largely reliant on cassava for food, particularly during drought, would be especially at risk of cyanide poisoning.
The group looked at a type of sorghum commonly fed to cattle in Australia and Africa and found it became less toxic at the highest CO2 level. But under drought conditions, leaf toxin levels rose.

Within the context of the modern industrialized farming, global warming and warmer temperatures with mild winters in temperate zones will lead to a surge in pathogens and pests. Not only will some pests be able to take advantage of rising temperatures to spread to higher latitudes and altitudes, but also to increase their rate of reproduction by adding an additional generation. During the growing season some insect pests can produce 500 progeny per female every two weeks and as many as 3,000 in a single generation. In general, losses to insects and mites are higher in warmer regions of the world.

According to the United Nations, agricultural mismanagement has damaged more than 552 million hectares – 38 percent of today’s cultivated area- since World War 2 and that overall, between 5 and 10 million hectares a year are currently being lost. Just 100 years at that rate would leave the world with but a patch of the land for agriculture that it has today.

Reference:

Bunyard, P. 1999. A hunger world. The Ecologist, v.29, no.2, pp.86-91.

Runeckles, V.C. 2002. Air pollution and climate change. In air pollution and plant life, second edition, eds. J.N.b. Bell and M. Treshow. Wiley, USA.

“The roots of Global Warming” a report published by Delhi Platform in year 2008.

http://www.globalsecurity.org/military/library/news/2008/09/mil-080904-irin04.htm
http://www.mail-archive.com/jharkhand@googlegroups.com/msg00065.html
http://www.indianexpress.com/news/jharkhand-declared-droughthit/497085/
http://samachaar.in/Uttar_Pradesh/20_Uttar_Pradesh_districts_declared_drought-hit_88045/
http://www.thaindian.com/newsportal/business/26-bihar-districts-declared-drought-hit-lead_100230110.html
http://en.wikipedia.org/wiki/Climate_change_and_agriculture
http://74.125.93.132/search?q=cache:vqTmwwbX0bQJ:www.imf.org/external/pubs/ft/fandd/2008/03/pdf/cline.pdf+global+warming+and+agriculture+cline&cd=1&hl=en&ct=clnk&gl=in
http://web.worldbank.org/WBSITE/EXTERNAL/COUNTRIES/SOUTHASIAEXT/0,,contentMDK:21571064~pagePK:146736~piPK:146830~theSitePK:223547,00.html
http://timesofindia.indiatimes.com/news/india/MP-to-witness-worst-drought-says-CM-Chouhan/articleshow/4909762.cms
http://www.redorbit.com/news/science/1660279/global_warming_37_percent_cause_of_droughts/index.html?source=r_science
http://uk.reuters.com/article/idUKTRE55S2KY20090629?pageNumber=3&virtualBrandChannel=0

Saturday, August 8, 2009

Fire erupted in National Highway in Jharkhand State of India.

Coal supply and environment are going to be badly affected.
Explosions are being heard.
By.
Dr. Nitish Priyadarshi





Ramgarh district administration of Jharkhand state of India on Friday (August 7,2009) suspended the movement of vehicles on the 35 Km stretch of National Highway (NH) 33 between Ranchi (capital of Jharkhand) and Patna (capital of Bihar). The underground fire erupted violently on 750 metre –stretch on highway on Friday. Explosions are also being heard.
Supplies of coal from this area to other parts of the country are going to be badly affected due to this fire and closure of the most important road. Other than environmental it is also going to affect the supply of the food grains to other parts of drought affected area of the Jharkhand state.
For detail story please scroll down this blog.

Tuesday, August 4, 2009

Sedimentation by Himalayan Rivers may cause Earthquakes and Land subsidence in Eastern India.

It's not a question of whether the big one is coming, only of when.
by.
Dr. Nitish Priyadarshi
Image of the Ganges River delta and the Bay of Bengal acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS). This image shows the massive amount of sediments delivered to the Bay of Bengal by the Ganges River, sediments that are derived from erosion of the Himalayan mountain range to the north.
Sediments deposited in Bay of Bengal


Sediment loads in Kosi River in Bihar.

The Indian landmass, a floating continent started to collide with the Asian landmass some 20 million years ago (m y). After its separation from South Africa and Madagascar the floating continent must have been like a Noah’s Arc carrying all its fauna and flora on its body. The great collision between the two landmasses led to the formation of the youngest and tallest mountain ranges, the Himalayas.

