eChapters

Flood diversion redirects part or all of an excessive flow away from a vulnerable river reach, settlement, or agricultural area. Water may be conveyed through diversion channels, floodways, canals, tunnels, spillways, or natural depressions and discharged into another river, reservoir, wetland, or safe storage area. A diversion scheme must have sufficient capacity and a dependable control structure while avoiding unacceptable flooding, erosion, sediment deposition, or environmental damage elsewhere. This chapter explains the purpose, principles, and methods of flood diversion. It covers site selection, diversion routes, hydraulic and structural components, design discharge, operational requirements, advantages, limitations, maintenance needs, and the role of diversions within integrated basin-level flood-control planning.

Flood estimation determines the probable magnitude and frequency of flood events for designing hydraulic structures and managing flood risk. Intense rainfall over a catchment generates excess water after interception, infiltration, evaporation, and depression storage have been satisfied. This runoff reaches the drainage system and may cause flooding when channel capacity is inadequate. Reliable estimates help engineers select suitable dimensions for dams, spillways, bridges, culverts, reservoirs, and other protective works. This chapter describes rainfall-based and streamflow-based estimation techniques, including the Rational and Cook’s methods, unit-hydrograph procedures, frequency distributions, Gumbel, log-normal and Log-Pearson Type III analyses, empirical formulae, flow-mass curves, and partial-duration series.

Hydrology examines the occurrence, circulation, distribution, and properties of water in the atmosphere and on Earth. Solar energy drives the hydrologic cycle through evaporation, condensation, precipitation, infiltration, runoff, and groundwater movement. Rainfall first satisfies interception, depression storage, evaporation, and infiltration before excess water begins flowing across the surface and into channels. When runoff entering a river exceeds its conveyance capacity, flooding may occur. This chapter explains clouds, precipitation measurement, rain-gauge networks, rainfall consistency, infiltration, runoff mechanisms, hydrographs, unit hydrographs, empirical runoff models, and stage-discharge relationships. These concepts provide the scientific foundation required for analysing floods and designing appropriate control measures.

Flood management is a continuing process of assessing flood risk and coordinating prevention, preparedness, response, recovery, and adaptation. Unlike flood control, which often emphasizes physical structures, integrated flood management accepts that floods cannot always be eliminated and seeks to balance their risks and beneficial functions. It protects life and property while considering river-basin development, environmental sustainability, social needs, and economic feasibility. This chapter explains flood-management concepts, objectives, purposes, and techniques. It discusses structural and non-structural actions, forecasting, watershed treatment, afforestation, rainwater harvesting, floodplain zoning, community preparedness, institutional responsibilities, interlinking proposals, and government programmes. Emphasis is placed on coordinated, basin-wide and risk-informed decision-making.

Flood routing predicts how a flood hydrograph changes as it passes through a river reach or reservoir. Storage, channel geometry, friction, inflow distribution, and outlet conditions generally reduce, delay, or otherwise modify the flood peak. Routing results help forecast downstream water levels, determine reservoir releases, design spillways and channels, issue warnings, and evaluate flood-control alternatives. This chapter introduces the continuity and storage principles underlying flood routing and distinguishes reservoir routing from channel routing. It discusses hydrologic and hydraulic approaches, including level-pool, Muskingum, and related techniques. Attention is also given to inflow and outflow hydrographs, routing coefficients, travel time, attenuation, data requirements, assumptions, calculations, and practical engineering applications.

A flood occurs when water exceeds the carrying capacity of a river, stream, drain, gully, or another natural or artificial channel and spreads over adjoining land. Its severity depends on water volume, depth, velocity, duration, timing, and the vulnerability of affected communities. Prolonged inundation can severely damage crops, property, infrastructure, water supplies, and human and animal life. Night-time floods may be particularly dangerous because warnings and evacuation become difficult. This chapter introduces flood occurrence and mechanisms, India’s and the world’s flood history, flood-prone regions, flood types and causes, major consequences, and the responsibilities of Indian flood-control and forecasting agencies.

