How streams are classified? The most popular measurable terms classifying the flowing water body into "the stream order" are discussed in this presentation. .
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
A drainage basin is an area of land where surface water converges to a single point, usually the exit of the basin. There are several types of drainage systems that form depending on the terrain and geology, including dendritic, parallel, rectangular, trellis, radial, and annular systems. Stream ordering schemes classify streams in a hierarchy based on how they join together. Quantitative analysis of drainage basins uses metrics like bifurcation ratio, length ratio, and drainage density to characterize aspects of the basin.
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.
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.
Flowing water has the ability to dissolve the soluble mineral substances available on its way. The processes enacted by streams are called as fluvial processes. The word “fluvius” is derived from the latin word meaning “ river”. The world fluvial is used to denote the running water as streams or rivers. Fluvial processes entail the erosion, transportation, and deposition of earth materials by running water. Fluvial processes and fluvial landforms dominate land surfaces the world over, as opposed to the limited effects of glacial, coastal, and wind processes.
The document discusses ocean tides and their causes. It explains that tides are caused by the gravitational pull of the moon and sun, which create two tidal bulges on Earth. The timing of tides is related to Earth's rotation and the moon's revolution, resulting in a tidal period of about 24 hours and 50 minutes. Tides can be semidiurnal (two high tides and two low tides per day) or diurnal (one of each per day), depending on coastal geography. Spring tides occur during new and full moons when gravitational forces are strongest, while neap tides happen at quarter moons with weaker forces.
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.
This document outlines groundwater management strategies for municipal officials. It notes that while the region receives abundant precipitation, local overuse and water quality problems are still possible if left unmanaged. It then describes a model groundwater protection ordinance that has been adopted by several Dutchess County towns. The ordinance establishes development standards and best practices to safeguard both groundwater quantity and quality. These include regulating certain land uses, prohibiting new underground fuel tanks, guidance for cluster subdivisions, and more rigorous pumping test requirements. The model aims to preserve aquifer and stream flows while also addressing issues like pharmaceutical contamination and climate change impacts. Towns can adopt this law or planning boards can apply its guidance under the State Environmental Quality Review Act.
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
A drainage basin is an area of land where surface water converges to a single point, usually the exit of the basin. There are several types of drainage systems that form depending on the terrain and geology, including dendritic, parallel, rectangular, trellis, radial, and annular systems. Stream ordering schemes classify streams in a hierarchy based on how they join together. Quantitative analysis of drainage basins uses metrics like bifurcation ratio, length ratio, and drainage density to characterize aspects of the basin.
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.
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.
Flowing water has the ability to dissolve the soluble mineral substances available on its way. The processes enacted by streams are called as fluvial processes. The word “fluvius” is derived from the latin word meaning “ river”. The world fluvial is used to denote the running water as streams or rivers. Fluvial processes entail the erosion, transportation, and deposition of earth materials by running water. Fluvial processes and fluvial landforms dominate land surfaces the world over, as opposed to the limited effects of glacial, coastal, and wind processes.
The document discusses ocean tides and their causes. It explains that tides are caused by the gravitational pull of the moon and sun, which create two tidal bulges on Earth. The timing of tides is related to Earth's rotation and the moon's revolution, resulting in a tidal period of about 24 hours and 50 minutes. Tides can be semidiurnal (two high tides and two low tides per day) or diurnal (one of each per day), depending on coastal geography. Spring tides occur during new and full moons when gravitational forces are strongest, while neap tides happen at quarter moons with weaker forces.
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.
This document outlines groundwater management strategies for municipal officials. It notes that while the region receives abundant precipitation, local overuse and water quality problems are still possible if left unmanaged. It then describes a model groundwater protection ordinance that has been adopted by several Dutchess County towns. The ordinance establishes development standards and best practices to safeguard both groundwater quantity and quality. These include regulating certain land uses, prohibiting new underground fuel tanks, guidance for cluster subdivisions, and more rigorous pumping test requirements. The model aims to preserve aquifer and stream flows while also addressing issues like pharmaceutical contamination and climate change impacts. Towns can adopt this law or planning boards can apply its guidance under the State Environmental Quality Review Act.
The document discusses groundwater and the water cycle. It describes how (1) water moves among oceans, atmosphere, Earth and biosphere in the water cycle through processes like infiltration, transpiration and precipitation; (2) there is a balance in the water cycle as annual precipitation equals evaporation globally; and (3) groundwater is water located underground in the saturated zone below the water table, where it moves slowly through pores and fractures in rock and soil.
The subsurface occurrence of groundwater may be divided into zones of aeration and saturation. The vertical distribution of groundwater is explained in this module.
Importance of Water
Hydrologic Cycle
Water Use and Resource Problems
Too Much Water
Too Little Water
Global Water Problems
Sharing Water Resources
Water Management
Providing Sustainable Water Supply
Water Conservation
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.
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.
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.
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.
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.
Groundwater occurs beneath the Earth's surface in pore spaces and fractures in rocks and sediments. It originates from rainfall and snowmelt percolating into the ground. Groundwater is found everywhere but is usually within 750 meters of the surface. It makes up about 1% of the total water on Earth but 35 times the amount of water in streams and lakes. Groundwater flows through the hydrologic cycle, entering the ground as precipitation and eventually emerging in streams, lakes, or oceans.
Groundwater is found underground in soil and rock pores and fractures. It is an important source of freshwater. Groundwater exists in three zones: the saturated zone where all pores are full of water, the capillary fringe just above it, and the aeration zone above that. The water table marks the top of the saturated zone. Groundwater interacts with streams, which can gain or lose water from interactions with the water table. Factors like porosity, permeability, and the slope of the water table influence groundwater storage and movement. Groundwater can emerge as springs, hot springs, or geysers, and be accessed via wells. Excessive pumping can cause problems like subsidence and saltwater contamination.
