eChapters

Abstract

Ennore is an industrial region having many industries on chemicals, fertilizers, refineries etc., discharging their effluents into the Buckingham canal. Present study focuses on the impact of tsunami on water quality of Buckingham Canal segment found to the north of Chennai city, Tamil Nadu, India, in addition to the human interferences. Water samples were collected from surface and near bottom at five locations covering about 20km stretch of the Buckingham Canal during high tide on the spring tide day before (December 2004) and after (January 2005) the mega tsunami. Various water quality parameters measured were pH, Temperature, Salinity, Dissolved Oxygen, Suspended Particulate Matter, Nutrients and Chlorophyll. The maximum depth observed in the canal was 2.5m in December, whereas a shallow depth of less than 0.5m was recorded in January. The water quality analyses confirmed the incursion of saline water (upto 32ppt) into the Canal. Not much variations were observed in Dissolved Oxygen and pH. Because of the organic pollution in the canal, the water was rich in nutrients before tsunami, whereas due to the large quantity of seawater invasion, dilution had occurred after tsunami. High turbidity was observed in January 2005 indicating the tsunami induced disturbance and resuspension of the sediments from sea bed.

Keywords: Tsunami, Ennore, Tamil Nadu, Buckingham Canal.

1.1 Geomorphology

Geomorphology is the scientific study of the origin and evolution of topographic and bathymetric features created by physical or chemical processes operating at or near the earth's surface.

The surface of the earth is unstable and affected by a combination of surface and geologic processes that cause tectonic uplift and subsidence. Surface processes are mainly physical and chemical action of water, wind, ice, igneous activity and activities of living organisms on the surface of the earth. Upliftment of mountain ranges, the growth of volcanoes, isostatic changes in surface elevation and formation of deep sedimentary basins are categorized under Geological processes.

Main geomorphological processes occurring in nature are as follows:

1.1.1 Aeolian processes

Aeolian processes include activities of the winds, its ability to shape the surface of the earth. Wind acts as an effective agent of erosion, transportation and deposition materials, and large supply of fine, unconsolidated sediments. Aeolian processes are important in desert (arid) environments.

1.1.2 Fluvial processes

Moving water in a river channel, is able to mobilize sediment and transport it downstream. The rate of sediment transport depends on the availability of sediment itself and the discharge by river.

River originates from mountain with V shaped valley, which later increases in size, merging with other rivers. The network of rivers thus formed is known as drainage system. These systems show four general patterns viz. dendritic, radial, rectangular, and trellis etc. In the mature stage, the river form alluvial flood plains, meanders and ox-bow lakes. Finally when it merges to ocean, forms delta.

Abstract

The dating of fluvial landforms by archaeological, epigraphical, historical, thermo-luminescence, radiocarbon, etc. are of greater significance because it not only provides information on the date of origin of such fluvial landforms but also isostatic, eustatic, climatic histories of the Quaternary period. Hence, the Geoscientists have always been giving greater importance to the dating of the fluvial landforms. In India, the Cauvery is one such river studied for its migratory melodrama with the help of satellite data and inferred that the river Cauvery has earlier flowed along the Hogenekkal-Chennai tract (PCS-1-Palaeo Channel System-1) during 500 thousand to 3000 YBP (years Before Present), then migrated towards southerly and flowed along the present day paths of Thoppurar, Vaniyar and Ponnaiyar rivers (PCS-2) during 2700-2300 YBP and further migrated southerly and entered into Tiruchirappalli-Thanjavur plains after 2300 YBP and finally anticlockwisely migrated in different parts of the present day Cauvery delta and stabilized as river Coleroon during 2100-750 YBP. Such broad chronological history was brought out on the basis of archaeological, epigraphical, historical, literature and few radiocarbon dating. In the present study, more number of radiocarbon dating was done in various palaeochannels of river Cauvery which has over all coincided with above observations and further provided discrete information on (1) the southerly migration of river Cauvery from PCS-1 to PCS-2 after 8000 YBP, (2) tectonic arching and splitting up of channels in Chennai region during above period, (3) gradual younging nature of palaeochannels from PCS-1 of Chennai region to PCS-3 of Tiruchirappalli – Thanjavur region, etc.

ACID SOILS: Acid soils with pH below 6.5 are widespread. Main limitations of these acid soils are low pH, low CEC, low status of bases, especially Ca, Mg, and K along with toxicity of Al and Mn. Use of acidifying fertilizers aggravates this situation.

