Assesment of groundwater_potential_zones_for_bruhat_bangalore_mahanagara_pali...Mohammed Badiuddin Parvez
Groundwater is an important natural resource in present day, but of limited use due to frequent failures in monsoon, undependable surface water, and rapid urbanization and industrialization have created a major threat to this valuable resource. The present work is an attempt to integrate RS and GIS based analysis and methodology in groundwater potential zone identification in the BBMP study area with an aerial extent of 715.95 km2. By Mohammed Badiuddin Parvez
Identification of Groundwater Potential Zones in Vaippar Basin, Tamil Nadu, I...SagarChougule11
Groundwater is prominent part of the earth’s fresh water as well as main source of drinking water and survival source for many lives on earth. Groundwater potential zone identification can be done using advanced as well as recently developed geospatial technology such as Remote Sensing and GIS. GIS technology is useful for capturing, storing, and analyzing spatial data with the help of computer programming techniques. Here in identification of groundwater potential zone using of spatial elements which are related for infiltration of water into ground. For the groundwater potential zone analysis using of spatial layers like geology, geomorphology, rainfall, lineament, land use/land cover, drainage density, soil texture, soil depth etc.
The presentation was given by Mr. Bas Kempen & Ms. V.L. Mulder, ISRIC, during the GSOC Mapping Global Training hosted by ISRIC - World Soil Information, 6 - 23 June 2017, Wageningen (The Netherlands).
Assesment of groundwater_potential_zones_for_bruhat_bangalore_mahanagara_pali...Mohammed Badiuddin Parvez
Groundwater is an important natural resource in present day, but of limited use due to frequent failures in monsoon, undependable surface water, and rapid urbanization and industrialization have created a major threat to this valuable resource. The present work is an attempt to integrate RS and GIS based analysis and methodology in groundwater potential zone identification in the BBMP study area with an aerial extent of 715.95 km2. By Mohammed Badiuddin Parvez
Identification of Groundwater Potential Zones in Vaippar Basin, Tamil Nadu, I...SagarChougule11
Groundwater is prominent part of the earth’s fresh water as well as main source of drinking water and survival source for many lives on earth. Groundwater potential zone identification can be done using advanced as well as recently developed geospatial technology such as Remote Sensing and GIS. GIS technology is useful for capturing, storing, and analyzing spatial data with the help of computer programming techniques. Here in identification of groundwater potential zone using of spatial elements which are related for infiltration of water into ground. For the groundwater potential zone analysis using of spatial layers like geology, geomorphology, rainfall, lineament, land use/land cover, drainage density, soil texture, soil depth etc.
The presentation was given by Mr. Bas Kempen & Ms. V.L. Mulder, ISRIC, during the GSOC Mapping Global Training hosted by ISRIC - World Soil Information, 6 - 23 June 2017, Wageningen (The Netherlands).
identification of ground water potential zones using gis and remote sensingtp jayamohan
the identification of ground water potential zones using gis and remote sensing.The study is conducted in the Muvattupuzha block.The various parameters used are geology,geomorphology,rainfall,soil type,etc.
Geohydrological study of weathered basement aquifers in Oban Massif and envir...iosrjce
The focus of this research is to model the geohydrology of the precambrian Oban Massif using
geospatial techniques. Groundwater control indicators such as geology, geomorphology, drainage density,
lineament density, land use / land cover and slope steepness were derived from landsat ETM+
imagery, ASTER
DEM and SRTM DEM. Image processing software such as ENVI 3.2, ARC GIS9.2 and PCI Geomatica were
used for image processing , digitizing and lineament density computation respectively. Weighted averages of the
groundwater controlling factors were used to produce thematic maps of geology, lineament density, drainage
density, slope steepness, land use/land cover and geomorphological units. The thematic maps were overlaid in a
GIS environment to model the ground water potential map of the area. Arc GIS, Arc View and Map Info were
used for geographic Information System analysis. ERDAS imagine 8.6 and ENVI 4.2 were used for
georeferencing, image analysis and coordinate transformation. ASTER DEM was used for analysis of
geomorphology. For vegetation, discrimination in land cover / land use mapping band 4: 3: 2 for landsat ETM+
was used. Unsupervised was used to have a general idea of the area. Supervised classification was used for
final land use/ land cover mapping. Result show that geology, lineament density, and slope steepness are the
most influential groundwater controlling factors of groundwater potential. Their degree of influence can be
summarized as geology > lineament density> slope>geomorphology>drainage density>land use / land cover.
From the groundwater potential map, four groundwater potential zones: very good, moderately good, fair and
poor. Successful boreholes drilled in the groundwater favourable potential areas should be reticulated to the
neighbourhood with poor groundwater potentials to salvage groundwater problem in the study area.