Every continent or island is bordered by a long or short coastline. Coastline is the line separating the land and sea. Coastal zones are the transition zones between terrestrial and marine habitat. They form an interface between land and oceanic natural processes. Coastal areas also are varied in their topography, climate and vegetation. Some are sandy beaches, rocky shores, with or without tidal inlets. The climate of a coast are controlled by the land and sea breezes and the humidity controlled by marine water. Waves are powerful tools for constructive and destructive activities. Hence. the geomorphology of beach, materials and processes are always not constant due to the impact of everlasting action of tides, waves and currents.
Fluvial processes create distinct landforms over time as a river ages. In the youth stage, the river valley is narrow with steep sides. Meanders begin to form in the maturity stage as the river widens and deepens. In the old stage, the river flows across a flat floodplain as it approaches being a featureless plain. Distinct landforms are produced at each stage as the river's erosional and depositional activities change.
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.
1. Deltas form where rivers enter bodies of standing water, depositing large amounts of sediment. They are common features where large rivers meet the ocean.
2. Deltas consist of a delta plain, delta front, and prodelta. The delta plain is the subaerial region with distributary channels, the delta front is the shallow underwater region where mouth bars form, and the prodelta is the deepest region where fine sediments settle out.
3. Deltas are classified based on dominant hydrodynamic processes, including river-dominated, tide-dominated, and wave-dominated deltas which have characteristic morphologies and sedimentary structures.
Isotope hydrology uses naturally occurring isotopes and tracers to understand hydrological processes like recharge rates and mechanisms, surface water and groundwater interactions, and pollution sources. Key applications include determining the origin and flow of water, and characteristics of aquifers. Environmental isotopes like hydrogen, oxygen, carbon, and radiogenic isotopes provide information over large spatial and temporal scales. Measurements of isotope ratios in water samples using mass spectrometry can reveal the origin and movement of groundwater and identify contamination sources. Isotope techniques are effective hydrological tools that provide insights not obtainable by other methods and are important for managing water resources.
The document discusses key concepts related to drainage basins and stream hydrology. It begins by defining a drainage basin and explaining how the drainage basin system operates, with water flowing overland or underground to streams and rivers. It then examines factors that affect runoff and infiltration rates within a basin, such as soil type and vegetation cover. Finally, it addresses drainage basin management techniques as well as stream ordering and concepts like laminar and turbulent flow.
The document discusses groundwater usage and management in India. It notes that groundwater provides 61% of irrigation needs, 85% of rural drinking water, and 45% of urban water supply. However, 803 of 5845 assessment units in India are overexploited, and levels are declining in many areas. The Central Ground Water Board's objectives include comprehensive aquifer mapping, management plans, capacity building, and regulation to shift from "groundwater development" to "groundwater management" in a sustainable way through community participation. The goals are to improve data accuracy, manage aquifers locally, ensure drinking water security, and sustainably develop groundwater resources.
Saltwater intrusion occurs when saline water from the ocean moves into freshwater aquifers located near the coast. It is often caused by groundwater pumping or construction activities that provide pathways for saltwater. Saltwater intrusion impacts freshwater resources and can lead to the loss of vegetation. The Ghyben-Herzberg relation describes the interaction between fresh and saltwater, and estimates that for every foot of freshwater above sea level, there will be 40 feet below. Management strategies aim to maintain groundwater levels and include conservation, alternative water sources, recharge, and monitoring wells.
The document discusses marine pollution and the ocean floor. It begins by defining marine geology as the study of the ocean floor through various scientific investigations. It then describes some key features and characteristics of the ocean floor, including its depth, landscape formed by plate tectonics, and differences in life depending on proximity to shore. The document also discusses the functions of marine geologists in exploring and studying the ocean floor to better understand the Earth.
Evolution of Geomorphic theory- Geomorphology ChapterKaium Chowdhury
1. Early theories of landscape evolution included catastrophism and uniformitarianism. Davis later proposed the cycle of erosion, which described fixed stages of landscape development over time.
2. Penck built on Davis's work by proposing ongoing tectonism could influence landscape evolution. He described waxing, uniform, and waning stages of development driven by changing uplift and erosion rates.
3. King further developed these ideas, arguing landscapes evolve through parallel slope retreat and may culminate in a pediment under certain conditions. Modern geomorphology views landscapes as intricate systems influenced by various dynamic factors and processes.
This document summarizes key concepts from a lecture on life in water. It discusses the hydrologic cycle and how it exchanges water among different reservoirs. It then describes various aquatic systems in more detail, including the ocean and its structure, shallow waters like coral reefs and kelp forests, marine shores and the intertidal zone, estuaries and wetlands, rivers and streams, and lakes. For each system, it outlines characteristics like temperature, salinity, oxygen levels, and how organisms have adapted to conditions in different parts of the system. It also discusses human impacts like pollution, overharvesting, and invasive species.
The document discusses several key topics related to energy flows on Earth:
- It describes how energy from the sun drives most energy flows on Earth through photosynthesis, winds, ocean currents, and other processes. Materials cycle but energy always flows and is lost.
- Key energy flows discussed include the water cycle, atmospheric circulation, ocean currents like the Gulf Stream, and energy and matter flows through ecosystems and food webs.
- The value of natural capital and ecosystem services are highlighted, with examples of how natural systems purify air/water and provide other valuable services at no cost.
- Overall the document provides a high-level overview of major global energy flows and how they interconnect critical Earth systems.
