The document discusses water quality modeling for groundwater, surface water, and watersheds. It provides an overview of modeling contaminant transport, including examples of modeling projects related to salinity, selenium, and nitrogen fate and transport. Specifically, it summarizes modeling of selenium contamination in the Arkansas River Valley aquifer system using RT3D and OTIS models to simulate nitrogen and selenium transport and evaluate mitigation strategies.
Impact of Climate Change on Groundwater ResourcesC. P. Kumar
This document summarizes the impact of climate change on groundwater resources. It discusses how climate change can affect factors like precipitation, temperature, and evapotranspiration, which then impact groundwater recharge and levels. Higher temperatures and variability in rainfall from climate change could mean more fluctuations in groundwater levels and potential saline intrusion in coastal aquifers. Quantifying the full impact on groundwater requires downscaling climate models and coupling them with hydrological models to estimate changes in groundwater recharge over time. Key concerns are potential decreases in groundwater supplies and quality issues, as groundwater serves as a major global source of potable water.
This document provides an introduction and overview of groundwater modeling. It discusses why groundwater modeling is needed for effective groundwater management. It outlines the modeling process, including developing a conceptual model, selecting governing equations, model design, calibration, validation, and using the model for prediction. It describes different types of mathematical models, including analytical, finite difference, and finite element models. It emphasizes that a modeling protocol should establish the modeling purpose and ensure the conceptual model adequately represents the system behavior. The document stresses the importance of calibration, verification, and sensitivity analysis to evaluate a model's ability to reproduce measured conditions and the effects of uncertainty.
Groundwater modeling has several purposes including understanding aquifer properties, characteristics, and response. It requires collecting hydrological, physical, and boundary condition data. Common groundwater modeling software includes MODFLOW and Sutra. The modeling process involves defining the problem, collecting data, choosing a code, running simulations, verifying results match field data through calibration, and using the model to inform management decisions.
This document provides information about an environmental analysis course submitted by a student. It includes the course title, number, student and department information. It then discusses key topics in environmental analysis including the components of the environment, biogeochemical cycles, types of pollution, the aims of environmental analysis, types of analysis, stages of analysis, concepts in environmental analysis, environmental chemistry, and green chemistry.
Data Requirements for Groundwater ModellingC. P. Kumar
Groundwater modeling requires data on the physical and hydrological framework of the aquifer. The physical framework data defines the aquifer geometry and properties, including topography, geology, aquifer thickness and boundaries. The hydrological framework data describes the flow in and out of the aquifer, such as water table elevations, recharge and discharge rates and areas. Collecting these types of data from existing sources and monitoring programs is the first step of any groundwater modeling study.
Impact of Climate Change on Groundwater ResourcesC. P. Kumar
This document summarizes the impact of climate change on groundwater resources. It discusses how climate change can affect factors like precipitation, temperature, and evapotranspiration, which then impact groundwater recharge and levels. Higher temperatures and variability in rainfall from climate change could mean more fluctuations in groundwater levels and potential saline intrusion in coastal aquifers. Quantifying the full impact on groundwater requires downscaling climate models and coupling them with hydrological models to estimate changes in groundwater recharge over time. Key concerns are potential decreases in groundwater supplies and quality issues, as groundwater serves as a major global source of potable water.
This document provides an introduction and overview of groundwater modeling. It discusses why groundwater modeling is needed for effective groundwater management. It outlines the modeling process, including developing a conceptual model, selecting governing equations, model design, calibration, validation, and using the model for prediction. It describes different types of mathematical models, including analytical, finite difference, and finite element models. It emphasizes that a modeling protocol should establish the modeling purpose and ensure the conceptual model adequately represents the system behavior. The document stresses the importance of calibration, verification, and sensitivity analysis to evaluate a model's ability to reproduce measured conditions and the effects of uncertainty.
Groundwater modeling has several purposes including understanding aquifer properties, characteristics, and response. It requires collecting hydrological, physical, and boundary condition data. Common groundwater modeling software includes MODFLOW and Sutra. The modeling process involves defining the problem, collecting data, choosing a code, running simulations, verifying results match field data through calibration, and using the model to inform management decisions.
This document provides information about an environmental analysis course submitted by a student. It includes the course title, number, student and department information. It then discusses key topics in environmental analysis including the components of the environment, biogeochemical cycles, types of pollution, the aims of environmental analysis, types of analysis, stages of analysis, concepts in environmental analysis, environmental chemistry, and green chemistry.
Data Requirements for Groundwater ModellingC. P. Kumar
Groundwater modeling requires data on the physical and hydrological framework of the aquifer. The physical framework data defines the aquifer geometry and properties, including topography, geology, aquifer thickness and boundaries. The hydrological framework data describes the flow in and out of the aquifer, such as water table elevations, recharge and discharge rates and areas. Collecting these types of data from existing sources and monitoring programs is the first step of any groundwater modeling study.
Climate Change Impact Assessment on Hydrological Regime of Kali Gandaki BasinHI-AWARE
The presentation focuses on the findings of the impact of climate change on the hydrological regime and water balance components of the Kali Gandaki basin in Nepal. The Soil and Water Assessment Tool (SWAT) has been used to predict future projections.
This document discusses various methods for sampling water. It begins by explaining that sampling must account for environmental heterogeneity and can involve static or dynamic systems. It then outlines five main sampling methods: systematic, random, judgmental, stratified, and haphazard. For each method, it provides an example of how it would be implemented for water sampling. It also discusses types of samples, equipment for surface and groundwater sampling, and considerations for continuous monitoring. The key points are that sampling must address spatial and temporal variability and that different methods have advantages for different sampling needs and environments.
