This document provides an inventory of springs in Karimba Panchayath, Palakkad District, Kerala. It identifies 36 springs through field surveys and GPS coordinates. The springs are classified as depression, contact, or fracture springs. Water quality analysis found pH and TDS were generally within limits, while electrical conductivity and coliform counts varied. Key threats identified were quarrying, landslides, and man-animal conflicts. The inventory aims to aid further environmental studies and management in the region.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
This document discusses the classification of springs based on hydrogeology. It defines different types of springs that form due to specific geological conditions: depression springs form in low-lying areas where the water table intersects land surface; contact springs occur at boundaries between permeable and impermeable rock layers; fracture springs form where joints or fractures intersect the surface; fault springs can develop along fault zones; and karst springs are commonly seen in limestone areas where solution features have formed. Spring discharge varies seasonally and by spring type, with factors like aquifer properties, catchment conditions, and recharge areas influencing output. A typology of springs is proposed considering geological setting and factors like discharge quantity and variability.
The document provides an overview of hydrology presented to Sir Hassan Rehman by Group #2. It discusses key topics of the presentation including the definition of hydrology, its scope and applications in civil engineering. It also examines various hydrological hazards such as floods, heavy rain, acidic rain and their effects. The presentation outlines steps to control hydrological hazards and discusses structures involved in hazard control as well as those affected by hazards. It concludes by asking if there are any questions.
Aquifer mapping is a multidisciplinary scientific process wherein a combination of geological, hydrogeological, geophysical, hydrological, and quality data are integrated to characterize the quantity, quality and movement of ground water in aquifers.
The Presentation gives the overview of the process necessary for accomplishing the task for the preparation of Ground water movements and identification carried out by Rajiv gandhi national drinking water mission project.
Springshed Management in HP_Dr Sunesh Sharma (PSI)_2014India Water Portal
This document summarizes a case study of springshed management in Sirmaur District of Himachal Pradesh, India. It provides demographic data and cropping patterns for the villages studied. Interventions included geological mapping, spring inventories, rain gauge installation, and formation of water management committees. Recharge structures like trenches and infiltration wells were constructed. Monthly water discharge was monitored and water quality improved after interventions. Impacts included formation of water user groups, increased and equitable access to water, improved source cleanliness, and a shift to more efficient irrigation patterns.
Morphometric analysis is the quantitative analysis of various characteristics of drainage basins based on parameters such as length, area, and relief. It involves categorizing parameters into linear, areal, and relief aspects to understand the geological structure, geomorphology, and hydrology of a basin. Common morphometric parameters studied include stream order, bifurcation ratio, stream number, length ratio, drainage density, texture ratio, and relief-related indices. Analyzing these parameters helps in watershed management and identifying groundwater potential and flood risks. While morphometric analysis provides quantitative insights, over-quantification without original thoughts and difficulties in precise measurements must be kept in mind.
Hydraulic geometry describes how a river's characteristics change with discharge both at a single cross section (at-a-station) and longitudinally along the channel (downstream). Key characteristics measured include depth, width, velocity, suspended sediment load, and slope. These parameters can be expressed as power functions of discharge and often follow similar patterns between rivers despite different settings. Hydraulic geometry was introduced by Leopold and Maddock to quantify these variations in channel geometry with flow.
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
This document discusses the classification of springs based on hydrogeology. It defines different types of springs that form due to specific geological conditions: depression springs form in low-lying areas where the water table intersects land surface; contact springs occur at boundaries between permeable and impermeable rock layers; fracture springs form where joints or fractures intersect the surface; fault springs can develop along fault zones; and karst springs are commonly seen in limestone areas where solution features have formed. Spring discharge varies seasonally and by spring type, with factors like aquifer properties, catchment conditions, and recharge areas influencing output. A typology of springs is proposed considering geological setting and factors like discharge quantity and variability.
The document provides an overview of hydrology presented to Sir Hassan Rehman by Group #2. It discusses key topics of the presentation including the definition of hydrology, its scope and applications in civil engineering. It also examines various hydrological hazards such as floods, heavy rain, acidic rain and their effects. The presentation outlines steps to control hydrological hazards and discusses structures involved in hazard control as well as those affected by hazards. It concludes by asking if there are any questions.
Aquifer mapping is a multidisciplinary scientific process wherein a combination of geological, hydrogeological, geophysical, hydrological, and quality data are integrated to characterize the quantity, quality and movement of ground water in aquifers.
The Presentation gives the overview of the process necessary for accomplishing the task for the preparation of Ground water movements and identification carried out by Rajiv gandhi national drinking water mission project.
Springshed Management in HP_Dr Sunesh Sharma (PSI)_2014India Water Portal
This document summarizes a case study of springshed management in Sirmaur District of Himachal Pradesh, India. It provides demographic data and cropping patterns for the villages studied. Interventions included geological mapping, spring inventories, rain gauge installation, and formation of water management committees. Recharge structures like trenches and infiltration wells were constructed. Monthly water discharge was monitored and water quality improved after interventions. Impacts included formation of water user groups, increased and equitable access to water, improved source cleanliness, and a shift to more efficient irrigation patterns.
Morphometric analysis is the quantitative analysis of various characteristics of drainage basins based on parameters such as length, area, and relief. It involves categorizing parameters into linear, areal, and relief aspects to understand the geological structure, geomorphology, and hydrology of a basin. Common morphometric parameters studied include stream order, bifurcation ratio, stream number, length ratio, drainage density, texture ratio, and relief-related indices. Analyzing these parameters helps in watershed management and identifying groundwater potential and flood risks. While morphometric analysis provides quantitative insights, over-quantification without original thoughts and difficulties in precise measurements must be kept in mind.