The document discusses groundwater and the water cycle. It describes how (1) water moves among oceans, atmosphere, Earth and biosphere in the water cycle through processes like infiltration, transpiration and precipitation; (2) there is a balance in the water cycle as annual precipitation equals evaporation globally; and (3) groundwater is water located underground in the saturated zone below the water table, where it moves slowly through pores and fractures in rock and soil.
The subsurface occurrence of groundwater may be divided into zones of aeration and saturation. The vertical distribution of groundwater is explained in this module.
Importance of Water
Hydrologic Cycle
Water Use and Resource Problems
Too Much Water
Too Little Water
Global Water Problems
Sharing Water Resources
Water Management
Providing Sustainable Water Supply
Water Conservation
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.
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.
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.
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.
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.
Groundwater occurs beneath the Earth's surface in pore spaces and fractures in rocks and sediments. It originates from rainfall and snowmelt percolating into the ground. Groundwater is found everywhere but is usually within 750 meters of the surface. It makes up about 1% of the total water on Earth but 35 times the amount of water in streams and lakes. Groundwater flows through the hydrologic cycle, entering the ground as precipitation and eventually emerging in streams, lakes, or oceans.
Groundwater is found underground in soil and rock pores and fractures. It is an important source of freshwater. Groundwater exists in three zones: the saturated zone where all pores are full of water, the capillary fringe just above it, and the aeration zone above that. The water table marks the top of the saturated zone. Groundwater interacts with streams, which can gain or lose water from interactions with the water table. Factors like porosity, permeability, and the slope of the water table influence groundwater storage and movement. Groundwater can emerge as springs, hot springs, or geysers, and be accessed via wells. Excessive pumping can cause problems like subsidence and saltwater contamination.
Every continent or island is bordered by a long or short coastline. Coastline is the line separating the land and sea. Coastal zones are the transition zones between terrestrial and marine habitat. They form an interface between land and oceanic natural processes. Coastal areas also are varied in their topography, climate and vegetation. Some are sandy beaches, rocky shores, with or without tidal inlets. The climate of a coast are controlled by the land and sea breezes and the humidity controlled by marine water. Waves are powerful tools for constructive and destructive activities. Hence. the geomorphology of beach, materials and processes are always not constant due to the impact of everlasting action of tides, waves and currents.
Fluvial processes create distinct landforms over time as a river ages. In the youth stage, the river valley is narrow with steep sides. Meanders begin to form in the maturity stage as the river widens and deepens. In the old stage, the river flows across a flat floodplain as it approaches being a featureless plain. Distinct landforms are produced at each stage as the river's erosional and depositional activities change.
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.
1. Deltas form where rivers enter bodies of standing water, depositing large amounts of sediment. They are common features where large rivers meet the ocean.
2. Deltas consist of a delta plain, delta front, and prodelta. The delta plain is the subaerial region with distributary channels, the delta front is the shallow underwater region where mouth bars form, and the prodelta is the deepest region where fine sediments settle out.
3. Deltas are classified based on dominant hydrodynamic processes, including river-dominated, tide-dominated, and wave-dominated deltas which have characteristic morphologies and sedimentary structures.
Isotope hydrology uses naturally occurring isotopes and tracers to understand hydrological processes like recharge rates and mechanisms, surface water and groundwater interactions, and pollution sources. Key applications include determining the origin and flow of water, and characteristics of aquifers. Environmental isotopes like hydrogen, oxygen, carbon, and radiogenic isotopes provide information over large spatial and temporal scales. Measurements of isotope ratios in water samples using mass spectrometry can reveal the origin and movement of groundwater and identify contamination sources. Isotope techniques are effective hydrological tools that provide insights not obtainable by other methods and are important for managing water resources.
The document discusses key concepts related to drainage basins and stream hydrology. It begins by defining a drainage basin and explaining how the drainage basin system operates, with water flowing overland or underground to streams and rivers. It then examines factors that affect runoff and infiltration rates within a basin, such as soil type and vegetation cover. Finally, it addresses drainage basin management techniques as well as stream ordering and concepts like laminar and turbulent flow.
The document discusses groundwater usage and management in India. It notes that groundwater provides 61% of irrigation needs, 85% of rural drinking water, and 45% of urban water supply. However, 803 of 5845 assessment units in India are overexploited, and levels are declining in many areas. The Central Ground Water Board's objectives include comprehensive aquifer mapping, management plans, capacity building, and regulation to shift from "groundwater development" to "groundwater management" in a sustainable way through community participation. The goals are to improve data accuracy, manage aquifers locally, ensure drinking water security, and sustainably develop groundwater resources.
Saltwater intrusion occurs when saline water from the ocean moves into freshwater aquifers located near the coast. It is often caused by groundwater pumping or construction activities that provide pathways for saltwater. Saltwater intrusion impacts freshwater resources and can lead to the loss of vegetation. The Ghyben-Herzberg relation describes the interaction between fresh and saltwater, and estimates that for every foot of freshwater above sea level, there will be 40 feet below. Management strategies aim to maintain groundwater levels and include conservation, alternative water sources, recharge, and monitoring wells.
The document discusses marine pollution and the ocean floor. It begins by defining marine geology as the study of the ocean floor through various scientific investigations. It then describes some key features and characteristics of the ocean floor, including its depth, landscape formed by plate tectonics, and differences in life depending on proximity to shore. The document also discusses the functions of marine geologists in exploring and studying the ocean floor to better understand the Earth.
Evolution of Geomorphic theory- Geomorphology ChapterKaium Chowdhury
1. Early theories of landscape evolution included catastrophism and uniformitarianism. Davis later proposed the cycle of erosion, which described fixed stages of landscape development over time.
