eChapters

Wet sieving procedure separates soil into different size aggregates. However, for comparing the aggregate size distribution among management treatments and soil types, it is convenient to use indices. Mean weight diameter (MWD) and water stable aggregate percentage are some of the common indices used in aggregate stability studies.

Mean Weight Diameter (MWD)

This index was proposed by Van Bavel (1949) and is being used widely. The entire soil sample is passed through an 8 mm sieve prior to analysis and is subjected to wet sieving procedure as described before. The parameter which Van Bavel (1949) called the MWD is equal to the sum of the product of (a) the mean diameter (d ) of each size fraction and (b) the proportion of the total sample weight (w ) occurring in the corresponding size fraction. The summation is carried out over all ‘n’ size fraction including the one that passes through the finest sieve.

Sulphur (S) occurs in different forms in soil viz., sulphites, sulphates , sulphides and in organic compounds. Plants absorb S in the form of sulphate(SO₄ ^2-) . The organic forms of S compounds become assimilable, especially following microbiological transformation into SO₄ ^2-. The mineralization of organic sulphur in a soil depends primarily upon the N:S ratio and any SO₄ ^2- formed may be fixed against extraction, particularly if much Fe and Ba is present or if soil is very acidic.

Principle

Beside some amount in the soil solution, available sulphur in mineral soils occurs mainly as adsorbed SO₄ ^2- ions. Both CaCl₂ and phosphate solutions (as monocalcium phosphate) are generally used for replacement of the adsorbed SO₄ ^2- ions. Use of Ca salts have a distinct advantage over those of Na or Na, as Ca prevents deflocculating in heavy textured soils and leads to easy filtration. SO₄ ^2- in the extract can be estimated turbid metrically using a spectrophotometer. Sulphur in the extract can also be measured by colorimetric method using barium chromate but the turbimertic method given below is mainly used in the soil testing laboratories.

Calcium (Ca) and magnesium (Mg) are the two most abundant alkaline earth cations in soils. They both occur as soluble ions in soil solution, exchangeable, non-exchangeable and in organic material. Soils from arid regions are richer in Ca (1-2% CaO), while those from humid zones have a low content (0.01-0.02% CaO). On the other hand exchangeable Mg is found in very small quantities in calcareous soils. Sometimes, in acid soils, Mg²⁺ represents the largest quantity of the sum of exchangeable bases.

Principle

The method is based on the principle that calcium, magnesium and a number of other cations form stable complexes with versenate (ethylendiaminetetraacetic acid disodium salt, EDTA) at different pH. A known volume of standard calcium solution is titrated with standard 0.01N EDTA solution using murexide (ammonium purpurate) indicator in the presence of NaOH solution.

The end point is a change of color from orange red to purple at pH 12 when the whole of Ca forms a complex with EDTA. Calcium plus Mg are also present in the solution and can be titrated with 0.01N EDTA using buffer solution and a few drops Eriochrome Black T indicator. The end point is a change of color from red to blue at pH 10. Beyond pH 10, magnesium is not bound strongly to Erichrome Black-T indicator to give a distinct end point.

Introduction
Oil palm (Elaeis guineensis Jacq.), a tropical perennial tree native to West Africa, is the most productive oilseed crop for biodiesel, yielding up to 5 tons of oil per hectare (Mekhilef et al., 2011). Indonesia and Malaysia are the largest global producers, accounting for over 85% of the world’s palm oil (Atabani et al., 2012). Palm oil is extracted from the fruit of the oil palm and is widely used in both food and fuel applications. However, its cultivation has raised environmental concerns, including deforestation, habitat loss, and carbon emissions (Gui et al., 2008). Efforts are being made to promote sustainable palm oil production to mitigate these impacts (Mekhilef et al., 2011). Deforestation, habitat loss, and carbon emissions are only a few of the serious environmental issues brought on by its cultivation (Fargione et al., 2008). Oil palm plantation growth has been connected to a decline in biodiversity, especially in tropical rainforests that are home to endangered species like Sumatran tigers and orangutans (Fitzherbert et al., 2008). According to Carlson et al. (2013), the conversion of peatlands for the production of oil palm contributes to climate change by increasing greenhouse gas emissions.
History of Oil Palm as Biodiesel Feedstock
Oil palm has been used for cooking and lighting for thousands of years in Africa and Southeast Asia (Obahiagbon, 2012). Research into its use as a biodiesel feedstock began in the 1980s, with Malaysia pioneering biodiesel development (Zainal et al.,2017).
• 1982: The Palm Oil Research Institute of Malaysia (PORIM) successfully tested palm oil-based biodiesel in diesel engines (Yusoff, 2006).
• Early 2000s: Commercial production expanded in Indonesia and Malaysia, driven by government policies and renewable fuel demand (Mekhilef, 2011).
• Sustainability challenges have led to the establishment of certification schemes such as the Roundtable on Sustainable Palm Oil (RSPO) (Ruysschaert & Salles, 2014).

