eChapters

Landscaping is both science and art and is an aspect of the environmental impact of a hotel that needs to be addressed. Understanding and blending the elements of both nature and construction is effective landscaping. Whether Landscaping is extensive or small consumes a large amount of water, fertilizers and herbicides and generates solid waste.

Ecogreen’s Greenscaping Operation provides cost-efficient and environmentally friendly solutions for landscaping. Greenscaping operation deals with two aspects:

1. Solid Waste Management, and

2. Water Conservation

Trees are major capital assets in cities Just as streets, sidewalks, public buildings and recreational facilities are a part of a community’s infrastructure, so are publicly owned trees. Trees — and, collectively, the urban forest — are important assets that require care and maintenance the same as other public property. Trees are on the job 24 hours every day working for all of us to improve our environment and quality of life. Urban forest provides many environmental benefits to our community. Aside from the obvious aesthetic benefits, trees within our urban forest improve our air, protect our water, save energy, and improve economic sustainability.

In other words, since most trees have been planted much of the tree cover is in urban areas as opposed to “natural lands”. Therefore, estimated pollutant uptake rates are higher for residential compared to natural or unmanaged lands. Possible management implications of these estimates are that air pollutant uptake benefits from tree planting may be optimized by planting in areas where air pollutant concentrations are elevated and where relatively high planting densities can be achieved thereby enhancing the health of urban dwellers.

Pollution is the term used to denote the hindrances caused to living organisms by way of contamination of their physical environment. Pollution to air, water, soil etc. is the major problem faced by the living community. Measures to control the emission of pollution into air, water or soil will certainly reduce the level of pollutants. Mitigation of pollution can be best achieved by combining nature with technology that increases the effectiveness of plants in removing pollution. Use of vegetation is an effective means of pollution control and many researchers have reported their advantages in mitigating pollution.

So far, the main approach has been to dig the polluting chemicals out of the ground and transport them to a landfill. However, after a decade of research, scientists in the early twenty-first century found that hundreds of species of plants, along with the fungi and bacteria that inhabit the ecosystem around their roots, seek out and often break down chemical molecules that can harm most other life.

In the mid-1980s, Dr. B.C. Wolverton and fellow researchers at NASA conducted several studies to determine whether plants could halt indoor pollution and provide a natural way to deal with the problem. It has been suggested by NASA and the Associated Landscape Contractors of America (ALCA) that plants are major pollution-absorbing devices: the common indoor plants might provide a natural way of helping combat “SICK BUILDING SYNDROME”. Common indoor plants may provide a valuable weapon in the fight against rising levels of indoor air pollution. These plants are not only decorative, but are also surprisingly useful in absorbing potentially harmful gases and cleaning the air inside modern buildings.

1.1 Weather

Firstly, what is weather? Simply, the conditions in the atmosphere above the earth is called weather. It refers to the conditions such as wind, rain and temperature, prevailing at a particular location during periods of hours or days. We often ask “what’s the weather like today”? Any individual can answer to this question as it requires only a short term experience or say exposure to the atmosphere. The TV news forecasters predict weather each day and inform about the temperature, cloudiness, humidity, or possibility of storm in the next few days. Weather is localised, say, it’s a hot and cloudy weather in one part of the country and dry and windy on the other part.

1.1.1 What are the factors that influence weather?

Before we try to understand the factors that influence weather, we must understand what the components that describe a weather conditions are? Is it the rains, or the air temperature or both? The answer to this question is not so easy, and it’s a bit complicated. There are many components that constitute weather. Weather components include rain, cloud cover, sunshine, winds, hail, snow, sleet, storms, thunderstorms, heat waves and many more. These components are sometimes referred as weather parameters or climate elements. Each of these components define weather patterns of a particular area. These components determine the status of local atmospheric conditions. Again, as a basic definition, weather is the state of the atmosphere and majority of weather phenomena occur in the lowest layer of the atmosphere, called as the troposphere. Does it mean that ground conditions such as the topography, water bodies and vegetation of a particular area has nothing to do with it? No, it is not so. The state of the atmosphere is subjected to various processes taking place not only in the atmosphere but also in the ocean, the sea-ice, the vegetation, etc. Weather parameters or the components of weather form a sequence of events, and the influences are far reaching and they do not remain solely in the atmosphere. For example, terrestrial radiation impacts the air temperature, air pressure and humidity. The terrestrial location also influences the cloud formation. The clouds may or may not turn into precipitation depending on the outcome (cloud or rain), which is by and large governed by troposphere. Likewise, a lack of precipitation affects not only weather conditions, but also soil moisture conditions that may result in lowering of water levels (ground water table) in soil. Wind speed and direction are governed by the atmospheric pressure and air temperature. So, all these parameters or components are interrelated and the weather conditions are the outcome of their interactions. Therefore, we can say that, the three main components of weather are temperature, precipitation and solar radiation. These components are influenced by different factors.