Here are the answers to the quiz questions:
1. Groundwater is flowing from Well A to Well B.
2. The hydraulic gradient is (102 m - 105 m) / 1000 m = 0.003
3. The flux is q = K i = 10 m/day * 0.003 = 0.03 m/day
4. The porosity is 250 mL / 1000 mL = 25%
5. The remaining 50 mL of water is held in the material by capillary forces.
6. The porosity would be less for clay than sand.
7. Less water would pour out if we use clay instead of sand.
8. [T/F] An aquiclude is
This document discusses groundwater hydrology and various aspects of wells. It defines groundwater and factors that influence its occurrence. There are four main types of geological formations - aquifers, aquitards, aquicludes, and aquifuges. The document describes properties of aquifers like porosity, permeability, and transmissibility. It also discusses Darcy's law, methods to measure soil permeability, and types of wells, well construction, and well development techniques.
•Initial (reconnaissance) assessment….
♦Basic knowledge of geological and environmental conditions
♦Review of previous investigation results
♦Measurements of water levels
♦Sampling & preliminary assessment of water quality
The hydrological cycle describes the continuous movement of water on, above, and below the surface of the Earth. Water is evaporated from bodies of water by solar energy, transpired from plants, and condensed into clouds. Clouds are moved by wind and precipitation falls as rain or snow and returns to bodies of water, either above or below ground. This cycle maintains a balance, but human activities like deforestation, agriculture, and industry can disrupt it and cause impacts like increased flooding and soil erosion.
Groundwater Management in Pakistan, by Dr Asad Sarwar Qureshi, IWMI PakistanGlobal Water Partnership
Groundwater is an important source of water in Pakistan, supplying over 57.9 BCM annually which is 40% of total water usage. It has led to increased crop yields and incomes but is now being overexploited in many areas. Over 1.2 million irrigation pumps extract groundwater, with depletion rates of 1.5 m/year on average. This poses many challenges including water quality deterioration, soil salinization, and non-compliance with water laws. Sustainable groundwater management is complex and requires solutions like improved surface water supplies and storage, rationalized cropping, increased use of alternative waters, and context-specific approaches depending on groundwater conditions. Climate change impacts will exacerbate water shortages unless urgent
Electrokinetic remediation of the pollutantsAnup Kumar
This document discusses electrokinetic remediation as a technique for removing organic and inorganic pollutants from soil. It provides details on the components of an electrokinetic remediation system and the transport mechanisms involved. Several types of electrokinetic remediation techniques are described, including direct electrokinetic remediation, and techniques combined with Fenton reactions, surfactants, biological processes, and ultrasonication. Case studies demonstrating the application and effectiveness of these techniques in removing various pollutants like atrazine, 2,4-DNT, diuron, and creosote from contaminated soils are also summarized.
Groundwater Data Requirement and AnalysisC. P. Kumar
The document discusses groundwater data requirements, acquisition, processing, and analysis. It outlines the types of physical and hydrological data needed for groundwater studies, including maps, cross-sections, and time-series data on water levels, quality, pumping, and other factors. Key points covered include establishing monitoring networks, validating data, preparing hydrographs, water table maps, and other tools to characterize the groundwater system and identify issues like contamination or over-pumping. Statistical methods for interpolating hydrological variables from point data across regions are also summarized.
This document provides an introduction to flood frequency analysis, which uses historical flood data to estimate the probability and recurrence intervals of future floods of given magnitudes. It discusses how flood frequency analysis is necessary for cost-effective design of bridges, dams, and other structures, as well as flood insurance and zoning. Two common methods for collecting flood data are described: annual peaks and partial duration series. Statistical approaches like the Weibull formula are commonly used to analyze the data and construct flood frequency curves showing the relationship between discharge magnitude and probability or recurrence interval.
Sea Water Intrusion(SWI) in coastal areas :
1. Occurrence of seawater intrusion
2.Factors that affect coastal aquifer
3.Changes by hydrological regime
4.Problems due to SWI
5.Ghyben-Herzberg relation
6.Methods to detect SWI
7.Control measures
This document discusses the sustainable management of water resources. It notes that river basins integrate economic, social, and environmental systems across political boundaries, so water management decisions should reflect this integrative nature. When systems are not managed sustainably, such as in the Aral Sea region where unsustainable irrigation practices depleted the sea, severe environmental, health, and economic problems can result. Achieving sustainable water resources management requires taking a basin-scale, multidisciplinary approach that considers impacts across different levels and balances current and future needs.
Climate change will have major impacts on water resources and society. While some impacts like heavier rainfall are more visible, changes like reductions in water supply and quality will also be significant. Vulnerability to climate change is determined by exposure to risks, sensitivity of systems, and adaptive capacity. India faces widespread poverty and many policy and community efforts are needed to build resilience, though many current responses only provide temporary relief. Adaptation is key to reducing the risks of climate change impacts on water and livelihoods.
This document discusses methods for estimating groundwater potential and balance. It provides an overview of key concepts like the hydrologic cycle, national water policy regarding groundwater, and the groundwater balance equation. The document also outlines data requirements, methodology, and methods for estimating individual components of the groundwater balance like recharge from rainfall, recharge from canals, and evapotranspiration from groundwater. Empirical formulas and norms from expert committees are presented for calculating various recharge coefficients.