Once the Himalayas started to rise a southward drainage developed. The Himalayas subsequently controlled the climate of the newly formed continent, and there started the season of monsoon as well. The river system thus developed because of rains and melting snow started to drain south into the fore-deep. The newly formed rivers were like sheets of water flowing towards the fore-deep carrying whatever came in their way. Once the rivers reached the plains their gradients became lesser, their hydraulics changed and they started to dump their load. During monsoons these rivers carried a sediment load which was many times more than their normal load. All the material they carried was dumped enroute their final destination, the Sea.

The sediments are carried from their point of origin to the local stream network commonly by mass weathering processes, typically soil creep, and eventually become part of the stream load. Very fine fragments move quickly along the network as suspended load, but the downstream progress of larger fragments is usually very slow. Thus, the weathering process does not end in the source area but continues to operate during the long process of stream transport.

Sedimentation rates generally cannot be expressed in absolute data because periods of rapid sedimentation alternate with periods of slower deposition, non-sedimentation, or erosion. Nevertheless, it is important to gain some understanding of the average values of net sedimentation in various depositional environments in order to better comprehend the geological and chemical processes that take place on the surface of the earth. An understanding of net sedimentation rates has become increasingly valuable with onset of intensive water pollution studies, because sedimentation is one of the most important processes in the removal of pollutants from natural waters.

Presently sedimentation loads are being considered as one of the possible cause of earthquakes. It works on the theory that deposition of sediments alters the loading of the earth’s crust and tectonic stresses in its interior. Such stresses could reactivate preexisting faults.
Combination of the biological, chemical, geological, and geographical factors that influence sedimentation rates are almost infinite, are different for each depositional environment, and have continuously fluctuated throughout the past.
The most extensive vertical deposition of sediments by Himalayan rivers flowing through Uttar Pradesh, Bihar, Jharkhand, and Bengal States of India, occurs during floods (July to October).

Coleman (1969) investigated channel deposition and erosion patterns of the braided Brahmaputra River in India during flooding and found that as the current velocity decreased, rapid sedimentation occurred, and as much as 3 m. of sediment was deposited along the channel bottom. When a meandering river floods its banks, its velocity is rapidly checked, and sediment deposition occurs adjacent to the banks. The rate of floodplain deposition usually ranges from several mm to several cm/year (Kukal, 1971).
Each year these rivers were flooded leaving behind a fresh layer of sediments. The Indo-Gangetic plains are a product of such floods. Study carried out by Rajiv Sinha, of Geoscience group, IIT Kanpur has brought to light amazing quantity of sediment load carried by the Ganga River in its present hydrodynamic regime. Gangetic Rivers erode bulk of the sediments from upstream areas in the Himalayas and deposit part of it in the alluvial plains and a significant part in the Bay of Bengal. His study reveals that the Ganga river annually erodes around 749 million tonnes of sediments, mostly from the Himalayas, brings about 729 million tonnes at Farrakka and finally dumps 95 million tonnes in the Bay of Bengal. Thus the floodplain of the Ganga gets an annual increment of about 65 million tonnes of sediments.

The quantity of sediments eroded by the river depends upon the gradient, distance from the source area and also the geology and geomorphology of the terrain. Thus Ganga at Haridwar and Yamuna at Allahabad are characterized by low sediment yield of 150-350t/km2/yr, while the eastern tributaries like Kosi and Gandaki carry a much higher sediment load of 1500-2000t/km2/year.

Along the river's traverse, large tributaries enter the Ganga and significantly increase its flow and change its character. The Ganga is joined by the Ram Ganga, Yamuna, Ghaghara, Gomti, Gandak and Kosi tributaries. The rivers of the Ganga basin carry one of the largest sediment loads in the world. Today sediment loads in the Ganga are higher than in the past due to the complete deforestation of the Gangetic plains and the ongoing deforestation of the Himalayan foothills.

Sedimentation in plains of Ganga River and Bay of Bengal.

In the plains Kosi (major tributary of Ganga) River is building up a large delta of its own through which its channels have wandered for centuries. It is believed that the Kosi originally joined the Mahananda, a river coming from the Darjeeling Himalayas. It is known that the Kosi flowed by Purnea (Bihar) 200 years ago, but its present course is about 160 km to the west of that place, having swept over an area of 10,500 sq. km on which it has deposited huge quantities of sand and silt (Krishnan, 1982). It now joins the Ganga 32 km west of Manihari but formerly it used to join that river near Manihari itself. The Kosi is notorious for its frequent and disastrous floods and the vagaries of its channels. In high flood it is said to have a flow of nearly one million cusecs loaded with much gravel, sand and silt (Krishnan, 1982).

The Hooghly River (main channel of the Ganga in West Bengal) estuary is notorious for its sand banks and dangerous shoals of which the James and Mary Sands, 56 km below Calcutta (now Kolkata) and between the mouths of the Damodar and Rupnarain, are well known. New areas are being reclaimed by the sediments brought down by the Ganga. These are known as the Sundarbans.