Forests are valuable renewable resources for humanity on Earth. The country’s forest cover has been estimated to comprise 19.39% of its entire geographical area. Forests consist primarily of trees that offer wood that can be transformed into solid, liquid, and gaseous fuels. Forests play a crucial role in regulating the Earth’s temperature by serving as carbon dioxide filters. They provide habitats and shelters for numerous species and also contribute to the visual beauty of the environment. Forests supply the necessary resources for a range of wood related industries, including pulp and paper, composite wood, rayon and other synthetic fibers, sporting goods, furniture, boat
construction, and matches. Timber plays a crucial role in the construction of buildings.Various products, such as bamboos, resins, gums, oils, fibers, medicines, katha, lac, shellac, etc., are derived from forests.
The country’s forest cover has been calculated to be 637,293 square kilometers, accounting for 19.39% of the country’s total geographic area. This falls short of the stipulated requirement, which is 30% of the entire land area. The geographic region is comprised of 11.48% dense forest, 7.76% open forest, and 0.15% mangrove. World Forest Day is observed on March 21st, while National Forest Day is celebrated on September 11th.

2.1 INTRODUCTION

GIS is a tool that can be used in varied disciplines ranging from civil engineering to business. Remote sensing data is often brought into GIS to have a complete data set in many natural resource application areas. Full capability of GIS is not used widely. Many a times people use GIS only for digitising maps and to do simple query on maps. But it can also be used in modeling, simulation and forecasting, only then one may regard GIS technology is utilised to its full potential. Some GIS softwares handle simple problems for location based services while other complex softwares posses advanced modules to do all types of spatial, network and 3D analysis. Integration of softwares used in natural resources study are being interfaced with GIS to create scenarios.

Remote sensing and GIS technology is useful in the following fields:

Introduction
The sun is the primary source of energy for all life on Earth. The primary energy source for the majority of ecosystems is limited to this one. Photosynthesis is performed by green plants, certain types of algae, and microorganisms. They utilize solar energy to fuel chemical reactions that combine basic inorganic components to create intricate organic chemicals. Elements undergo a cyclical process as they move through the different compartments of an ecosystem.
Photosynthesis is the process by which solar energy is captured and transformed into food in the form of chemical energy. Food comprises fundamental elements such as carbon, hydrogen, nitrogen, and other necessary elements, along with stored energy. The components present in the food undergo recycling. The flow of energy and nutrients begins with the producers, then moves to the consumers, and ultimately returns to the producers through the activity of decomposers. Energy, in contrast to materials, is not subject to recycling. Food traverses the food web, resulting in energy dissipation. Typically, just a mere 10% of the energy accumulated in a certain trophic
level, such as the producers, is effectively passed on to the subsequent trophic level, such as the herbivores. This is referred to as the energy pyramid. Ultimately, the energy available in the trophic level becomes so depleted that it cannot sustain any higher trophic levels. Consequently, the presence of fourth order consumers in any ecosystem is extremely rare.
The biotic component, often known as the life component of the environment, encompasses a diverse array of plants, animals, and bacteria, which form interconnected communities.

Abstract

The Mesozoic sediments contribute around 54% of the oil and 44% of the gas reserves of the world (Bois et al. 1982). Indian Mesozoic basins occupy an area of about 400 x 103 sq. km and are characterized as frontier basins under category II - IV. These basins are mostly overlain by the Deccan Traps of Late Cretaceous age and are least explored. Deccan Syneclise is one of the largest Mesozoic basins in India, covering an area of ~ 273 x 103 sq. km. Geophysical studies have inferred hidden sub-trappean Mesozoic sediments with thickness up to 2.5 km. It is considered that requisite heat generation due to Deccan Trap volcanism soon after the Cretaceous sedimentation may have acted as a catalyst in hydrocarbon generation. Surface geochemical prospecting surveys along with carbon isotopic studies have been used to assess hydrocarbon generation potential of this part of the basin. The area adjoining Nandurbar beneath Narmada-Tapti region of Deccan Syneclise was selected for geochemical studies where geophysical studies have shown considerable sediment thickness. Surface geochemical studies indicate the generation of light gaseous hydrocarbons, C1 and SC2+ in the range of 3 to 1187 ppb and 1 to 1449 ppb, respectively. The carbon isotopic signatures of selected soil gas samples dC13 CH4 in the range of - 24 to -39.4‰ PDB) suggest thermogenic origin