Climate change is caused by both natural as well as anthropogenic causes and it has been changing since the inception of earth-atmosphere (Figure 2.1). In a broader sense, anthropogenic activities (human activities) also must be considered as natural one in longer time scale as human and their activities are also a part of natural-ecosystem-functions. Among the natural phenomena, volcanic eruptions and continental drifts significantly affect the earth’s precipitation and temperature. A huge volume of CO₂ is released due to volcanic eruption at a little span of time-period which heated up the earth-atmosphere. Climate variability is primarily governed by rise in sea temperature, movement of warm water from the Western Pacific towards Peru, and El Nino which occurs at an intervals of 3-7 years. Climate variability also influenced the alteration in temperature and precipitation world wide. And persistent climate variability cause long term climate change. Therefore, basically three drivers that causes climate change are, the alteration in the energy of sun received by earth-atmosphere (natural causes), variations of ref lectivity of earth-surface- atmosphere system (natural as well as anthropogenic causes) and fluctuations in the greenhouse effect (natural as well as anthropogenic causes).

3.1 Chemistry of greenhouse gases (ghgs)

Greenhouse gases (GHGs) are atmospheric-gases that have capabilities to absorb and radiate-back the infrared (IR) radiation in the earth-atmosphere system (Figure 3.1). In this process the atmospheric-gases absorb and radiate- back IR radiation in lower atmosphere effectively emitting and absorbing heat energy heat energy. They maintain the heat budget of earth-atmosphere and keep our plant warm. If we typically see the chemistry of those gases, the key point is that they should have dipole moments. This is the property which makes them capable to absorb and radiate-back the range of IR radiation. In a molecule when valence-electrons are not equally shared in a bond between the two atoms, a slight positive charge is developed above one atom and a negative charge on the other atom. That charge difference of the different atoms in a molecule generates the dipole moment. For instance, in water vapour (H₂O- vapour), an unequal sharing of electrons and or separation of charge causes dipole moment. In H₂O, the centre has a positive charge at the hydrogen atoms and negative charges are located on the oxygen atom. The magnitude of dipole- charges, vibration and stretching of O-H bond generates certain frequency of the oscillating dipole moment that actually regulates the absorption capacity of IR radiation by H₂O vapour.

The measurement of greenhouse gases (GHGs) has been started during middle of the last century. Initially, CO₂ and water vapour were measured with other common meteorological variables like temperature, sunshine hours, rainfall, humidity etc., for monitoring the weather condition and pollution. The absolute or relative concentrations of gasses in atmosphere are used to measure basically for monitoring purpose. However, limited studies were dealt with actual gaseous exchanges of fluxes. The concern about gaseous flux measurement and GHGs-exchanges started after 1900s when people got concerned about anthropogenic pollution, environmental sustainability and climate change issues. The GHGs-exchanges in earth-atmosphere systems primarily occur due to change in meteorological variables, soil responses and physiological activities of crops. If we are interested for environmental data inventories, then absolute GHGs concentrations of atmosphere at a specific time is required. However, presently researchers, students, environmentalists, climate scientists are primarily interested for quantitative data on GHGs fluxes and or GHGs-exchanges. They want to know what and how much quantity of a particular GHG is emitting from unit area at unit time.

Flux refers to the amount of any gas emitted per unit area per unit time. The dimension of that is M A^-11 T^-1. (Where, M= Mass/ Quantity; A= Area; T= Time). The SI unit of flux is g m²s^-1. Therefore, flux is a vector. It has magnitude as well as direction. As for example positive flux of CO₂ from earth surface means, CO₂ is moving out from earth surface to atmosphere. If it moves in opposite direction then the flux would be negative. In that case CO₂ gas may be absorbed by the soil surface from adjacent atmosphere. Similarly, GHGs fluxes of earth surface are either positive or negative. Generally, positive GHGs flux refers to emission of GHGs from earth to atmosphere and vice versa.

5.1 Impact of climate change on agriculture

Climate change has both positive and negatively impact on agriculture, food security and land degradation. Climate change could exacerbate the land degradation processes by increases in rainfall intensity, drought frequency and severity, dry spells, f looding, heat stress, sea-level rise and permafrost thaw. The 1/4^th of ice-free land area in the world is prone to human-induced anthropogenic degradation (Certini and Scalenghe, 2011; Hooke et al., 2012). Soil erosion rate is 20-100 times faster than that of soil formation in agricultural field. The erosion rate is least is zero-tillage (non-disturbed field) and maximum at conventional intensive tillage practices. Climate change further exacerbates the land degradation. The permafrost areas, dry-lands, low-lying coastal regions, river deltas are more vulnerable. The occurrence of drought in dry-land was increased by around 1% per year during 1961-2013 periods. On an average 380-620 million people globally experienced desertification who lived in dry-land areas (1980s and 2000s) in South and East Asia, North Africa, Middle East, Sahara region, and Arabian peninsula. Moreover, people who are already living in degraded/ desertified regions are more negatively affected by climate change.

Specifically, the land surface air temperature has increased about twice as much as the global average temperature since the pre-industrial era. The land-surface air temperature has increased relatively higher than the world’s average surface (land and ocean) temperature since the pre-industrial era (1850-1900). The average land-surface air temperature has enhanced by 1.53°C (1.38-1.68°C), whereas, world’s surface (including land and ocean) air temperature has enhanced by 0.87°C (0.75-0.99°C). Subsequently, global warming triggered the frequency, intensity and duration of heat waves and related damage. The direct and indirect impacts of climate change on global agriculture is summarised below for an overall idea about the importance of the issues.

What is mitigation of GHGs emission? We must be clear about the answer of this fundamental question. In simple term, the mitigation of GHGs emission is the way or means by which the emission of those gases could be reduced. As we know from the previous chapters of this book that the GHGs emission could be occurred from natural as well as anthropogenic activities. Natural activities included volcanic eruptions, ocean current fluctuations, continental drifts which are responsible for emission of huge amount of CO₂ and other GHGs. The reduction of emissions from those natural activities is beyond our capabilities. However, the human induced emissions of GHGs emission could be reduced. We studied in previous chapters that fossil fuel burning, industrial and energy sector pollution, deforestation, land use change and agricultural could contribute to GHGs emission considerably. Mitigation techniques are different for each of those sectors that governed by lot of interrelated factors. In actual sense, the mitigation of GHGs emission should includes all the measures that can curtail the anthropogenic emission from all sectors. But that is out of the scope of this book. In this book, we specifically address the mitigation principles, options and efficiency of different techniques/ practices in agriculture only.

In that aspect, the mitigation of greenhouse gases emissions in agriculture is defined as “the means and ways by which emissions of GHGs could be reduced from agriculture”. The ways and means actually referred to the techniques and practices and their amalgamation in agricultural sector both in production, processing and consumption aspects. So, mitigation is not only a techniques or combination of techniques it is actually an integrated approach for reducing greenhouse gases emission from agricultural systems. Primarily, there are two complementary approaches for mitigation of GHGs emissions from agriculture. Those two approaches are (i) supply-side and (ii) demand- side options or pathways. The supply-side approaches includes scientific land- use-changes, improvement of crop management, better livestock management practices, enhancing carbon storage in biota, soil carbon sequestration, significant substitution of fossil fuel by bio-fuels and use of renewable energy in agriculture. On the other hand, demand side approaches, taken in to account of shifting in the dietary pattern from non-vegetarian to vegetarian, curtail down the food loss and waste, and reducing the supply-chains (Figure 6.1). We can see, most of the approaches in supply-side are technology driven, while, approaches in demand-side are socio-economical and or policy driven. In this chapter we would thoroughly discuss the principles of mitigation, options of mitigation, mitigation cum adaptation approaches to reduce GHGs emission and climate change and few strategies to cope up with the vagaries of climate change.

7.1 Economics and Valuation of ghgs emissions

Since the late 20^th century, it has been largely accepted that cause of high concentration of GHGs in atmosphere is induced by human activities. Greenhouse gas emissions and related climate change has opened up debate on overall economic losses and ways to reduce these loses. Moreover, apart from curbing monetary losses; the global political leaders as well as reputed economists are looking towards making money by saving the emissions. Recently, the researchers have started to emphasize on the actual value added to the ecosystem by curbing emissions, discrete of the economic benefits. This section will discuss the economics and ecosystem services related to the management of GHG emissions.

Origin

The initiative to curb the emissions started in 1992 with the United Nations Framework Convention on Climate Change (UNFCCC) at the Earth Summit in Rio de Janeiro. The Convention took place from 3 to 14 June, 1992. The UNFCCC is an international environmental treaty designed to “stabilize greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system”. The UNFCCC had non-binding limits on greenhouse gas emissions for individual countries and the framework was only meant for formulating precise international treaties (called “Protocols” or “Agreements”). It contained no execution mechanisms, however, it considered some negotiations and suggestions to formulate the action plans and regulation guidelines under UNFCCC to fulfill the objective of reduction of GHG emissions to the desired level.

Minerals are the building blocks of the earth’s crust. Derived inorganically, either as chemical elements or more often as chemical compounds, minerals are essentially solid. Minerals often form crystals, while aggregate of minerals constitute a rock. Mineralogy is the discipline devoted to the study of minerals including their formation, occurrence, properties, composition and classification . Needless to say, the subject of mineralogy is the foundation of crystallography, petrology and other branches of geology.

Section A dealing with Minerals comprises nine chapters. Chapter I presents salient features of the earth including composition. and structure of the crust mantle and core. Chapter II presents their categories and the how minerals derive their names. Since minerals are essentially a combination of atoms and molecules the significance of chapter III which deals with crystal chemistry cannot be over emphasized.. Chapter IV and V deal with physical and optical properties of minerals which are crucial in identifying them in hand specimens and under the polarising microscope. Classification of minerals and their occurrence is dealt in a general way in chapter VI while descriptive mineralogy is presented in Chapters VII ( Silicate Mnerals) and VIII ( Non-Silicate Mnerals). Minerals are no doubt a subject of serious scientific curiosity but ultimately their use to man is by far the most important theme. Chapter IX therefore is devoted exclusively to different uses that are minerals are put to. The chapter ends with eye opening information as to the quantum of minerals that man uses, taking one of the most industrialized nation USA as an example.

The Mineral Kingdom presents a dazzling floral-display in the form of natural crystals. This is what makes mineralogy a very fascinating subject both for an amateur as well as an expert. Unless one visits the celebrated Lechuguilla cave in New Mexcio, USA it will be difficult to visualize the breathtaking beauty that crystals present. This, over 160 km cave is lined with gigantic as well as delicate gypsum crystals- as thin as human hair to several centimetres across and 6 m long . Crystals come in all shapes, sizes and colours. Their beauty and regular shape has not only attracted the scientists but made them objects of magical and mythical powers in many cultures of the world.

The study of crystals - including their growth, structure, classification by form and their physical properties forms the subject of crystallography. As of today one can’t think of this subject without x-ray crystallography, however, this being not in your syllabus only an introduction will be presented in the last chapter, while the entire section will be devoted to fundamental aspects of crystal morphology.

The section comprises four chapters. Chapter I describes and introduces the theme, presents a brief historical background of the development of the subject and gives some fundamental definitions. Chapter II presents the morphological elements including symmetry elements( plane, axes and centre of symmetry), parameters, indices, notation of crystal faces and other related aspects which are the basis for dividing crystals of all shapes and sorts into six or seven systems and several sub-types. This chapter will help you understand as to why mineral galena belongs to cubic system, while gypsum is monoclinic, or as to why an octahedron is represented by a symbol (111) but a cube with (100). Chapter III describes the seven systems and their sub-types and ends with an account of twinning- a curious feature quite often encountered among crystals. The section ends with a preliminary idea about stereographic projection and x-ray crystallography.

A rock is the home for minerals. In other words, naturally occurring coherent aggregate of minerals (or glassy mass) will constitute a rock. Like in a family, more often, there are several members(minerals) within a rock but occasionally just one mineral also makes a rock( olivine in dunite, quartz in quartzite and calcite in marble). The root word petros is of Greek origin, meaning rock and a petrologist is one who specializes in the study of rocks. The three main categories of rocks are distinguished on the basis of their origin. Igneous rocks are the ones that have solidified from a molten state in deep seated conditions, as also on the surface while Sedimentary rocks are formed from the erosion of preexisting rocks and subsequent re-deposition or precipitation of the resulting material at or near the surface. Metamorphic rocks on the other hand, are formed by the action of heat or pressure or both on preexisting rocks.

The theme of rocks is split into five chapters. The first chapter introduces the theme of petrology, petrography and petrogenesis., presents rocks as the storehouses of minerals and their grouping into three classes. The second chapter presents all the important aspects of igneous rocks( plutonic, hypabasal and volcanic) including their forms, texture, structure, chemistry and classification and variation diagrams. It also presents a somewhat sufficient description of different kinds of igneous rocks under the categories of ultrabasic, basic, intermediate acid and alkalic rocks. The chapter ends with an introduction to some of the peculiar kinds of igneous rocks and also presents a brief account of causes of diversity among igneous rocks.

Chapter III is devoted to the study of sedimentary rocks beginning with nature and categories of sediments and general factors that affect sedimentary process. Sequence of breakdown, sedimentary minerals, depositional environment , classification of sediments and sedimentary rocks is the next theme followed by primary and secondary and biogenic structures. The next theme is a description of important sedimentary rocks under different categories ( rudaceous, arenaceous, asrgillaceous and rocks of biogenic origin). The chapter ends with introducing sedimentary rocks as the home for natural resources.

Chapter IV dwells on metamorphic rocks distinguishing between metamorphism and metasomatism. Metamorphic minerals and naming metamorphic rocks is the next theme. Next, agents and types of metamorphism is followed by grade, zones, index minerals and metamorphic facies. Textures, structures and the description of metamorphic rocks comes next. The use of triangular plots in metamorphic petrology is introduced and ends with considering metamorphic process in the light of global tectonics.

The last chapter is a short but important chapter- The Rock Cycle which combines the three important geo-processes of igneous activity, sedimentary process and metamorphism while presenting a birds eye view of them. It considers the movement, not only of matter but also the energy that drives the rock cycle. The chapter closes with introducing the rock-cycle-mineral deposits relationship.

As milk to a cow or fruit to a tree, ore is to Earth Sciences. Different academic and scientific aspects of geology are of no consequence to a common man. Ores and ore minerals from which valuable constituents could be extracted profitably is what the world is after- be it the continental masses, oceanic depths, desolate icy Antarctic tracts or now, even other planets of the solar system. The subject of economic geology is thus a subject of greatest interest among other natural sciences.

This last section will dwell on the theme of metallic and non metallic ore deposits. The first chapter begins with fundamental definitions, signifying the importance of minerals in human affairs. It also looks at ore minerals against the background of average crustal composition and presents a glossary of important terms in economic geology. The second chapter is a lengthy chapter devoted to the ways ore deposits are formed ( ore genesis). Broadly, the processes are described under two categories, the internal processes and the surface processes. Fuel minerals are taken separately towards the end of this chapter. Chapter III briefly introduces the relationship between location of minerals deposits to the revolutionary theme of global tectonics which attempts to answer why a mineral deposits occurs where it occurs.

The fourth chapter is devoted entirely to the Indian Mineral Deposits. It begins with a few important themes of mineral economics and dwells on the description of important Indian Mineral Deposits as to their geology, geography and economic potential. Lastly, the fifth chapter exclusively deals with the facts and figures of the Indian Mineral Industry presenting recent available data of resources, production, import, export and future prospects. It also gives a brief introduction to the important geo-scientific organizations of the country.

Introduction

In Indian agriculture, horticulture sector has made considerable progress after independence and as a result, horticulture has emerged as one of the major drivers of growth in the agricultural and allied sector. The horticulture sector includes large number of crops viz., fruits, vegetables, ornamental crops, spices, tuber crops, plantation crops, medicinal and aromatic crops, mushroom and their post harvest management. On the production and productivity front, the horticulture sector outperformed conventional food crops. Between 200405 and 201415, horticultural output achieved an annual growth of about 7 per cent as compared to around 3 per cent growth in food grain production. This increase in production has come from an increase in acreage and even larger increase in productivity. Over the last decade, the area under horticulture grew by about 3% per annum and annual production increased by 5.4%. Thereby, India has maintained its second rank in the global production of fruits and vegetables, next only to China. India’s fruit productivity is better than that of China, though China is the largest fruit producing country.

The country is currently producing 295.2 million tonnes of horticulture produce from an area of 24.9 million hectares, which has surpassed the estimated food grain production of 275.68 million tonnes (201617). Though the production of food grains and horticultural produce are not meaningfully comparable due to fundamental differences in resource requirements, their farming practices, characteristics of produce and most importantly, their nutritional and medicinal properties as well as energy value. The special attention was given to the this sector, especially after the introduction of the Horticulture Mission for North East and Himalayan States (HMNEH) and the National Horticulture Mission (NHM) during 11^th Plan period, owing to bumper fruit production. Given the increasing pressure on land, growth strategies have been focusing on raising productivity through high density plantations, protected cultivation, micro irrigation, quality planting material, rejuvenation of senile orchards and an emphasis on post harvest management and marketing of produce for better price realization.

Introduction

The Indian hot arid zone occupies an area of 0.32 million km to forming a continuous stretch in the north western states of Rajasthan, Gujarat, Punjab, Haryana and scattered land masses in the states of Maharashtra, Karnataka and Andhra Pradesh, 70 per cent of it falls in western Rajasthan. Low and erratic rainfall, extreme temperatures, long sunshine duration (6.6-10 hours), low relative humidity (30-80 per cent), high wind velocity (9-13 km/h) and high evapo transpiration (1600-1800 mm) and characteristic features of the region. Moreover the soils are poor in nutrients and scarcity of water and recurring droughts are perennial constraints. Despite hostile conditions, the western arid Rajasthan supports a large human and livestock population and a variety of flora and fauna. However, the ever increasing human and livestock population and development activities exert enormous pressure on the natural resource in the region. These areas experience an annual rainfall between 100 and 500 mm with a coefficient of variation varying from 40 to 70%. The region is characterized by low and erratic rainfall with extremes of temperature (1–48 °C), high wind velocity and sandy soils. In dry and arid region, wind erosion affects 13.5% in India (Sehgal et al., 1994, Kar et al.,1959). Wind erosion is very active in the Indian Thar Desert and poses severe multifaceted problems (Dey et al., 2016). Loss of nutrient-rich particles from agricultural fields has been occurring due to suspension of fine particles in air and deposition of eroded soil. Among terrain properties, soil aggregate distribution, surface roughness, soil moisture and vegetation cover are important factors influencing wind erosion. Indiscriminate grazing in the region also further destroys vegetation and exposes the land surface, thus making it more vulnerable to wind erosion.

Introduction

Horticultural crops comprising of fruits, vegetables, flowers, medicinal and aromatic plants, and mushrooms play an important role in meeting the livelihood, nutritional security and socio-economic development of farmers. India’s horticulture production (287 mt) surpassed food grain output (265 mt) fifth year in a row in 2016-17 (First Advance Estimates, 2016-17). Horticultural crops together contribute around 30.4% to the agricultural GDP from nearly 14% of the total cropped area, and contribute nearly 37% to the export of the agricultural commodity from the country (Anonymous, 2015). Fruits and vegetables are an important part of the human diet and a major source of biologically active substances such as vitamins and secondary metabolites. India is the second largest producer of fruits and vegetables in the world, with a combined production of 260.7 million metric tons (91.7 million metric tons of fruits and 169 million metric tons of vegetables) during 2016-17.

Rapid growth in horticultural production has been accompanied by heavy use of pesticides thus causing major concern over health effects. Heavy pesticide use occurs, in part, because numerous pests attack horticultural crops, including the fruit itself, reducing market value and yield on high-value crops. Pesticide use raises safety concerns for agricultural workers who apply pesticides. Concern is particularly high in flower production because of heavy spraying in enclosed conditions. Potential food safety risks from pesticide residues are also a significant issue for importers of fresh fruits and vegetables and a market-risk factor for exporters who may have shipments detained or rejected if residues exceed allowable limits (George et al., 2003).

The increased use of chemical pesticides on horticultural crops has raised a number of economic, ecological and health concern. Economic concerns arise from the over reliance and use of chemical pesticides which increase the costs of production. Indiscriminate use of pesticides has resulted in ecological problems of common pests developing resistance, elimination of natural enemies and other beneficial arthropods, and environmental pollution. Human health concerns focus on risks from shortcomings in protective clothing, large deviations from recommended doses/situations, and excessive run-off into the soil and water sources. These concerns are exacerbated by poorly regulated internal markets for pesticides that have fostered usage of banned or outdated products; creating a situation that if not stopped will negatively impact on horticultural exports to countries with more stringent regulatory requirements for fresh crop produce. Meeting these food safety requirements has become a major challenge for the fresh produce export sector of many countries. To ensure and maintain export compliance, grower and consumer safety, and environmental integrity; farmers, government and development partners are developing programmes designed to improve pesticides usage, regulation and management on horticultural crops (Karungi et al., 2011). In this chapter, major important horticultural crops grown in India have been selected to illustrate trends in pesticide usage and regulation, and the development and application of alternative pest management practices through farmer participation and training.

Introduction

Vegetables are important constituents of Indian agriculture and play important role in nutritional security due to their short duration, high yield, nutritional richness, economic viability and ability to generate on-farm and off-farm employment. Vegetables form an integral part of staple diet in India where 42% population is vegetarian and vegetables are sources of daily requirement of nutrients, vitamins and minerals. Our country is blessed with diverse agro-climates with distinct seasons, making it possible to grow wide array of vegetables. The role of vegetable cultivation in the country’s nutritional security, poverty alleviation and employment generation is becoming increasingly important. There are vast opportunities available in export sector, which need to be harnessed to their fullest ability. Vegetable crops have high yield potential and calories per unit area compared to that of cereals in the shortest time. Additionally, vegetable cultivation creates employment in rural sector, as it is a labour intensive farming practice. Vegetables are good source of ready farm income, besides being rich in health building substances, especially protective nutrients (Kalia, 2010 and Meena et al., 2016).

Introduction

Arid Horticulture denotes cultivation of fruits and vegetables under dry and arid regions. Arid region in India is stretched over 39.54 million ha (31.71 million ha is under hot arid region and 7.38 million ha under cold arid region) comprising about 12.02% of the total area of the country. Most of the precipitation in north-western arid region takes place from July to September. Occasional frost has also been a grave issue for horticultural crops, especially, aonla and moringa (Dhandar and Saroj, 2004). The region is exemplified by low and erratic rainfall with extremes of temperature (1–48°C), high wind velocity and sandy soils (Bhandari et al. 2014). Growing of annual crops restricted only a particular season of the year is the merely source of livelihood for the inhabitant of these region. These crops often encounter abiotic stresses like drought, hot and desiccating winds during their growth period leading to poor productivity. These regions have tremendous potential for cultivation of perennial fruit trees.

Introduction

Plant growth and productivity are adversely affected by various abiotic stresses. Plants are frequently exposed to a plethora of stress conditions such as low temperature, salt, drought, flooding, heat, and oxidative stress. Various anthropogenic activities have accentuated the existing stress factors. All these stress factors prevent them from reaching their full genetic potential and limit the crop productivity. In the event of growing concerns of uncertainties in climatic conditions, the abiotic stresses have become the major threat to agriculture production worldwide (Bray et al., 2000). The plant responses to abiotic stress condition are believed to be complex in nature as these are the reflections of integration of stress effects and responses at various levels of plant organization. To provide tolerance against stresses, plants are equipped with several inbuilt physiological and biochemical mechanisms occurring at cellular level. An understanding of processes linked to these mechanisms is vital in optimizing the crop growth and productivity under stress conditions.