eChapters

Introduction

Increase in atmospheric carbondioxide (CO₂) and other green house gases viz. methane (CH₄), nitrous oxide (N₂O) and CFC (Chloro-Flouro- Carbon) due to fossil fuel burning, rapid industrialization and deforestation, which reduces the amount of earth’s radiation, that escapes to space. Role of these gases to change in climate over a longer period of time is the key issue of climate change. Climate change is a change in climate over time, whether due to natural variability or as a result of human activity (IPCC 2007).

IPCC :The UNEP (United Nations Environment Programme) and WMO (World Meteorological Organization) jointly established IPCC (Inter-governmental Panel on Climate Change) to assess available scientific information on climate change as well as to study its impact during 1988. Since establishment, IPCC has produced five major assessment reports. According to IPCC, climate change is defined as a movement in climate system as a result of internal changes within climate or interaction among its components. Frequency of extreme events (viz. heat waves, intense rain, floods, droughts etc.) are reported to follow increasing trend. Fig.1 is showing natural climatological cycle in the earth throughout different seasons as various components of climate system (IPCC 1996).

Introduction

`The living and nonliving components of ecosystems, as well as the conditions and processes that occur within them, create services thus connecting ecosystems and human cultures. The preservation of Earth’s biological diversity and the protection of the benefits, or “ecosystem services,” those functioning ecosystems bring to humanity are two primary goals of environmental conservation. Agroforestry is increasingly viewed as providing ecological services, environmental advantages, and economic gains as part of a multifunctional working landscape. The multifunctional importance of agroecosystems was emphasized in both the Millennium Ecosystem Assessment (MES 2005) and the International Assessment of Agricultural Science and Technology for Development (2008).

India has shown to the world that with 2.4 % of the land and 4 % of the water resources available at the global level, it can provide the food security to its millions. A record production of almost 265 million tonnes in 2013-14 is a testimony to the strides taken in the field of agriculture. However, the agriculture sector faces many new challenges in the future and climate change (global warming) is perhaps the most formidable one.

The new emerging demands of the relatively more-affluent Indian population, particularly its middle class, coupled with a net cultivated area unlikely to exceed 143 Mha in 2050 as well as an estimated rainfed agriculture to cover around 45 % of the net sown area, are further compounded with the harsh reality that highly productive agricultural land is being continuously lost out to the industry and urban sectors. How will the country meet the target of 400 Mt of food grain production is the mute question, in a situation where natural resource base is continuously degrading and climate change with its attendant impact is adversely affecting the agricultural production system (Singh, 2014).

13.1 Introduction

Eutrophication, means an increase in chemical nutrients — typically compounds containing nitrogen and phosphorus in an ecosystem. It may occur on land or in water. The term is however often used to mean the resultant increase in the ecosystem’s primary productivity (Fig. 13.1), in other words excessive plant growth and decay and even further impacts, including lack of oxygen and severe reductions in water quality and in fish and other animal populations.

Introduction

In the recent years, climate change emerged as the single most pressing problem globally, and accordingly received an increased attention (Berrang-Ford et al., 2011). It is evident that human activities are responsible for the climate change. Natural processes may also lead to climate variability and change. The climate change forecasts resulted from simulation models indicate that the future climate is likely to turn into more capricious nature with more occurrences of extreme events (IPCC, 2013b). Future projections according to the World Bank (2010) reveal the need of raising food production by 1.8% per annum between 2005 and 2050 due to climate change rather than 1% per annum if there were no impact of climate change. The effect of climate change can be seen on the quantity and quality of various components in the global hydrologic cycle (Milly et al., 2005; Bates et al., 2008).