Abstract

The groundwater behaviour in hard rock aquifer systems has always remained enigmatic owing to the heterogeneity of the aquifer systems. This is the reason why there are a lot of failures in groundwater targeting and management in hard rock aquifer systems even after the employment of many modern technologies. For precise groundwater targeting in hard rock aquifer systems various parameters like lithology, the type and the degree of structural deformation, the degree of weathering, geomorphology, etc., will have to be analysed which involves spatial analysis of voluminous data. In the sphere of spatial modelling, GIS plays an important role. Hence, a newer study has been carried out in parts of Madurai, Dindigul and Theni districts, Tamil Nadu, to identify the groundwater provinces and their functions using GIS. In the said study, GIS images were generated on the groundwater targets through GIS integration of transmissivity, permeability, storage co-efficient and water level. Such GIS image showing groundwater maxima was overlaid with GIS image of fracture maxima, subsurface geology maxima and the geomorphology maxima and thus by various GIS based spatial manipulations, aquifers controlled by structure, geomorphology, subsurface geology, and combinations of the above various variables were brought out. This has provided potential method for precise targeting of groundwater.

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.

Introduction
In the global perspective, water contamination is a significant issue. Every day, it is the cause of almost 14,000 deaths. The most valuable natural resource on Earth is water, which makes up more than 70% of its surface.
Definitions
• The term “water pollution” refers to the contamination of water bodies by human activity, which can be detrimental to the plants and organisms that call thesem bodies of water home. It can be characterized as any alteration in the quality of water brought about by human activity that makes it less suitable for any of its positive uses, actual or potential. Excess of any substance or heat that could endanger people, animals, or aquatic lifeMan’s actions alter the quality or composition of water, either directly or indirectly, making it unfit for any purpose.
Sources of Water Pollution
• Point source pollution, which is defined as pollution having a distinct source and point of entry into the water, making it easy to identify. It describes impurities that find their way into a waterway by a covert channel, like a ditch or pipe. For instance, contaminants include metals and organics in municipal and industrial discharge pipelines.

Introduction
Historian “Donald Worster” tells us that fertilizers are not a replacement for rich soil. The soil is a resource for which there is no substitute. Time and climate have an impact on how soils develop as well. In humid and warm climates, soils develop more
quickly than in excessively dry or cold regions. In 15 years, under perfect temperature circumstances, soft parent material may develop into 1 centimeter of soil. It could take hundreds of years for a hard parent material to turn into soil in unfavorable climate conditions.
Definition
The land’s thin layer of soil is made up of a combination of minerals, organic matter, living things, air, and water that work together to support the growth of plants. The source material’s transformation into soil was influenced by a number of elements.
The accumulation of persistent poisonous compounds, chemicals, salts, radioactive elements, or disease-causing agents in soil that negatively impacts plant growth and animal health is known as soil pollution.

Introduction
The term “noise” originates from the Latin word “nausia.” There are negative repercussions of noise pollution on our bodies and minds. In general, the amount of noise and the length of exposure determine how much noise pollution there is. These
days, noise is a constant in our lives due to the advancements in industry, technology, and machinery.
Definition
Unwanted sound released into the atmosphere that poses a health risk is referred to as noise pollution.
The term “unwanted or unpleasant sound that causes discomfort” refers to nose pollution.
Another definition of noise pollution is “wrong sound, in wrong place at wrong time.”
Distinction Between Noise Pollution and Sound Pollution:
Sound is defined as the lowest level of 50 dB that is pleasant to listen to. Noise pollution is defined as any sound that is louder than 95 dB and bothersome to listen to.
Sources of Noise Pollution
1. Factories and industries, community and religious activities, and modes of transportation (air, train, and road) are the primary sources of noise pollution.
2. In metropolitan regions, automobiles, factories, industries, railroads, and airplanes are the main man-made sources.

Introduction

In the last two decades global climate change has perceptible and marked impact on the monsoon pattern in India. Delayed and inadequate monsoon has become a recurrent feature and the country is in the grip of drought-flood cycles. Right from the beginning of large scale irrigation that brought green revolution and food self sufficiency to the country, there is a strong feeling that full potential of rivers of the country is not tapped (Table 1).