Estimation of plant available phosphorus content in soil has been attempted using several extractants. However, Bray’s reagent and Olsen’s reagent are the two common extractants used in India. Bray’s reagent (0.03 N NH₄F and N HCl) is used for acid soils, where, the fluoride ion complexes with Fe and Al in soil and thus releases the bound P. The Olsen’s reagent (0.5 M NaHCO₃) is used for neutral-alkaline soils.

Boron occurs as anion in soils and isrequired by plants in very small quantity. Water soluble B makes the estimate of its availability to plants. Total boron in soils varies from 20 to 200 mg kg^-1 and available (water soluble) boron in soils ranges from 0.03 to 12 mg kg^-1 respectively. The threshold value ranging from 0.1 to 0.5 mg kg^-1 (water soluble B) depends upon the soil type, crops, and other factors, below which the response to applied boron may be expected. Its availability is affected by soil pH as under:

Biogas typically comprises 60-65% methane (CH4), 35-40% carbon dioxide (CO2), and 0.5-1.0% hydrogen sulfide (H2S), along with traces of water vapor. It is approximately 20% lighter than air and has an ignition temperature of 650-750°C. The calorific value of raw biogas is around 20 MJ/m³ (4,713 kcal/m³).
Unlike Liquefied Petroleum Gas (LPG), biogas cannot be converted into a liquid state under normal temperature and pressure. The critical temperature for methane liquefaction is -82.1°C at a pressure of 4.71 MPa, making liquefaction complex and energy-intensive. However, biogas can be upgraded by removing impurities like CO2 and H2S and compressing it into cylinders for use in three-wheelers, cars, pickup vans, or stationary engines at remote locations.
Since Compressed Natural Gas (CNG) technology is already wellestablished, upgraded biogas (also called biomethane) which has similar composition and energy content can serve as a direct substitute for CNG in all its applications. The calorific value of upgraded biogas (with CO2 removed) increases to around 34 MJ/m³, compared to 20 MJ/m³ for raw biogas.
Techniques for Biogas Purification
To enrich biogas and increase its methane content, various purification methods are employed:
1. Water Scrubbing
This physical absorption process involves pressurizing biogas and feeding it into the bottom of a packed column, while water is introduced at the top. The CO2 and H2S dissolve into the water as it flows downward, while methane rises and is collected. The water used can

Environment in which crops are grown dictates their final yield. Of these environmental factors, climate and weather the uncontrolable factors, have maximum influence on crop productivity. Vagaries of weather subject a crop to different ecological situations from year to year leading to differential responses of crops to input resources. This situation limits the use of costly inputs for realizing optimum yield. While weather itself cannot modify, the hazardous weather can often be mitigated by agronomic management. Therefore, the primary requirement for initiating agronomic measures against weather hazards is foreknowledge of weather situation that is likely to develop in an area.

Abstract

During natural disasters, mostly panic and curiosity lead to greater causalities. But the tsunami is such a disaster which no one have witnessed during their life time nor heard of from their ancestors. On 26, December 2004, tsunami has struck all of a sudden many South Asian coasts including the east coast of Tamil Nadu and Andhra Pradesh causing greater devastation and causalities. This historical event has taught us many lessons and the paper deals with some aspects related to tsunami from the citizen’s view point.

Keywords: Natural calamities, Tsunami mechanisms, Mitigation strategies, Citizen’s perspective.

INTRODUCTION

The tsunami that ravaged the coasts of South India had left tell tale signs that affirm the need for early warning systems as well as well-planned mitigation measures for the benefit of the affected. Over the last 12 months, since the tsunami struck the east coast of India on 26 Dec. 2004, numerous seminars, discussions, programmes and project proposals have been deliberated on various aspects that deserve attention. Government agencies, self-help groups and non-governmental organizations (NGOs) have done commendable post-tsunami work. All sections of the society have responded both emotionally and rationally to the event in an unprecedented manner. In retrospect, to the informed citizen – one who has heard about the event, read about it and discussed it with others, though not have had the ‘experience’ of the natural disaster by himself / herself - what do all these mean ? the tragedy and its aftermath. This paper documents the issues that a citizen would like to ponder over so as to understand the various dimensions of the post-tsunami activities and draw a few lessons that the tragedy had taught us. The major issues pertain to (i) the mechanisms (ii) the coastal vulnerability and the need for assessment (iii) mitigation strategies (iv) media exposition (v) communication networking and (vi) educational facilitation.

