eChapters

Abstract

A field experiment was conducted in an aericendoaquept (pH, 6.67; organic carbon,  CEC,) to study the relative efficiency of different organic manures on the changes in some selected soil properties growing rape (cv. B-9) in a randomised block design replicated thrice using different combinations of organic and inorganic chemical fertilizers (T1- NPK 100%, T2- Compost 100%, T3- Compost 50% + NPK 50%, T4- Vermicompost 100%, T5- Vermicompost 50% + NPK 50%, T6- FYM 100% and T7- FYM 50% + NPK 50%). However, the objectives of the study was to assess the relative efficiency of organic manures with respect to availability of nutrients in relation to yield of rape affected by combined application of organic manures and chemical fertilizers. The results show that the amount of available N, organic carbon content, CEC and K contents were found highest in the treatment T5 where Vermicompost 50% + NPK 50% was applied combinedly.

Appendix-'F'    :    Chemical and Industrial Disaster Mitigation
    
Appendix-'G'    :    Emergency Procedure for Handling Chemical Disasters
    
Case Study    :    Bhopal Gas Tragedy 1984

Acetic acid            
    

Molecular weight    60.05        
    Melting point (^ºC)    17        
    Boiling point (^ºC)    118        
    Flash point (^ºC)    40        
    Auto-ignition point (^ºC)    426        
    Specific gravity at 20^ºC    1.05        
    Molarity of the concentrated acid (M)    17.4    
    1 M solution    57.5 ml concentrated acid per litre

INTRODUCTION

Prunus avium, commonly called wild cherry, sweet cherry is a species of cherry, a flowering plant in the rose family Rosaceae. Cherry is the fruit of many plants of the genus Prunus, and is a fleshy drupe (stone fruit) and packed with healthy nutrients and excellent antioxidants. Cherries are mostly eaten as dessert fruit or more conveniently in the brined, frozen or canned state. The cherry fruits of commerce usually are obtained from a limited number of species such as cultivars of the sweet cherry, Prunus avium. The name 'cherry' also refers to the cherry tree, and is sometimes applied to almonds and visually similar flowering trees in the genus Prunus, as in "ornamental cherry", "cherry blossom", etc. Wild cherry may refer to any of the cherry species growing outside of cultivation, although Prunus avium is often referred to specifically by the name "wild cherry" in the British Isles. Basically, cherries are native to Europe and Asia regions. De Candole reported that the cherry first grew wild in northern Persia and the Russian provinces south of the Caucasus. From there, it spread rapidly because they are attractive to birds; hence the name Prunus avium L. or bird cherry.

1.    Introduction
    
2.    Resources
    2.1    Crustacea
    2.2    Zooplankton
    2.3     Mollusca
    2.4     Insecta
    2.5     Thallophyta
    
3.    Biosynthesis
    
4.    Structure
    
5.    Detection and Estimation of Chitosan
    
6.    Specification of Chitin and Chitosan
    
7.    Economics of Chitin Recovery and Production
    
8.    Social and Economic Value of Chitosan
    
9.    Production of  Chitosan from Chitin
    
10.    Production of Glucosamine Hydrochloride
    
11.    Recent Advances in Applications of Chitin and Chitosan
    11.1    Applications of chitin, chitosan and glucosamine hydrochloride
    
12.    Advantages of Chitosan
    12.1    Cholesterol and overweight lowering
    12.2    Cholesterol lowering in Human
    12.3    Osteoarthritis prevention and Treatment
    12.4    Carrier for nasal application of drugs
    
13.    Conclusion
    
References and Further Reading

Chromosome number and nuclear DNA amount are important biodiversity characters together provide a very powerful method for determining evolutionary relationships. Furthermore provide an estimate of relatedness between species that in turn suggest reasons underlying the success or failure of crosses, even for interploidy hybridization. It is expected that species that are cytogenetically most similar will be easiest to hybridize and produce viable interspecific offspring (Thomas, 1993). Hence, it is important to study karyotypes and other characters of the genome of the species involved in a breeding programme.

According to Jackson (1971) and Stebbins (1950) the karyotype is the phenotypic appearance of the somatic chromosomes in contrast to their genic content.