Hydraulic geometry describes how a river's characteristics change with discharge both at a single cross section (at-a-station) and longitudinally along the channel (downstream). Key characteristics measured include depth, width, velocity, suspended sediment load, and slope. These parameters can be expressed as power functions of discharge and often follow similar patterns between rivers despite different settings. Hydraulic geometry was introduced by Leopold and Maddock to quantify these variations in channel geometry with flow.
This document discusses basin morphometry, which involves quantitatively measuring the shape and geometry of drainage basins. It describes various linear, aerial, and relief properties that are measured, such as stream order, length, and number, drainage density, basin area and relief. These morphometric properties provide insights into surface processes, tectonic activity, and hydrological characteristics like flooding and sediment yield. Quantifying basin morphology allows comparisons between basins and improved modeling of terrain and hydrological systems.
This document discusses methods for groundwater exploration, including the lithological method. It begins with an introduction about groundwater and the need to explore new sources as existing shallow sources are depleted. The objectives of groundwater exploration are to identify locations where it is available through regional and detailed surveys. Surface exploration methods are described, including the lithological method of studying rock characteristics. Key concepts like porosity, permeability, lineaments, faults and joints are also explained in the context of understanding subsurface groundwater distribution. The conclusion states that lithological analysis is a basic first step to aid other exploration methods.
Introduction
Water resources of India at a glance
Hydrogeological cycle
Exploration of groundwater
Groundwater potential zone
Indicators
Sensors
Rules for selection of imagery
Conclusion
Reference
Concept and approach of springshed development and management 22 jan 2020India Water Portal
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
This document discusses principles of groundwater flow. It defines Darcy's law, which governs groundwater movement, and presents the governing equations for confined and unconfined aquifers. It also discusses flow nets, which can be used to graphically analyze groundwater flow, and the Dupuit equation, which approximates unconfined flow between two bodies of water. The document provides an example problem applying the Dupuit equation to calculate groundwater discharge to two rivers separated by 1,000 meters.
Classification either on quality or type based for groundwater can offer great advantages especially in regional groundwater management. It provides a short, quick processing, interpretation for a lot of complete hydro-chemical data sets and concise presentation of the results. There is a demonstrable need for a quality assurance, with the advanced usage of world's largest fresh water storage i.e Ground water. Its getting depleted over the years and the quality of the same degrading with a rapid pace. Ground water Quality is assessed mainly by the chemical analysis of samples. The data obtained from the chemical analysis is key for the further classification, analysis, correlation etc. Graphical and Numerical interpretation of the data is the main source for Hydro-chemical studies. In this paper we test the performance of the many available graphical and statistical methodologies used to classify water samples including: Collins bar diagram, Stiff pattern diagram, Schoeller plot, Piper diagram, Durov's Double Triangular Diagram, Gibbs's Diagram, Stuyfzand Classification. This paper explains various models which classify, correlate etc., summarizing the water quality data. The basic graphs and diagrams in each category are explained by sample diagrams. In addition to the diagrams an overall characterization of hydro-chemical facies of the water can be carried out by using plots which represents a water type and hardness domain. The combination of graphical and statistical techniques provides a consistent and objective means to classify large numbers of samples while retaining the ease of classic graphical presentation.
Drainage pattern and their significanceAvinashAvi110
The document discusses drainage patterns, their classification, and significance. It outlines different types of drainage patterns including dendritic, trellis, rectangular, parallel, and radial patterns. Drainage patterns are influenced by factors like slope, rock type, geologic structures, climate, and geomorphic history. Improper drainage can lead to flooding while well-developed drainage increases water storage and supplies, supports irrigation, and affects groundwater potential and sustainability. Different drainage patterns reveal information about the underlying geology.
This document presents information about groundwater and aquifers from a student presentation. It defines an aquifer as a saturated, permeable geologic unit that can transmit significant groundwater. It describes different types of aquifers including unconfined, confined, perched, artesian, and leaky aquifers. Examples are given of good aquifers like gravel, sand and limestone that allow easy groundwater movement, and poor aquifers like solid granite with low permeability.
Learning about Springs & Groundwater_ Dr.Jared Buono and Dr. Himanshu Kulkarn...India Water Portal
This is the presentation by Dr.Jared Buono and Dr. Himanshu Kulkarni on Springs, Aquifers and Ground Water. It talks about how springs are related to Ground water management and vice-versa.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
There are three main types of channels: straight channels found in the upper zone on rock, braided channels in the middle zone on coarse alluvial material with several intersecting channels, and meandering channels in the lower zone on fine alluvial material that regularly change position across the floodplain. The long profile of a river shows it has a concave shape from the steeper upper reach to gentler lower reach, with an ideal graded long profile existing in a state of dynamic equilibrium between erosion and deposition rates.
Fluvial Morphology handbook for students.
Contents are: definition, scope, importance of Fluvial Morphology, sediment load, channel pattern and process, role sediment to build delta, Reynolds number, Froude Number, channel pattern of Tista and Jamuna River, causes and consequences of flood, benefit of flood, flood and floodplain, hydraulic geometry, water resource management (in Bangladesh), hydrograph, origin and development of river, tributary and distributary and many more.
Groundwater levels fluctuate due to various factors. Secular variations occur over years due to changes in storage and recharge/discharge amounts. Seasonal variations result from rainfall and irrigation on well-defined cycles. Diurnal variations happen within a day due to tidal effects. Other causes of groundwater level changes include stream flows, evaporation, transpiration, atmospheric pressure, wind, rainfall, ocean tides, earth tides, external loads, earthquakes, urbanization, volcanic eruptions, roads, and continental drift.
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
Groundwater is water located beneath the Earth's surface. It is an important natural resource. Groundwater hydrology studies the occurrence, movement, and quality of subsurface water. Porous media such as rocks and unconsolidated deposits allow water to flow through voids and openings in the subsurface. Groundwater exists in saturated and unsaturated zones, with the saturated zone below the water table containing all interconnected voids filled with water. Aquifers are water-bearing formations that can supply usable amounts of groundwater. Properties like porosity, hydraulic conductivity, and storativity help determine how much and how quickly groundwater can flow through the subsurface.