Surface Water and Groundwater InteractionC. P. Kumar
The document discusses various aspects of planning and managing surface water and groundwater interaction and integration. It begins with an introduction on the hydrologic cycle and the impacts of human development on groundwater and the environment. It then covers topics like surface water and groundwater interaction, groundwater contamination from urbanization, industrial activity, mining and agriculture, environmental flows, groundwater over-abstraction, and challenges in groundwater-surface water modeling. The presentation aims to highlight the importance of understanding the linkages between groundwater and surface water for effective management of water resources.
This document discusses using hydrological models like SWAT, MODFLOW, and SEAWAT to assess the impacts of climate change on water resources. It provides an overview of these models, including their inputs, outputs, capabilities, and examples of case studies applying the models. Specifically, SWAT is highlighted as it can be used at the watershed scale to model processes like precipitation, evapotranspiration, infiltration, surface runoff, and streamflow under different climate scenarios. The document emphasizes the importance of hydrological modeling and tools like MODFLOW for understanding and predicting hydrologic system responses to climate change.
A pumping test is a field experiment in which a well is pumped at a controlled rate and water-level response (drawdown) is measured in one or more surrounding observation wells and optionally in the pumped well (control well) itself; response data from pumping tests are used to estimate the hydraulic properties of aquifers, evaluate well performance and identify aquifer boundaries.
- The document discusses equations for analyzing groundwater flow in confined and unconfined aquifers.
- For confined aquifers, the continuity equation is integrated over the aquifer thickness to derive an equation using transmissivity. Examples are presented of steady horizontal and radial flow.
- For unconfined aquifers, Dupuit assumptions are used and the continuity equation is solved for steady 1D flow using the water table elevation. Worked examples are provided for both confined and unconfined cases.
The document discusses various types of drinking water and their characteristics, as well as WHO and Pakistan water quality standards. It provides details on parameters for bottled water quality limits and methods for water quality analysis. Several studies on water sources and quality in Gilgit-Baltistan are summarized. Spring water is described as naturally filtered and free from contamination, while bottled water may be affected by plastic toxicity, UV radiation during processing, and chemicals added through reverse osmosis.
Engineered Nanoparticles in Food: Implications for Food Safety and Consumer H...Nebraska Water Center
The document summarizes the Platte River Recovery Implementation Program, which aims to protect habitat for threatened and endangered species in the central Platte River Basin. The Program is a collaborative effort between Colorado, Nebraska, Wyoming and the Department of the Interior to provide sufficient water flows and habitat. Key aspects include land and water acquisition, habitat restoration, adaptive management, and governance structure with stakeholder involvement to achieve species recovery goals.
Climate Change Impact Assessment on Hydrological Regime of Kali Gandaki BasinHI-AWARE
The presentation focuses on the findings of the impact of climate change on the hydrological regime and water balance components of the Kali Gandaki basin in Nepal. The Soil and Water Assessment Tool (SWAT) has been used to predict future projections.
This document discusses various methods for sampling water. It begins by explaining that sampling must account for environmental heterogeneity and can involve static or dynamic systems. It then outlines five main sampling methods: systematic, random, judgmental, stratified, and haphazard. For each method, it provides an example of how it would be implemented for water sampling. It also discusses types of samples, equipment for surface and groundwater sampling, and considerations for continuous monitoring. The key points are that sampling must address spatial and temporal variability and that different methods have advantages for different sampling needs and environments.
Here are the answers to the quiz questions:
1. Groundwater is flowing from Well A to Well B.
2. The hydraulic gradient is (102 m - 105 m) / 1000 m = 0.003
3. The flux is q = K i = 10 m/day * 0.003 = 0.03 m/day
4. The porosity is 250 mL / 1000 mL = 25%
5. The remaining 50 mL of water is held in the material by capillary forces.
6. The porosity would be less for clay than sand.
7. Less water would pour out if we use clay instead of sand.
8. [T/F] An aquiclude is
This document discusses groundwater hydrology and various aspects of wells. It defines groundwater and factors that influence its occurrence. There are four main types of geological formations - aquifers, aquitards, aquicludes, and aquifuges. The document describes properties of aquifers like porosity, permeability, and transmissibility. It also discusses Darcy's law, methods to measure soil permeability, and types of wells, well construction, and well development techniques.
•Initial (reconnaissance) assessment….
♦Basic knowledge of geological and environmental conditions
♦Review of previous investigation results
♦Measurements of water levels
♦Sampling & preliminary assessment of water quality
The hydrological cycle describes the continuous movement of water on, above, and below the surface of the Earth. Water is evaporated from bodies of water by solar energy, transpired from plants, and condensed into clouds. Clouds are moved by wind and precipitation falls as rain or snow and returns to bodies of water, either above or below ground. This cycle maintains a balance, but human activities like deforestation, agriculture, and industry can disrupt it and cause impacts like increased flooding and soil erosion.
Groundwater Management in Pakistan, by Dr Asad Sarwar Qureshi, IWMI PakistanGlobal Water Partnership
Groundwater is an important source of water in Pakistan, supplying over 57.9 BCM annually which is 40% of total water usage. It has led to increased crop yields and incomes but is now being overexploited in many areas. Over 1.2 million irrigation pumps extract groundwater, with depletion rates of 1.5 m/year on average. This poses many challenges including water quality deterioration, soil salinization, and non-compliance with water laws. Sustainable groundwater management is complex and requires solutions like improved surface water supplies and storage, rationalized cropping, increased use of alternative waters, and context-specific approaches depending on groundwater conditions. Climate change impacts will exacerbate water shortages unless urgent
Electrokinetic remediation of the pollutantsAnup Kumar
This document discusses electrokinetic remediation as a technique for removing organic and inorganic pollutants from soil. It provides details on the components of an electrokinetic remediation system and the transport mechanisms involved. Several types of electrokinetic remediation techniques are described, including direct electrokinetic remediation, and techniques combined with Fenton reactions, surfactants, biological processes, and ultrasonication. Case studies demonstrating the application and effectiveness of these techniques in removing various pollutants like atrazine, 2,4-DNT, diuron, and creosote from contaminated soils are also summarized.
