Showing posts with label Uttar Pradesh. Show all posts
Showing posts with label Uttar Pradesh. Show all posts

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

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.

http://adsabs.harvard.edu/abs/2007AGUFM.B23B1269G
http://www.agu.org/pubs/crossref/2008/2007JF000909.shtml
http://www.indianexpress.com/news/silting-not-pollution-chocking-ganga/376907/
http://www.auburn.edu/~alleykd/envirolitigators/gangatext.htm
http://science.jrank.org/pages/6563/Subsidence-Geologic-subsidence.html
http://disc.sci.gsfc.nasa.gov/oceancolor/additional/science-focus/ocean-color/sedimentia.shtml
http://geology.geoscienceworld.org/cgi/content/abstract/28/12/1083
http://www3.interscience.wiley.com/journal/68501812/abstract?CRETRY=1&SRETRY=0
http://en.wikipedia.org/wiki/1906_San_Francisco_earthquake
http://www.onepetro.org/mslib/servlet/onepetropreview?id=00014598&soc=SPE&speAppNameCookie=ONEPETRO
http://www.indiaenvironmentportal.org.in/content/palaeoliquefaction-evidence-prehistoric-largegreat-earthquakes-north-bihar-india
http://timesofindia.indiatimes.com/NEWS/City/Patna/Bihar-vulnerable-to-quakes/articleshow/977183.cms

Wednesday, July 9, 2008

Land splitting creates panic in Uttar Pradesh State of India- Groundwater depletion is not the only cause.

Jharkhand and Bihar may face such phenomenon.
by

Dr. Nitish Priyadarshi

Several wide cracks on the earth has developed in different parts of Uttar Pradesh state of India. Areas covered are Hamirpur, Jalaun, Orai, Rai Barelly, Allahabad, and Kanpur. Reports are also coming from the neighbouring states where people are scared of this phenomenon.

This year on April 16 small quantities of molten rock erupted near a habitation at Sandhwa near Indore city of Madhya Pradesh state, leaving neighbours awestruck. Locals said that the eruption began with a small explosion causing two-feet wide gap in the soil.

With incidents of land splitting reported from various parts of North India, many people are asking : is doomsday at hand?

According to a saying in Hindu religion “land splitting is not a good sign. Incidents of land splitting are accompanied with deaths, mayhem and pogroms”.

Releasing a fear psychosis is building up among the villagers where incidents of land splitting have been reported in the recent past, the state government is now on an over drive to dispel the fear by giving a scientific angle to the whole process.
According to the experts, the cracks developed due to steep fall in the groundwater level. Decline in the groundwater level meant the space under the surface was now occupied by gases, which often could support the weight of the layers above. Different layers of the earth tend to move as a result, leading to cracks on the surface. Geologists say that due to the groundwater scarcity, soil was not able to bind the water molecules. As a result, the earth’s crust in various districts was developing cracks.


Land subsidence is a natural geological occurrence; however, it has been greatly accelerated by humans through excessive groundwater pumping. Generally speaking, land subsidence occurs at accelerated rates when water is pumped from an aquifer faster than it is replenished; it can also occur due to oil pumping and mining operations.


When a fissure reaches the surface, it is generally as a hairline crack, often less than an inch wide. It is after a rainstorm that the real problems emerge: As surface water flows into a fissure, it quickly expands into a giant crevasse, which could grow large enough to swallow a house. It is a process that can happen quite rapidly.


With continued groundwater depletion, we will continue to see new fissures forming," "and we cannot be sure exactly where they will form. Furthermore, it is unclear how many fissures may have already formed that have yet to surface. Even if we were able to recharge the aquifers, it could take decades, perhaps longer, before we stopped seeing new fissures."


Such fissures are called blind fissures, because they are not visible until they surface.
If we believe that groundwater depletion is the only phenomenon behind land subsidence then the states like Jharkhand, Bihar etc. should now be on high alert where the groundwater pumping is high.


But seeing the cases of land splitting in big scale in Uttar Pradesh and its adjoining States, only groundwater depletion is behind such phenomenon doesn’t seems true. Groundwater depletion may play important role, but it is not the only cause behind the splitting of lands. Fissures often make their first appearance as a narrow crack in the surface which was not reported from these places earlier.

If it has been true then most parts of the states of North India especially Bihar, Jharkhand, Chattisgarh etc. must have developed cracks on the earth, which fortunately is not here, neither it was reported earlier in the past.

Jharkhand State which faces acute groundwater shortage during summer season never faced such phenomenon of land splitting.

The scientists also pointed out that the areas where cracks in the earth’s crust have appeared were closer to the rivers and have sandy soil. Rampant mining of sand could also be a reason for the cracks. This theory also doesn’t satisfy because if rampant mining is one of the cause then cracks would have covered almost all parts of the India where river sand mining for construction purpose is very common.

There are difference in opinion. According to US based geologist, land breaches reported in the Indo-Gangetic belt could be due to the motion of a massive granite body underneath. Other geologists say there are two massive underground rock mountains for many kilometers along the banks of the Ganga river which are striking against each other and which might prove dangerous.

From last two years the most stable zone of Jharkhand is experiencing mild tremors in frequent interval which is not normal. We just can not jump into any conclusion by only experiencing such tremors but it is also true that something unusual is happening beneath the earth crust.

Does this fissures is something to do with movements of Indian subcontinent towards Eurasia?

What ever may be the causes but it is clear that in future we are going to see more of such types of land depletion.