This module gives an overview of general applications of current hydrogeological aspects. It is for the basic understanding of students and research scholars.
Prospect of Rain Water Harvesting In the Islands of the Sundarbans, the Activ...inventionjournals
International Journal of Humanities and Social Science Invention (IJHSSI) is an international journal intended for professionals and researchers in all fields of Humanities and Social Science. IJHSSI publishes research articles and reviews within the whole field Humanities and Social Science, 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
The document discusses the negative effects of coal mining in Jharkhand, India. It notes that coal mining has led to land degradation, loss of biodiversity, water pollution, exposure of toxic substances, and disruption of local communities' livelihoods. A case study of Jharkhand highlights how mining in the region has contaminated water sources and increased water-borne diseases in local tribes, reducing average life expectancy. Women and children are particularly impacted by needing to travel long distances to access clean water and living in unhygienic conditions. Mining waste has polluted rivers with heavy metals like arsenic and manganese, posing health risks.
This document discusses basin morphometry, which involves quantitatively measuring the shape and geometry of drainage basins. It describes various linear, aerial, and relief properties that are measured, such as stream order, length, and number, drainage density, basin area and relief. These morphometric properties provide insights into surface processes, tectonic activity, and hydrological characteristics like flooding and sediment yield. Quantifying basin morphology allows comparisons between basins and improved modeling of terrain and hydrological systems.
This document discusses methods for groundwater exploration, including the lithological method. It begins with an introduction about groundwater and the need to explore new sources as existing shallow sources are depleted. The objectives of groundwater exploration are to identify locations where it is available through regional and detailed surveys. Surface exploration methods are described, including the lithological method of studying rock characteristics. Key concepts like porosity, permeability, lineaments, faults and joints are also explained in the context of understanding subsurface groundwater distribution. The conclusion states that lithological analysis is a basic first step to aid other exploration methods.
Introduction
Water resources of India at a glance
Hydrogeological cycle
Exploration of groundwater
Groundwater potential zone
Indicators
Sensors
Rules for selection of imagery
Conclusion
Reference
Concept and approach of springshed development and management 22 jan 2020India Water Portal
Over the last decade, demand for spring management has increased as traditional spring sources have started drying up or becoming contaminated. In response, communities, NGOs and state agencies began dedicated spring protection programmes. In the Himalayas, the State of Sikkim and organizations such as Central Himalayan Action and Research Group (CHIRAG) and People Science Institute (PSI) started identifying and protecting spring recharge areas around 2007. The difference between these programmes and many other previous efforts is that they went beyond supply-side improvements to focus on the use of hydrogeology to map springsheds for targeted interventions.
The Advanced Centre for Water Resources Development and Management (ACWADAM), a research and capacity-building organization comprised of hydrogeologists and other experts began lending their expertise and building capacity of stakeholders. ACWADAM provides technical support, training and materials in hydrogeology to all network partners as well as others in India and the region. Similar programmes began independently in most of the mountain regions of India. Arghyam, a funding organization that was supporting many of these programmes, noticed that these disparate initiatives shared commonalities despite geographic diversity. They thus organized and funded a meeting of these various organizations in June 2014, and the Springs Initiative was born.
The springs initiative aims to tackle the current water crisis and to ensure safe and sustainable access to water for all, by promoting responsible and appropriate management of aquifers, springsheds, and watersheds and conserving ecosystems in partnership with communities, governments and other stakeholders.
This presentation has been developed as a part of the springs initiative to promote an understanding of springs and their role in mountainous areas.
This document discusses principles of groundwater flow. It defines Darcy's law, which governs groundwater movement, and presents the governing equations for confined and unconfined aquifers. It also discusses flow nets, which can be used to graphically analyze groundwater flow, and the Dupuit equation, which approximates unconfined flow between two bodies of water. The document provides an example problem applying the Dupuit equation to calculate groundwater discharge to two rivers separated by 1,000 meters.
Classification either on quality or type based for groundwater can offer great advantages especially in regional groundwater management. It provides a short, quick processing, interpretation for a lot of complete hydro-chemical data sets and concise presentation of the results. There is a demonstrable need for a quality assurance, with the advanced usage of world's largest fresh water storage i.e Ground water. Its getting depleted over the years and the quality of the same degrading with a rapid pace. Ground water Quality is assessed mainly by the chemical analysis of samples. The data obtained from the chemical analysis is key for the further classification, analysis, correlation etc. Graphical and Numerical interpretation of the data is the main source for Hydro-chemical studies. In this paper we test the performance of the many available graphical and statistical methodologies used to classify water samples including: Collins bar diagram, Stiff pattern diagram, Schoeller plot, Piper diagram, Durov's Double Triangular Diagram, Gibbs's Diagram, Stuyfzand Classification. This paper explains various models which classify, correlate etc., summarizing the water quality data. The basic graphs and diagrams in each category are explained by sample diagrams. In addition to the diagrams an overall characterization of hydro-chemical facies of the water can be carried out by using plots which represents a water type and hardness domain. The combination of graphical and statistical techniques provides a consistent and objective means to classify large numbers of samples while retaining the ease of classic graphical presentation.
Drainage pattern and their significanceAvinashAvi110
The document discusses drainage patterns, their classification, and significance. It outlines different types of drainage patterns including dendritic, trellis, rectangular, parallel, and radial patterns. Drainage patterns are influenced by factors like slope, rock type, geologic structures, climate, and geomorphic history. Improper drainage can lead to flooding while well-developed drainage increases water storage and supplies, supports irrigation, and affects groundwater potential and sustainability. Different drainage patterns reveal information about the underlying geology.