INTRODUCTION
 
Citrus is the most economically important fruit crops widely grown in developed and developing countries of the world and is one of the main sources of vitamin C. There is also an increasing demand of “high quality fresh citrus” driven by World Health Organization recommendations. Citrus fruits contain the largest number of carotenoids found in any fruit and extensive array of secondary compounds with pivotal nutritional properties such as vitamin E, provitamin A, flavonoids, limonoids, polysaccharides, lignin, fiber, phenolic compounds, essential oils etc. These substances greatly contribute to the supply of anticancer agents and other nutraceutical compounds with anti-oxidant, inflammatory, cholesterol and allergic activities, all of them are essential to prevent cardiovascular and degenerative diseases, thrombosis, cancer, atherosclerosis and obesity. In spite of these beneficial traits there is still a major need to improve fruit quality to meet current consumer’s demand.

Introduction

Rainfed agro-ecosystems occupy a considerable place in Indian agriculture, covering 80 M ha in arid, semi-arid and sub-humid climatic zones; constituting nearly 57% of the net cultivated area. Rainfed areas contribute almost 100% of forest products, 84-87% of coarse-grain cereals and pulses, 80% of horticulture, 77% of oilseeds, 60% of cotton and 50% of fine cereals including rice, wheat, maize, sorghum etc (Srinivasarao et al., 2010; 2011). Rainfed regions support 60% of livestock, 40% of human population and contribute 40% of food grains and several special-attribute commodities such as seed spices, dyes, herbs, gums, etc. (Srinivasarao et al., 2011). It is estimated that even after achieving the full irrigation potential, barring for successful completion of river linking project, nearly 45 to 50% of the total cultivated area will remain dependent on rain. Undoubtedly, the rainfed agriculture would continue to occupy a prominent place in Indian agriculture for a long time to come (Venkateswarlu et al., 2011). Despite the progress made so far, rainfed agriculture in India encounters multiple risks and constraints relating to biophysical and socio-economic issues. Agricultural productivity in rainfed areas continues to remain low and unstable due to weather aberrations, nutrient disorder and poor socio-economic status of farmers.

Recent increase in extreme climate events threatens disruptive impacts on both animal and agriculture (Battisti and Naylor, 2009). Climate change is a global phenomenon, but its negative impacts are more severely felt by the poor people in developing countries. Moreover, rural poor communities rely greatly for their survival on animal and agriculture which belong to the most climate-sensitive economic sectors. Climate change is expected to intensify existing problems and create new combinations of risks. The incidences of droughts, snow-storms and blizzard like events have increased rapidly. The situation has further worsened due to factors such as widespread poverty, over dependence on rain-fed agriculture, inequitable land distribution, limited access to capital and technology, inadequate infrastructure, long term weather forecasts and inadequate research and extension. The impact of climate change is expected to heighten the vulnerability of animal systems and reinforce existing factors that are affecting animal production systems in many parts of the world.

The extreme weather events of the present day and the expected future climate scenarios at global and regional scales have been attributed to the changes in the atmospheric chemical composition and the massive amounts of greenhouse gases (GHGs) emitted by humans since the industrial revolution, bringing about the global warming and resulting in Climate Change. Further, the natural disasters like flash floods are attributed to the highly conspicuous human interventions with nature – the earth and its atmosphere. The parody of the situation is that, while the GHGs sourcing countries are mainly the developed ones, the sink of the result are the agrarian-dominated and eco-sensitive economies of the tropics. Invariably, tropical regions are to be affected the most, because, on the one hand the general circulation of the atmosphere directly and naturally causes divergence of the polluted air from extra tropical regions towards tropics, while on the other, the industrialization within the tropical regions too would affect the local atmosphere. Karnataka State, being located well within the tropics, can be truly impacted by the climate change caused by anthropogenic sources and it is demarcated into 10 agroclimatic zones (Fig. 9.1) based on crops, soils and climate. Climate experts have warned that Karnataka is likely to be more vulnerable to climate change than other states in India.