Abstract

The paper deals with the roles played by the NGO’s in the relief and rescue phase of Dec, 2004 tsunami and the effective role played by NCRC -NGO Coordination and Research Centre - in the rehabilitation phase along Tamil Nadu coast by creating successful partnership with government and the public.

Keywords: The Role of NGO’s, Tsunami 2004, Relief and Rehabilitation, NGO Coordination Research Centre.

INTRODUCTION

The scale of the tsunami disaster was unprecedented and the response too was out of the ordinary. Tamil Nadu was the worst affected state in India with Nagapattinam district being the most affected with over 6000 lives lost, about 40,000 houses damaged or destroyed and 1.96 lakh people affected. Relief poured in from both government and non-governmental organizations, including the religious organizations, and the first few days witnessed heartwarming outpourings of help and support.

There were about 400 NGOs and an equal number of volunteers to help in the relief operations which included food, clothing, household utensils and bedding. With such a large scale of external support, mainly from organizations and people from outside Nagapattinam, it was not surprising that chaos and confusion marked the first few days of relief operations still. Based on the experience of some professionals experienced in disaster management, a coordination platform was created called the NGO Coordination Cell. This platform was managed by two NGOs, who had long standing field presence in Nagapattinam, viz., South Indian Federation of Fishermen Societies and SNEHA, with the mandate and support of the District Administration. The main role of this platform was to meet the field based requirements of all the relief camps with the resources and materials available with the NGOs and the Govt. The paper briefly deals with challenges faced by the NGO’s in relief and Rehabilitation of the historical Dec 2004, Tsunami.

Abstract

Subsequent to December 26^th 2004 historical Tsunami, The Government of India has conceived a master plan for setting up Tsunami Warning System (TWS) similar to Pacific Ocean Tsunami Warning System. Concurrently, the union Govt has also initiated scientific studies through Department of Science and Technology and the significant amongst these are the

• All India Co-ordinated Programme on Tsunami disaster and risk assessment using GIS technology and
• Bilateral programme with Norway to know the know – how and capacity building in the fields of Landslides and Tsunami

As a part of this bilateral mission, the authors visited institutions connected to Geohazards and Tsunami affected areas of Norway. The article briefly narrates the salient inferences on the Tsunami scenario and the related studies in Norway.

Keywords: Landslides triggered tsunamis, Norway

Introduction
Food Chains
Food chains are made up of organisms that eat and are devoured by one another as a means of transferring energy from the source in plants. “The transfer of energy from plants through a series of organisms with repeated eating and being eaten” is one definition of it.
A food chain is the movement of energy from producers at one trophic level to consumers at the next. In a food chain, energy moves only in one direction. An understanding of food chains can provide important insights into how ecosystems work.
• Grazing food chain
Grazing food chains and detritus food chains are the two main categories of food chains.
The food chain known as grazing begins with living green plants, moves through grazing herbivores, and ends with carnivores. Such a food chain places an immediate demand on ecosystems for solar radiation. From an energy perspective, these chains are very significant.

Atmospheric pressure is the force per unit area exerted on a surface by the weight of air above that surface in the atmosphere of earth. The gas molecules of the atmosphere are pulled towards the earth by the force of gravity and hence exert a force on earth surface. In most circumstances atmospheric pressure is closely approximated by the hydrostatic pressure caused by the weight of air above the measurement point. Atmospheric pressure inf luences other weather elements in a significant way. Small changes in air pressure may not be felt, but they are important for bringing a change in weather. Atmospheric pressure can be calculated as the summed weight of all gas molecules between a horizontal plane and top of the atmosphere and divided by the area of the plane. Low pressure areas have less atmospheric mass above their location, whereas high pressure areas have more atmospheric mass above their location.

FACTORS AFFECTING ATMOSPHERIC PRESSURE

Air pressure never remains constant. Air pressure is greatly influenced by air temperature, altitude, water vapour presence in the air, rotation of earth, etc. However, these factors are not independent of each other in affecting the atmospheric pressure.

Temperature: Hot air expands and exerts low pressure. Cold air contracts and exerts high pressure. Thus, increase in temperature decreases the air pressure. Places nearer to equator experience low pressure due to prevalence of high temperature. The air being cold and heavy throughout the year a high pressure belt is created in both polar regions.

Altitude: Pressure varies smoothly from the earth’s surface to the top of the mesosphere. The pressure depends on the density or mass of the air. The density of air depends on its temperature. The density of air decreases with increase in height so the pressure also decreases with increase in height. At low altitudes above the sea level, the pressure decreases by about 1.2 kPa for every 100 metres.