This document presents information about groundwater and aquifers from a student presentation. It defines an aquifer as a saturated, permeable geologic unit that can transmit significant groundwater. It describes different types of aquifers including unconfined, confined, perched, artesian, and leaky aquifers. Examples are given of good aquifers like gravel, sand and limestone that allow easy groundwater movement, and poor aquifers like solid granite with low permeability.
Learning about Springs & Groundwater_ Dr.Jared Buono and Dr. Himanshu Kulkarn...India Water Portal
This is the presentation by Dr.Jared Buono and Dr. Himanshu Kulkarni on Springs, Aquifers and Ground Water. It talks about how springs are related to Ground water management and vice-versa.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
There are three main types of channels: straight channels found in the upper zone on rock, braided channels in the middle zone on coarse alluvial material with several intersecting channels, and meandering channels in the lower zone on fine alluvial material that regularly change position across the floodplain. The long profile of a river shows it has a concave shape from the steeper upper reach to gentler lower reach, with an ideal graded long profile existing in a state of dynamic equilibrium between erosion and deposition rates.
Fluvial Morphology handbook for students.
Contents are: definition, scope, importance of Fluvial Morphology, sediment load, channel pattern and process, role sediment to build delta, Reynolds number, Froude Number, channel pattern of Tista and Jamuna River, causes and consequences of flood, benefit of flood, flood and floodplain, hydraulic geometry, water resource management (in Bangladesh), hydrograph, origin and development of river, tributary and distributary and many more.
Groundwater levels fluctuate due to various factors. Secular variations occur over years due to changes in storage and recharge/discharge amounts. Seasonal variations result from rainfall and irrigation on well-defined cycles. Diurnal variations happen within a day due to tidal effects. Other causes of groundwater level changes include stream flows, evaporation, transpiration, atmospheric pressure, wind, rainfall, ocean tides, earth tides, external loads, earthquakes, urbanization, volcanic eruptions, roads, and continental drift.
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
Groundwater is water located beneath the Earth's surface. It is an important natural resource. Groundwater hydrology studies the occurrence, movement, and quality of subsurface water. Porous media such as rocks and unconsolidated deposits allow water to flow through voids and openings in the subsurface. Groundwater exists in saturated and unsaturated zones, with the saturated zone below the water table containing all interconnected voids filled with water. Aquifers are water-bearing formations that can supply usable amounts of groundwater. Properties like porosity, hydraulic conductivity, and storativity help determine how much and how quickly groundwater can flow through the subsurface.
This module gives an overview of general applications of current hydrogeological aspects. It is for the basic understanding of students and research scholars.
Prospect of Rain Water Harvesting In the Islands of the Sundarbans, the Activ...inventionjournals
International Journal of Humanities and Social Science Invention (IJHSSI) is an international journal intended for professionals and researchers in all fields of Humanities and Social Science. IJHSSI publishes research articles and reviews within the whole field Humanities and Social Science, 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
The document discusses the negative effects of coal mining in Jharkhand, India. It notes that coal mining has led to land degradation, loss of biodiversity, water pollution, exposure of toxic substances, and disruption of local communities' livelihoods. A case study of Jharkhand highlights how mining in the region has contaminated water sources and increased water-borne diseases in local tribes, reducing average life expectancy. Women and children are particularly impacted by needing to travel long distances to access clean water and living in unhygienic conditions. Mining waste has polluted rivers with heavy metals like arsenic and manganese, posing health risks.
Sustainable Water Management in Cascade System: A model in Environmentally Se...Dr. P.B.Dharmasena
This document summarizes a presentation given at the International Water Conference in Sri Lanka on sustainable water management in tank cascade systems. Some key points:
- Tank cascade systems are a traditional Sri Lankan method of water resources management that store, convey, and utilize water across interconnected tanks and streams. This helps mitigate droughts and floods.
- The Village Tank Cascade System was declared a Globally Important Agricultural Heritage System by the UN's FAO for its sustainable practices.
- Challenges include high amounts of water lost to the sea each year, lack of coordination between water agencies, and ignoring traditional management systems.
- Tank cascades provide multiple benefits like food/water security, biodiversity,
Introduction
Origin of tank cascade concept
Tank cascade systems of Sri Lanka: Anatomy, distribution and definitions
Importance of cascade approach
Traditional tank-village ecosystem – adaptive capacity for the present situation
The document contains the study of the effects of coal mining in the state of Jharkhand in India. The unregulated coal mining has fully disrupted nature's stability. So many ecological issues has sprouted out due to 'merciless' mining. Overlooking the environmental concerns has been the primary factor for the lot of environmental repercussions. The degrading effects have also left its impacts on the social and cultural life of the tribal people.
MANAGEMENT OF NATURAL RESOURCES MADE BY MANASI INGLE AND GROUP CLASS XD K.V.B...Shephali Bose
The document discusses various topics related to natural resource management including pollution of the Ganges river, sustainable development practices like reduce, reuse and recycle, conservation of forests and biodiversity, management of water resources through traditional localized systems versus large dams, issues related to displacement due to dams, and community-based watershed management approaches. It provides details on conflicts between different stakeholders in forests and irrigation systems, and alternatives to large infrastructure projects that focus on decentralized local control and management of resources.
Watershed Restoration In Maragalakanda, Moneragala, Sri Lankaearthseva
The document describes a watershed restoration pilot project in Moneragala, Sri Lanka. The project site was an 8-acre degraded home garden with no trees, poor soil, and no water or biodiversity. After establishing shade trees and analog forestry techniques over two years, there was over 25% shade cover. Gullies on the land were planted with native riparian vegetation, creating a lush canopy. This led to increased soil moisture retention, more surface biodiversity like frogs and lizards, and improved water quality in the streams.