2. Penck built on Davis's work by proposing ongoing tectonism could influence landscape evolution. He described waxing, uniform, and waning stages of development driven by changing uplift and erosion rates.
3. King further developed these ideas, arguing landscapes evolve through parallel slope retreat and may culminate in a pediment under certain conditions. Modern geomorphology views landscapes as intricate systems influenced by various dynamic factors and processes.
This document summarizes key concepts from a lecture on life in water. It discusses the hydrologic cycle and how it exchanges water among different reservoirs. It then describes various aquatic systems in more detail, including the ocean and its structure, shallow waters like coral reefs and kelp forests, marine shores and the intertidal zone, estuaries and wetlands, rivers and streams, and lakes. For each system, it outlines characteristics like temperature, salinity, oxygen levels, and how organisms have adapted to conditions in different parts of the system. It also discusses human impacts like pollution, overharvesting, and invasive species.
The document discusses several key topics related to energy flows on Earth:
- It describes how energy from the sun drives most energy flows on Earth through photosynthesis, winds, ocean currents, and other processes. Materials cycle but energy always flows and is lost.
- Key energy flows discussed include the water cycle, atmospheric circulation, ocean currents like the Gulf Stream, and energy and matter flows through ecosystems and food webs.
- The value of natural capital and ecosystem services are highlighted, with examples of how natural systems purify air/water and provide other valuable services at no cost.
- Overall the document provides a high-level overview of major global energy flows and how they interconnect critical Earth systems.
This document describes freshwater biomes and their characteristics. It discusses the two main types of freshwater ecosystems: lentic, which includes still bodies of water like ponds and lakes, and lotic, which includes running water bodies like streams and rivers. It outlines the different biological groups found in aquatic ecosystems, including plankton, nekton, periphyton, neuston, and benthos. It also explains the zones and characteristics of lentic and lotic systems.
This document provides information on collecting, storing, and treating rainwater. It discusses the benefits of rainwater harvesting such as being a primary water source, recharging aquifers, and providing water security. Various components of a rainwater harvesting system are described, including collection surfaces, conveyance methods, first flush diverters, storage containers, and pumping systems. Methods for calculating rainfall catchment and storage sizes are presented. Basic maintenance and treatment options like chlorination and filtration are also covered. The overall document serves as a guide for setting up a rainwater harvesting system.
Freshwater ecosystems include lakes, ponds, rivers, streams, springs, and wetlands. There are two main types - lentic ecosystems, which are standing bodies of water, and lotic ecosystems, which are running water. Lentic ecosystems can be further divided into zones based on depth and vegetation. Lotic ecosystems have rapid zones with strong currents and pool zones with slower currents. Wetlands are areas that are periodically saturated or flooded with shallow water and support unique plant and animal communities. Forested wetlands include swamps and floodplain forests while tidal freshwater marshes occur along estuaries. Freshwater ecosystems provide important resources but occupy a small area globally.
The document provides a water quality report card for streams in the Great Swamp Watershed. It acknowledges the efforts of volunteers and funders who supported water quality monitoring programs. Various water quality parameters are described, including how they impact aquatic life. Each of the major streams in the watershed is given grades for different parameters based on data collected in 2014. Primrose Brook and the upper reaches of Great Brook received the best grades overall, while Black Brook and the lower reaches of Great Brook showed the most impairment. Continued monitoring and improvement efforts are recommended.
This document discusses the dimensions and patterns within river ecosystems. It describes how characteristics of streams change longitudinally from upstream to downstream, becoming wider, slower, and deeper. Changes also occur at the reach scale, with alternating riffles and pools. Laterally, streams have channels, banks, floodplains, and sometimes complex networks of interwoven channels. Vertically, velocity decreases with depth and exchanges occur with groundwater. Species distribution varies across these dimensions and over time. The document also examines how human activities like agriculture, forestry, mining, and urbanization impact watersheds and river ecosystems.
This document discusses several topics related to watersheds and water resources:
1. It provides information on the Russian River Watershed in California, noting it drains 1,485 square miles and its mainstem is 110 miles long.
2. It explains the ordering system for streams, with smaller tributaries joining to form higher order streams.
3. It describes the characteristics of headwater, transition, and flood plain areas of streams, including differences in temperature, slope, fish and plant life.
4. It outlines the water cycle, noting the sun provides energy to evaporate water from various sources, which condenses to form clouds and returns to Earth as precipitation.
This document provides an overview of different ecosystem types, including terrestrial ecosystems like forests, grasslands, deserts, and mountains, and aquatic ecosystems like marine and freshwater. It defines ecosystem as a biological environment consisting of organisms and abiotic components that interact. It describes various forest, grassland, desert, and tundra biomes and their locations. It also outlines the economic and environmental importance of ecosystems in providing resources and regulating climate and water.
Science View Importance of Groundwater and Surface-Subsurface InteractionsIwl Pcu
This document discusses the complex interactions between groundwater and surface water systems. It notes that groundwater flows are influenced by surface water bodies through processes like seasonal water levels and evaporation. It also provides examples of gaining and losing streams based on interactions with groundwater. Additionally, it emphasizes the importance of accounting for stream-aquifer exchanges in water resource models and outlines some challenges around shared water resources in places like the Middle East.
This document discusses water systems and the global water cycle. It describes the three main types of ecosystems - marine, freshwater, and terrestrial - and notes that most global ecosystems are water-based. It then explains the key components of the water cycle, including storages like oceans, groundwater, and glaciers, and flows like evaporation, precipitation, melting, and streams. It notes that the ocean conveyor belt and Gulf Stream play an important role in distributing heat and affecting climate. Finally, it discusses some human impacts like unsustainable water use, changes to flows and storages, and water pollution.