Abstract

The anomalies observed in the reverine systems have been demonstrated to be the potential tool in deciphering the tectonically active zones. Such various drainage anomalies viz: radial drainages, anomalous compressed meanders, eyed drainage and the youthful floodplains observed in Annamali – Palani - Varushanad hill ranges of the Western Ghats of Tamil Nadu show that the N-S and NE-SW trending faults are tectonically active in the recent years.

Introduction
 
Arid western part of Rajasthan which contains the Indian segment of the Thar Desert, accounts for ~62% of the country’s hot arid area and is a region of low rainfall. Under such physico-climatic situation, fluvial processes function much less frequently and more episodically than the aeolian processes, but their impacts on landforms and society are large, as noticed on several occasions in arid regions. There is a distinct east-west gradient of rainfall and temperature in the region. Along the eastern margin bordering Aravallies, the mean annual rainfall is 500 mm while in the westernmost part at Jaisalmer, it is less than 150 mm. The rainfall is largely monsoon driven which brings 80 - 90 per cent of total rainfall received during the year. There is large inter-annual rainfall variability of rainfall which leads to climatic extremes of drought and floods of different magnitudes. For example on an average, the Thar Desert in India experiences flood-causing rainfall in 2-3 years in a decade, but a maximum of 5 flood causing rainfall years in a decade was recorded during the 1950s, 1970s and the 1990s (Rao et al. 2006).

Water vapour changes to the liquid water through condensation process. Condensation is the direct cause of the various forms of precipitation. It occurs as a result of changes in air volume, temperature, pressure or humidity. Water vapour can also be converted directly into the solid form through a process called sublimation. The latent heat expended in evaporation is liberated in the process of condensation. Four mechanisms may lead to condensation.

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.

Introduction
Chapter 11 delves into the intricate relationship between food sciences, human nutrition, and their collective impact on food security and global sustainability. The science of sustenance, encompassing food processing, preservation, quality, safety, and nutrition, is crucial for understanding how to feed a growing global population while minimizing environmental impact. The chapter begins by exploring food processing and preservation techniques, which are essential for extending the shelf life of food products and preventing food wastage. Traditional and modern food processing methods are discussed, highlighting their role in maintaining food quality and safety. The importance of food preservation is emphasized, along with emerging trends in food technology that address current and future challenges. Food quality and safety are vital components of the food sciences, ensuring that the food consumed by populations is not only nutritious but also free from harmful contaminants. The chapter examines the factors influencing food quality, including environmental conditions, handling practices, and storage methods. The principles of food safety are outlined, addressing the critical need for stringent measures to prevent foodborne illnesses. The challenges in maintaining food safety in the face of global trade and climate change are also discussed. Nutritional requirements and their role in human health are covered in the next section. This part of the chapter introduces fundamental concepts of nutrition, such as macronutrients, micronutrients, and dietary guidelines that promote health and well-being. The importance of balanced diets is underscored, with an emphasis on the need for proper dietary assessment methods to ensure adequate nutrient intake. The concept of food security is then explored, considering the various factors that influence the availability, accessibility, and affordability of food. The chapter discusses strategies for enhancing food security, including improving agricultural practices, reducing food waste, and addressing socio-economic inequalities. The integration of food sciences and human nutrition is presented as a critical approach to achieving sustainable food security. The chapter also examines the impact of food sciences and human nutrition on global warming. Food production, as a significant source of greenhouse gas emissions, is analyzed with respect to its environmental footprint. Strategies for efficient resource utilization, policy advocacy, and research innovation are