SOIL LOSS ESTIMATION IN GIS FRAMEWORK: A CASE STUDY IN CHAMPABATI WATERSHEDAM Publications
RUSLE (Revised Universal Soil Loss Equation) is widely used to predict average annual rate of soil erosion. RUSLE parameters were assessed using Satellite Remote Sensing (RS) and GIS with a view to model soil erosion in CHAMPABATI watershed in Assam state. Assessment of soil erosion is useful in planning and conservation works in a watershed or basin. Modelling can provide a quantitative and consistent approach to estimate soil erosion under a wide range of conditions. The parameters of RUSLE model were estimated using remote sensing data and the erosion probability zones were deter-mined using GIS. The five major input parameters used in the study are Rainfall Erosivity Factor (R), Slope Length and Steepness Factor (LS), Soil Erodibility Factor (K), Cover and Management Factor (C) and Support Practice Factor (P). The R factor had been determined from monthly TRMM rainfall data of study area. The soil survey data from www.fao.org was used to develop the K factor and DEM of study area was used to generate topographic factor (LS). The value of P & C factor was obtained from land use land cover map & LANDSAT image respectively. Estimating C factor in this study involves the use of Normalized Difference Vegetation Index (NDVI), an indicator which shows vegetation cover, using the regression equation in Spatial Analyst tool of GIS Software. After generation of input parameters, analysis was performed for estimation of soil erosion using RUSLE model by spatial information analysis approach. The quantitative soil loss (t/ha/year) ranges were estimated and classified the watershed into different levels of soil erosion severity and also soil erosion index map was developed. The average annual soil losses of the study Watershed were then grouped into different severity classes based on the criteria of soil erosion risk classification suggested by FAO (2006). The estimated average annual soil loss for the study area is 5.8044 million t. yr-1.
Abstract Remote sensing has its application in various fields like geology and mineral exploration, geomorphology and modern geomorphic process modeling, nature mitigation studies, hazard zone mapping, eco system study in hills, plains, riverine, coastal, marine and volcanic landforms, forest and biomass inventory, fishery. Remote sensing plays a vital in various fields. This technique along with the GIS has been to study the geomorphological, hydro geological, land use/land cover, lithological, structural aspects/ features in the parts of Anaimalai, Pollachi and Udumalpet block of TamilNadu. Integrated approach using geographic information system provides cost effective support in resources inventory including land use mapping, comprehensive data base for resources, analytical tools for decision making and impact analysis for plan evaluation. GIS accept large volumes of spatial data derived from a variety of sources and effectively store, retrieve, manipulate, analyze and display all forms of geographically referenced information. Maps and statistical data can be obtained from the spatial integration and analysis of an area using GIS software. In order to assess the natural resource availability and its potentiality in parts of Anaimalai, Pollachi and Udumalpet block, Tamil Nadu, an integrated remote sensing and GIS based study has been conducted by adopting the standard procedures. The groundwater potential zone of any area is depends on geological formations; geomorphologic unit’s recharges characters, topography, and thickness of weathered and fractured zones. In the present study, area was taken to locate groundwater potential zones by integrated different thematic maps, remote sensing and geographic information system techniques. To find out the ground water potential zones, different thematic maps have been prepared and integrated each of them. They are mainly geology, geomorphology, land use / land cover, lineament etc. Groundwater potential zones have been prepared with help of integrating different thematic maps. This study area is finally to get the groundwater potential zones we have to classified few area such as high, moderate and low potential zones. Index Terms: Remote sensing, GIS, lithology, Geomorphology, Hydrology, landforms etc.
IJRET : International Journal of Research in Engineering and Technology is an international peer reviewed, online journal published by eSAT Publishing House for the enhancement of research in various disciplines of Engineering and Technology. The aim and scope of the journal is to provide an academic medium and an important reference for the advancement and dissemination of research results that support high-level learning, teaching and research in the fields of Engineering and Technology. We bring together Scientists, Academician, Field Engineers, Scholars and Students of related fields of Engineering and Technology.
Delineation of potential groundwater recharge zones plays a vital role in sustainable management of groundwater resources. The present study is carried out to identify the groundwater potential recharge zones in Multan, Pakistan by using Remote Sensing (RS) & Geographical Information System (GIS) for augmenting groundwater resources. In Multan district (Punjab, Pakistan), the increasing population and expansion of land use for agriculture have severely exploited the regional ground water resources. Land Use Land Cover (LULC) change is an accelerating phenomenon on the surface of earth driven by anthropogenic activities including urban expansion, deforestation, and climatic variations. Intensive pumping has resulted in a rapid decline in the level of water table as well as its quality. Better management practices and artificial recharge are needed for the development of sustainable groundwater resources. In order to address these issues Geographic information system (GIS) and Remote sensing (RS) are the most efficient methods for the identification and detection of Land Use patterns. All of these techniques are used for mapping and identification of groundwater potential analysis. This groundwater potential information will be useful for the effective identification of appropriate locations for extraction of water. This study should be done to delineate groundwater potential recharge zones by using different thematic layers that were overlaid in ArcGIS. In the overlay analysis, the weights (for various thematic layers) are allocated based on a review of published literature or by expert opinion. The assigned weights are then normalized and modified using the analytical hierarchical process (AHP). The potential recharge map thus obtained and divided into four zones (poor, moderate, good, and very good) based on their influence to groundwater recharge.
identification of ground water potential zones using gis and remote sensingtp jayamohan
the identification of ground water potential zones using gis and remote sensing.The study is conducted in the Muvattupuzha block.The various parameters used are geology,geomorphology,rainfall,soil type,etc.