In South Asia, vulnerabilities to the climate change are the largest in semi-arid and arid countries, where rainfall is concentrated over a few monsoon months, year to year variations are high, and where water resources are decreasing (Lenton, 2004). Cruz et al. (2007) indicated that climate trends and variability can be characterized by increased air temperatures, which are more pronounced during the winters compared to the summers. Across the entire Asia, both spatial and temporal variability in rainfall trends observed during the past few decades may be attributed to climate change. It is likely to happen that climate change will extend the dry season when negligible or very low flows occur, which particularly affects the water management process due to inability to rely on water storage reservoirs or groundwater resources situated at great depths (Giertz et al., 2006).

Abstract

Alleviating plant salt stress and remediating saline soils are of great economic interest. Beneficial microbes such as arbuscular mycorrhizal (AM) fungi, plant growth promoting rhizobacteria (PGPR), etc. are associated with many plant species including trees. These beneficial microbes can cope up with salinity and help the plants to survive in such soils. Diversity status of beneficial microbes from the samples collected from different salt affected areas was investigated by many researchers. They screened and identified the efficient PGPR isolates isolated from saline areas for plant growth hormone (IAA) production and phosphate solubilization. The significance and highlights of the recent research as well as the past understanding of beneficial microbes and their role in reclamation of saline areas is discussed in this paper.

4.1 INTRODUCTION

Database management system is a computer program to store, search, manipulate retrieve and give the result. Vast amount of spatial data are available and it is necessary to arrange them, store them for retrieval and analysis. Attribute data adds intelligent to GIS. Without database, a GIS will be just a Cad software. Cad softwares do not have database. GIS softwares have their own databases besides it has the potential to link with external database like Oracle, MS Access, MS Excel, Informix, INGRESS, Sybase and dbase. The data available in paper has to be digitally stored in a proper order. Previously the data were stored in a a flat file format where the data was stored without any structure. But to search and retrieve and analyse the database, database structures were developed. There are of 4 types of database structures namely Hierarchical, Network, Relational database and Object orientation.

Tables are made of rows and columns. Rows represent a map feature. Columns represents characteristic of map feature. Row is called a record or a tupule column is a field or an item. Table 4.1 is a table where rows 1, 2 and 3 represent the locations with the soil types. A column soil type represents various soil types.

18.1 Introduction

The commercially available water quality simulation models with various dimensions (1D, 2D and 3D) and database software designed to quantify movement and concentration of contaminants in lakes, streams, estuaries, and marine environments. The following water quality models were described below (Table 18.1).

18.2 Environmental Fluid Dynamics Code

The Environmental Fluid Dynamics Code (EFDC) is a multifunctional surface water modeling system, which includes hydrodynamic, sediment-contaminant, and eutrophication components. It has been applied to over 100 water bodies including rivers, lakes, reservoirs, wetlands, estuaries, and coastal ocean regions in support of environmental assessment and management and regulatory requirements. IT is a state-of-the-art hydrodynamic model that can be used to simulate aquatic systems in one, two, and three dimensions. It has evolved over the past two decades to become one of the most widely used and technically defensible hydrodynamic models in the world. It uses stretched or sigma vertical coordinates and Cartesian or curvilinear, orthogonal horizontal coordinates to represent the physical characteristics of a waterbody. It solves three-dimensional, vertically hydrostatic, free surface, turbulent averaged equations of motion for a variable-density fluid. Dynamically-coupled transport equations for turbulent kinetic energy, turbulent length scale, salinity and temperature are also solved. The model allows for drying and wetting in shallow areas by a mass conservation scheme.

Abstract

Since the first oil well drilled successfully in 1859, crude oil has been a serious problem around world, including Indonesia. As a source of all petroleum products, crude oil is very complex component and divided into aliphatic, aromatic, resin and asphaltene. Petroleum products have been used for daily life and created large amounts of pollutants in environment and ecosystems around the globe. The pollutants should be treated by certain method; among them, bioremediation has several advantages to resolve the problem. In 2003, Ministry of Environmental (MoE) – Republic Indonesia was endorsed with a new regulation about biological treatment or bioremediation for crude oil contaminated soil (MoE regulation No. 128/2003). The most important to be noted in bioremediation process is the presence of microbes with certain metabolite capabilities. The degradation rate also can be improved and sustained by ensuring the adequate required factors. This article describes the removal of crude oil by utilization of microbial potentials, factors affecting biodegradation, and how they are applied in Indonesia.