Hydrometeorology forecasting is limited to forecasting of occurrence of rainfall to a greater extent. Although several countries all over the world have developed and established hydrometorological forecasting with focus on occurrence of floods and droughts, still there is very limited success. Floods are associated with occurrence of continuous heavy rainfall due to movement of low-pressure systems like cyclones and depression overflow into rivers, reservoirs and breaching of bunds. In countries like India, the floods occur on the average in 70 lakh hectors of area and the economic loss due to floods and expenditure on relief operations mounting year after year besides loss of life. Foods occur at all of a sudden leaving little time for planning mitigation or rescue operation. Flood forecasting in based on impact assessment of heavy rainfall assessments to identify the exact area that is likely to be affected. It requires more intensive research. Forecasting of droughts is still an area of serious concern. There is need to strengthen regional capabilities to develop forecasting techniques for occurrence of flood and droughts through proper analysis of historical data in conjunction with meteorological forecasts and remote sensing data. Though flood alerts are issued, the identification of exact area and the extent to which flood impacts are not very clear most of the times heavy rainfall warnings are not just sufficient until and unless the vulnerable areas can be clearly specified. The medium range forecasting will be extremely useful for issuing flood alerts.
14.1. Forecasting Droughts
Long range forecasting of seasonal rainfall can indicate the possibility of receiving excess or deficit rainfall over larger regions. In India, there is considerable progress in development of long range forecast of Southwest monsoon rainfall. This forecast also indicating the regions which may get surplus or deficit rainfall and for indifferent parts of a given region as well. However, there is serious dearth of local expertise to further analyse and interpret the long-range forecast for a given area on the basis of local climate data. The advantages of reliable long-range forecast are still unexpected. Almost one fifth of the area in India gets affected by draught most of the years. The drought affects are more severe in arid and semi arid regions. Prediction of occurrence of drought and its intensity, period of occurrence and the areas to be affected by drought is very important. During recent years, there is considerable increase in the occurrence of droughts due to climate change which is attributed mainly to atmospheric pollution. The physics of the pollution is consistent and not the policies support in handling hydrometerological disasters. There are instances where in flood and droughts occurred in the same

This chapter introduces the biological and physiological foundations of forest ecosystems, focusing on the structure, growth, development, adaptation, and survival of trees. It examines tree growth and development, photosynthesis, respiration, water transport, nutrient uptake, and plant responses to environmental stresses. The chapter also explores forest biodiversity, forest–atmosphere interactions, forest ecology, microbiology, entomology, and pathology. Particular attention is given to physiological, morphological, and anatomical responses of woody plants to drought, flooding, temperature extremes, salinity, and other abiotic stresses. These concepts provide a scientific basis for understanding tree health, forest productivity, adaptation, conservation, and sustainable forest management.

Forest microclimate is the climate within a forest in contrast to a nearby open area created by a clearing or pasture. A robust observation is that less sunlight reaches the ground in a forest than in open areas, but this depends on the size of the clearing, the height of trees surrounding the clearing, and the location in the clearing (relative to the edge) where measurements are obtained. Daytime temperature is generally lower in forest than in open areas, with greatest differences during the growing season; but this, too, is subject to edge effects and whether the canopy is sparse or dense. Wind near the ground is less than in exposed areas or above the canopy. Another point is that there are various microclimates within a forest canopy. The environment of the forest overstory differs from that of the understory, and this has important consequences for species conservation and protection from climate change. The forest microclimate has important implications for habitat and biodiversity conservation and may act to buffer forest understory organisms from the severity of climate change. Forest microclimates differ not only in contrast with open land, but also vertically with position in the canopy (Fig. 8.1).

This chapter introduces the principles and practices involved in the collection, processing, evaluation, storage, and management of forest seeds. It examines forest seed biology and variability, seed quality and viability assessment, seed dormancy, and methods used to overcome dormancy. The chapter also addresses seed handling, storage, pest management, certification, and the integration of seed technology with genetic improvement programmes. By connecting seed quality with successful regeneration and tree improvement, the chapter provides a foundation for producing healthy and genetically suitable planting material for forestry and conservation programmes.