Geohydrological study of weathered basement aquifers in Oban Massif and envir...iosrjce
The focus of this research is to model the geohydrology of the precambrian Oban Massif using
geospatial techniques. Groundwater control indicators such as geology, geomorphology, drainage density,
lineament density, land use / land cover and slope steepness were derived from landsat ETM+
imagery, ASTER
DEM and SRTM DEM. Image processing software such as ENVI 3.2, ARC GIS9.2 and PCI Geomatica were
used for image processing , digitizing and lineament density computation respectively. Weighted averages of the
groundwater controlling factors were used to produce thematic maps of geology, lineament density, drainage
density, slope steepness, land use/land cover and geomorphological units. The thematic maps were overlaid in a
GIS environment to model the ground water potential map of the area. Arc GIS, Arc View and Map Info were
used for geographic Information System analysis. ERDAS imagine 8.6 and ENVI 4.2 were used for
georeferencing, image analysis and coordinate transformation. ASTER DEM was used for analysis of
geomorphology. For vegetation, discrimination in land cover / land use mapping band 4: 3: 2 for landsat ETM+
was used. Unsupervised was used to have a general idea of the area. Supervised classification was used for
final land use/ land cover mapping. Result show that geology, lineament density, and slope steepness are the
most influential groundwater controlling factors of groundwater potential. Their degree of influence can be
summarized as geology > lineament density> slope>geomorphology>drainage density>land use / land cover.
From the groundwater potential map, four groundwater potential zones: very good, moderately good, fair and
poor. Successful boreholes drilled in the groundwater favourable potential areas should be reticulated to the
neighbourhood with poor groundwater potentials to salvage groundwater problem in the study area.
SOIL LOSS ESTIMATION IN GIS FRAMEWORK: A CASE STUDY IN CHAMPABATI WATERSHEDAM Publications
RUSLE (Revised Universal Soil Loss Equation) is widely used to predict average annual rate of soil erosion. RUSLE parameters were assessed using Satellite Remote Sensing (RS) and GIS with a view to model soil erosion in CHAMPABATI watershed in Assam state. Assessment of soil erosion is useful in planning and conservation works in a watershed or basin. Modelling can provide a quantitative and consistent approach to estimate soil erosion under a wide range of conditions. The parameters of RUSLE model were estimated using remote sensing data and the erosion probability zones were deter-mined using GIS. The five major input parameters used in the study are Rainfall Erosivity Factor (R), Slope Length and Steepness Factor (LS), Soil Erodibility Factor (K), Cover and Management Factor (C) and Support Practice Factor (P). The R factor had been determined from monthly TRMM rainfall data of study area. The soil survey data from www.fao.org was used to develop the K factor and DEM of study area was used to generate topographic factor (LS). The value of P & C factor was obtained from land use land cover map & LANDSAT image respectively. Estimating C factor in this study involves the use of Normalized Difference Vegetation Index (NDVI), an indicator which shows vegetation cover, using the regression equation in Spatial Analyst tool of GIS Software. After generation of input parameters, analysis was performed for estimation of soil erosion using RUSLE model by spatial information analysis approach. The quantitative soil loss (t/ha/year) ranges were estimated and classified the watershed into different levels of soil erosion severity and also soil erosion index map was developed. The average annual soil losses of the study Watershed were then grouped into different severity classes based on the criteria of soil erosion risk classification suggested by FAO (2006). The estimated average annual soil loss for the study area is 5.8044 million t. yr-1.
Abstract Remote sensing has its application in various fields like geology and mineral exploration, geomorphology and modern geomorphic process modeling, nature mitigation studies, hazard zone mapping, eco system study in hills, plains, riverine, coastal, marine and volcanic landforms, forest and biomass inventory, fishery. Remote sensing plays a vital in various fields. This technique along with the GIS has been to study the geomorphological, hydro geological, land use/land cover, lithological, structural aspects/ features in the parts of Anaimalai, Pollachi and Udumalpet block of TamilNadu. Integrated approach using geographic information system provides cost effective support in resources inventory including land use mapping, comprehensive data base for resources, analytical tools for decision making and impact analysis for plan evaluation. GIS accept large volumes of spatial data derived from a variety of sources and effectively store, retrieve, manipulate, analyze and display all forms of geographically referenced information. Maps and statistical data can be obtained from the spatial integration and analysis of an area using GIS software. In order to assess the natural resource availability and its potentiality in parts of Anaimalai, Pollachi and Udumalpet block, Tamil Nadu, an integrated remote sensing and GIS based study has been conducted by adopting the standard procedures. The groundwater potential zone of any area is depends on geological formations; geomorphologic unit’s recharges characters, topography, and thickness of weathered and fractured zones. In the present study, area was taken to locate groundwater potential zones by integrated different thematic maps, remote sensing and geographic information system techniques. To find out the ground water potential zones, different thematic maps have been prepared and integrated each of them. They are mainly geology, geomorphology, land use / land cover, lineament etc. Groundwater potential zones have been prepared with help of integrating different thematic maps. This study area is finally to get the groundwater potential zones we have to classified few area such as high, moderate and low potential zones. Index Terms: Remote sensing, GIS, lithology, Geomorphology, Hydrology, landforms etc.