The water : its management and occurencenikhil kadam
The document discusses water resources and pollution. It provides details on the water cycle and sources of water, including that only a small fraction of water is available for human use. It also discusses types of water pollution like sediment, oxygen-demanding wastes, and nutrient enrichment. Solutions to sustainable water use and pollution prevention are outlined.
Combating surface and groundwater pollution in armeniaVarduhi Surmalyan
Armenia is a landlocked country located in the Caucasus region between Europe and Asia. It has a population of 3 million and its capital and largest city is Yerevan. Key points about Armenia's water resources include:
- Surface and groundwater pollution is an issue requiring monitoring and combating measures.
- Major rivers include the Araks and Akhuryan, and Lake Sevan is a major freshwater source, though it faces threats from pollution and requires restoration efforts.
- Investment is needed to restore or construct new wastewater treatment facilities to address untreated sewage pollution of water bodies.
- Monitoring of water quality and quantity is conducted by various state organizations and NGOs play a role in management
- Measuring transpiration is key to understanding plant functioning and its effects on hydrology. Transpiration accounts for 30% of rainfall on average and varies between ecosystems.
- Heat pulse methods like the heat ratio method can precisely measure transpiration rates across a wide range, including low or reverse flows. This provides insights into plant water use and impacts on water resources.
- Comparing water use of different species like bamboo versus eucalypts could help predict effects of land use changes on water supplies in places like Kenya. Precise transpiration measurements are needed to understand these impacts.
The document discusses Pennsylvania's drainage patterns and watersheds. It describes the five major watersheds in Pennsylvania and their tributaries. It also summarizes the key organisms found in freshwater streams, including algae, invertebrates, and vertebrates. Additionally, it outlines several abiotic factors that affect biodiversity in freshwater ecosystems, such as temperature, current, substrate, sunlight, and dissolved substances.
Ens water pollution power point teacher copy period 10 env sciMcGuffey HS
Water is distributed unevenly around the world, with most freshwater frozen in polar ice caps and glaciers. Humans have increased runoff through activities like agriculture, leading to issues like soil erosion. Groundwater exists in aquifers, which can be confined or unconfined. Most global water use is for agriculture, though industrial and domestic use is growing. Water pollution can come from point sources like factories or non-point sources like agriculture. Many pollutants can contaminate water supplies and harm aquatic life. While laws and programs have improved water quality, non-point pollution from sediment, nutrients and pathogens remains a challenge.
- Lakes, rivers, wetlands and forests are part of the natural freshwater cycle. As populations increase, demand for water and energy is growing rapidly, creating challenges as freshwater is scarce in many regions.
- The article presents a study of net water evaporation from the Eastmain-1 Reservoir in Quebec, Canada, based on field measurements from 2008-2012. The study found that the reservoir's net evaporation is close to zero, meaning the reservoir does not significantly increase water loss through evaporation compared to pre-impoundment conditions.
- Methodology included using eddy covariance systems to measure evaporation from the reservoir and evapotranspiration from surrounding forests and wetlands. Results showed annual evap
Assessment of Quality of the Chambal River Using Combination with That of Kot...ijtsrd
The present study was conducted to understand the physico chemical characteristics of Chambal River, in National Chambal sanctuary in Madhya Pradesh. The Chambal River is located in west central India and flows through three Indian states Madhya Pradesh, Rajasthan and Uttar Pradesh. The Chambal also forms part of the Rajasthan Madhya Pradesh boundary. The stretch of Chambal river contained in the National Chambal sanctuary located at 25 º 23 26 º 52N, 76 º 28 79 º 15E is extending up to 600 km downstream from Kota Rajasthan to the confluence of the Chambal with Yamuna river. On the basis of various parameters studied, Chambal River in this stretch can be placed under the category of Class C as per CPCB standards. The Chambal river water in the sanctuary area is pollution free and can serve as a good habitat for many aquatic flora and fauna including endangered species.The Chambal River originates from the summit of Janapav hill of the Vindhyan range at an altitude of 854 m above the msl at 220 27’ N and 750 37’ E in Mhow, district Indore, Madhya Pradesh. The river has a course of 965 km up to its confluence with the Yamuna River in the Etawah district of Uttar Pradesh. It is one of the last remnant rivers in the greater Ganges River system, which has retained significant conservation values. It harbours the largest gharial population of the world and high density of the Gangetic dolphin per river km. Apart from these, the major fauna of the River includes the mugger crocodile, smooth coated otter, seven species of freshwater turtles, and 78 species of wetland birds. The major terrestrial fauna of the adjacent areas are Indian wolf, golden jackal, caracal, jungle cat, desert cat, ratel, small Indian civet and neelgai. Unlike other rivers of greater Ganges drainage system the Chambal River is relatively unpolluted. Dr. Nitin Gupta | Dr. Rakesh Kumar Dubey | Dr. SM Nafees "Assessment of Quality of the Chambal River Using Combination with That of Kota District" Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Volume-6 | Issue-3 , April 2022, URL: https://www.ijtsrd.com/papers/ijtsrd49612.pdf Paper URL: https://www.ijtsrd.com/other-scientific-research-area/other/49612/assessment-of-quality-of-the-chambal-river-using-combination-with-that-of-kota-district/dr-nitin-gupta
This document discusses different sampling methods used in research studies. It describes probability sampling methods like simple random sampling, stratified random sampling, cluster sampling, and systematic sampling. It explains that probability sampling allows for statistical measurement of random error. The document also covers non-probability sampling methods including convenience sampling, quota sampling, judgmental sampling, snowball sampling, and self-selection sampling. These do not allow for statistical measurement of variability and bias. The key sampling methods and their advantages and disadvantages are summarized.
Habituation is a form of non-associative learning where an animal stops responding to a stimulus after repeated exposure. Experiments were conducted with mice and women's groups to study habituation. When exposed to a loud surprised noise, mice initially reflexed but this response decreased with repeated exposure. Habituation helps animals filter irrelevant stimuli from their environments. For example, prairie dogs give alarm calls less frequently for humans they encounter regularly near their trails, conserving their energy. Elephants and other animals in Serengeti National Park also learn to ignore photo safari vans after repeated safe encounters.
Under conditioned learning, Little Albert's experiment is popular as experiment performed on human being. The power point presentation provides brief introduction on the Little Albert's Experiment and similar other experinces
Two broad categories of behaviors are Proximate and Ultimate behaviour. The presentation gives a brief introduction on Proximate and Ultimate causes of behaviour
This document discusses population ecology and population dynamics. It defines key concepts like population size, density, births, deaths, immigration, emigration, natality and mortality. It explains that population ecology studies how populations change over time in terms of these factors. The growth of a population is determined by the equation N=B-D+I-E, where N is population size, B is birth rate, D is death rate, I is immigration, and E is emigration. For a closed population, the growth rate r can be calculated using the equation dN/dt=rN, where r is the intrinsic growth rate.
1) Ecology developed as a field of study over thousands of years, with early concepts found in ancient Hindu and Greek texts from 600 BC and 370 BC.
2) In the 18th and 19th centuries, key thinkers like Linnaeus, Darwin, and Humboldt made important contributions relating to biogeography, natural selection, and interactions between organisms and their environment.
3) The term "ecology" was coined by Ernst Haeckel in 1866, and the field expanded in the 20th century with pioneering work by Shelford, Elton, Tansley, and Eugene Odum on concepts like food webs, ecosystems, and ecosystem ecology.
This document discusses limiting factors and three laws related to limiting factors:
1. Shelford's Law of Tolerance states that organisms have minimum, maximum, and optimal thresholds for environmental factors that determine their success. Outside the thresholds, survival rates decline.
2. Liebig's Law of the Minimum states that growth is limited not by total resources but by the scarcest resource. Like a barrel limited by its shortest stave, increasing the limiting factor increases growth until a new factor becomes limiting.
3. Blackman's Law of Limiting Factors says that when a process depends on multiple factors, its rate is determined by the slowest factor.
Research involves defining problems, formulating hypotheses, collecting and evaluating data, reaching conclusions, and testing those conclusions. It is a systematic process that requires accurate data collection and adherence to ethical standards. Research aims to generate new knowledge and insights through logical reasoning using both inductive and deductive methods. The purpose of research can be descriptive, explanatory, or exploratory. There are different types of research methodologies including basic vs applied, descriptive vs exploratory, correlational vs explanatory, qualitative vs quantitative, and conceptual vs empirical research.
The document discusses the physical and chemical properties of lakes. It describes several key factors that influence lake biology, including temperature, light penetration, depth, turbidity, and dissolved solids. Temperature affects water density and stratification. Light penetration is influenced by factors like latitude, season, time of day, and suspended materials; it determines the depth of photosynthesis. Turbidity is caused by suspended settling and non-settling matters. Color of lake water can indicate composition like algae, clay, diatoms, or dinoflagellates. These physical and chemical attributes shape the ecosystem of each lake.
The document describes the marine biome. It discusses that there are two main types of aquatic biomes: marine water and fresh water. The marine biome is characterized by salt water and is the largest biome. It describes the six major marine ecosystems: (1) open marine, (2) ocean floor, (3) coral reef, (4) estuary, (5) saltwater wetland, and (6) mangrove ecosystems. These ecosystems have unique characteristics and provide habitat for diverse marine species.
Melatonin is a hormone that regulates circadian rhythm and is highest at night. It is produced in the pineal gland and retina in response to darkness. The suprachiasmatic nucleus acts as the brain's master clock, regulating melatonin production and sleep-wake cycles. Too little melatonin can cause insomnia while too much is associated with seasonal affective disorder. Exposure to blue light from screens suppresses melatonin. Consuming certain foods and vitamins, avoiding screens before bed, and sleeping in darkness can help boost natural melatonin levels.
This document discusses biological rhythms, including circadian, circatidal, circalunar, semilunar, and circannual rhythms. It defines biological rhythms as natural cycles in a body's chemicals or functions controlled by an internal clock. The three main properties of biological rhythms are that they have self-sustaining pacemaker mechanisms, maintain normal cyclicity without environmental cues, and are genetically inherited. Examples of biological rhythms discussed include circadian (24-hour), circatidal (twice daily), circalunar (monthly), and circannual (yearly) rhythms exhibited in various animal species' behaviors and life cycles.
The document discusses sexual dimorphism and reproductive strategies in animals. It notes that there is a fundamental asymmetry between males and females, with females producing fewer offspring that require more resources, while males can aim for more offspring. This leads to sexual selection strategies like monogamy, polygyny, and promiscuity. It uses birds as a case study, noting traits like plumage, beaks, weapons, ornaments, and song that have developed through sexual selection. Female birds often choose mates based on traits like bright colors that act as honest signals of health. Fisher's runaway model is discussed as explaining the evolution of attractive but challenging traits that increase sexual differences.
This document discusses parental care and parent-offspring conflict from an evolutionary perspective. It explains that parental care involves behaviors that increase offspring survival at a cost to the parent's ability to invest in other offspring. While parental care benefits offspring fitness, it limits parental reproduction. This can lead to conflict between parents and offspring over how much care is provided as their interests are not fully aligned. The document outlines Robert Trivers' theory of parent-offspring conflict and how it results from differing relatedness levels between parents, offspring, and siblings.