Groundwater Data Requirement and AnalysisC. P. Kumar
The document discusses groundwater data requirements, acquisition, processing, and analysis. It outlines the types of physical and hydrological data needed for groundwater studies, including maps, cross-sections, and time-series data on water levels, quality, pumping, and other factors. Key points covered include establishing monitoring networks, validating data, preparing hydrographs, water table maps, and other tools to characterize the groundwater system and identify issues like contamination or over-pumping. Statistical methods for interpolating hydrological variables from point data across regions are also summarized.
This document provides an introduction to flood frequency analysis, which uses historical flood data to estimate the probability and recurrence intervals of future floods of given magnitudes. It discusses how flood frequency analysis is necessary for cost-effective design of bridges, dams, and other structures, as well as flood insurance and zoning. Two common methods for collecting flood data are described: annual peaks and partial duration series. Statistical approaches like the Weibull formula are commonly used to analyze the data and construct flood frequency curves showing the relationship between discharge magnitude and probability or recurrence interval.
Sea Water Intrusion(SWI) in coastal areas :
1. Occurrence of seawater intrusion
2.Factors that affect coastal aquifer
3.Changes by hydrological regime
4.Problems due to SWI
5.Ghyben-Herzberg relation
6.Methods to detect SWI
7.Control measures
This document discusses the sustainable management of water resources. It notes that river basins integrate economic, social, and environmental systems across political boundaries, so water management decisions should reflect this integrative nature. When systems are not managed sustainably, such as in the Aral Sea region where unsustainable irrigation practices depleted the sea, severe environmental, health, and economic problems can result. Achieving sustainable water resources management requires taking a basin-scale, multidisciplinary approach that considers impacts across different levels and balances current and future needs.
Climate change will have major impacts on water resources and society. While some impacts like heavier rainfall are more visible, changes like reductions in water supply and quality will also be significant. Vulnerability to climate change is determined by exposure to risks, sensitivity of systems, and adaptive capacity. India faces widespread poverty and many policy and community efforts are needed to build resilience, though many current responses only provide temporary relief. Adaptation is key to reducing the risks of climate change impacts on water and livelihoods.
This document discusses methods for estimating groundwater potential and balance. It provides an overview of key concepts like the hydrologic cycle, national water policy regarding groundwater, and the groundwater balance equation. The document also outlines data requirements, methodology, and methods for estimating individual components of the groundwater balance like recharge from rainfall, recharge from canals, and evapotranspiration from groundwater. Empirical formulas and norms from expert committees are presented for calculating various recharge coefficients.
Surface Water and Groundwater InteractionC. P. Kumar
The document discusses various aspects of planning and managing surface water and groundwater interaction and integration. It begins with an introduction on the hydrologic cycle and the impacts of human development on groundwater and the environment. It then covers topics like surface water and groundwater interaction, groundwater contamination from urbanization, industrial activity, mining and agriculture, environmental flows, groundwater over-abstraction, and challenges in groundwater-surface water modeling. The presentation aims to highlight the importance of understanding the linkages between groundwater and surface water for effective management of water resources.
This document discusses using hydrological models like SWAT, MODFLOW, and SEAWAT to assess the impacts of climate change on water resources. It provides an overview of these models, including their inputs, outputs, capabilities, and examples of case studies applying the models. Specifically, SWAT is highlighted as it can be used at the watershed scale to model processes like precipitation, evapotranspiration, infiltration, surface runoff, and streamflow under different climate scenarios. The document emphasizes the importance of hydrological modeling and tools like MODFLOW for understanding and predicting hydrologic system responses to climate change.
A pumping test is a field experiment in which a well is pumped at a controlled rate and water-level response (drawdown) is measured in one or more surrounding observation wells and optionally in the pumped well (control well) itself; response data from pumping tests are used to estimate the hydraulic properties of aquifers, evaluate well performance and identify aquifer boundaries.
- The document discusses equations for analyzing groundwater flow in confined and unconfined aquifers.
- For confined aquifers, the continuity equation is integrated over the aquifer thickness to derive an equation using transmissivity. Examples are presented of steady horizontal and radial flow.
- For unconfined aquifers, Dupuit assumptions are used and the continuity equation is solved for steady 1D flow using the water table elevation. Worked examples are provided for both confined and unconfined cases.
The document discusses various types of drinking water and their characteristics, as well as WHO and Pakistan water quality standards. It provides details on parameters for bottled water quality limits and methods for water quality analysis. Several studies on water sources and quality in Gilgit-Baltistan are summarized. Spring water is described as naturally filtered and free from contamination, while bottled water may be affected by plastic toxicity, UV radiation during processing, and chemicals added through reverse osmosis.