IJRET : International Journal of Research in Engineering and Technology is an international peer reviewed, online journal published by eSAT Publishing House for the enhancement of research in various disciplines of Engineering and Technology. The aim and scope of the journal is to provide an academic medium and an important reference for the advancement and dissemination of research results that support high-level learning, teaching and research in the fields of Engineering and Technology. We bring together Scientists, Academician, Field Engineers, Scholars and Students of related fields of Engineering and Technology.
Delineation of potential groundwater recharge zones plays a vital role in sustainable management of groundwater resources. The present study is carried out to identify the groundwater potential recharge zones in Multan, Pakistan by using Remote Sensing (RS) & Geographical Information System (GIS) for augmenting groundwater resources. In Multan district (Punjab, Pakistan), the increasing population and expansion of land use for agriculture have severely exploited the regional ground water resources. Land Use Land Cover (LULC) change is an accelerating phenomenon on the surface of earth driven by anthropogenic activities including urban expansion, deforestation, and climatic variations. Intensive pumping has resulted in a rapid decline in the level of water table as well as its quality. Better management practices and artificial recharge are needed for the development of sustainable groundwater resources. In order to address these issues Geographic information system (GIS) and Remote sensing (RS) are the most efficient methods for the identification and detection of Land Use patterns. All of these techniques are used for mapping and identification of groundwater potential analysis. This groundwater potential information will be useful for the effective identification of appropriate locations for extraction of water. This study should be done to delineate groundwater potential recharge zones by using different thematic layers that were overlaid in ArcGIS. In the overlay analysis, the weights (for various thematic layers) are allocated based on a review of published literature or by expert opinion. The assigned weights are then normalized and modified using the analytical hierarchical process (AHP). The potential recharge map thus obtained and divided into four zones (poor, moderate, good, and very good) based on their influence to groundwater recharge.
Groundwater Potential Zone Identification of Karwi Area, Mandakini River Basi...inventionjournals
International Journal of Engineering and Science Invention (IJESI) is an international journal intended for professionals and researchers in all fields of computer science and electronics. IJESI publishes research articles and reviews within the whole field Engineering Science and Technology, new teaching methods, assessment, validation and the impact of new technologies and it will continue to provide information on the latest trends and developments in this ever-expanding subject. The publications of papers are selected through double peer reviewed to ensure originality, relevance, and readability. The articles published in our journal can be accessed online.
In developing accurate hydro geomorphological analysis, monitoring, ability to generate information in spatial and temporal domain and delineation of land features are crucial for successful analysis and prediction of groundwater resources. However, the use of RS and GIS in handling large amount of spatial data provides to gain accurate information for delineating the geological and geomorphological characteristics and allied significance, which are considered as a controlling factor for the occurrence and movement of groundwater used IRS LISS II data on 1: 50000 scale along with topographic maps in various parts of India to develop integrated groundwater potential zone
Identification Of Ground Water Potential Zones In Tamil Nadu By Remote Sensin...IJERA Editor
A case study was conducted to find out the groundwater potential zones in Salem, Erode and Namakkal districts, Tamil Nadu, India with an aerial extent of 360.60 km2. The thematic maps such as geology, geomorphology, soil hydrological group, land use / land cover and drainage map were prepared for the study area. The Digital Elevation Model (DEM) has been generated from the 10 m interval contour lines (which is derived from SOI, Toposheet 1:25000 scale) and obtained the slope (%) of the study area. The groundwater potential zones were obtained by overlaying all the thematic maps in terms of weighted overlay methods using the spatial analysis tool in Arc GIS 9.3. During weighted overlay analysis, the ranking has been given for each individual parameter of each thematic map and weights were assigned according to the influence such as soil −25%, geomorphology − 25%, land use/land cover −25%, slope − 15%, lineament − 5% and drainage / streams − 5% and find out the potential zones in terms of good, moderate and poor zones with the area of 49.70 km2, 261.61 km2 and 46.04 km2 respectively. The potential zone wise study area was overlaid with village boundary map and the village wise groundwater potential zones with three categories such as good, moderate and poor zones were obtained. This GIS based output result was validated by conducting field survey by randomly selecting wells in different villages using GPS instruments. The coordinates of each well location were obtained by GPS and plotted in the GIS platform and it was clearly shown that the well coordinates were exactly seated with the classified zones.
Evaluation of morphometric parameters derived from Cartosat-1 DEM using remot...Dr Ramesh Dikpal
The quantitative analysis of drainage system is
an important aspect of characterization of watersheds.