Water vapour: Water vapour content of air is low in cold areas than that in dry areas. Hence, moist air of high temperature in dry areas exerts less pressure compared to cold air.

Livestock population meet the protein requirement of humans in addition to meeting from plants. The food chain starts from fodder crops to animals and from animals to humans. In human physiology, digestion of plant protein is much easier than animal protein, but however the digestion depends on climate (temperate climate, sub-tropical climate, tropical climate etc.,) wherein human kind live. Similar to crops, there is strong interaction between livestock and meteorological weather elements (temperature, relative humidity, wind etc.). But detailed study has not been published elaborately in scientific journals in the past. The weather elements have greater influence on livestock productivity in terms of milk, meat, skin, wool etc., pest and disease infestation and their housing needs. In this chapter how weather elements influence shed management, pest and disease problem and animals’ productivity and are discussed. In majority of the Veterinary and Animal Science University in India, they have one division on animal climatology, wherein both research and extension aspects are being attended. However, in depth research is the need of the present decade, since little works have been done in the past on animal climatology.

Irrespective of weather elements, the heat stress due to the combination of temperature and relative humidity plays important role in affecting the productivity of animals. There is a range of thermal conditions within which animals are able to maintain a relatively stable body temperature by means of behavioral and physiological means. Heat stress results from the animal’s inability to dissipate sufficient heat to maintain homeothermy (Sejian et al., 2017). High ambient temperature, relative humidity and radiant energy compromise the ability of the animals to dissipate heat. As a result, there is an increase in body temperature, which in turn initiates compensatory and adaptive mechanisms to re-establish homeothermy and homeostasis. Homeostasis refers to the tendency to maintain a balanced or constant internal state that is optimal for functioning. Animals have a specific balanced or normal body temperature. When there is a problem with the internal functioning of animal body, this temperature may increase, signaling imbalance. As a result, body attempts to solve the problem and restore homeostasis for normal body temperature. These readjustments generally referred as adaptations and this is essential for survival of the animals.

Introduction

Environmental problems have come to the forefront as one of the most important issues in transport policy. For a number of pollutants the road transport sector is one of the most significant contributors to environmental pollution. Vehicular emissions have been identified as one of the major contributors in deteriorating air quality in the urban centers. The problem has further been compounded by the concentration of large number of vehicles and comparatively high motor vehicle/population ratios in these cities. Substantial SPM, RSPM CO₂ and No_x are emitted. The problem of air pollution has assumed serious proportion in some of the major metropolitan cities of India. Therefore, CPCB has 296 monitoring stations all over India covering major cities.

The air pollution situation in most of the cities is still far from satisfactory. In India the major air pollution reason is automotive smoke and smoke from industries. New channels are also publishing pollution levels in selected metropolitan cities. The most polluted city in Asia is Pune. The SPM and RSPM levels are displayed at various squares to create awareness among the masses.

Smaller cities like Nanded, Parbhani and Yavatmal are not covered under National Ambient Air Quality Monitoring (NAAQM) scheme of Central Pollution Control Board (CPCB). The National Ambient Air Quality Standards for suspended particulate matters (SPM) are based on gravimetric measurement. Standards for Respirable suspended particulate matters (RSPM) are also based on gravimetric measurement. The development in terms of number of vehicles and building construction has also reached at the doors of these cities and towns. Nanded city having population of 5.5 lakhs has total number of Auto rickshaws more than 5,000. In the present study, Nanded city has been selected to check particulate matters and gaseous pollutants. Since, the city is one of the important Pilgrimage and commercial centre.

Introduction
The lives of the local population are disrupted by large-scale projects such as dam construction, mining, highway construction, or the designation of a national park, and they are frequently forced to relocate to a new location. Relocating individuals is a significant challenge as it diminishes their capacity to survive solely on their customary natural resource base and intensifies psychological strain. 33 to 56 million people have been displaced by 54 projects in India over the past 50 years.
Resettlement and Rehabilitation of People
Major projects like dams, mines, expressways, and other industrialization-related projects, as well as some conservation strategies like the creation of national parks, can cause disruptions to people’s lives and force them to relocate to an alternate location. Relocating individuals from their birthplace is a grave concern as it diminishes their capacity to survive only on their customary natural resource base, so adding to their psychological strain. It is difficult for the displaced individuals to adjust to a new lifestyle in a new location. Due to the indirect effects of the Green Revolution—the building of thousands of dams since India’s independence—thousands of people havebeen displaced. These impoverished locals have essentially paid for the construction of the dams. Even if the government has set enough time to relocate these displaced individuals and offer them a sufficient package for rehabilitation, this rarely happens.

