WATERSHED NOTES SOL 6.7, 6.9, 6.5 Videos:Nye Rivers and Streams, Erosion; Schlessinger Media “All About Land Formations Chap5 and 6 A watershed is the land that water flows across, under, or through on its way to a stream, river, lake, wetland, or other body of water. http://www.unesco.org/water/ http://ga.water.usgs.gov/edu/watercycle.html http://gomex.erma.noaa.gov/erma.html#x=89.51660&y=24.64702&z=5&layers=1613+ 1759+3023+3582+3575+497 Gulf oil leak http://water.epa.gov/type/watersheds/whatis. cfm Federal Govt. website A watershed is an area of land where all the water including rain, snowmelt and groundwater flows into the same stream, lake, river or bay. The boundary of a watershed is not tied to any political boundaries, but to the topography of the land. A ridgeline, or high area, separates one watershed from another. Water flows from the ridgeline down, often to an elevated plain or plateau. A steep slone, called a fall line, often connects the plateau to the low plains. At the water's edge is the riparian buffer, a crucial area because it is the last section of land before the water begins. Small watersheds encompass small land areas and typically drain into small bodies of water. The runoff from small watersheds characteristically joins together with that from other small watersheds to form a larger watershed. Usually, the larger the body of water, the larger its watershed. http://multimedia.wri.org/watersheds_2003/index.html (Watersheds of the world) Areas of higher elevations, such as ridgelines and divides, separate watersheds. http://www.recyclebank.com/recycling The Virginia Department Virginia. of Game and Inland Fisheries defines 12 major watersheds in Virginia. http://va.water.usgs.gov/projects/wshed_model.html (multi-state regional watershed map) www.cnr.vt.edu/PLT/watersheds.html maps (VA 12 watersheds) http://va.water.usgs.gov/ (data site for ground water and various/real time) http://www.vims.edu/bridge/archive0203.html (nice watershed notes) http://www2.ctic.purdue.edu/kyw/Quizzes.html ONLINE QUIZZES and other information links http:/ga.water.usgs.gov/edu/ ( many links for watershed and use) http://water.usgs.gov/education.html GREAT GENERAL RESOURCE SITE http://ga.water.usgs.gov/edu/wateruse.html WATER USE INFO http://www.conservationinformation.com/?action=learningcenter_kyw_whatisawatershed watershed vocabulary worksheet (see this file pg 24) http://ga.water.usgs.gov/edu/dictionary.html http://earthtrends.wri.org/maps_spatial/watersheds/ncamerica.php http://www.glencoe.com/sec/science/webquest/content/virginiawatershed.shtml WEBQUEST SITE The 3 major regional watershed systems in Virginia lead to the Chesapeake Bay, the North Carolina sounds, or the Gulf of Mexico. 60% of Virginia is part of the Chesapeake Bay watershed, which covers 64,000 square miles in six states. This includes five watersheds in Virginia: the James River, York River, Rappahannock River, Potomac and Shenandoah Rivers, and the Eastern Shore. ************************************************************************ Two of Virginia’s watersheds empty into the Albemarle Sound in North Carolina; they include the Chowan River (containing the southern portion of Virginia Beach and Chesapeake) and the Roanoke River. ************************************************************************ The Big Sandy River and the New River eventually empty into the Ohio River. The Clinch, Powell, and Holston Rivers empty into the Tennessee River, which meets the Ohio River just before it empties into the Mississippi River. River systems are made up of tributaries of smaller streams that join along their courses. Rivers and streams generally have wide, flat, border areas, called flood plains, onto which water spills out at times of high flow. Virginia has 497 sub-watersheds, which are made up of small creeks and streams that filter into larger ones before merging into rivers. http://www.dgif.virginia.gov/education/sol/watersheds.asp Virginia’s Watersheds Virginia Watersheds USGS Hydrologic Unit River Systems For use with Science SOLs – 4.8, 6.7, ES9, Bio9 Chesapeake Bay and MidAtlantic Region: Eastern Shore Drainage: Pocomoke River Machipongo River Chincoteague River Potomac Drainage: Potomac River Shenandoah River Occoquan River North River Middle River Little Wicomico River Dry River York Drainiage: South River South Anna River Po River Pamunkey River North Anna River Ni River New Found River Mattaponi River Little River Rappahannock Drainage: Western Branch Corrotoman River Ware River Thorton River Robinson River Rappahannock River Rapidan River Portobago Creek Pankatank River North Fork Thorton River Massaponax River Hazel River Great Wicomico River James Drainage: James River Rivanna River Maury River Cowpasture River Jackson River Buffalo River Piney River Appomattox River Chickahominy River Lynch River Roach River Rockfish River Tye River Pedlar River Nansemond River Hardware River Bullpasture River South Atlantic Region Chowan Drainage: Warwick Branch South Meherrin River Nottoway River North Meherrin River Middle Meherrin River Meherrin River Little Nottoway River Chowan River Blackwater Swamp Blackwater River Assomoosick Swamp Roanoke Drainage: Banister River Big Otter River Blackwater River Dan River Falling River North Mayo River Pigg River Roanoke River Sandy River Stinking River Turkeycock River Yadkin