Using watershed as a basin unit in morphometric analysis
is the most logical choice because all hydrological and
geomorphic processes occur within the watershed. The
Budigere Amanikere watershed a tributary of Dakshina
Pinakini River has been selected for case illustration.
Geoinformatics module consisting of ArcGIS 10.3v and
Cartosat-1 Digital Elevation Model (DEM) version 1 of
resolution 1 arc Sec (*32 m) data obtained from Bhuvan
is effectively used. Sheet and gully erosion are identified in
parts of the study area. Slope in the watershed indicating
moderate to least runoff and negligible soil loss condition.
Third and fourth-order sub-watershed analysis is carried
out. Mean bifurcation ratio (Rb) 3.6 specify there is no
dominant influence of geology and structures, low drainage
density (Dd) 1.12 and low stream frequency (Fs) 1.17
implies highly infiltration subsoil material and low runoff,
infiltration number (If)1.3 implies higher infiltration
capacity, coarse drainage texture (T) 3.40 shows high
permeable subsoil, length of overland flow (Lg) 0.45
indicates under very less structural disturbances, less runoff
conditions, constant of channel maintenance (C) 0.9 indicates
higher permeability of subsoil, elongation ratio (Re)
0.58, circularity ratio (Rc) 0.75 and form factor (Rf) 0.26
signifies sub-circular to more elongated basin with high
infiltration with low runoff. It was observed from the
hypsometric curves and hypsometric integral values of the
watershed along with their sub basins that the drainage
system is attaining a mature stage of geomorphic development.
Additionally, Hypsometric curve and hypsometric
integral value proves that the infiltration capacity is high as
well as runoff is low in the watershed. Thus, these mormometric
analyses can be used as an estimator of erosion
status of watersheds leading to prioritization for taking up
soil and water conservation measures.
Watershed delineation and LULC mappingKapil Thakur
Watershed Delineation - a watershed as an enormous bowl. As water falls onto the bowl’s rim, it either flows down the inside of the bowl or down the outside of the bowl. The rim of the bowl or the watershed boundary is sometimes referred to as the ridgeline or watershed divide. This ridge line separates one watershed from
another.
Topographic maps created by the United States Geological Survey can help you to determine a watershed’s boundaries.
Land use and land cover map (LULC Mapping) -
Land cover indicates the physical land type such as forest or open water whereas land use documents how people are using the land. … Land cover maps provide information to help managers best understand the current landscape. To see change over time, land cover maps for several different years are needed.
Evaluation of Groundwater Resource Potential using GIS and Remote Sensing App...IJERA Editor
Environment and Development are the two wheels of the cart. However, they become antagonists at some
points. It has been witnessed many a times that development is done at the cost of environment. Analysis and
assessment tools like GIS along with Remote Sensing have proved to be very efficient and effective and hence
useful for management of natural resources. Groundwater is a precious resource of limited extent. In order to
ensure a judicious use of groundwater, proper evaluation is required. There is an urgent need of planned and
optimal development of water resources. An appropriate strategy is required to develop water resources with
planning based on conjunctive use of surface and subsurface water resources. Integrated remote sensing and GIS
can provide the appropriate platform for convergent analysis of diverse data sets for decision making in
groundwater management and planning. Sustainable water resources development and management necessarily
depends on proper planning, implementation, operation and maintenance. The interpretation of remote sensing
data in conjunction with conventional data and sufficient ground truth information makes it possible to identify
and outline various ground features such as geological structures, geomorphic features and their hydrologic
characters that may serve as direct or indirect indicators of the presence of ground and surface water. Remotely
sensed data provides unbiased information on geology, geomorphology, structural pattern and recharging
conditions, which logically define the groundwater regime of an area. Groundwater resource potential has been
evaluated in Pulivendula-Sanivaripalli, Kadapa district, Andhra Pradesh, India, using remote sensing and
Geographic information system. Under this study, three thematic maps viz. Geological map (Lithology and
Structure), Geomorphological map and Hydro morphological maps were prepared. These thematic maps have
been integrated with the help of GIS. Appropriate weightage has been assigned to various factors controlling
occurrence of groundwater to assess the groundwater potential in each segment of the study area. The area has
been classified into high potential, moderate potential, low potential and non-potential zones landforms ground
water development on the basis of hydromorphological studies. Some of the favorable locations have been
suggested to impound the excessive run off so as to augment the ground water resources of the area.