Inss In Aila Response And Post Response Need Assesment 2009Murshid Alam Sheikh
The document summarizes INSS's response efforts to Cyclone Aila, which caused widespread damage in Sundarban, India in May 2009. It describes the extensive damage to homes, crops, livestock and infrastructure. INSS provided relief through distribution of food, supplies and temporary shelter. Key activities included distributing NFI kits to over 20,000 families, food to over 33,000 families, repairing tube wells, constructing emergency latrines, cleaning villages and ponds, and public health activities through volunteers. The response aimed to reduce mortality and morbidity for over 30,000 affected households in the worst hit blocks of South 24 Paraganas district.
This is a presentation made to IESL members on 29th December 2019 at The Sigiriya Air Force premises.
Water resources management master plan in Sri Lanka includes not only irrigation but many more purposes.
The document discusses challenges facing India's rivers, including hydrologic and ecological transformations from human activities and climate change. It summarizes a study on estimating ecological flows in the Son River to protect endangered species like gharials and turtles. The study involved field measurements of river flows and habitat to develop a framework for adaptively managing dam releases. Updates are provided on a project studying the Gandak River basin, including mapping of gharial and dolphin distributions and examining irrigation efficiency to restore river flows and biodiversity. Solutions discussed include linking water use to ecological flows and using treated wastewater.
1. The document analyzes flood hazards in Dakshin Dinajpur district of West Bengal, India. It finds the main causes of flooding are insufficient river depths, heavy rainfall, water logging in low-lying areas, and weak embankments.
2. When flooding occurs, it leads to issues like river bank erosion, inundation of crops, forests, and homes, loss of lives and livestock. During major floods in the 1990s and 2000s, thousands of hectares were flooded and hundreds of thousands of people and livestock were affected.
3. To reduce flood hazards, the document recommends increasing river depths through dredging, strengthening flood protection infrastructure like embankments and sluice gates,
This document summarizes the outcomes of a scoping study on water security in peri-urban areas of Khulna, Bangladesh. 11 preliminary study sites were identified that face issues like water scarcity, flooding, wastewater discharge, and vulnerability to climate change impacts. Key research questions were outlined related to understanding the impacts of urbanization on peri-urban communities, water availability and quality trends, climate change vulnerabilities, and community strategies for reducing vulnerabilities. The scoping study utilized participatory methods to engage stakeholders and identify priority issues to guide further research and action.
Manchhar Lake is Pakistan's largest freshwater lake, located in Sindh province. It is oval-shaped and varies in size from 30 to 200 square miles depending on the season. The lake faces severe pollution problems from toxic waste discharged through drains, which has reduced its biodiversity and bird populations. Efforts are needed to reduce pollution and protect this important wetland habitat.
Manchhar Lake is Pakistan's largest freshwater lake, located in Sindh province. It is oval-shaped and varies in size from 30 to 200 square miles depending on the season. The lake faces severe pollution problems from toxic waste discharged through drains, which has reduced its biodiversity and bird populations. Efforts are needed to reduce pollution and protect this important wetland habitat.
Manchhar Lake is Pakistan's largest freshwater lake, located in Sindh province. It is oval-shaped and varies in size from 30 to 200 square miles depending on the season. The lake faces severe pollution problems from toxic waste discharged through drains. This waste has turned the lake water green and toxic, reducing the fish population and number of migratory birds that visit. Efforts are needed to reduce pollution and save this important habitat.
Manchhar Lake is Pakistan's largest freshwater lake, located in Sindh province. It is oval-shaped and varies in size from 30 to 200 square miles depending on the season. The lake faces severe pollution problems from toxic waste discharged through drains, which has reduced the number of migratory birds from 20,000-30,000 to much lower levels and made the water unsuitable for humans and fish. Efforts are needed to reduce pollution and protect the biodiversity of this once-beautiful lake and habitat.
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Slide on spring dissertation
1. INVENTORY OF SPRINGS IN
KARIMBA PANCHAYATH,
PALAKKAD DISTRICT
Suparna s
CUARMES019
Dept.Environmental science
University of calicut
UNDER THE SUPERVISION OF
SATHEESH R
HEAD ,NRM DIVISION
IRTC PALAKKAD
2. INTRODUCTION
WHAT IS A SPRING ?
A spring is a point at which water flows from an aquifer to the
Earth’s surface.
INVENTORY OF SPRINGS
Inventory of springs is an important step towards the detailed
study of environmental areas such as Groundwater trend
analysis,Water quality analysis,land usage,human-animal conflict
study, Irrigation,water shed development.
Inventory of springs’ deals with the mapping of natural springs in
karimba panchayath
3. A large proportion of population in this region depends on
spring water for fulfilling their livelihood and domestic needs
such as drinking and irrigation.
Spring water is considered as purest water than other forms
of freshwater.
Studies indicates that the deforestation,landuse-
change,intense grazing,reduced water retention capacity of
the catchments declining rainfall in some localities have led
to diminishing discharge of the springs
4. Classification of springs
1. Depression spring : Formed when water table reaches the
surface due to topographic undulations.Topographic depression
intersects an unconfined aquifer.
2. Contact spring : Water-bearing stratum overlies an impermeable
stratum.Water discharges where the contact zone between the
strata intersects the landsurface.
3. Fracture spring : Occurs due to existence of jointed or
permeable fracture zones in low permeability rocks.The fracture
zone between two opposing rock strata provides a flow path for
groundwater to discharge.
5. OBJECTIVES
To prepare the inventory of all springs in Karimba
Panchayath.
Analysis of Spring water quality and water usage
pattern.
Impacts observed on springs caused by various
human interventions.
6. MATERIALS AND METHODS
STUDY AREA
Karimba panchyath is a grama panchayth situated in palakkad
district, mannarkad block.The largest town in karimba panchayth
is kalladikodu.The total geographical area of this panchayath is
69.22 sq Km.
.Karimba panchayath is rich in traditional farming and water
harvesting systems.The major crops cultivated in this panchayath
is pepper, rubber,arecanut,coconut,nutmeg,mango,paddy,banana.