This document discusses mate selection strategies in animals. It defines sexual selection as selection arising through variation in mating success, and distinguishes between intra-sexual selection through male-male competition and inter-sexual selection through female choice of males. Different mating systems like monogamy, polygyny, and promiscuity influence the strength of sexual selection and variance in male mating success. Specific mate selection strategies discussed include harem defense polygyny, where males defend territories containing multiple females; lekking polygyny, where males aggregate and compete on leks to display for females; and polyandry in some jacana species, where females mate with and leave eggs with multiple males.
This document discusses several principles and theories of mate selection, including:
1) Bateman's Principle, which found that males can increase reproductive success through multiple matings while females are limited by the number of offspring they can produce;
2) Fisher's Runaway Model, which proposes that female mate preferences evolve for traits that confer survival advantages to offspring, leading to a runaway process of increasingly exaggerated male traits;
3) Fisher's Sexy Son Hypothesis, which suggests females evolve preferences for males with traits that will benefit their sons' reproductive success;
4) Zahavi's Handicap Hypothesis, where extravagant male traits act as honest signals of genetic quality because only high
The use of Nauplii and metanauplii artemia in aquaculture (brine shrimp).pptxMAGOTI ERNEST
Although Artemia has been known to man for centuries, its use as a food for the culture of larval organisms apparently began only in the 1930s, when several investigators found that it made an excellent food for newly hatched fish larvae (Litvinenko et al., 2023). As aquaculture developed in the 1960s and ‘70s, the use of Artemia also became more widespread, due both to its convenience and to its nutritional value for larval organisms (Arenas-Pardo et al., 2024). The fact that Artemia dormant cysts can be stored for long periods in cans, and then used as an off-the-shelf food requiring only 24 h of incubation makes them the most convenient, least labor-intensive, live food available for aquaculture (Sorgeloos & Roubach, 2021). The nutritional value of Artemia, especially for marine organisms, is not constant, but varies both geographically and temporally. During the last decade, however, both the causes of Artemia nutritional variability and methods to improve poorquality Artemia have been identified (Loufi et al., 2024).
Brine shrimp (Artemia spp.) are used in marine aquaculture worldwide. Annually, more than 2,000 metric tons of dry cysts are used for cultivation of fish, crustacean, and shellfish larva. Brine shrimp are important to aquaculture because newly hatched brine shrimp nauplii (larvae) provide a food source for many fish fry (Mozanzadeh et al., 2021). Culture and harvesting of brine shrimp eggs represents another aspect of the aquaculture industry. Nauplii and metanauplii of Artemia, commonly known as brine shrimp, play a crucial role in aquaculture due to their nutritional value and suitability as live feed for many aquatic species, particularly in larval stages (Sorgeloos & Roubach, 2021).
Professional air quality monitoring systems provide immediate, on-site data for analysis, compliance, and decision-making.
Monitor common gases, weather parameters, particulates.
The binding of cosmological structures by massless topological defectsSérgio Sacani
Assuming spherical symmetry and weak field, it is shown that if one solves the Poisson equation or the Einstein field
equations sourced by a topological defect, i.e. a singularity of a very specific form, the result is a localized gravitational
field capable of driving flat rotation (i.e. Keplerian circular orbits at a constant speed for all radii) of test masses on a thin
spherical shell without any underlying mass. Moreover, a large-scale structure which exploits this solution by assembling
concentrically a number of such topological defects can establish a flat stellar or galactic rotation curve, and can also deflect
light in the same manner as an equipotential (isothermal) sphere. Thus, the need for dark matter or modified gravity theory is
mitigated, at least in part.
EWOCS-I: The catalog of X-ray sources in Westerlund 1 from the Extended Weste...Sérgio Sacani
Context. With a mass exceeding several 104 M⊙ and a rich and dense population of massive stars, supermassive young star clusters
represent the most massive star-forming environment that is dominated by the feedback from massive stars and gravitational interactions
among stars.
Aims. In this paper we present the Extended Westerlund 1 and 2 Open Clusters Survey (EWOCS) project, which aims to investigate
the influence of the starburst environment on the formation of stars and planets, and on the evolution of both low and high mass stars.
The primary targets of this project are Westerlund 1 and 2, the closest supermassive star clusters to the Sun.
Methods. The project is based primarily on recent observations conducted with the Chandra and JWST observatories. Specifically,
the Chandra survey of Westerlund 1 consists of 36 new ACIS-I observations, nearly co-pointed, for a total exposure time of 1 Msec.
Additionally, we included 8 archival Chandra/ACIS-S observations. This paper presents the resulting catalog of X-ray sources within
and around Westerlund 1. Sources were detected by combining various existing methods, and photon extraction and source validation
were carried out using the ACIS-Extract software.
Results. The EWOCS X-ray catalog comprises 5963 validated sources out of the 9420 initially provided to ACIS-Extract, reaching a
photon flux threshold of approximately 2 × 10−8 photons cm−2
s
−1
. The X-ray sources exhibit a highly concentrated spatial distribution,
with 1075 sources located within the central 1 arcmin. We have successfully detected X-ray emissions from 126 out of the 166 known
massive stars of the cluster, and we have collected over 71 000 photons from the magnetar CXO J164710.20-455217.
This presentation explores a brief idea about the structural and functional attributes of nucleotides, the structure and function of genetic materials along with the impact of UV rays and pH upon them.