Compared to the Peninsular rivers, the three main Himalayan river systems are mighty giants. The Indus carries to the sea an average of about a million tons of silt per day, the Ganges a little less and the Brahmaputra a little more (Krishnan, 1982). The Irrawaddy has been estimated to transport about two-third million tons of silt per day. The Himalayan rivers are fed both by rain and snow, by rain during June to September and by snow during the warmer half of the year. In their courses through the mountains they have good gradients and carry much coarse materials including pebbles and boulders, brought in by glaciers and also torn off from the beds and banks. They carry enormous quantities of fine sand and silt derived from the Himalayas as well as from higher peninsular up-lands.

The Ganga and the Brahmaputra have changed their courses in the plains frequently in historic and pre-historic times leaving behind huge sediments in the plains. Deposition of sediments in Bihar, Bengal, and in Bay of Bengal is going on from the geological past. Millions of tons of sediments are being deposited per day by the Himalayan rivers in the Eastern India thrusting pressure over the crust below.

Now it is widely accepted that huge sediment loads may cause mild to high tremors even in the non-seismic zone. This may be due to the great lateral thrust of sediment load contributing to stress imbalances or due to the reactivation of subterranean faults by the newly developed stresses or due to increased pore pressure in the adjoining rocks which lowers their shearing strength, resulting in earthquake occurrence.

An earthquake is generally caused by dislocation in the earth’s crust along pre-existing cracks or faults. The cause of earthquakes is probably the existence of such faults or cracks in the bottom of the depression hidden under alluvium. Moreover, there are well marked reversed faults at the junction of the outer and the inner Himalayas, and when dislocation occurs along these faults, earthquakes result.

An additional factor favoring dislocation along such surface or subterranean faults is the strain which exists between the Himalayas and the Bihar plains. This strain is due to the following facts. The section of the Himalaya north of the Bihar is the highest mountain region of the world. The higher a region, the more it is subjected to erosion. So, vast amount of sediments are being eroded from the Himalayas and carried down to the Bihar plains as in the case of Kosi river which contributes heavy sediment in Bihar plains. The silt yield of the Kosi is about 10 cubic yard /acre/yr, one of the highest in the world. As the mountains are eroded they are deloaded and have a tendency to rise. On the other hand, the plains get loaded by the sediments and have a tendency to subside. These opposed tendencies of movements between the Himalayas and the Bihar plains cause strain in the hinge-zone, i.e. in the southern part of the mountains. Here fault already exists. Dislocation may occur along these faults as a result of the strain and devastating earthquakes may result.

The entire area has undergone downwarping due to Himalayan upheaval resulting in the formation of transverse faults and dislocations in the basement rocks, along pre-existing faults or cracks aided with occasional earthquakes. The foothills of the Himalayas, the Indo-Gangetic plains and the sedimentary basins of Vindhyans are all quake-prone areas of the Bihar state.

Several faults have been identified in the region and some have shown evidence of movement during the Holocene epoch. The West Patna Fault runs in a NE-SW direction from near Arrah in the south to the Nepalese border near Madhubani in the north. Running almost parallel to it is the East Patna Fault which extends from the south-east of Patna in the south to the Nepalese border to the east of Madhubani. Another fault, this one also lying parallel to the previous two, is the Munger-Saharsa Ridge Fault which runs from Biharsharif to near Morang in eastern Nepal. Apart from these there are east-west running tear faults in the region that control the courses of the main rivers.
The Gandak fan is bounded by the courses of the Ghagra and Rapti in the west, the Ganga in the south and the Rohini in the north. The courses of all these streams are along faults (Mohindra and Prakash, 1994).

The Gangetic plains, of which the Kosi megafan forms a part, is bound by E-W faults, which on analogy with the main boundary thrust may be thrust faults. The Kosi megafan is bound on the west by a NE trending prominent sinistral fault causing an offset of some 20 km of the Siwaliks juxtaposed against the Gangetic alluvium. There are several NW trending faults on the eastern fringes of the Kosi megafan (Mahadevan, 2002).

Bengal basin, having an area of 89000 square kilometers and sedimentary fill of 10-15 km, is the northernmost of the east coast basins of India . Indian Shield and Shillong massif form the western and northern limits of Bengal Basin. Eastwards the Basin extends into Bangladesh and is bounded by Arakan Yoma geanticlinal uplift. Southwards Basin plunges into Bay of Bengal beneath the continental shelf. Tectonically the basin can be divided into four structural elements i.e. basin margin fault zone, shelf, hinge zone/slope break and basin deep.