Introduction

Water and food security are the key challenges under climate change as both are highly vulnerable to continuously changing climatic patterns. Climate change has resulted in increases in globally averaged mean annual air temperature and variations in regional precipitation and these changes are expected to continue and intensify in the future. The projected changes in climate patterns over India include increase in surface temperature, variations in rainfall, increasing occurrence of extreme weather events like floods and droughts, rise in sea levels and impact on the Himalayan glaciers. Sectors of the Indian economy are most likely to be impacted by such changes in climate are those dependent on natural resources, namely agriculture, water and forestry. The likely impacts such as reduction in food production, water scarcity, loss of forest biomass Climate change is expected to bring more intense and more frequent extreme weather events including droughts and floods in India. The global atmospheric concentration of carbon di-oxide CO₂ for increased from preindustrial value of about 280 ppm to about 410 ppm at the present (2021). The global increase in CO₂ concentration is primarily due to fossil fuel use and land use change. Atmospheric methane was 1803 ppb in 2011, this is 150% greater than before 1750. Atmospheric nitrous oxide (N₂O) was 324 ppb in 2011, this is 150% greater than before 1750 (Table 1). These increase in GHGs have resulted in warming of the climate system by 0.74°C between 1906 and 2005.

Nanomaterials are a rapidly growing technological sector with diverse applications. These nanomaterials are categorized into distinct groups according to their shape, size, and materials used in their fabrication. The synthesis of nanomaterials follows different strategies that are tailored to their specific applications. This chapter describes the different approaches used for the synthesis of nanomaterials, including top-down, bottom-up, and hybrid approaches. Furthermore, this chapter discusses the advantages and disadvantages of each fabrication method and explores the diverse applications of nanomaterials across multiple fields.

Introduction

Climate change is a statistically significant variation in either the mean state of the climate or in its variability, persisting for an extended period (typically decades or longer). Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures. Eleven years from 1995-2006 rank among the twelve warmest years in the instrumental record of global surface temperature (since 1850). The 100-year linear trend (1906-2005) of 0.74 [0.56 to 0.92] °C is larger than the corresponding trend of 0.6 [0.4 to 0.8] °C (1901-2000) and over the 21st century average temperature of earth surface is likely to go up by an additional of 1.8-4°C (IPCC, 2007). This temperature increase can be attributed to the altered energy balance of the climate system resulting from changes in atmospheric concentrations of the green house gases (GHGs). Among the principal components of radiative forcing of climate change, CO₂ has the highest positive forcing leading to warming of climate. CO₂ has the least global warming potential among the major green house gases but due to its much higher concentration in the atmosphere; it is the major contributor towards global warming and climate change. Agriculture sector in India contributes 28% of the total GHG emissions (NATCOM, 2004). The global average from agriculture is only 13.5% (IPCC, 2007). In future, the percentage emissions from agriculture in India are likely to be smaller due to relatively much higher growth in emissions in energy-use transport and industrial sectors. The emissions from agriculture are primarily due to methane emissions from rice fields, enteric fermentation in ruminant animals and nitrous oxides from application of manures and fertilizers to agricultural soils (NATCOM, 2004).

This section explores how nanoparticles have a significant influence on sensing and detection, explaining how they have revolutionized analytical capabilities. Our trip through many kinds of nanomaterials, such as metal nanoparticles, semiconductor nanomaterials, and carbon-based structures, aims to explore their distinct features and how they might be used for novel sensing methods. The intricacies behind sophisticated sensor technologies are clarified through an examination of plasmonic sensing, quantum dot applications, and conductive nanomaterial responses. In order to improve selectivity, the chapter emphasises surface modifications and biomimetic coatings as key components of strategic functionalization techniques.