Introduction

Rice is known as the grain of life, and is synonymous with food for Asians. In addition to being a staple food and an integral part of social rites, rituals, and festivals in all Asian countries, it has a medicinal value too, which was clearly recognized by the medicine systems of the region. Ancient Ayurvedic treatises laud the Raktashali red rice as a nutritive food and medicine. The medicinal value of other rices such as Sashtika, Sali, and parched rice have been documented in the Charaka Samhita (c. 700 BC) and the Susruta Samhita (c. 400 BC), in the treatment of various ailments such as diarrhea, vomiting, fever, hemorrhage, chest pain, wounds, and burns.

According to late Dr. Richaria, the well known rice scientist, 4, 00,000 varieties of rice existed in India during the Vedic period. According to his estimates, even today 2, 00,000 varieties of rice exist in India - a truly phenomenal number. Farmers in every part of country have a deep knowledge of their own rice varieties, This has enabled them to harvest a crop even under the most severe stress situations. Traditional paddy varieties are location specific and has its own advantages viz. saline tolerant, drought tolerant, pest tolerant, used for specific purpose such as roofing material for houses etc.

4.1 Introduction

The energy census survey has become the basis for planning & implementation of the village development based on conventional and non conventional sources which are appropriate to the local needs. The continuous and widespread use of non commercial sources of energy in the rural area is resulting in the large scale destruction of the environment. While the rural people get non conventional fuels at almost zero private cost, the social cost for meeting their energy needs has been increasing over the year. Hence the non conventional fuels acquired a special significance in the energy context.

The rural energy problem is multi dimensional & needs to be tackled through a multi dimensional integrated approach which would include augmentation of energy supply resources, technology transfer for optimum & productive use of resources, R & D inputs in particular for developing low cost energy options for the rural poor, education & training for rural users, linkage with various rural development programmes including village & small scale industries programme and adequate institutional & financial support. The multi dimensional approach for making a village self sufficient in energy planning is illustrated in Fig.4.1.

The geologists of the Indian subcontinent have all along been of the opinion, that, the southern part of the Indian Peninsula is a stable shield area. But, the recently acquired IRS-1A image of June, 1988 vividly displays spectacular geomorphic anomalies suggesting that this part of the Indian subcontinent is prone to earth movements. In order to unearth more evidences on such earth movements / neotectonism in Tamil Nadu, the IRS-1A image of Coromandel coast of Tamil Nadu was analysed ( Fig. 1).

OBSERVATIONS

• The IRS-1A image conspicuously displays three contrasting morphotectonic domains in the study area marked by the western undissected Tertiary upland (Vallam upland), central highly dissected Tertiary upland (Pattukottai -Mannargudi upland) and the eastern Cauvery delta (Fig 1 and 2). These three domains are separated by two conspicuous N-S trending lineaments (E and F, Fig.1 and 2) namely the Tanjavur - Avadaiyarkovil lineament in the west and Kumbakonam -Muttupet lineament in the east.
• In addition, two more E-W trending lineaments (G and H, Fig.1 and 2) are also observed trifurcating the undissected Vallam upland into three blocks.
• Along these lineaments, especially the Tanjavur -Avadaiyarkovil and Kumbakonam -Muttupet lineaments, the rivers show conspicuous drainage anomalies in the form of drainage deflection, drainage compression etc., wherever they transect the lineaments.

    In recent years, the global demand for renewable and sustainable energy sources has led to increased interest in biogas production from agricultural residues and lignocellulosic biomass. Among these, paddy straw an abundant agricultural by-product—has gained attention as a potential substrate for anaerobic digestion and biofuel generation.
However, the biochemical conversion of paddy straw into biogas is limited by its complex lignocellulosic structure, which makes it resistant to microbial degradation. Therefore, pretreatment of biomass is a critical step to enhance its digestibility and improve the overall efficiency of biogas production.
Objective
The primary objective of pretreatment is to break down the structural and compositional barriers within lignocellulosic biomass that hinder microbial degradation and enzymatic hydrolysis. Specifically, pretreatment aims to:
1. Disrupt lignin structure and reduce cellulose crystallinity.
2. Increase surface area and porosity of the biomass for microbial access.
3. Improve enzymatic hydrolysis efficiency for higher sugar and methane yields.
4. Minimize sugar loss and avoid the formation of inhibitory byproducts.
5. Enhance biogas yield and the rate of biodegradation.
6. Achieve these improvements in a cost-effective and scalable manner