Inventory of 36 springs were spotted at this region and most of
springs were identified as perennial springs.
7. DATA COLLECTION.
Data is collected from the field directly.
Inventory of springs were carried out with the help of native
people of the study area and also by preparation of question airs.
A handheld GPS was carried out to spring locations for
identification of the geocoordinates of the springs,GPS mobile
application is used in accordance with the availability.
Spring ID was given in a pattern,i.e the first 2 letters consist of
name of the state Kerala(Ke),Mannarkad block panchayath (Ma)
and Karimba grama panchayath (Ka) was taken respectively and
finally the numbering as (01,02,03....35) was given in the order
for identification
8. METHODOLOGY FOR WATER QUALITY ANALYSIS
Measuring of discharge of spring water is done by carrying a 1
liter bottle and measuring its discharge in liter per minute
SL.
No.
WATER QUALITY PARAMETERS METHEDOLOGY ADOPTED
1 pH Electrometric method
2 Electrical conductivity Water quality analyzer
3 Total dissolved solids Water quality analyzer
4 Alkalinity Acid base titration
5 Coliform Most probable number method
10. SPRING INVENTORY DATA SHEET
Spring ID : Ke Ma Ka 01
Name : Mankulam
Area : Moonekar
Village : Karimba
Landmark : Chulliyamgulam
Latitude : 10° 55’ 41.26” N
Longitude : 76° 34’ 2.12 ” E
Elevation : 397.8m
(with GPS)
Discharge : 8LPM
Diameter of the pipe : ½ inch
Land ownership : This is a private property.
Type of spring : Fracture spring
Seasonality of spring: Perennial
11. Number of people depending on spring water: At present 3
families are mainly depending on spring water this is mainly
used for drinking purposes.
Land use around the spring: The main plantations that is covered
around the region i.e the lower landuse area is rubber, cocconut,
coffee, arecanut. And the upper region is covered by forest.
12. Most common animal species found around the region:
Elephant,Deer, Leapord, Wild Ox, Monkey, Snakes, Leopard,
babbler ,koel, parrot,myna, sparrow, Monarch butterfly ,Common
jezebel.
From the PRA conducted(enclosed in Annexure 1) it is noticed
that Barking Deer an animal which became extinct from past few
years.
Wild animal like elephant creates a major conflict that the
common people are not able to collect the spring water from the
pipes because these elephants destroy the connection pipes and
people are in trouble and they are unable to use the water.
13. Spring ID : Ke Ma Ka 02
Name : Maruthuamkadu
Area : kalamkunnu mundanadu
Colony
Village : Palakkayam village
Landmark : Marathumkadu
U.P school
Latitude :10°55’.1.14” N
Longitude : 76°33’0.76” E
Elevation : 123.4 m
Discharge : 7 LPM
Diameter of the pipe : ¼ Inch pipe
Type of spring : Contact spring
Seasonality of the spring : Perennial
14. Ownership : Government property.
Number of families depending on spring water: at present 6 families are using
this water for all purpose like drinking,irrigation
THREATS THAT IS OBSERVED IN THIS REGION.
• Active quarrying is one of the leading environmental problem that are faced
by the common people.Quarrying has started 25 years ago there are no legal
policies framed to stop this quarry .
• A large mountain is completely destroyed due to quarry . Families who are
staying in this locality are facing many problems .Most of the houses which
are constructed were completely destroyed and many people were injured
due to falling of asbestos sheet when quarrying was taking place.The injured
people were not given treatment facilities by the panchayath..
15. • 15-16 houses are present around this quarry most of the people
shifted there house to relief camps.
• legal actions were not taken by the government to stop this
quarry.
16. RECOMMENDATIONS.
• Environmental clearance should be given by the authorities
• Quarrying has become a major threat in this locality.Legal steps
should be taken for regulating the quarrying.
17. Spring ID : Ke Ma Ka 03
Name : Parakuzhi
Area : Vakkodu Colony
Village : Karimba
Landmark : Chulliyampali
Latitude : 10°54’ 56.7”N
Longitude : 76°32’ 9.97”E
Elevation : 124.6 m
Ownership : Private property
Seasonality of the spring : Perennial
Type of spring: Fracture spring
18. • 1 year before the water was used by people at present no body
is using the water.
• In this area,rubber is cultivated from the last 15-20 years
,recently the rubber cultivation is changed to pineapple
cultivation.This process is repeated at certain intervals of time.
• Landslide occured in this region during the floods and this has
become a threat in that region. .
• 1 year before the water was used by people but now no one is
using.
19. Spring ID : Ke Ma Ka 04
Name : Vakkodu
Area : Vakkodu
Village : Karimba
Landmark : chulliyampalli
Lattitude : 10°54’ 7.42”N
Longitude : 76° 32’ 9.83”E
Elevation : 89.2m
Ownership : Private property
Seasonality of the spring: Perennial
Type of spring : Fracture spring
20. • The main landuse covering the lower region is rubber plantation.
• At 2018 heavy flood occured in this locality causing landslide
has lead a major problem .The spring in this region is in partially
damaged condition.
• This water is not used from the last one year.
21. Spring ID : Ke Ma Ka 05
Name : Kallamkunnu
Area : Moonnekar
Village : Karimba
Landmark : Anakallu Quarry
Lattitude : 10°55’ 30.75”N
Longitude : 76°33’26.49”E
Elevation : 320 m
Ownership : Private property.
Discharge : 2 ½ LPM
Diameter of the pipe: ½ inch
Seasonality of the spring: Perennial
22. • Number of families depending on spring water: From past 42
years only 1 family is using spring water for all there purposes.
This area belongs to Karimba plantations.
• Man-Animal conflict is experienced in this area, wild pigs travel
at night and break the connection pipes and people are unable to
store the water in their tanks.
• : Most common animal species found around the region: wild
pigs, elephant,deer, wild ox are some of the species found.