Introduction
Human activity on the environment is the root cause of many environmental issues. The standard of the environment we live in must be each of our own concerns. The quality of our surroundings can be enhanced or degraded by our individual actions. As a result, people must feel obligated to preserve the environment by leading ethical and ecologically conscious lives.
Conservation
best possible use of human, environmental, and cultural resources in national development programs. The Latin terms “servare” (keep watch) and “con” (together) denote this.
Conservation Goals
1. Preservation of the environment’s quality.
2. Assure a steady supply of valuable material. Role of Individuals in Conserving Resources
The Diversity of Life
1. Gain an appreciation for all living things.
2. Make regular efforts to plant trees.
3. Cut back on the amount of wood and paper goods you use, recycle paper goods, and purchase recycled goods.

Introduction
A natural disaster refers to a significant and harmful occurrence caused by the Earth’s natural processes. Examples of natural disasters include floods, storms, tornadoes, volcanic eruptions, earthquakes, tsunamis, and other geologic phenomena. A natural calamity can result in fatalities or destruction of property, and usually leads to economic harm, the extent of which is determined by the afflicted population’sability to bounce back and the availability of infrastructure.
Categories of Natural Disasters/ Catastrophes
Floods
A flood is the result of water overflowing and covering land. According to the EU Floods Directive, a flood is defined as the temporary  inundation of territory that istypically not submerged in water. Flooding can occur when the amount of water in ariver or lake exceeds its  capacity, causing the water to overflow and breach its normal borders. The size of a lake or other body of water may alter due to seasonal variations in precipitation and snow melt. However, it is not considered a substantial flood unlessthe water submerges land that is utilized by humans, such as villages, cities, populated areas, highways, and farms.

Abstract

A study on colloids in groundwater and its relationship with the geochemical parameters is reasonably essential because of its facilitating nature to transport radionuclides in groundwater. Colloid sampling has been carried out in the coastal aquifers of southeast coast of India. Two different bore wells were selected based on the distance from the coast to collect groundwater samples. On the basis of the result achieved from this study, a reliable representation is emerging. The values of pH and EC are governed by the different size fraction of colloids. In this study, the relation between different size fractions of groundwater colloids and its pH, TDS and EC were carried out. These parameters were analyzed in the lab and its influence with four fractions of colloid like 1.2, 0.8, 0.45 and 0.22 µm have been discovered by smooth scatter plot. The accumulation of particles weighting by normal weighing instrument. There is an higher accumulation of particles found in Kalpakkam than Anupuram in all the size fractions. For separation of particles high frequency pressure was used by ultrasonic cleaner had been carried out. This method is very simple and more reasonable than any other methods.

Introduction
The rapid advancement of information technology in recent years has led to an explosion in the awareness of environmental concerns and issues pertaining to human health. UNEP created UNEP net, the green global Internet, as well as the satellite communication system.
Information technology is necessary for environmental management.
The general population, especially in developing nations, and decision- and policymakers still have limited or no access to this information in a readily comprehensible format. Politicians and the general public have not yet been able to personally experience the effects of ozone layer depletion, climate change, or biodiversity loss. These are all new challenges, and scientists strongly advise taking more immediate action than legislators are able to. Thus, it is more crucial than ever to close the knowledge gap between scientists and decision-makers in order to formulate environmental policy.
UNEP created the Global Resource Information Database in 1985 in an effort to close this information gap and give the world’s population access to current, trustworthy environmental data. Telecommunications and geographic information technology were used as strategic tools to do this, with the former being used for information exchange and analysis and the latter for information distribution.

The term biodiversity is used by Walter and Roses in 1985. Biodiversity means the existence of a large number of different kinds of animals and plants which make a balanced environment. According to “Convocation on biological diversity (1992)”-Biodiversity is present in terrestrial, ocean and aquatic ecosystem. This diversity present in between same species, different species and in different ecosystem.

1.1 R and R studio

R has become the world-wide language for statistics, predictive analytics, and data visualization. R is not limited to statistics; it has a wide range of tools for spatial analysis and digital image analysis and can handle any process needed for image analysis flexibly. It offers a wide range of methodologies for digital image processing, from the most basic to the most complex. As an open source project, it’s freely available for a range of platforms, including Windows, Mac OS X, and Linux. An integrated development environment (IDE) for R, R Studio, allows interactive execution of R functions with user interface. RStudio is available in two formats - RStudio Desktop and RStudio Server - both available in free and fee-based (commercial) editions.

1.1.1. Download and install R

The R software setup files can be downloaded from any of the widely distributed Comprehensive R Archive Network (CRAN). To download R, please choose your preferred CRAN mirror, a location close to you. Follow the following steps: