eChapters

Abstract

The landslide vulnerability of the state of Mizoram is already high due to lithology, structure, geomorphology and seismotectonics and also the rainfall, like the other states of the northeastern region of India. The extensive mining activities along the highways for the building and road materials appear to cause additional problems of landslides. So two prominent landslides occurring in Keifang and Tlungvel quarries,Mizoram were studied. Besides taking stock of the geosystems, boreholes were drilled in both slides and from the total depth drilled and the modified core recovery, the RQD were worked out for the rocks which indicates that geotechnically the rocks of Keifang quarry are weak when compared to Tlungvel quarry. The geophysical surveys too lead to similar inferences. On the basis of the studies a set of mitigation strategies have been suggested.

ABSTRACT

The present work relates to geological and commercial aspects of pyroxene syenite (Green Onyx) occuring in and around Sivamalai of Periyar District in Tamil Nadu. The alkaline complex of Sivamalai comprises syenites-, nepheline syenite and their variants. Pyroxene syenite is possibly the oldest within the syenite complex occurring as minor massifs, elongated linear bodies, -arcuate islands and enclaves within feldspar syenite are observed in the hillocks North East of Sivamalai, namely Chennimalai and its southern extensions. On the commercial point of view, the pyroxene syenite in the study area occupies nearly 30 square -kilometres area and can be categorised as Kalleri Block, Neykkarampalayam Block and Sivamalai Block. The observed petrographic and petrochemical characters of the alkaline rocks of the study area favours magmatic origin for these rocks. A detailed geological study and random market survey of individual syenite bodies proved the true worthiness of the material Green-Onyx as a dimensional stone with substantial resources and market potential.

Abstract

The damages caused by the tsunami surge of 26, December 2004 could not be recuperated. There is no second opinion for the above statement as attested by the consequences of tsunami surge on the coastal landforms, human lives, properties, biological assets, etc., The attempt made to evaluate the damages caused by the tsunami surge along the study area divulges various factors regarding the response of the coastal environment to this weird phenomenon. Kanyakumari district witnessed the tidal inundation of 50 – 450 m, the least along Colachel and the maximum in Kanyakumari and Muttom coasts. Run-up elevations were seen even up to 6 m in Manakudi and Colachel coasts. In major parts, the beaches of the study area had endured lofty erosion of beach sediments. High occurrence of Casualty was reported in the Coasts of Colachel, Kotilpadu, Manakudi and Azhikkal. Similarly, loss of man-made structures were also observed to be high along the Coast of Manakudi, Colachel, Kotilpadu, Azhikkal and Muttom. Costly articles like boats, fishing nets, etc., were also damaged in Kanyakumari, Pallam, Muttom, Kadiapatanam, Kesavanputhenthurai and Colachel. The quality of water has also been found to be affected with high level of pH and TDS in the coasts of Manakudi and Colachel. Such Colossal damages in the area is attributed to its geo-position exactly at the receiving point of the diverted tsunami surge by Sri Lanka. Bathymetry also seems to have played a crucial role in determining the intensity and angle of the seismic wave propagation in the area.

Keywords: Tsunami, India, Damages in Kanyakumari, Evaluation, Map, GIS.

Abstract

Natural resources and agricultural production processes vary spatially. Capturing the spatial variations in data and knowledge of natural resources and production processes has been a major challenge for efficient and sustainable management of agricultural production systems. Geographical Information Systems (GIS) provide an effective platform for storing and mapping spatial data and modeling the relevant processes. Huge volumes of geospatial data on specific themes such as soils, water, climate, and other natural resources, are being collected by public and private agencies. However, currently it is difficult for most users to access the data and integrate them into a GIS platform to derive useful information and knowledge for specific applications. There is a need to create geospatial data and knowledge systems that can provide efficient, on-demand and remote access of spatial data to users to enable development of a variety of GIS applications for agricultural and natural resources management. The design of a prototype geospatial library to provide web-based access to geospatial data, services, and learning and knowledge resources that can support agricultural and natural resources management is presented. The design is scalable and sufficiently general to allow a range of agricultural and natural resources management applications across different spatial scales.

Keywords: Agriculture, GIS, Geospatial library, Knowledge Management, Natural Resources

The term ‘geo’ is a Greek word, it means the earth, and the term ‘spatial’ means parameter/feature measured, mapped or modeled with reference to distance or space. The geospatial technology refers to the technology that measure, model, analyze, map, or predict the features or phenomena that occur on earth and its surface.

Food security is paramount for developing any nation reliant upon sufficient crop production. The decline in crop production significantly impacts food security, leading to an imbalance between global food demand and agricultural output. Multiple factors contribute to reduced agricultural productivity, including abiotic factors like water scarcity, poor soils, and unsuitable temperatures, as well as biotic factors such as pests, diseases, and weeds attacking crops. These challenges result in inefficient input utilization and decreased crop yields, ultimately threatening food security. Pests, diseases, and weeds profoundly impact plant health, causing substantial losses in crop production. Geospatial technology is employed throughout the agricultural cycle, from initial crop health assessment to forecasting disease outbreaks. Despite the significant challenges global and local agriculture face in achieving optimal outputs and securing food for the world population, the wealth of geospatial data and technological advancements plays a crucial role. They aid decision-makers in formulating strategies to combat various pests and diseases affecting plant health and food crops, thereby contributing to improved agricultural outcomes and food security. This chapter provides a comprehensive appraisal of existing literature to elucidate the role of geospatial technologies, encompassing Geographic Information System (GIS), remote sensing, and the Global Navigation Satellite System (GNSS), which are utilized for data collection, mapping, analyzing distribution, and predicting events related to plant health.

Introduction

High degree of spatial variability in soil properties is observed at different scales. This variability is generally originated from the combined effect of physical, chemical or biological processes operating with different intensities at different scales (Goovaerts 1998). Knowledge of this spatial variationof soil properties is important in several land management applications e.g. variable rate application of nutrient and water in agricultural production system, land suitability classifications, modeling water balance components at landscape scales, precision farming etc. The concept of ‘management zone’ was also evolved in response to this large variability with the main purpose in efficient utilization of agricultural inputs with respect to spatial variation of soils and its properties (Franzluebbers et al. 1996, Atherton et al. 1999, Malhi et al. 2001). Therefore, an appropriate understanding of spatial variation of soil properties is essential. The most important way to gather knowledge in this aspect is to prepare soil maps through spatial interpolation of point-based measurements of soil properties. Here, a case study is discussed where soil water retention at two critical levels e.g. field capacity (FC) and permanent wilting point (PWP) was spatially characterized through geostatistical approaches. Because these two soil moisture contents guide farmers to apply right amount of irrigation water at right time. The study was carried out at the experimental farm of ICAR-Indian Agricultural Research Institute, New Delhi, India (28°37′-28°39′ N, 77°8′ 30″-77°10′30″ E, 217-241 m above mean sea level). A detailed discussion of the study is available in Santra et al. (2008)

Introduction

Soil organic carbon (SOC) content plays a key role in maintaining soil fertility in agricultural farm. At present, there has been great interest to reduce the atmospheric CO₂ level through a chain of increasing vegetation carbon pools first and then to store them as soil carbon pool. To quickly assess the soil carbon restoration programmes, it is important to know how much soil carbon is stored in an agricultural farm through adoption of different land management practices. Average SOC content is considered in most soil carbon pool calculations in spite of its large spatial variation in landscape, and thus leads to inaccurate estimate of SOC stock for an area. Therefore, reliable estimates of SOC pools and their spatial variability are essential to establish the soil carbon sequestration programmes at different landscape scales. Here, a case example of assessing the spatial variation at a typical agricultural farm is discussed. The experimental field was located at Badoda village of Jaisalmer district, Rajasthan covering an area of about 76.12 ha. The farm lies between 265^o2′30″-26°53′30″ N and 71°12′15″-71°13′15″ E (Fig. 24.1) and 20 km away from Jaisalmer city in eastward direction. Elevation of the farm ranged from 232 m to 248 m above mean sea level with an overall slope from south to north. Among total area of the farm, 85.38% area was under cultivation in four main blocks: block A, B, C, and D whereas rest area was under grassland.

Abstract

Any naturally occurring phenomena varies both in space and time. This variability is a result of various natural process and hence deterministic. Geostatistics is a tool to help us to characterize spatial variability and uncertainty resulting from imperfect characterization of the variability. Geostatistics involves the theory of regionalized variables, which dates back to the early fifties and includes concepts of random function and stationarity. Geostatistical mapping can be defined as analytical production of maps by using field observations, explanatory information, and a computer program that calculates values at locations of interest. There area number of spatial prediction models depending on the amount of statisticsinvolved in the analysis. Kriging is a generic name adopted by the geostatisticians for a family of generalized least- squares regression algorithms and various kriging algorithms viz., punctual kriging, block kriging, co-kriging and universal kriging are explained in this paper. Applications of geostatistics can be found in many varied disciplines ranging from the geology to soil science, hydrology, meteorology, environmental sciences, agriculture and even structural engineering and some of its applications are summarized in this paper.

Keywords :Geostatistics, spatial variability, kriging, model

It is a non-accelerated frictionless horizontal motion where pressure gradient balances coriolis acceleration as shown in Fig.4.1 in both the hemispheres.

Abstract

The recent disastrous tsunami of December 26, 2004 has not only alarmed the administrative and the planning machinery to have tsunami mitigation strategies for India. But also signalled the geoscientists to have a deeper look on the phenomenon of tsunami and the vulnerabilities of the Indian coasts. In this context, the authors have conducted a study primarily to evaluate the responses of the coastal Geosystems to the tsunami inundation, as it is a very vital component in f raming strategies for mitigating the effect of tsunami. The study has revealed that the central coastal parts of Tamil Nadu, namely Cuddalore – Nagapattinam districts, which were worst affected by the recent tsunami, expose a combination of landforms of tectonic, fluvial, fluvio – marine and marine processes. These different landforms have responded differently to the recent tsunami viz: as facilitators, carriers, accommodators, absorbers, barriers etc. on the basis of the same, different eco – friendly, cost effective and result oriented methods are suggested to mitigate the effects of tsunamis.

Introduction

Tsunami is an unfamiliar term and also a scantily referred term in the dictionaries in India till December 26, 2004. Even the students of geosciences were all along been taught about the origin and impact of tsunamis by citing examples from the Pacific Ocean. But the term tsunami has now become a widely known and a commonly deliberated phenomenon in India amongst various cross sections of the society irrespective of age and literacy. However, the historical tsunami data (USGS & GSI websites)

13.1 Introduction

Geothermal energy is the nature-based heat generated from within the earth. Underneath the earth’s relatively thin crust, temperature range from 1000 to 4000°C & in some areas, pressures exceed 138 MPa is available. Geothermal energy is most likely generated from radioactive thorium, potassium and uranium dispersed evenly throughout the earth’s interior which produce heat as part of the decaying process. This process generates enough heating, keep the core of the earth at temperature approaching 400°C. Composed primarily of molten nickel & iron, the core is thought to be surrounded by a layer of molten rock, the mantle at approximately 100°C. Nine major crustal plates float on the mantle & currents in the mantle cause the plates to drift, colliding in some areas and diverting in others. When two continental plates converge a complex series of chemicals in the form of molten magna rises in the earth’s crust and depending upon its magnitude, it may break the crust and reach at the earth surface. Volcano, hot spring, geysers & fumaroles are natural geothermal resources near the surface and perhaps where economic drilling operations can tap their heat and pressure.

Geraniaceae is a family of about 7 genera and 830 species which are
cosmopolitan in distribution and found widely in temperate and tropical regions.
Only 3 genera and about 25 species have been reported from India, mainly
from Himalayas. Some of the larger genera along with their approximately
reported species in parenthesis include Geranium (430), Pelargonium (280),
Erodium (80) and Monsonia (25). Well-known ‘geranium oil’ is distilled from
Pelargonium odoratissinum.
Pelargonium (syn. Geraniums, Stork bills) is an extremely popular garden
plant and has considerable economic importance in the market of ornamental
plants. Its genotypes and hybrids are grown in temperate regions. Its value as a
potential essential oil yielding crop is also mentioned. Geranium oil is widely
used in perfumery, cosmetics, pharmaceutical, and food industries. Oil has
anti-microbial, and pesticidal activities. The genus Pelargonium comprises
more than 280 species in 13 sections of which 33 have been originated in
southern parts of South Africa (Van der Walt and Vorster, 1988). It has been
reported that nearly 80 per cent diversity of Pelargoniums is centered in Cape
Province if African continent (South Africa, Zimbabwe and Mozambique).
Pelargoniums are popular seed and vegetatively propagated bedding and
pot plants with numerous phenotypes (Fish type, Ivy leaved, Regal, Angels,
Fancy leaves, Scented, Oak leaf) and cultivars (Double/ Bar/ Centre/ Ring/
Vein/ Picotee pattern/ Tulip/ Carnation/ Phlox/ Birds egg flowered) available
on the world market. True geranium is a bushy, aromatic plant. The stem is
cylindrical, woody at the base, pubescent, green when young and turning
brown with age. The leaves are highly aromatic in nature. Flowers are regular
and devoid of spur like appendages.

Introduction
Geranium is also known as cranesbill, scented geranium/rose geranium. It is adaptable over a wide range of soil conditions and drought tolerant. Being perennial aromatic herb, it is cultivated for rose scented essential oil extracted from leaves and tender shoots. The oil thus obtained is also called pelargonium oil or rose-geranium oil. The oil is of varied colour from colourless to pale yellowbrown or greenish. The genus Pelargonium belongs to the family Geraniaceae.
Origin
Geranium is native to sub-tropical southern Africa, and the most popular of bedding and green-house plants. The genus Pelargonium consists of about 600 species, which are annual, biennial, and perennials found in Cape province of South Africa.
Botany
The cultivated geraniums may belong to herbaceous to woody with thick fleshy leaves of round to lobed shape and deep cut. The flowers are present in terminal clusters with varying colours from white to pink, deep red and violet. Cultivated species are hybrids, having double flowers of mixed colours.

.1. Origin and distribution

• Native of the Cape Province in South Africa.

• Grown in India, South Africa, Belgium, China, Congo, Egypt, France, Madagascar, Morocco, Reunion Islands, Spain, former USSR countries.

• Commercially cultivated mainly in Nilgiris and Kodaikanal hills of Tamil Nadu, and in and around Bangalore in Karnataka.

5.2. Economic importance

• Very profound and strong rose like odour.

• Also known as rose geranium.

• Chief constituent of oil - geraniol and citronellol.

Abstract: Pelargonium (syn. Geranium), has become mainstay in temperate landscapes because of its ease of production and cultivation, long lasting bloom, range of plant habits and diversity of uses (perfumery, cosmetic, pharmaceutical and food industries). Confusion exists about nomenclature and taxonomic revision has attempted. Pelargoniums are popular seed and vegetatively propagated bedding and pot plants with numerous phenotypes (Fish type, Ivy leaved, Regal, Angels, Fancy leaves, Scented, Oak leaf) and cultivars (Double/ Bar/ Centre/ Ring/ Vein/ Picotee pattern/ Tulip/ Carnation/ Phlox/ Birds egg flowered) available on the world market. Their continued popularity has warranted extensive breeding and development of novel phenotypes particularly trailing growth habit, reduced plant size, compact form, manipulation of flowers (size, number, coloration, longevity, timing) and disease resistant cultivars. Increasing knowledge of the inheritance of traits, molecular genetic techniques and biotechnological applications are valuable tools aiding modern pelargonium breeders. The need of new cultivars remains strong as divergence among pelargonium market types increases, production system becomes more specialized and new market develops.

Geranium (Pelargonium spp.) belongs to the family Geraniaceae. The name Pelargonium was introduced by Johannes Burman a Dutch Botanist in 1738, from the Greek word “Pelargos” means stork because the seed head looks like a stork’s beak. Due to their long and beak-shaped fruits, they are also known by the name of cranesbills. Geraniums are popular flowering plants and grown as decorative pot plants for indoor and outdoor. There is a world demand for the rose geranium essential oil of Pelargonium species which contains geraniol, linalool and citronellol, substitutes for the expensive attar of roses in the perfume trade. Pelargonium species was known for their medicinal value by the earliest indigenous people (Swanepoel, 2009).

ORIGIN AND DISTRIBUTION

The plants originated from South Africa (Swanepoel, 2009), as well as Reunion, Madagascar, Egypt and Morocco and were introduced to European countries such as Italy, Spain and France in the 17^th century. Geranium includes around 422 species of flowering annual, biennial and perennial plants. Both Geranium and Pelargonium are genera in the Family Geraniaceae. Linnaeus originally included all the species in one genus. Geranium, but they were later separated into two genera by Charles L’ Heritier in 1789. Although members of the Pelargonium genus are often referred to as ‘Pelargoniums’ to try to avoid confusion, many people still use the older common name of ‘Geranium’.

Most of the Pelargonium plants cultivated in Europe and North America have their origins in South Africa. Geranium robertianum is found throughout Europe, Asia and North Africa where it grows on a variety of soils, rocks, tree trunks and decaying organic matter such as logs. It is a component of virtually all forest types there. In the Pacific Northwest it is primarily found west of the Cascade crest although it extends along the Columbia River in Klickitat County. Ecological structure of Geranium robertianum L. populations under natural conditions and in the garden in Poland. Geranium farreri found in China, in south Gansu and north-west Sichuan.

Geranium (Pelargonium spp.) belongs to the family Geraniaceae. The name Pelargonium was introduced by Johannes Burman a Dutch Botanist in 1738, from the Greek word “Pelargos” means stork because the seed head looks like a stork’s beak.  Due to their long and beak-shaped fruits, they are also known by the name of cranesbills. Geraniums are popular flowering plants and grown as decorative pot plants for indoor and outdoor. There is a world demand for the rose geranium essential oil of Pelargonium species which contains geraniol, linalool and citronellol, substitutes for the expensive attar of roses in the perfume trade. Pelargonium species was known for their medicinal value by the earliest indigenous people (Swanepoel, 2009).

Scientific name: Pelargonium graveolens L. Herit
Family: Geraniaceae
Geranium, scientifically known as Pelargonium graveolens L. Herit, belongs to the Geraniaceae family. This aromatic plant is highly valued for its essential oil, which boasts an intense rose-like fragrance. Geraniol and citronellol are the primary constituents of this oil. There are approximately 600 species within the genus Pelargonium, many of which possess a pleasant odor, although only a few have attained commercial significance.
Types of Geranium
There are two primary types of geranium: Algerian or Tunisian Type: Characterized by slender, erect plants with dark pink flowers. This variety contains 0.3% oil, with 57% 1-citronellol. It is commonly grown in the Nilgiris and is unsuitable for wet conditions. Reunion or Bourbon Type: Produces more bushy growth with light-pink flowers. The oil has a higher 1-citronellol content (59.4%). This variety is grown in the Nilgiris and Anamalais and is more suitable for wet conditions.

Gerbera (Gerbera jamesonii), a tender, stemless, perennial flowering plant, belongs to family Asteraceae. Gerbera was named in honour of the German botanist and naturalist “Traugott Gerber” who was a friend of Carolus Linnaeus. Gerbera is very popular and widely used as cut flower or as a decorative garden plant. It was discovered in 1878 near Barberton, eastern Transvaal (South Africa), therefore, referred as the Barberton daisy or Transvaal daisy. It is ideal for beds, borders and pots and is the fifth most important cut flower in the world.

ORIGIN AND DISTRIBUTION

Gerbera is originated from South Africa. The native distribution of genus Gerbera comprising 30 species, extends to Africa, Madagascar, tropical Asia and South America (Hansen, 1985 and Bremer, 1994). Whereas, it was also reported that gerbera is found in the temperate and tropical parts of Asia and Africa and about 7 species are recorded in India. This plant is distributed in the temperate Himalayas from Kashmir to Nepal. Gerbera is commonly seen on the dry slopes near Shimla and on hillsides above Gulmarg in Kashmir (Anon., 1956). The G. jamesonii is found naturally in grassland in sandy soils in Mpumalanga and Barberton district. The genus Gerbera has approximately 14 southern African species, some of which are found only in Western Cape. G. aurantica is endemic to the mist belt grassland region of KwaZulu-Natal and is known from approximately 9 scattered populations from Helahela in the south to Babanango in the north. This species is under threat of extinction due to habitat fragmentation and degradation. In India they are distributed in temperate Himalayas at altitudes of 1300-3200 metres and observed from Kashmir to Nepal.

The genus Gerbera is named in honour of German naturalist Traugott Gerber who travelled in Russia in 1743 and started first botanical garden in Moscow. However, for species i.e. jamesonii, it is a matter of different opinion. The jamesonii was named for Dr. L. S. Jameson, a British colonial statesman in South Africa who was one of the discoverers of this species, whereas in some literature, the species was named after Robert Jameson who collected live specimens while on a prospecting expedition to the Barberton district in 1884, even though the species collected on three earlier occasions by other people. In 1888, Medley Wood, the curator of the Durban Botanical Garden sent plants to Kew, which subsequently flowered. This is native to South Africa, Madagascar, Asia, South America and Indonesia.

The first official description of South African species G. jamesonii was made by J.D. Hooker in Curtis Botanical magazine with coloured illustration in 1889. An active society on this subject is to be found in Australia under the name W.A. Gerbera Society. The society has used a classification system of gerbera. The breeding of gerbera started at the end of the nineteenth century in Cambridge, England, when two South African sp. were crossed. G. jamesonii native to Natal and Transvaal and G. viridifolia from western Cape were crossed together by R. Irwin Lynch in 1887, after both these species were introduced to Cambridge Botanic Gardens by Jameson and the hybrid was named as G. x cantabrigensis.