Abstract

It is evident from the previous studies that, in the crystalline terrain, the Fractures / lineaments act as master conduits for the groundwater movements and also act as favorable loci for groundwater storage. Because of this, the mapping of fracture patterns has become very popular among geoscientists. However, after witnessing failures and the fractures turned out to be water barren at many instances, geoscientists have started concentrating more on understanding the origin and the morphology of the fractures for precise groundwater targeting. In this context, a study has been conducted in parts of Western Ghats in Madurai, Dindigul and Theni districts of Tamil Nadu, South India, using remote sensing and geographic information system (GIS). In the said study, the maxima zones of transmissivity were studied in relation to fractures systems, which are normally reflected as lineaments in satellite images in the area. This study in general indicates that the transmissivity is controlled by the fractures, which are interestingly the active faults of the Quaternary period in the area.

1. Introduction
The term “plastic” is derived from the Greek word “Plasticos" whichmeans to be capable of molding into various sizes and shapes. Daily usedsynthetic plastics are categorized based on their physical and chemicalproperties, such as thermoplastic and thermosetting. (i) Thermoplastics: Astheir names suggest, thermoplastic polymers melt and turn into a plastic orrubbery state when exposed to heat. They have various numbers of polymericchains and are the most widely used plastics in day-to-day life. Examples ofthermoplastics are Polystyrene(PS), Polyvinylchloride (PVC), Polypropylene(PP), Polyethylene Terephthalate (PET), Polyethylene (PE) etc. (Massy,2017), (Sharma et al., 2017). (ii) Thermosetting polymers: As the namesuggests, they set or harden permanently when heated (Massy, 2017). Due totheirstrong crosslinked structure, they are non-recyclable polymers. Examplesinclude Polyurethanes(PUR), Phenol formaldehyde, Melamine formaldehyde,and Polyester Resin (PR) (Sharma et al., 2017). Different polymers and theirapplications are illustrated in Fig. 1.

ABSTRACT

This paper demonstrates the ability of FTIR for analyzing compositional structures of naturally occurring crystals namely gypsum and calcite. As these two crystals occur in a wide variety of geological environments and are susceptible to compositional and structural changes influenced by pressure, temperature, crystallization fluids and so many other factors, these are extensively studied by geoscientists for interpretation of paleoenvironment, modeling diagenesis of sediments and deducing sediment maturity for hydrocarbon exploration, study of these two crystals is important. Naturally occurring gypsum and calcite crystals collected from Cretaceous marine deposits of Ariyalur area were chosen for the present study as extensive occurrences of hydrocarbons are reported from offshore region of Cauvery basin and exploratory works are going on in the onland region. It is observed that the vibrational spectra of studied crystals show specific patterns in terms of stretching patterns of O-H, C-O, C=O, SO₄ and CO₂. As FTIR offers fast, cost-effective, non-destructive method of analyses of natural compounds, as it is proven useful, it can be utilized extensively in academic research and commercial exploration activities by geoscientists.

Keywords : Spectral characterization, calcite, gypsum, diagenesis, paleoclimate, hydrocarbon exploration.

Introduction

Geostatistics is a branch of statistics that deals with the analysis and modelling of geo-referenced data. Its main aims are to quantify spatial variability and to create maps from point observations. Of course there is much more to geostatistics than just that and indeed some of the other uses of geostatistics are addressed in this chapter too, but the emphasis is on the assessment of spatial variability and geostatistical interpolation.

The first step of geostatistical interpolation is to quantify the spatial correlation structure of the variable of interest. This can be done by examining the observations and how these vary in space. Next spatial interpolation makes use of the quantified spatial correlation to derive optimal predictions at unobserved locations and create a map. The interpolation error is quantified as well, which helps to design optimal spatial sampling schemes that balance data collection costs and map accuracy. All this will be explained in this chapter, but in order to do so we first need to explain the statistical theory that underlies geostatistical interpolation followed by representation of the spatial correlation structure, the basics of geostatistical interpolation (‘kriging’), kriging extensions and spatial stochastic simulation.