Drainage: Ararat River Ohio Region New River Drainage: Knob Fork Laurel Fork Little River Muskrat Branch New River Tract Fork Wolfpen Branch Big Sandy Drainage: Cranes Nest River Levisa Fork River McClure River Pound River Russell Fork Tug River Tennessee Region Holston Drainage: Big Moccasin Creek Holston River Possum Creek Walker Creek Whitetop Laurel Creek Clinch Drainage: Clinch River Guest River Little River Powell River Rivers and streams carry and deposit sediment. As water flow decreases in speed, the size of the sediment it carries decreases. http://www.chesapeakebay.net/ http://www.chesapeakebay.net/glossary.aspx?menuitem=14875 GLOSSARY OF WATERSHED TERMS The Estuary System An estuary is a partially enclosed body of water where fresh water from rivers and streams mixes with salt water from the ocean. It is an area of transition from land to sea. Estuaries are among the most productive environments on earth, creating organic matter and providing many different types of habitat that support diverse communities of plants and animals. The Chesapeake Bay Estuary Chesapeake Bay is the largest of 130 estuaries in the United States. About half of its water volume comes from salt water from the Atlantic Ocean. The other half drains into the Bay from its enormous 64,000-square-mile watershed. Because of this mix of fresh and salt waters, the Bay's salinity gradually increases as you move from north to south. Of the 50 major tributaries that flow into the Bay, just three deliver about 80 percent of the fresh water. The Susquehanna River (48 percent) The Potomac River (19 percent) The James River (14 percent) As a highly productive estuary, the Chesapeake provides an array of critical habitats for thousands of species of fish, birds, mammals and other wildlife. Migratory waterfowl stop and feed in wetlands, marshes, open waters and shallow waters during their seasonal flights. Anadromous fish like shad and sturgeon spawn in the Bay watershed's freshwater rivers and streams. Underwater bay grass beds growing in shallow waters protect juvenile fish and blue crabs, as well as molting blue crabs, from predators. In addition to serving as wildlife habitat, the wetlands that fringe estuaries also perform valuable functions like filtering polluted runoff, absorbing flood waters and preventing erosion. Estuaries support educational and recreational activities like boating, angling, swimming and bird-watching. They are also commercially important, serving as nursery grounds for commercial fish and shellfish. Chesapeake Bay is home to Baltimore and Hampton Roads, two of the North Atlantic's five major shipping ports. Estuaries are partially enclosed bodies of water where freshwater from streams and rivers meets salty ocean water. Bays, lagoons, harbors, inlets, and sounds are examples of estuaries. Estuaries perform important functions, such as providing habitat for many organisms and serving as nurseries for their young. A very large number of fish that are used commercially return from the ocean to spawn in the protective waters of estuaries. 75% of commercial fish catch and 80% of recreational fish catch make their home in estuaries. Oysters, clams, and crabs thrive in the bays and inlets. Estuaries provide a habitat for endangered and threatened birds. People depend on estuaries for trade, food, and shelter from violent open ocean water. Among other benefits, estuaries provide recreation in the form of swimming, boating, fishing, surfing, and bird watching. Estuaries act as a natural laboratory for scientists and students. The economy of many coastal communities is directly linked to the aesthetic beauty of the estuary nearby. Like our rivers and streams, estuaries are in danger as a result of human activity. Much trash and sediment from upriver are carried into the estuary. Chemical contamination in an estuary can linger for years and close down fishing in those areas. Silt and other sediment caused by erosion can suffocate bottom-dwelling plants and animals. Nutrients from upstream make their way into the estuary and cause overenrichment of the water and oxygen depletion. Altering the natural water flow primarily by dredging and filling wetlands for development purposes has devastating effects on the estuary. Wetlands act as a buffer zone to the estuary by filtering and breaking down nutrients. The Chesapeake Bay is an estuary where fresh and salt water meet and are mixed by tides. It is the largest estuary in the contiguous United States and one of the most productive. However, the population around the Chesapeake Bay has reached 15 million people and the bay’s natural resources are being threatened. (VA Dept of Ed.) www.vanaturally.com/guide/water.html Loudoun County monitering locations http://www.loudounwatershedwatch.org/pdf/LWW_Educational_Map.pdf (Loudoun Illustrative map/student copy) Watershed Flow Chart Toxic-substances from industries Habitat for animals Nutrient runoff Absorb excess water Filter pollutant CREEKS, STREAMS, LAKES, MAJOR RIVERS WETLANDS ESTUARY Recreation Wastewater Soil erosion Trap sediment Replenish groundwater Habitat for plants & animals Pathogens http://www.winchesterstar.com/showarticle_new.php?sID=6&folde rname=20090325&file=Spout%20Run_article.html http://www.dispatch.com/content/stories/local/2015/11/17/Newarkcreek-fish-kill.html thousands of fish killed