The tectonic history of Bengal Basin indicates that the drainage pattern in the Bengal basin as a whole had been and is greatly controlled by the tectonic features of the basin. Considerable evidence has been recorded of significant tectonic movements within and along the boundary of the basin in late Tertiary and the Quaternary times. Auden (1949) postulated that the western margin of the Bengal basin is faulted and the major tectonic movements have taken place along this zone in the Pleistocene.

Rocks at the depth in crust are subjected to the load pressure of the overlying column of rocks and sediments. This pressure is related to the thickness and mean density of the overlying material or sediments. Several million years under stress, most rocks will exhibit the kind of ductile behaviour familiar to all geologists. The rocks under higher stresses, however, will fracture and generate earthquakes (Park, 1983).

The San Francisco earthquake of 1906 was a major earthquake that struck San Francisco, CA and the coast of Northern California at 5:12 A.M. on Wednesday, April 18, 1906. The 1906 San Francisco earthquake was caused by a rupture on the San Andreas Fault, a continental transform fault that forms part of the boundary between the Pacific Plate and the North American Plate. This fault runs the length of California from the Salton Sea in the south to Cape Mendocino to the north, a distance of about 800 miles (1,300 km). The earthquake ruptured the northern third of the fault for a distance of 296 miles (477 km). The maximum observed surface displacement was about 20 feet (6 m); however, geodetic measurements show displacements of up to 28 feet (8.5 m).
It was interpreted that earthquake was caused due to large seasonal sediment loads in coastal bays that overlie faults as a result of the erosion.

Sedimentation also cause land subsidence. Subsidence may result from the accumulation of large volumes of sediment at the earth's surface in what is known as a sediment basin. An obvious setting in which this occurs is at river deltas. Each day, the Mississippi River deposits up to 1.8 million metric tons of sediment at its mouth near New Orleans. The weight of this sediment contributes to a gradual subsidence of the land on which New Orleans resides. Basins between mountains also can subside due to the weight of accumulating sediments.

Wherever sediments accumulate, we can be certain that in some other locality, a source has been relatively elevated with respect to the place where the strata are being deposited.

A delta is a subsidence-prone area because it receives a huge volume of sediments, which can be compressed due to post depositional consolidation, and the load of which can result in detectable isostatic sinking of the earth's crust.

In the year 2008 lots of reports were there regarding development of big cracks on the surface overnight in many parts of Uttar Pradesh state of India. This may be the side effects of land subsidence.

Two prehistoric seismic events dated to have occurred: (i) during 1700 to 5300 years BP and (ii) earlier than 25,000 years BP. From last several years Ganga Basin has not been affected with any major tremors or earthquakes, except of 1833, 1934 and 1988 earthquakes which rocked North Bihar and Nepal. Seeing the load of sediments, possibilities of major earthquakes cannot be ruled out in Eastern India including Bihar, neighbouring Uttar Pradesh and Jharkhand, and Bengal Basin. Most affected areas may be Munger, Dharbanga, Purnia, Bhagalpur, Saharsa, Supaul, Katihar, Patna in Bihar State, Sahibganj, Godda, Pakur etc. of Jharkhand State. It's not a question of whether the big one is coming, only of when.

Reference:

Auden, J.B., 1949. Proc. Ind. Nat. Instt. Sciences.,15.

Coleman, J. M., 1969. Brahmaptura River: Channel processes and sedimentation. Sed. Geol.,3, pp. 129-239.

Dasgupta, S., Pande, P., Ganguly, D., Iqbal, Z, Sanyal, K, Venkatraman, N.V., Dasgupta, S., Sural, B., Harendranath, L., Mazumdar, K., Sanyal, S., Roy, K., Das, L.K., Misra, P.S., Gupta, H. 2000. "Seismotectonic Atlas of India and its Environs", Geological Survey of India.


Krishnan, M.S. 1982. Geology of India and Burma. CBS publishers and distributors, India.

Kukal, Z., 1971. Geology of Recent Sediments. New York: Academic Press (in Czechoslavakia: Prague, Czechoslovak Academy Sci.), 490p.

Mahadevan, T. M. 2002. Geology of Bihar and Jharkhand. Geological society of India, Bangalore.

Mathur, S.M., "Physical Geology of India", National Book Trust of India, 1998.


Mohindra, R. and Prakash, B. 1994. Geomorphology and neotectonic activity of the Gandak mega-fan and adjoining areas, middle Gengetic Plains. Jour. Geol. Soc. India, v.43, pp. 149-157.

Park, R.G., 1983. Foundations of Structural geology. Blackie & Son Ltd. Glasgow.

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