Nanomaterials, a cornerstone of nanotechnology, encompass a broad array of particles showcasing remarkable properties and diverse applications. This chapter outlines the classifications and applications of various nanomaterials, including organic, semiconductor, metal, metal oxide, and carbon-based nanoparticles. Each type offers unique characteristics, such as biodegradability, optical and electrical properties, making them valuable in fields like drug delivery, electronics, and catalysis. Furthermore, this study focuses on the interactions of nanoparticles with living organisms, emphasizing their impact on immune systems across plants, invertebrates, and humans. 

The deliberation on the methodology has been made to understand the concept, methods, and techniques which were utilized to design the study, collection of information, analysis of the data and interpretation of the findings for revelation of truths and formulation of theories. This chapter deals with the method and a procedure used in the study and consists of eight main parts-
• Locale of research
• Pilot study
• Sampling Design and Framework
• Empirical measurement of the variables
• Item analysis and experts rating for devising scoring technique on dependent variables
• Preparation of interview Schedule
• Pre testing of Interview Schedule
• Techniques of Data collection
• Statistical Tools used for Analysis of Data
5.1. Locale of Research
The present research has been carried out at Kasthodanga, Mollabalia, Madhpur, Baksha, and Mitrapur villages of Kasthodanga gram panchayat in Haringhata block; Rautari, Ghetu Gachhi, Maniktala para, Tentul Baria, Maheswarpur from gram panchayat in Chakdaha block of Nadia district; Boinchigram, Goara, Chau bera, Uttarkhanda, Champahati villages of Bantika- Boinchi gram panchayat in Pandua Block; Dhopapara, Beleswar, Ichhapura, Tiornai, Baksagari from Dhopapara gram panchayat in Balagarh block of Hooghly district from the Alluvial zone of West Bengal. From the Terai zone of West Bengal, Elejanerkuthi, Kalabarighat, Hourgari, Ghughumari, Gokuler Kuthi, Hirar kuthi from Coochbehar- 1 block; Pundibari, Kalarayerkuthi, Sukhdhanerkuthi, Khagribari, Singimari Paschimpar, Basdaha Natibari, villages of Coochbehar- 2 block; Mirer Kuthi, Kismat Dasagram, Bara Shakdal, Kochabari, Bamanhat-ii, Durganagar, villages of Dinhata 2 block

1. Introduction 
The intersection of nanotechnology and microalgal biodiesel production presents a compelling avenue for addressing the pressing challenges of sustainability, energy security, and environmental conservation (Cai et al., 2021a). Microalgae, microscopic photosynthetic organisms, have emerged as a promising source for biodiesel due to their high lipid content, rapid growth rates, and potential for cultivation in diverse environments as compare to other sources as given in Fig. 1. However, the commercialization of microalgal biodiesel has been hampered by various limitations, including low lipid productivity, inefficient harvesting techniques, and high production costs. Nanotechnology, with its ability to manipulate materials at the nanoscale, offers innovative solutions to enhance various stages of microalgal biodiesel production. From cultivation to processing, nanomaterials and nanodevices hold the potential to optimize efficiency, increase yields, and reduce environmental impacts. By improving light penetration, nutrient delivery, and CO2 utilization, nanotechnology-enabled systems enhance microalgal growth and lipid accumulation (Li et al., 2019; Cai et al., 2021b). Moreover, nanoscale structures facilitate the development of efficient harvesting methods, minimizing energy consumption and water usage. In biodiesel processing, nanocatalysts exhibit superior catalytic activity, enabling faster reaction times and higher yields in transesterification processes. Nanostructured membranes enhance the purification and separation of biodiesel, ensuring high-quality end products with minimal impurities. Despite these advancements, challenges such as scalability, cost-effectiveness, and environmental sustainability of nanotechnology-based microalgal biodiesel production persist (Zhao et al., 2018; Zhang et al., 2019). This chapter aims to provide an overview of the current status and future prospects of integrating nanotechnology into microalgal biodiesel production. Through a 2 | Nanotools for Microalgal Biodiesel Production comprehensive analysis of recent advancements, challenges, and opportunities, we seek to elucidate the potential of nanotechnology to drive the commercialization and widespread adoption of sustainable microalgal biodiesel. By fostering interdisciplinary collaborations and leveraging emerging technologies, we can pave the way towards a more sustainable and energy-efficient future.