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...Wasswaderrick3
In this book, we use conservation of energy techniques on a fluid element to derive the Modified Bernoulli equation of flow with viscous or friction effects. We derive the general equation of flow/ velocity and then from this we derive the Pouiselle flow equation, the transition flow equation and the turbulent flow equation. In the situations where there are no viscous effects , the equation reduces to the Bernoulli equation. From experimental results, we are able to include other terms in the Bernoulli equation. We also look at cases where pressure gradients exist. We use the Modified Bernoulli equation to derive equations of flow rate for pipes of different cross sectional areas connected together. We also extend our techniques of energy conservation to a sphere falling in a viscous medium under the effect of gravity. We demonstrate Stokes equation of terminal velocity and turbulent flow equation. We look at a way of calculating the time taken for a body to fall in a viscous medium. We also look at the general equation of terminal velocity.
BREEDING METHODS FOR DISEASE RESISTANCE.pptxRASHMI M G
Plant breeding for disease resistance is a strategy to reduce crop losses caused by disease. Plants have an innate immune system that allows them to recognize pathogens and provide resistance. However, breeding for long-lasting resistance often involves combining multiple resistance genes
Nucleophilic Addition of carbonyl compounds.pptxSSR02
Nucleophilic addition is the most important reaction of carbonyls. Not just aldehydes and ketones, but also carboxylic acid derivatives in general.
Carbonyls undergo addition reactions with a large range of nucleophiles.
Comparing the relative basicity of the nucleophile and the product is extremely helpful in determining how reversible the addition reaction is. Reactions with Grignards and hydrides are irreversible. Reactions with weak bases like halides and carboxylates generally don’t happen.
Electronic effects (inductive effects, electron donation) have a large impact on reactivity.
Large groups adjacent to the carbonyl will slow the rate of reaction.
Neutral nucleophiles can also add to carbonyls, although their additions are generally slower and more reversible. Acid catalysis is sometimes employed to increase the rate of addition.
2. Physical Methods
• Stream order is a measure of the
relative size of streams.
• Range from smallest, first-order,
to the largest, the twelfth-
order(Amazon)
• Over 80% of total length of
Earth’s rivers and Streams are
headwater streams(first and
second order)
3. • As water travels from
source to mouth, the
streams tend to increase
in width, depth, and
discharge.
4. First order streams
• Perennial: carry water
all year
• Smallest streams
• Have no permanently
flowing tributaries
5. Second Order Streams
• Two first order
streams come together
to form one second
order streams.
• However, if a first
order stream joins a
second order, it is still
a second order
6. Third Order Stream
• When two second
order streams come
together, it forms a
third order stream.
• How has the width of
the stream changed
since it was 2nd order?
How about since 1st
order?
7. Fourth Order Stream
• When 2 third order
streams come
together,it forms a
fourth order stream
• How has the width and
canopy changed since
1st, 2nd, and 3rd order
stream?
8. Stream order
• Two of the same order
streams must come
together before that
stream goes up one
level.
12. Types of organic matter
• DOM- Dissolved organic matter
– Soluble organic compounds (<0.5 um) that leach
from leaves, roots, decaying organisms, and other
terrestrial sources
– Microbial sources: algal exudates, senescent
bacteria
– 50% is humic material- HDOM
– Largest pool of organic matter in streams
13. Dynamic Equilibrium
• Stream forms equilibrium between physical
parameters (width, depth, velocity, and sediment load, both means
and extremes) and biological factors
– SEASONAL: Uniform energy processing over
time; different species exploit different available
organic substrates as efficiently as possible
– SPATIAL: Energy loss from upstream = energy
gain/income for downstream
14. Energy Sources- Headwaters
• Shading: Riparian vegetation, limits
light to stream, low autotrophic
production
• Photosynthesis/Respiration (P/R) ratio
will be less than 1 (heterotrophic
stream)
• Lots of CPOM: allochthonous
carbon/energy sources (leaves from
watershed)
• Low temperture
15. Energy Sources- Midreach
• Stream broadening, more light
• P/R > 1, autotrophic production
(phytoplankton, periphyton, macrophytes)
• More FPOM, b/c CPOM
processed upstream
• Energy source is autochthonous.
• High temp variation
16. Energy Sources- Lower Reaches
• Increasing turbidity, even
wider stream, increased
macrophytes
• P/R < 1, net heterotrophic
• Mostly FPOM (vs. CPOM
in the headwaters)
• High phytoplankton, not
enough to cause the river
to become autotrophic
• Large volume, low temp
17.
18. Connections from
upstream to downstream
habitats control flow of
energy and carbon in
fluvial ecosystems, as
well as the species of
aquatic organisms
River Continuum Concept: Vannote et al. 1980
Theme: importance of
light availability in
controlling in situ
production (e.g. P/R)
19. 4 - 6
1 - 3
> 6
STREAM ORDER
River Continuum Concept- BENTHIC INVERTEBRATES
CPOM
CPOM
CPOM
FPOM
FPOM
FPOM
Collectors
Shredders
Scrapers/Grazers
Collectors
Collectors
TESTABLE HYPOTHESIS- Taxonomy is the tool to measure this
20.
21. RCC and Fish Communities
• Headwaters: cool water species (e.g., trout)
• Lower reaches: warm water species (e.g., carp)
• Most headwater fishes feed on invertebrates
• Mid to lower reaches, piscivorous species are also
abundant
• Lower reaches, planktivorous species may be present
22.
23.
24. Construction of a dam
changes the means and
extremes to which the stream
biota are adapted
Construction of a dam can
correspond to a “resetting” of
the river continuum, by
trapping material and making
sunlight more available to
support autotrophic growth.
25. What we have learnt………
• How to name and count river order
• The river continuum concept (RCC) and its
features
• Change in biota and physical features across
the stream orders