Engineered Nanoparticles in Food: Implications for Food Safety and Consumer H...Nebraska Water Center
The document summarizes the Platte River Recovery Implementation Program, which aims to protect habitat for threatened and endangered species in the central Platte River Basin. The Program is a collaborative effort between Colorado, Nebraska, Wyoming and the Department of the Interior to provide sufficient water flows and habitat. Key aspects include land and water acquisition, habitat restoration, adaptive management, and governance structure with stakeholder involvement to achieve species recovery goals.
This document summarizes research on the temporal and spatial variation of the herbicide atrazine in surface waters. It discusses how atrazine occurrence occurs in pulses following rain storms and varies considerably between locations only miles apart. Studies found atrazine co-occurs with other agrichemicals and is a sentinel for their presence. Testing found surface water samples triggered gene expressions in lab animals linked to adverse health. The research also demonstrated how atrazine levels varied greatly across the massive Mississippi River basin within a single day, reflecting the challenges of addressing watershed-scale contamination that spans vast geographies and jurisdictions.
Mp gw ground water quality in jabalpur urban area with emphasis on transport ...hydrologywebsite1
The final report summarizes the results of a groundwater quality study conducted in Jabalpur, Madhya Pradesh, India from 2009 to 2014. The study focused on assessing contamination in the Omti Nalla drainage system and leakage from sewage systems into groundwater. Water quality parameters such as nitrates, sulfates, bacteria, and heavy metals were analyzed at 60 monitoring wells over the study period. The results were used to evaluate spatial and temporal variations in groundwater quality, identify sources of contamination, and inform future water management plans.
This document outlines the requirements for accreditation of water analysis laboratories in the Philippines. It discusses personnel requirements including minimum staffing levels, physical plant specifications, required equipment and references, quality assurance programs, fees, and the accreditation/renewal process. Laboratories must meet standards for facilities, trained personnel, appropriate equipment and adherence to standard testing methods to ensure accurate and reliable water quality analysis. Requirements are periodically updated to maintain high standards.
sciencepowerpoint.com delivers a four part 2150+ slide PowerPoint slideshow becomes the roadmap for an amazing and interactive science experience. Complete with bundled homework package, many built-in quizzes, hands-on activities with directions, unit notes, answer keys, video links, rubrics, review games, and much more.
This unit aligns with the Next Generation Science Standards and Common Core Standards for ELA and Literacy in Science and Technical Subjects. See preview for more information.
Areas of Focus within The Rivers Unit -Watersheds, Rivers of the United States, Sections of a River, Parts of River (Vocabulary), Stream Order, Erosion and Deposition, Water Quality, Chemical Properties of Water, Bio-Indicators of Water Quality (EPT richness), Physical Properties of Water Quality, Rivers and Flooding, Factors that Control Flooding, Types of Flooding, Tsunami's, Wetlands, Flood Prevention, Levees, Dams and Ecosystem, Importance of Dams, Impacts of Dams, Hydropower, Parts of Dam, Salmon (Life Cycle), Systems of Help Salmon, Fish (General), Layering in a Lake, Lake Turnover, Nutrients and Lakes.
Teaching Duration = 4+ Weeks + PowerPoint Review Games
Ryan Murphy M.Ed
www.sciencepowerpoint.com
The document discusses methods for analyzing water quality and pollution. It outlines physical, chemical, biological, and microbiological measurements that can be used to assess water quality, choose treatment methods, determine treatment efficiency, trace pollution sources, and analyze microbial infection risks. Specific tests are described to measure levels of various chemical and biological substances that affect water potability, health, toxicity, and pollution. Bacteriological examinations including total count, E. coli, and coliform tests are also summarized.
This document provides an overview of key concepts in surface water hydrology. It defines surface water hydrology and discusses watersheds, overland flow, rivers, lakes, sediment transport, water measurement, flood events, and the use of GIS mapping. Key terms are defined such as runoff, infiltration, river morphology, lake zones, discharge measurement, flood frequency, and probable maximum precipitation. Diagrams illustrate watersheds, hillslope flow, river cross-sections, lake layers, and more. Equations for rational formula and discharge calculation are also presented.
The document discusses the physical, chemical, and biological properties of water. It notes that water has a unique ability to absorb large amounts of heat due to its high specific heat capacity. Chemically, water's hydrogen-oxygen structure gives it adhesive properties and allows it to dissolve many substances. Biologically, water can adhere to surfaces, cohere to itself, and participate in chemical reactions due to these physical and chemical traits, demonstrating its importance for living things.
This document summarizes a presentation on advancements in irrigation technology and their impact on water management. It provides background on the presenter and his research team. It then discusses various irrigation technologies including center pivots, mobile drip irrigation, variable rate irrigation, and soil water sensors. It highlights the benefits of these technologies but also challenges in their use. The presentation aims to improve irrigation and nitrogen use efficiency through better measurement and application of water and nutrients.
This document discusses water pollution, including its causes, sources, types, effects, and methods of prevention. It defines water pollution as the contamination of water bodies by human and natural activities. The two main sources are point source pollution from single identifiable sources like factories, and non-point source pollution from multiple diffuse sources like agricultural runoff. Various types of water pollution are described, and effects include harm to aquatic life, disruption of food chains, diseases in humans, and destruction of ecosystems. Prevention methods center around proper waste disposal, reduced chemical usage, and wastewater treatment.
This document outlines a research project to improve the simulation of nitrogen and phosphorus fate and transport in irrigated agricultural watersheds in semi-arid regions. The project aims to: 1) Enhance the Soil and Water Assessment Tool (SWAT) by integrating it with MODFLOW and RT3D to better simulate surface-subsurface flow and reactive transport processes. 2) Improve understanding of the key processes governing nitrogen and phosphorus movement, transformation, and storage in agricultural watersheds. 3) Assess remediation strategies for nitrogen and phosphorus contamination under varying climate scenarios. The enhanced model will be tested and results disseminated to help watershed managers.
Water is neutral, stable, and does not decompose easily. It can act as a catalyst and react with many substances like metals, non-metals, oxides, and carbides. Water reacts with metallic oxides to form alkalis, and with non-metallic oxides to form acidic solutions. It reacts with chlorine to form hydrochloric and hypochlorous acids. Noble metals like silver, gold, and platinum are largely unaffected by water.
Irina Bokova is nominated by Bulgaria for UN Secretary-General. She currently serves as the Director-General of UNESCO. She has extensive experience in foreign affairs and international organizations, having served as Bulgaria's Minister of Foreign Affairs and Ambassador to France and UNESCO. Bokova's background demonstrates her commitment to issues like education, gender equality, freedom of expression, and cultural dialogue.
19th Ateneo Graduate School of Business Marketing Forum on Understanding and Measuring Customer Satisfaction with Dr. Donald Lim, President and CEO of Yehey
This document lists 25 research publications from 1998 to 2016 related to nonalcoholic fatty liver disease and associated conditions. The publications report on studies investigating:
1. The association between nonalcoholic steatohepatitis and betaine insufficiency.
2. The role of IGF binding protein-3 and palmitate in hepatic inflammation.
3. A method for isolating microRNA from high density lipoprotein.
4. An animal model of nonalcoholic fatty liver disease and hepatocellular cancer.
5. Distinct hepatic lipid and eicosanoid profiles in lean and obese subjects with alcohol use.
Electrical resistivity data interpretation for groundwater detection in titta...eSAT Journals
Abstract The present study aims to detect the groundwater potential in Tittagudi Taluk of Cuddalore District, Tamil Nadu, India using electrical measurement. Electric resistivity data interpretation was carried out using Schlumberger configuration with electrode spacing (AB/2) of 100 m distance. The VES was calculated by multiplying the resistance by constant obtained from the Schlumberger formula. The resistivity curves were analysed with curve matching techniques along with the help of computer programme. The sub-surface lithology was evaluated and correlated with the available borehole data. The results of quantitative interpretation of geoelectrical data indicated that the layer system having minimum of two layers to a maximum of eight layers in the area. The low and high resistivities obtained are ranging from 0.5 to 27755 ohm/m respectively. Majority of resistivity curves are falling in ‘A’ type. The contact zone of sedimentary and crystalline rock formations are clearly delineated on Northeast to Southwest directions along Sirumangalam, Agaram and Sirumalai habitations. The prominent low resistivity anomaly observed in and around Adari area (VES. 03), this have been encountered in all the iso-resistivity contour maps, indicating that, a trend of structural elements like a weaker zone or lineament or fracture occurred in NE direction of the study area which may be a favorable zone for targeting groundwater. Key words: Electrical Measurements, Tittagudi Taluk, Schulmberger Configuration And Iso-Resistivity Maps.
This document summarizes a study on microbial metal cycling and bioaccumulation in roadside soils and streams. The study aims to establish relationships between urbanization and pollutant concentrations in a local stream ecosystem. Researchers analyzed metal concentrations in insects, soils, and sediments from different zones of a creek. They also investigated microbial oxidation and reduction of antimony species from roadside soils and isolated bacterial strains to study metabolic pathways. Preliminary results found higher arsenic and lead levels in downstream insects and trace antimony reduction by soils microbes. The study provides background on metal pollution impacts and aims to further examine seasonal shifts and microbial antimony processing.
Impact of contaminants on groundwater quality in patcham, south east england.Alexander Decker
This study investigated the impact of contaminants on groundwater quality in Patcham, South-East England. Data from weather stations and loggers in boreholes was used to analyze potential contaminant pathways through the chalk aquifer. Laboratory tests found that parameters like pH, conductivity and ions were within WHO guidelines, indicating water quality was suitable for use. The chalk aquifer is an important water source but is vulnerable to surface contaminants due to its karst nature with features like swallow holes.
This poster summarizes a study analyzing changes in water quality in the Allegheny River and its tributaries in Pennsylvania. Water samples were collected from 14 sites between 2013-2015 and analyzed for parameters like dissolved metals, bromide, chloride, and sulfate. Ratios of these parameters indicate impacts from abandoned mine drainage and hydraulic fracturing wastewater. In particular, Blacklick Creek, impacted by both issues, shows high bromide and strontium resembling fracking wastewater. Downstream sites on the Allegheny also reflect these elevated levels, demonstrating impacts on water quality in the region.
This document presents a framework for setting realistic expectations for water quality improvements based on changes in agricultural activities. The framework considers how chemicals and sediment from fields enter the stream network through different flowpaths like surface runoff, subsurface drainage, and groundwater. It also accounts for how the chemical behavior of different substances influences their transport. The framework can be used to evaluate how specific agricultural management practices might affect water quality in different hydrologic settings by trapping, reducing, or removing chemicals and sediment. Examples are given to illustrate how the framework can set expectations for practices like buffer strips and no-till tillage.
The document summarizes a study that was conducted to determine sources of water pollution in Appiakrom community, Ghana. The study examined a dam, pond, and two boreholes used by the community. Laboratory analysis of water samples found that the dam, which supplies water to the district, had been polluted by anthropogenic activities. The rusty nature of one borehole was attributed to underground parent materials. The pond interfaced with the dam, and pollution could flow between the two sources. The authors recommend blocking channels between the pond and dam, and practicing zero-fertilizer farming near the dam to reduce pollution.
Calidad del agua para agricultura fao 29-ayers y westcot 1985-okiPIEDRON
This document provides guidelines for evaluating water quality for agricultural irrigation. It discusses four main water quality problems: salinity, infiltration rate, toxicity, and miscellaneous other issues. For each problem, the document describes guidelines for interpreting water quality data, potential impacts on crops, and management options. It provides water quality guidelines in tables and discusses experiences using various water qualities from different locations worldwide.
Ryan E. Emanuel (Lumbee), Associate Professor, Department of Forestry and Environmental Resources, North Carolina State University - September 2016
UCAR Congressional Briefing
Water influences ecological processes and patterns; ecosystems influence water quantity and quality; ecohydrology focuses on these water-life interactions.
UCAR Congressional Briefing
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EVALUATION OF GROUNDWATER QUALITY OF VAIPPAR BASIN, TAMIL NADU, INDIA: A GEOI...SagarChougule11
The Vaippar Basin, one of the important basins of Tamil Nadu is located between 9° 0' 05" & 9° 44' 56" N latitudes and 77° 23' 25" & 78° 17' 02" E longitudes with an area of 5339 sq.km. Groundwater samples were collected from 91 different locations in the Vaippar basin, Tamil Nadu, India. Groundwater quality data for the period of 30 years (1983 to 2013) of both pre-monsoon and post-monsoon periods were used to analyze the groundwater quality aspects of the Vaippar basin. The physico-chemical parameters such as Total Dissolved Solids (TDS), pH, HCO3-, Ca2+, Mg2+, Na+, K+, SO4-, NO3- and Cl have been analyzed to determine the geological and non-geological source of contamination. An overall hydrogeochemical analytical study using Electrical Conductivity, Sodium Adsorption Ratio (SAR), Sodium percentage (Na%) and Residual Sodium Carbonate (RSC) values reveals that most of the groundwater samples collected from the study area are suitable for drinking, irrigation, and industrial purposes.
11.ground water quality assessment of nagercoil townAlexander Decker
The document analyzes the physico-chemical characteristics of water samples collected from 15 hand pumps in 3 towns in Nagercoil, India. Testing found that pH, total alkalinity, hardness, nitrate, sodium, potassium, iron and phosphate levels were above permissible limits in some samples. The study concludes that higher levels of dissolved constituents were found due to greater interaction of groundwater with geological materials.
Ground water quality assessment of nagercoil townAlexander Decker
This document summarizes a study analyzing the physico-chemical characteristics of water samples collected from 15 hand pumps in Nagercoil Town, Tamil Nadu, India. The study found that the pH of the water samples was slightly acidic, and that total alkalinity, total hardness, nitrate, sodium, potassium, iron and phosphate levels were above permissible limits. The document provides details on the materials and methods used to collect and analyze the water samples. It discusses the results, noting that hardness, total dissolved solids, chloride, fluoride, and nitrate levels exceeded guidelines in some locations. The conclusion states that higher dissolved constituents were found due to interaction with geological materials.
The document analyzes water quality data from the Euphrates River (Shatt Al-Hillah) in Iraq collected over 2010-2011.
It assessed water quality for both civilian (drinking water) and agricultural (irrigation water) uses. Water quality parameters like pH, turbidity, salts and minerals were measured monthly at 4 stations and compared to Iraqi, WHO and EPA standards.
For drinking water, most parameters met Iraqi and WHO standards except for sulfates and total dissolved solids (TDS) which exceeded limits. For irrigation water, salinity levels showed problems for some classifications while sodium and chloride hazards were mild-moderate. The study aims to evaluate Euphrates water suitability for different uses
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Quantitative water quality survey of wetland habitats at a contaminated brown...David Bryan
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Water Quality Modeling for Groundwater, Surface Water, and Watersheds: Basic Theory and Applications
1. Water Quality Modeling for Groundwater,
Surface Water, and Watersheds:
Basic Theory and Applications
Ryan Bailey
Dept. of Civil and Environmental Engineering
Colorado State University
rtbailey@engr.colostate.edu
1
5. Research Projects
• Selenium in Groundwater Systems
• Salinity in Groundwater Systems
• Small Island Water Resources Assessment
• Groundwater in the Ogallala Aquifer Region
• Nutrient transport in subsurface tile drains
• Groundwater-surface water interactions
• Coupled land surface / groundwater modeling
6. Outline
1. Importance of Water Quality (Case Study)
2. Basics of Water Quality Modeling (Transport)
3. Projects using Water Quality Modeling
6
9. Groundwater Contamination
Case Studies – Woburn, Massachusetts
TCE
(tetrachloroethylene)
• Solvent for organic materials (used for
dry cleaning, degreasing automotive
parts, paint strippers)
• First synthesized in 1821 (Michael
Faraday)
• Group 2A carcinogen (likely to cause
cancer)
• Central nervous system depressant
• Dissolves fats from skin (skin irritation)
• Banned from use in new dry-cleaning
machines in 2007
• EPA drinking water: < 5 ppb (µg/L)
C2Cl4
10. Tanneries, Dry Cleaning, Textile Mills,
Paper Industries, Chemical Companies
http://sphweb.bumc.bu.edu/otlt/MPH-Modules/PH/Woburn/Woburn_print.html
Groundwater Contamination
Case Studies – Woburn, Massachusetts
11. Incidents of Leukemia
Where did the TCE originate from? Who is at fault?
Groundwater Contamination
Case Studies – Woburn, Massachusetts
12. Groundwater Contamination
Case Studies – Woburn, Massachusetts
1964-1967
http://sphweb.bumc.bu.edu/otlt/MPH-Modules/PH/Woburn/Woburn_print.html
Dump chemicals (TCE)
Trichloroethylene
Until 1960s
Dry Cleaning
Tannery
13. Complaints about the water in east Woburn
began after Well G began pumping water
in November of 1964
Complaints forced pumping to stop in
October 1969, but they were reopened
whenever the demand for water increased
during the summer or when there was
drought. Whenever Wells G and H began
pumping, there were complaints about the
"putrid, ill-smelling, and foul water."
Groundwater Contamination
Case Studies – Woburn, Massachusetts
How to pinpoint origin of contamination at Wells?
15. Water Quality Effects
Chemicals
Toxin and Carcinogen
Skin disorders, keratosis, cardiovascular, respiratory
• Mobilized by weathering reactions, biological
activity, volcanic emissions, mining, use of arsenical
pesticides
• Groundwater: increased contact between water and
rocks (high vulnerability)
• Large scale contamination in Bangladesh
16. Water Quality Effects
Chemicals
Toxin and Carcinogen
Skin disorders, keratosis, cardiovascular, respiratory
• Mobilized by weathering reactions, biological
activity, volcanic emissions, mining, use of arsenical
pesticides
• Groundwater: increased contact between water and
rocks (high vulnerability)
• Large scale contamination in Bangladesh
24. Water Quality Effects
Modeling Transport in Rivers and Aquifers
O’Connor et al. (2010)
1. Advection
2. Dispersion
3. Chemical Reactions
25. Water Quality Effects
Modeling Transport in Rivers and Aquifers
O’Connor et al. (2010)
1. Advection
2. Dispersion
3. Chemical Reactions
26. Water Quality Effects
Modeling Transport in Rivers and Aquifers
O’Connor et al. (2010)
1. Advection
2. Dispersion
3. Chemical Reactions
27. Water Quality Effects
Modeling Transport in Rivers and Aquifers
O’Connor et al. (2010)
1. Advection
2. Dispersion
3. Chemical Reactions
Sorption
Redox reactions
28. Water Quality Effects
Modeling Transport in Rivers and Aquifers
O’Connor et al. (2010)
1. Advection
2. Dispersion
3. Chemical Reactions
1. Conservation of Mass
2. Partial Differential Equation
3. Numerical Methods (model)
42. Selenium
Contamination
Selenium (Se): the “double-edged sword” element
< 40 µg/day: Muscular dystrophy; Liver, muscle, heart disease, Cardiovascular cancer
> 400 µg/day: Nervous system, growth retardation, deformities
Particularly harmful to aquatic life (waterfowl and fish)
43. Selenium
Contamination
1980s: Kesterson Reservoir
- High Se drainage water
- Deformation of water fowl
(bioaccumulation)
Kesterson Reservoir, CA
1990s and 2000s
- Reports from sites worldwide
- Se contamination in groundwater
and surface water.
- Deformation of water fowl, fish
- Also: deficiency (Finland, China)
44. Selenium
Contamination
1980s and 1990s: National Irrigation Water Quality Program
Shale Bedrock + Irrigation = Se Problem
Arkansas River Valley, CO
(high flow + O2,NO3)
48. Selenium
Modeling in Arkansas River Valley
Fort Lyon
Holbrook
Highline
Catlin
RF Ditch
Otero
6 Irrigation Canals
Highline
Otero
Catlin
Rocky Ford Ditch
Holbrook
Fort Lyon
Pumping Wells Depth to Bedrock (~15 m)Surface Shale
49. Selenium
Modeling in Arkansas River Valley
Fertilizer Loading (N)
NO3 leaching, interaction with shale
Release of Selenium into groundwater
55. Selenium
Modeling in Arkansas River Valley
• Crop type for each irrigated field
• Distribution of Shale
• Plant, Harvest, Plowing days
• Fertilizer (time and amount) (N)
• Root zone hydrology
• Nitrogen cycling
• Oxidation of Selenium from shale
RT3D
OTIS
Concentration of
NO3 and Se in
Aquifer and River
77. Groundwater Contamination
Case Studies – Woburn, Massachusetts
Where did the TCE originate from? Who is at fault?
MODFLOW model
+
MT3DMS model
(TCE, PCE)
(1960-1986)
Maura Metheny, 2004
(Ohio State University
84. Concluding Remarks
• Water quality a concern in many parts of the worlds
• Water-borne diseases still occur in many regions
• Numerical models can be used to track contaminants in the environment
(groundwater and surface water)
• Models can be used to explore effect of management practices on
contamination and remediation
• Models can be used to determine historical patterns of contaminant
transport
89. Dr. John Snow
• 1838: Admitted to the Royal College of
Surgeons of England
• One of the first physicians to use anesthesia
(ether, chloroform) for surgey
• 1853: personally administered chloroform to
Queen Victoria during birth
• Skeptic of “miasma” theory (cholera spread
by “bad air”)
• 1854: investigated cholera outbreak in Soho
Soho (London, England)
90.
91. How to prove?
1. Woman several km from neighborhood died
2. Men in brewery did not die
3. Families with deaths in other neighborhoods always sent
their children to fetch water from the Broad Street pump
Theory