• Landuse: lower region is covered by different planations mainly
coocunt,nutmeg,bannana,rubber,arecanut,mango and upper
region is covered by forest.
23. Spring ID : Ke Ma Ka 06
Name : Kariyatti
Area : Moonnekar
Village : Karimba
Landmark : Chulliyanpalli
Lattitude : 10°55’42.55”N
Longitude : 76°33’56.78”E
Discharge : 10 LPM
Elevation : 208.6 m
Diameter of the pipe: 1 ¼ inch
Ownership : Private property
Seasonality of the spring: Perennial
Type of spring : Depression spring
24. • Number of families depending on spring water:Only one
family is using the water for all purposes from past 10 years.
Family who are living in this area have no other source of
water they mainly depend on spring water.
25. Spring ID : Ke Ma Ka 07
Name : Cherumala
Area : Kallumthodu
Village : Karimba
Landmark : Chulliyanpalli
Lattitude : 10°54’45.4”N
Longitude : 76°33’49.9”E
Ownership : Forest land
Seasonality of the spring: Perennial.
• A spring box is present in which the water is collected and
stored
26. Spring ID : Ke Ma Ka 09
Name : Marathamkaadu
Area : Kallamkunnu
Village : Palakkayam
Landmark :Marathumkkad U.P School
Lattitude : 10°55’52.19”N
Longitude : 76°32’24.93”E
Elevation : 218.8m
Ownership : Private property
Discharge : 6 ½ LPM
Type of spring: fracture spring
27. Diameter of the pipe: ½ Inch pipe
Number of families depending on spring water: at present only 1
family is using the water that is only used for domestic purpose.
In this region no cultivation is done.
28. Spring ID : Ke Ma Ka 10
Name : Kurumugham
Area : Karimala
Village : Karimba
Landmark : Moonnekar church
Lattitude : 10°55’42.24”N
Longitude : 76°34’7.31”E
Elevation : 210.6
Seasonality of the spring: Seasonal
Type of spring : Depression spring
Ownership : Private property
29. WATER QUALITY ANALYSIS OF SPRING SAMPLES
SPRING ID pH Electrical
conductivity
Total
dissolv
ed
solids
Alkalinit
y
Colifor
m
Ke Ma Ka 28 8.05 90.44 50.18 45 74
Ke Ma Ka 26 7.79 51.37 43.20 25 240
Ke Ma Ka 24 7.92 54.09 31.57 30 23
Ke Ma Ka 18 8.06 58.40 33.80 32 96
Ke Ma Ka 17 6.0 51.31 28.32 25 1100
Ke Ma Ka 11 8.23 94.1 55.66 50 23
Ke Ma Ka 08 7.92 45.95 26.82 25 120
Ke Ma Ka 06 7.82 69.48 39.71 35 67
Ke Ma Ka 03 7.97 76.15 41.83 40 480
Ke Ma Ka 01 7.85 82.98 46.55 43 250
30. Majority of samples have Ph range within the desirable limit.
Ke Ma Ka 17 Ph is less than the permissible limit but the Ph is
also close to neutral level.
TDS is within the permissible limit.
Alkalinity is permissibile within the limit.
Electrical conductivity is higher in Ke Ma Ka 11(94.1) and low
conductivity in Ke Ma Ka 08 (45.95).
Coliform bacteria is higher in Ke Ma Ka 17 (1100) and the
water is not potable to drink.
31. Consolidated data sheet of Spring Inventory
Sl
No
Spring ID Name Latitude Longitude Elevation Ownership
Seasonal /
Perennial
Type of
spring
Use of water
No.of families
depending
Any
environmental
issues faced
1 Ke Ma Ka 01 MANKULAM 10° 55’ 41.26” N 76° 34’ 2.12”E 397.8 m Private Perennial Fracture Drinking 3 No issues
2 Ke Ma Ka 02 MOONEKAR 10° 55’ 67.6” N 76° 33’ 89.7” E 105.8 m Private Perennial Fracture Irrigation 1 -
3 Ke Ma Ka 03 MARUTHUAMKADU 10° 55’.1.14”N 76°33’0.76”E 123.4 m Government Perennial Contact Drinking & irrigation 6 Quarrying
4 Ke Ma Ka 04 MARUTHAMKADU 10° 55’ 1.14” N 76°33.1565”E 300.3 m Government Perennial Contact Drinking - -
5 Ke Ma Ka 05 MARUTHAMKADU 10°55’24.11”N 76°32’43.11”E 361.7 m Government Perennial Depression Irrigation - -
6 Ke Ma Ka 06 MARATHAMKADU 10°55’52.19”N 76°32’24.93”E 218.8m Private Perennial Fracture Domestic - -
7 Ke Ma Ka 07 KALLADIKODUMALA 10°54’2.69”N 76°33’ 3.85”E 306.4 m Government Perennial Fracture Domestic - -
8 Ke Ma Ka 08 KALLADIKODUMALA 10°54’3.20”N 76°33’3.85”E 380.5 m Government Perennial Fracture Domestic 18 -
9 Ke Ma Ka 09 PARAKUZHI 10°54’56.7”N 76°32’ 9.97”E 124.6 m Private Perennial Fracture - - -
10 Ke Ma Ka 10 VAKKODU 10°54’ 7.42”N 76°32’ 9.83”E 89.2 m Private Perennial Fracture - - land slide threat
11 Ke Ma Ka 11 KALLAMKUNNU 10°55’ 29”N 76°33’ 17”E 175 m Private Perennial Fracture Drinking - -
12 Ke Ma Ka 12 KALLAMKUNNU 10°55’ 30.75”N 76°33’ 26.49”E 320 m Private Perennial Fracture Domestic - -
13 Ke Ma Ka 13 KALLAMKUNNU 10°55’ 27”N 76°33’ 14”E 357 m Forest land Perennial Fracture - - -
14 Ke Ma Ka 14 KALLAMKUNNU 10°55’24”N 76°33’ 10”E 102 m Private Perennial Fracture - - -
15 Ke Ma Ka 15 KALLAMKUNNU 10°55’ 32.43”N 76°33’ 24.15”E 250 m Private Perennial Depression Irrigation - -
16 Ke Ma Ka 16 KARIYATTI 10°55’ 31.98”N 76°33’ 47.08”E 309.1 m Private Perennial Fracture Drinking 4 -