The State of Kerala has witnessed an unprecedented and unusual flood which devastated the entire State during August 2018 after the notorious 1924 flood, popularly known as the flood of 1099. Heavy rainfall from 14 to18 August 2018 led to flash floods across the State. This was aggravated by the dam opening and subsequent water level in the downstream of the rivers. 33 dams were opened across the State. This has caused the river water to flow into the inland areas. Rivers overflowed and inundated the river side villages and towns. It was reported that the water levels at many places were of the order of 20 feet. Landslides were the major threat that claimed many human lives. A chain of mud slip/land slide events took place during the heavy rainfall period at the time of flood across the mid and high lands of the State, which are ecologically sensitive areas. Even before the heavy rainfall events started on 14th August, 2018 there were major rainfall events on August 8thand 9th. On 9thAugust 2018, Nilambur (Malappuram District) recorded extremely heavy rainfall of 400 mm which is a record rainfall in 24 hours as far as the State is concerned.

The State of Andhra Pradesh in the present form came into being on June 2, 2014 as a result of the Andhra Pradesh Reorganization Act. The state has 13 districts out of which nine are along the coast of Bay of Bengal and four are land locked in the southern part. A part of Khammam district, which is now in the Telangana state, was also added to the East and West Godavari districts of the State of Andhra Pradesh. The existing data for these two districts do not include this part and this fact is to be borne in mind. The state has a geographical area of 1.602 lakh km2 with a population of 49.83 million. The state in the current form is more agrarian compared to the undivided state as about 62 per cent of population depends on agriculture as a source of livelihood. Yet, the contribution of agriculture to the state’s gross domestic product is only 17 per cent. Though the state is known as ‘rice bowl of India’, not all is well with agriculture in the state. Some parts, especially the coastal districts, are prone to incidence of cyclones and floods while some other districts, Rayalaseema districts, are chronically drought-prone. 

The Inter-governmental Panel on Climate Change  has confirmed that change in climate system is gradually leaving a strong impact. Observations undoubtedly show that there is increasein global temperatures, wide spread melting of snow and ice, and rising global mean sea level. Global climate has shown warming of 0.89 [0.69 to 1.08] °C over the period 1901–2012 which is mainly attributed to anthropogenic activities. Scientific findings indicate that warming is more pronounced than expected and the impact would be particularly severe in the tropical areas, which mainly consist of developing countries, including India (Shukla, 2016). Thus, climate change is a great challenge which is continuously being faced by the sustainable economic growth of the India. Climate sensitive sectors like agriculture, forestry, hydrology oriented sectors faces major threat due to projected changes in climate. India Meteorological Department (IMD) in 2012 reportedincreasing temperature trends during last 112 years and increase in heavy rainfall events and decrease in low and medium rainfall events over India.

Climate change has become a global threat as its impact is evident on the Earth. In the coming decades,the severity of climate change is expected to aggravate the ecosystem. Due to its vulnerable ecosystem and geographical location, the North eastern region (NER)of India that is home to about 40 million people is considered as one of the most climate sensitive areas in the country. The NER is among India’s least developed region andscarce information is available on the impact of climate change in this region. However, initial scientific research and field observations confirm that the region is suffering from the impacts of climate change already. The region comprising 0.26 million km2area occupying 8% of nation’s territoryconsists of the states of Assam, Arunachal Pradesh, Manipur, Meghalaya, Mizoram, Nagaland, Tripura and Sikkim. These states consist of a part of the east Himalayan region, which extends eastwards from Arunachal Pradesh to the Darjeeling hills of West Bengal. The entire region is a part of Indo-Burma and Himalayan hotspots i.e. characterized by rich biodiversity, heavy precipitation and high seismicity.

Agriculture is very intensely influenced by weather and climate. While farmers are often compliant in managing weather and annual variability, there is however a high degree of adaptation to the local climate. This may be in the form of conventional infrastructure, native agricultural practices or personal experience. Climate change an in this way be relied upon to affect the agriculture, possibly threatening established characteristics of farming systems and provide chances for improvements. The role of climate change in influencing human activities and the natural environment is all around acknowledged. This may go from an extreme event enduring just a couple of hours (i.e. hurricane, thunderstorm and showers) through to the multi-year dry spells (Maracchi et al., 2005). Increase in concentration of greenhouse gases in the atmosphere further contribute to climate change. This results in a strong impact on human activities and natural environments. Essential areas, for example agriculture and forestry, will be more susceptible than auxiliary and tertiary segments, for example manufacturing and retailing (Parry et al., 1998).