Evaluation of Groundwater Resource Potential using GIS and Remote Sensing App...IJERA Editor
Environment and Development are the two wheels of the cart. However, they become antagonists at some
points. It has been witnessed many a times that development is done at the cost of environment. Analysis and
assessment tools like GIS along with Remote Sensing have proved to be very efficient and effective and hence
useful for management of natural resources. Groundwater is a precious resource of limited extent. In order to
ensure a judicious use of groundwater, proper evaluation is required. There is an urgent need of planned and
optimal development of water resources. An appropriate strategy is required to develop water resources with
planning based on conjunctive use of surface and subsurface water resources. Integrated remote sensing and GIS
can provide the appropriate platform for convergent analysis of diverse data sets for decision making in
groundwater management and planning. Sustainable water resources development and management necessarily
depends on proper planning, implementation, operation and maintenance. The interpretation of remote sensing
data in conjunction with conventional data and sufficient ground truth information makes it possible to identify
and outline various ground features such as geological structures, geomorphic features and their hydrologic
characters that may serve as direct or indirect indicators of the presence of ground and surface water. Remotely
sensed data provides unbiased information on geology, geomorphology, structural pattern and recharging
conditions, which logically define the groundwater regime of an area. Groundwater resource potential has been
evaluated in Pulivendula-Sanivaripalli, Kadapa district, Andhra Pradesh, India, using remote sensing and
Geographic information system. Under this study, three thematic maps viz. Geological map (Lithology and
Structure), Geomorphological map and Hydro morphological maps were prepared. These thematic maps have
been integrated with the help of GIS. Appropriate weightage has been assigned to various factors controlling
occurrence of groundwater to assess the groundwater potential in each segment of the study area. The area has
been classified into high potential, moderate potential, low potential and non-potential zones landforms ground
water development on the basis of hydromorphological studies. Some of the favorable locations have been
suggested to impound the excessive run off so as to augment the ground water resources of the area.
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
info@kuddlelife.org
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
Natural farming @ Dr. Siddhartha S. Jena.pptxsidjena70
A brief about organic farming/ Natural farming/ Zero budget natural farming/ Subash Palekar Natural farming which keeps us and environment safe and healthy. Next gen Agricultural practices of chemical free farming.
WRI’s brand new “Food Service Playbook for Promoting Sustainable Food Choices” gives food service operators the very latest strategies for creating dining environments that empower consumers to choose sustainable, plant-rich dishes. This research builds off our first guide for food service, now with industry experience and insights from nearly 350 academic trials.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
Willie Nelson Net Worth: A Journey Through Music, Movies, and Business Venturesgreendigital
Willie Nelson is a name that resonates within the world of music and entertainment. Known for his unique voice, and masterful guitar skills. and an extraordinary career spanning several decades. Nelson has become a legend in the country music scene. But, his influence extends far beyond the realm of music. with ventures in acting, writing, activism, and business. This comprehensive article delves into Willie Nelson net worth. exploring the various facets of his career that have contributed to his large fortune.
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Introduction
Willie Nelson net worth is a testament to his enduring influence and success in many fields. Born on April 29, 1933, in Abbott, Texas. Nelson's journey from a humble beginning to becoming one of the most iconic figures in American music is nothing short of inspirational. His net worth, which estimated to be around $25 million as of 2024. reflects a career that is as diverse as it is prolific.
Early Life and Musical Beginnings
Humble Origins
Willie Hugh Nelson was born during the Great Depression. a time of significant economic hardship in the United States. Raised by his grandparents. Nelson found solace and inspiration in music from an early age. His grandmother taught him to play the guitar. setting the stage for what would become an illustrious career.
First Steps in Music
Nelson's initial foray into the music industry was fraught with challenges. He moved to Nashville, Tennessee, to pursue his dreams, but success did not come . Working as a songwriter, Nelson penned hits for other artists. which helped him gain a foothold in the competitive music scene. His songwriting skills contributed to his early earnings. laying the foundation for his net worth.
Rise to Stardom
Breakthrough Albums
The 1970s marked a turning point in Willie Nelson's career. His albums "Shotgun Willie" (1973), "Red Headed Stranger" (1975). and "Stardust" (1978) received critical acclaim and commercial success. These albums not only solidified his position in the country music genre. but also introduced his music to a broader audience. The success of these albums played a crucial role in boosting Willie Nelson net worth.
Iconic Songs
Willie Nelson net worth is also attributed to his extensive catalog of hit songs. Tracks like "Blue Eyes Crying in the Rain," "On the Road Again," and "Always on My Mind" have become timeless classics. These songs have not only earned Nelson large royalties but have also ensured his continued relevance in the music industry.
Acting and Film Career
Hollywood Ventures
In addition to his music career, Willie Nelson has also made a mark in Hollywood. His distinctive personality and on-screen presence have landed him roles in several films and television shows. Notable appearances include roles in "The Electric Horseman" (1979), "Honeysuckle Rose" (1980), and "Barbarosa" (1982). These acting gigs have added a significant amount to Willie Nelson net worth.