17 Ke Ma Ka 17 KARIYATTI 10°55’ 42.55”N 76°33’ 56.78”E 208.6 m Private Perennial Depression Domestic 1 -
18 Ke Ma Ka 18 CHERUMALA 10°54’ 49.4”N 76°33’ 48.0”E 193 m Private Perennial Fracture Domestic 8 -
19 Ke Ma Ka 19 CHERUMALA 10°54’ 49.4”N 76°33’ 48.0”E 198 m Private Perennial Fracture Domestic and irrigation 1 -
20 Ke Ma Ka 20 CHERUMALA 10°54’ 46.4”N 76°33’ 47.1”E 209 m Private Perennial Contact Irrigation 1 -
21 Ke Ma Ka 21 CHERUMALA 10°54’45.4”N 76°33’ 49.9”E 200 m Forest land Perennial Spring box - - -
22 Ke Ma Ka 22 CHERUMALA 10°54’ 39”N 76°33’ 10”E 156 m Private Perennial Fracture Irrigation 4 -
23 Ke Ma Ka 23 CHERUMALA 10°55’ 38”N 76°32’ 10”E 320.1 m Private Perennial Contact Domestic 6 -
24 Ke Ma Ka 24 CHERUMALA 10°55’ 23.53”N 76°34’ 16.23”E 245.8 m Private Perennial Contact Nobody - -
25 Ke Ma Ka 25 CHERUMALA 10°55’ 3”N 76°32’ 44”E 300.2 m Private Perennial Contact - - -
26 Ke Ma Ka 26
THUDUKKADU
COLONY
10°54’48.42”N 76°34’8.17”E 210.6 m Private Perennial Fracture Domestic 1 -
27 Ke Ma Ka 27 MANALATHODU 10°55’23.61”N 76°34’16.61”E 279.2 m Private Perennial Fracture Nobody - -
28 Ke Ma Ka 28 MANALATHODU 10°55’28.62”N 767°34’ 15.87”E 164.2 Private Perennial Fracture Domestic 1 -
29 Ke Ma Ka 29 MANALATHODU 10°55’37”N 76°32’12”E 390 m Forest land Perennial - - -
30 Ke Ma Ka 30 KURUMUGHAM 10°55’40.57”N 76°34’5.04”E 135.9 m Private Perennial Depression Domestic 6 -
31 Ke Ma Ka 31 KURUMUGHAM 10°55’35.39”N 76°34’5.99”E 260 m Private Perennial Depression Nobody - -
32 Ke Ma Ka 32 KURUMUGHAM 10°55’36.5”N 76°33’59.12”E 220.3 m Private Perennial Depression Nobody - -
33 Ke Ma Ka 33 KURUMUGHAM 10°55’42.24”N 76°34’7.31”E 210.6 m Private Seasonal Depression Nobody - -
34 Ke Ma Ka 34 KURUMUGHAM 10°55’46.58”N 76°34’4.96”E 239.2 m Private Perennial Nobody - -
35 Ke Ma Ka 35 KURUMUGHAM 10°55’39.32”N 76°33’48.08”E 262.4 m Private Perennial Fracture Nobody - -
32. CONCLUSION
• The present study deals with the inventory of springs in
Karimba Panchayath. Inventory of 35 springs were done in the
study area and 34 springs were found to be perennial and only 1
spring was identified as seasonal
• The inventory of springs is very essential as a first step towards
analyzing water usage, keep track of land usage, analyzing the
trend of water abundance and adopting further scientific
conservative measures to protect the precious resource.
• There are 35 families in the study area directly dependent on
spring water as a major source for drinking and domestic
purposes.
33. • Discharge was noted throughout the study there may be decline in
the discharge if unfavorable natural conditions like precipitation
is insufficient, rate of evaporation decreases, adverse climate
change etc.
• The landuse around the spring shows a variety of forest,
plantation, agricultural field, mixed vegetation. The water quality
parameters were analyzed and the results showed that the spring
water is potable to drink and except in 2 samples coliform
bacteria level was observed to be high.
• Further studies are necessary that more springs can be present in
the study area . Springs should be located, mapped and analyzed.
• Thorough environmental impact study must be conducted and the
quarrying is to be regulated that is observed from the study area.
35. PARTICIPATORY RURAL APPRAISAL
1. Name of the spring :
2. Spring Location :
3. Name of the village:
4. Landuse around the spring location:
5. Geographic location using GPS:(Latitude), (Longitude)
6. Elevation from MSL:
7. Ownership: Private/Govt land/Forest land:
8. Type of spring: Depression/Contact/Fracture
9. Seasonality of the spring: Seasonal/Perennial
10. How many months water is available?
11. Discharge in LPM
12. Climatic conditions of that area?
13. Number of families depending on spring water:Purpose : Drinking/Agricultural.
14. Change in availability of water in the last 3 decades:
15. Is there any change in availability of water from the spring:?
16. Any quarries are operating above the spring location or below?
17. Drilled borewells?Yes/No
18. Did you noticed any kind of species (Flora or fanuna) that became extinct in the nearby area?
19. Whether any conflicts experienced in utilizing spring water?
20. Deforestation is happened or not? If yes, give details (Quarrying/ Construction/Conversion to
agricultural land).
21. Whether spring boxes constructed for collecting water?
22. Any chance of contamination of spring water? If yes, Give details of contamination