Global warming is the biggest long term threat to life on earth. Rise in temperature may drive thousands of species to extinction, trigger more frequent floods and droughts and sink low lying islands and coastal areas by rising sea levels. It is the result of rising atmospheric content of CO₂ mainly owing to burning of hydrocarbons or fossil fuels like as petrol and diesel. Destruction of forests and their degradation too contribute to rise in carbon dioxide levels. The IPCC (2006) projected the rate of warming for the 21st century to be between 0.8 and 4.4^ºC at various stabilized CO₂ levels in atmosphere and it is most likely to be 3°C by the end of this century. It could cost global economy almost $7 trillion by 2050, is equivalent to a 20% fall in growth if no action is taken on greenhouse gas emissions. If action is taken, it will cost only $350 billion due to climate change already taken place, just 1% of the global GDP. The winter 2007 was the warmest and recorded 0.85^ºC above average of 12oC and the previous highest was 0.71^ºC, which occurred in 2002 in Northern Hemisphere. The entire Europe Union recorded the warm winter, having more than 2^ºC above average. New York experienced the highest temperature of 21.7^ºC on a day in January, 2007 and the second highest was recorded as 17.2^ºC in 1950. The year 2007 was the warmest winter in the NHS. However, floods and excess rains were also noticed due to hurricanes and tropical storms worldwide in 2007. The year 2010 was the warmest year in India, followed by 2009. It was the second warmest year globally after 1998. It was also one of the wettest years globally in recent years and it was a landmark in annals of climatology.

Bihar’s economy is highly dominated by agriculture and allied sectors. Around 85 to 90 percent of the population still lives in rural areas, where agriculture along with animal husbandry, is the main source of their livelihood. In Bihar, the gross and net sown area is estimated at 8.26 and 5.64 million hectares, respectively. Nearly 60 per cent area under cultivation in the state is rainfed (Anon, 2008). The region comes under sub-humid subtropical monsoon climate. Most of the annual rainfall (almost 85 per cent) received from south-west monsoon, occurs during June to September (Sattar, 2010). There are three crop growing seasons in the state commonly known as kharif, rabi and zaid. The important kharif season crops, which are planted in May-June and harvested in September–October, are rice, maize, sesame, sorghum and bajra. Pigeon pea is an important long duration pulse crop sown during kharif season as sole crop or intercropped with maize. The important rabi crops which are sown in October–November and harvested in February–March are wheat, rabi maize, potato, chickpea, lentil, rapeseed, mustard, barley.

Introduction

Climate is a measure of the average pattern of variation in temperature, humidity, atmospheric pressure, wind, precipitation and other meteorological variables in a given region over long period of time. Climatic change refers to the shifts in the mean states of the climate or in all its variability, persisting for an extended period (decade or longer). The expected climatic change includes an increase in average temperature, an increase in CO₂ concentration and varied rainfall regimes due to increased ultra violet-B radiation. Fossil fuel burning and deforestation have emerged as principal anthropogenic sources of rising atmospheric CO₂ and other greenhouse gases and consequent global warming and climatic change.

3.1    Factors Contributing to Climate Change
    3.1.1    Natural Causes to Climate Change
    3.1.2    Human Causes to Climate Change
    
3.2    Climatic Trends
    3.2.1    Global level
    3.2.2    National level
    
3.3    Climate Projections
    3.3.1    Global level Projections on Future Changes in Climate
    3.3.2    Climate Projections at the National level
    3.3.3    Climate Projections at the Regional level
    3.3.4    Projections of Extremes in Rainfall and Temperature
    
3.4    Consequences of Climate Change on Droughts and Agriculture
    3.4.1    Impact of Climate Change on Agriculture in some States of India
    
References