Television Appearances
Nelson's char
Willie Nelson Net Worth: A Journey Through Music, Movies, and Business Ventures
33. shyam sundhar, s. sanjeevi prasad and indrani mukherjee
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Journal of Global Resources Volume 6 (01) August 2019-January 2020 Page 207-213
UGC–CARE Listed Journal in Group D ISSN: 2395-3160 (Print), 2455-2445 (Online)
33
COMPARATIVE STUDY OF HIGH RESOLUTION SATELLITE IMAGES TO DEMARCATE
GROUNDWATER POTENTIAL ZONES IN SRIPERUMBUDUR, CHENNAI
Shyam Sundhar.V1, S. Sanjeevi Prasad2 and Indrani Mukherjee3
1Research Scholar, 2Assistant Professor, 3M.Sc. Student,
Department of Geography, University of Madras, Chennai, India
Abstract: The study focuses comparison of hyperspectral and multispectral imagery for
identifying the groundwater potential zones and aquifers of Sriperumbudur region. It also tries
to identify which image tends to be better for groundwater analysis without ground truth
verification. In present going to field and then selecting spot for digging the groundwater is
tiring and time taking. The need of conservation and its resource assumes more importance
than ever before. Water scarcity has always remained a problem in the city of Chennai. For
conserving of water, the study attempts to mark the potential zone which is exposed for
getting polluted and contributing to health risk. The various thematic maps have been
prepared such as landuse pattern, soil type, geology, geomorphology and lineament were
used for identifying the potential zone. Weightage and ranking were given to each parameter
before overlaying all the parameters. Therefore, the study is to sort the problem of ground truth
verification for identifying area, and identify the zone through remote sensing and Geographical
Information System (GIS).
Key words: Groundwater Potential, Hyperion, Geographical Information System
Introduction
Groundwater resource is considered to be the most important freshwater resource. With
increasing population in the metropolitan is not only threat to the reserve but also its quality.
The fast growing population needs a continuous supply for freshwater. For protecting these
zones, we need to find the zones and demarcate them. Hence taking Chennai as our study
area which is also a metropolitan city of India as well as it faces acute water scarcity
throughout the year. The groundwater potential zones are first identified and analyzed to find
out the status or condition of the zones in relation with the quality and what will be health
risks. To identify the groundwater potential zones, techniques of GIS and remote sensing
has been used. Thematic maps like geology, soil, and lineament has been prepared to
enhance the exploration of potential groundwater zones. Groundwater is presently found to
be most important freshwater source. As the rising population needs supply of water
therefore it has become mandatory to discover the potential zone of groundwater. A
standard technology applied to predict groundwater potential zone using remote sensing and
GIS techniques using various tools. Many thematic maps were created such as slope map,
lineament maps etc. The most significant recent breakthrough in remote sensing has been
the development of hyperspectral sensors and software to analyses the resulting image data.
Fifteen years ago only spectral remote sensing experts had access to hyperspectral
images or software tools to take advantage of such images. Over the past decade
hyperspectral image analysis has matured into one of the most powerful and fastest growing
technologies in the field of remote sensing.
Methodology
With satellite imagery of IRS-P6-LISS-IV (2013) lineament map was prepared, with same
parameters layer stacking of Hyperion image was also done to analyses the advantage. When
all this parameter was processed, then final overlay map with potential zone was derived.
Finally, NDVI was derived to analyses the presence of aquifer in the zone. The aquifer map
was compared with potential zone map to analyses the potential zone derived.
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Figure 01: Study Area Sri Perumbudur
Multispectral Analysis
As we can see in the map the tree features are dominant in the study area which are:
Argillaceous and calcareous sandstone and Granet-biotite-sillimanite graphite gneiss. The
clay is in least quantity in the area. The sand and silt is found only in the south eastern and
southern part of the study area.
Figure 02: Geology Map Figure 03: Soil Map
The map shows the area has 6 different types of soil which are: Clay, Clay loam, Sand,
Loamy sand, Miscellaneous land, Sandy clay loam, and Sandy loam. The western part of the
study area is dominated by loamy sand. The eastern part of the study area is covered by the
clay soils and less part is loamy sand. The study area shows good proportion of loamy sand
which helps in higher level of water penetration.
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Lineament Map and Geomorphological Map
This map shows that the maximum fractured areas in the study area are in western part. More
fractured areas were found in the northern and southern part of the study area in compare to
the central part of the study area. The maximum fracture lines are parallel to the eastern
boundary of the study area which is also a coastal line. The western part of the area has less
number of fractures in compare to the eastern part. This map shows the geomorphologic
features of the study area and 4 geomorphologic features are identified in the study area which
is: Alluvial Plain, Coastal Plain, Flood Plain, Pedi plain Structural hill. As we can see the coastal
plain is found along the coastal line and the alluvial plain is found in the western central part of
the study area, Pedi plain is found in the west northern and west southern part of the study
area and the flood plain is found in a linear manner in the central part of the study area. High
percolation of groundwater is found in the coastal plain and the others having low percolation
capacity.
Figure 04: Geomorphological Map Figure 05: Lineament Map
Figure 06: Land use and Land cover Map
Table 01: Land use Classification in Area
Land use Classification Area (in Hectares)
Vegetation 15129.4
Water bodies 2957.4
Settlement 50087.3
Wasteland 6741.0
Total 74915.5
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The map shows settlements, water bodies, vegetation and wasteland of the area. Here the
water bodies are very less and the settlements are more in the area. The LULC map suggests
that there is high population attraction due to satisfactory water availability.