Introduction

Global food production, already under the credit crunch, must double by 2050 to level off hunger. According to the UN World Food Programme (WFP), this will be possible only if food security is given top priority. The food security has become a complex issue influenced by climate and non-climate induced stressors which operate independently or in combinations are tackled appropriately. This climate induced stress is further augmented by climate change which affects agriculture and food production in complex ways. It affects food production directly through changes in agro-ecological conditions and indirectly by affecting growth and distribution of incomes, and thus demand for agricultural produce. Climate change has emerged as a major challenge in achieving goals of sustainable agriculture. Climate change refers to any change in climate over time, whether due to natural variability or/and as a result of human activity (IPCC, 2007). Agriculture impacts climate change with greenhouse gas emissions, and is at the same time impacted by effects of climate change as well. Amongst elements of climate change, the most important relate to increasing uncertainty in availability of water due to increasing frequency of drought and/or excess water events resulting in uneven water availability over time and space. Drought is a normal, recurring feature of the climate in most parts of the world. Drought is defined as the absence of rainfall or supplemental irrigation for a period of time sufficient to deplete soil moisture and injure plants. According to USDA drought occurs when annual precipitation is 75 percent of normal, or monthly precipitation is 60 per cent of normal. Drought stress results when water loss from the plant exceeds the ability of roots to absorb water and when the plant’s water content is reduced enough to interfere with normal plant processes.

Introduction

Ground water (GW) resources in most areas of world are shrinking at an alarming rate and may not meet the ever increasing demands from agriculture and industry in future. Large decreases in GW levels (up to 200 m in some places) have been observed due to over exploitation (Toze, 2006). It accounts for more than 65% irrigation water and 85% of drinking water supplies lies in a critical state. Many areas of the world, already experiencing stress on water availability, which placed severe strains on existing resources with resulting environmental impacts. Half of the population of the developing world suffers from at least one disease caused by insufficient water supply and sanitation.

Sun is the prime source of energy injected into the earth’s atmosphere. The sun is the nearest star to the earth. It is a hot ball of glowing gases at the heart of the solar system. Its radiant energy is practically the only energy source to the earth. Very small and insignificant quantities of energy are available from other sources such as the interior of the earth, the moon, and other stars. Without the sun’s intense energy and heat, there would be no life on earth.

NATURE AND PROPERTIES OF SOLAR RADIATION

The mean distance of the sun from the earth, also known as one astronomical unit (1 AU), is approximately 1.496 × 10⁸ km, though the distance varies as the earth revolves round the sun in an elliptical orbit. At this average distance, light travels from the sun to earth in about 8 minutes and 19 seconds. The energy of the sunlight supports almost all life on earth by photosynthesis, and drives earth’s climate and weather. The minimum sun-earth distance is about 0.983 AU and the maximum is approximately 1.017 AU. The earth is at its closest point to the sun (perihelion) on around January 3 and at its farthest point (aphelion) on around July 4.

Abstract

The paper presents an approach of selecting suitable areas for artificial groundwater recharge structures through remote sensing and integrated terrain analysis by statistical method. The study area “Ayyar basin” is an aquifer system of gneisses and charnockite litho-units in Tiruchirappalli district, Tamil Nadu. The area has witnessed a steady decline in groundwater table. Hence, the scope for artificial groundwater recharge was studied in this area with the help of Tamil Nadu State Council for Science and Technology (TNSCS&T).