Hyperion Analysis
Figure 08: Spectral Index Map Figure 09: Layer Stacking Map
Soil and Geology Map
The layer stacking has been done using band 10, 20 and 31 for soil and geology the layer
stacking helps to derive the yellow colour, which helps in identifying the various soil and rock
type by deriving the spectral reflectance in the map. The soil line of the soil reflectance
spectra, characterizes the soil type, defines vegetation indices, and corrects the plant canopy
reflectance from the optical soil property effects. Also with same band combination and
reflectance geology can be identified. Therefore, the reflectance value suggests mostly the
area is covered with the clayey materials. Also granite is identified with wavelength of least
reflectance value. The lesser reflectance value suggests that they have very minimum
capacity of holding water for soil. This compactness, porosity and permeability characterize the
area capability to penetrate water and recharge in the natural aquifer beneath.
Lineament Map
The map shows lineament distribution of the study area. The lineament shows the fractures of
the land which will penetrate or allow the water to percolate into the reach water table. The
lineament which is derived using band no.4 shows that the region is having high density of
lineament present especially in the southern part of the covered study area. Therefore, we can
estimate high penetration.
Fig 10: Lineament Map Figure 11: NDVI Map
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Normalized Difference Vegetation Index (NDVI)
The area basically shows coverage of medium level of vegetation coverage but also in few
patches are of higher vegetation. Water body’s area also identified along where higher
vegetation coverage is found. The area is maximum under medium coverage of vegetation,
which signifies that soil holds enough moisture for plants to grow. Also soil and geology helps
to promote its growth. After analyzing of all the features from the settled parameters the maps
have been overlay upon each other and with help of overlay analysis the potential zone map
has been prepared. Following were the ranks and weightage to given to each map before
overlaying them: With the given parameters the followed map was derived and that was divided
into three different zones:
High potential zone Medium potential zone Low potential zone
Table 02: Weightage and Ranking
Parameters Ranking Weightage (% of influence)
Geology 1 40
Lineament 2 35
Geomorphology 3 15
Soil 4 10
Figure 12: Potential Zone Map (LISS-IV) Figure 13: Potential Zone Map (HYPERION)
Potential Groundwater Zone Map
An overlay map has been prepared to show the possible potential zone for groundwater. The map
has been divided into three zones. The zones are marked as I, II and III. The derived map
suggests that the eastern part is highly potential zone with suitable geology and geomorphology
combination to enhance its aquifer to recharge and store the water. The western side is basically
medium potential zone and the northern zone is low potential it’s a minimum area. Therefore, we
can say the area is having good potential zone. So the area is having satisfactory water
potential in this area. Therefore, with done analysis and available data we can say that there is
aquifer present in zone. Along with information that it has satisfactory groundwater level and
quality we can say that it is recharged regularly and this helps it maintain its quality and marks it to
be safe.
The groundwater zone map has been prepared using Hyperion image. The rasters of soil,
geology and lineament are overlaid upon each other. The map is divided into three potential
zones that is high, medium and low potential water zone. The maximum zone comes under
medium potential zone and the southern part is having high potential zone. But the area
shows that there is good amount of lineament distribution, which shows that there is good
source of water penetration to charge water table. Hence we can say that area is satisfactorily
potential for groundwater.
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Aquifer Map
The principal aquifer system map has been derived from the secondary source. Here the
map shows various aquifers formed over the area and is compared with the derived potential
zone map. As per the principal aquifer system suggests that aquifers are mainly formed out of
four type rock system. The soil and the rock promote the storage and recharge of the
aquifers. The prepared map of the potential zone when compared with the aquifer map it
shows that aquifers are found mainly in the areas where there is suitable combination of soil,
geology, geomorphology, soil and lineament. The zone where medium and high potential
zone are concentrated, there mainly aquifers are spotted in the map. Hence we can interpret
that potential zone helps aquifer to develop.
Figure 14: Principal Aquifer System
Conclusion
While working with two different sets of satellite images different features were observed while
processing and analyzing: For multispectral image processing there should be satellite image
as well as geochemical data to derive the overlay analysis due to lesser amount of bands
whereas for hyperspectral image geochemical maps can be derived using the specific band
combination. There are more than 100 bands so combination of bands can be selected as per
requirement. In terms of area multispectral cover larger area in shorter temporal resolution i.e.
5 days, but hyperspectral covers lesser area in temporal resolution of 200 days. So to be
keeping updated and cover larger area multispectral is more preferable. Multispectral has
better spatial resolution but resolution for hyperspectral it’s not so clearer since the former has
5.8m and later has 30m resolution.
For processing and interpreting multispectral it’s easier as we derive can true colour
composite easily than processing Hyperion. Through the study it has being identified that
there cannot be full assurance of recharging the water table, through remote sensing analysis.
As we can find out that there is maximum content of clay which signifies that there is high
amount of porosity but this doesn’t contribute for recharging aquifers as the specific yield tends
to be negative. Hence it can be suggested that Hyperion is better for analysing potential zones
as the geophysical data can be derived with the Hyperion image. Better thematic layouts
can be given from the Hyperion image. As a limitation we can say that there should be
ground truth verification to suggest about presence and recharge of aquifers.
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