when truck crashed. Today's Troublemakers Sediments - from soil erosion Farm erosion- Phosphates and nitrates(fertilizers) from agricultural sources Waste from livestock factory farms- Improperly treated sewage - from overflows during storm events, or from failing septic systems Industrial wastes such as acids, oils, and grease - from factories and other industrial facilities Acids and leachates - from abandoned mines and dumps Encroaching salt water - from the ocean Urban and suburban stormwater flows - from storm events into groundwater supplies Herbicides and pesticides - from water and sediments running off the land C h e m i c a l f i e l d t e s t k i t s . D i s s o http://winchesterstar.com/article_details.php?ArticleID=6571 l v e d o x y g e n . Winchester Star article WETLANDS Wetlands form the transition zone between dry land and bodies of water, such as rivers, lakes, or bays. Wetlands can be marshes, swamps, bogs or fens. Marshes (source: http://www.epa.gov/owow/wetlands/types/marsh.html) Marshes are defined as wetlands frequently or continually inundated (covered) with water, characterized by emergent soft-stemmed vegetation adapted to saturated soil conditions. There are many different kinds of marshes, ranging from the prairie potholes to the Everglades, coastal to inland, freshwater to saltwater. All types receive most of their water from surface water, and many marshes are also fed by groundwater. Nutrients are plentiful and the pH is usually neutral leading to an abundance of plant and animal life. Marshes can be tidal or non-tidal. The presence of marshes in a watershed helps to reduce damage caused by floods by slowing and storing flood water. Marsh vegetation and microorganisms also use excess nutrients for growth that can otherwise pollute surface water such as nitrogen and phosphorus from fertilizer. In fact, marshes are so good at cleaning polluted waters that people are now building replicas of this wetland type to treat wastewater from farms, parking lots, and small sewage plants. Both estuarine (salty or brackish water) and palustrine (freshwater) wetlands perform important functions, including regulating runoff by storing flood waters; reducing erosion by slowing down runoff; purifying water by filtering sediments, trapping nutrients, and breaking down pollutants; and recharging groundwater. They also provide food and shelter for fish and other aquatic life and nesting and resting areas for migratory birds. Other names for wetlands include swamps, marshes, and bogs, which are characterized primarily by their vegetation: Swamps are wetlands where the most common plant types are trees (cypresses, willows, oaks), vines (poison ivy), and shrubs. They occur in low-lying areas near slow-moving rivers and need a steady supply of water in order for trees to grow. Marshes are treeless wetlands sometimes called wet meadows. Grasses, reeds, cattails, and nonwoody plants called rushes and sedges are common marsh plants. Marshes often form on floodplains where rivers overflow their banks. Bogs are characterized by low to medium-height woody plants. The only source of freshwater in a bog is rain. Since no streams carrying nutrients flow into bogs, plants, such as the Venus flytrap, get nutrients from insects. Because water does not drain from a bog, dead plant material builds up and sinks to the bottom. Eventually a substance called peat is formed. Gardeners use peat from a plant called sphagnum moss, which, when dried, can hold up to 20 times its weight in water. At one time, wetlands were thought to be useless, disease-ridden, mosquito-breeding wastelands that should be improved. Many were drained, filled, and destroyed to make room for residential and commercial developments. It is only recently that people have begun to understand the importance of these valuable areas. As people become more educated about their natural benefits, public support for protection and restoration of wetlands increases. ECOSYSTEM An ecosystem is made up of the living community and the nonliving factors that affect the organisms living in it. The nonliving, physical features of the environment are the abiotic factors, which determine ecosystem type and its distribution of plants and animals. Abiotic factors include: 1. water quality(includes acidity), 2. topography, 3. landforms, 4. geology, 5. climate, 6. soil types, 7. amount of sunlight, and 8. air quality or oxygen availability. The health of an ecosystem is directly related to its water quality. One thing that all watersheds have in common is people. Human activity can alter abiotic factors and thus accelerate or decelerate natural processes. Human activity can affect water quality in two ways: 1)by changing the ecological processes that naturally purify water, 2)and by adding pollutants. For example, people can affect the rate of natural erosion one way or the other. Plowing cropland can cause greater erosion, while planting trees can lessen it. Preserving or destroying wetlands is another example, because wetlands regulate runoff, reduce erosion, purify water by filtering it, and recharge groundwater. Point Pollution vs Non-point Pollution Land-use changes upstream can cause runoff pollution problems for people, plants, and animals downstream that depend on clean, usable water. This form of pollution is called non-point-source pollution (NPS), because the pollution does not come from a single source, such as the discharge from a sewage treatment plant or a factory. NPS pollution is caused mainly by storm-water runoff. When it rains hard, water runs off farmland, city streets, construction sites, lawns, and driveways, carrying sediment, nutrients, pesticides, oil and gasoline, bacteria, and other pollutants with it. One of water’s unique properties is its ability to dissolve a wide variety of compounds. Thus, water-soluble materials easily pollute water, which then carries these harmful substances into our waterways and other bodies of water. The four primary NPS pollutants are sediment, nutrients, toxic chemicals, and disease-causing pathogens. Sediment is soil carried by rainwater into streams, rivers, and lakes. It cuts light needed by aquatic plants, blocks up waterways, and covers up aquatic habitat. Often the sediment from farmland also carries pesticides and nutrients. Toxic chemicals, such as pesticides, herbicides, and oil and gasoline, can damage and/or kill aquatic animal and plant life. Nutrients, particularly nitrogen and phosphorus, over-enrich bodies of water, causing excessive growth of algae. When algae die, bacteria decompose it, decreasing the water’s dissolved oxygen level in the process. Low oxygen can kill or cause distress to aquatic animals. Algae also cloud the water and block much-needed sunlight. Pathogens enter bodies of water primarily through human or animal waste. Water-quality monitoring is the collection of water samples in order to analyze chemical and/or biological parameters. Simple parameters include pH, temperature, salinity, dissolved oxygen, turbidity, and the presence of macro-invertebrate organisms. http://water.usgs.gov/nwc/NWC/pH/html/ph.html (U.S. acid rain/PH map) In the past, streams and rivers were often used to dispose of human waste, and open sewers were common. During the mid-1800s, public health officials recognized the connection between disease outbreaks and contamination of public wells and drinking water. Advances in water treatment and sanitary sewers have helped eliminate diseases associated with human waste. SALINITY Partial list of euryhaline fish(can live in fresh or brackish or salt water Herring Lamprey Molly Puffer fish Salmon Shad Striped bass Sturgeon Tilapia Trout Stenohaline describes an organism, usually fish, that cannot handle a wide fluctuation in the salt content of water. Haddock(salt), Goldfish(fresh) http://www.windows.ucar.edu/tour/link=/earth/Water/salinity.html&edu=elem WATER POLLUTANTS Toxic Pollution Gasoline, oil, pesticides. Industrial discharge, runoff from streets and other impervious surfaces. Threatens human health, harms aquatic organisms. Visual observations of oil spills. Macro-invertebrate population. Pathogen Pollution Thermal Pollution Mostly bacteria. Sewage carrying human and animal waste. Hot water. Water used to cool industrial and power plants; water runoff from extremely hot, paved surfaces. Spreads disease causing micro-organisms that typically cause gastrointestinal problems. Decreases dissolved oxygen level, influences survival of aquatic organisms, increases rate of bacteria growth. Total coliform test or fecal coliform test. Thermometer. Macro-invertebrate population. Dissolved oxygen. Weathering 6.5c ESS pg102 http://en.wikipedia.org/wiki/Erosion Water (rain, ice, snow) has shaped our environment by physically and chemically weathering rock and soil and transporting sediments. Freezing water can break rock without any change in the minerals that form the rock (physical weathering). This usually produces small particles and sand. Water with dissolved gases and other chemicals in it causes the minerals in rocks to be changed, leading to the deterioration of the rock (chemical weathering). http://www.fgmorph.com (good photo sight erosion) Erosion is displacement of solids (sediment, soil, rock and other particles) usually by the agents of currents such as, wind, water, or ice by downward or down-slope movement in response to gravity or by living organisms (in the case of bioerosion). Erosion is distinguished from weathering, which is the process of chemical or physical breakdown of the minerals in the rocks, although the two processes may be concurrent. A certain amount of erosion is natural and, in fact, healthy for the ecosystem. For example, gravels continuously move downstream in watercourses. Excessive erosion, however, does cause problems, such as receiving water sedimentation, ecosystem damage and outright loss of soil. Approximately 40% of the world's agricultural land is seriously degraded. CAUSES OF EROSION The rate of erosion tenses on many factors, including the amount and intensity of precipitation, the texture of the soil, the gradient of the slope, ground cover from vegetation, rocks, land use, how much water there is, and possibility of erosion from speed of a stream. The first factor, rain, is the agent for erosion, but the degree of erosion is governed by other factors. You expect areas with high-intensity precipitation, sandy or silty soils and steep slopes to be the most erosive. Soils with a greater proportion of clay that receive less intense precipitation and are on gentle slopes tend to erode less. Logging can cause increased erosion rates due to soil compaction, exposure of mineral soil, for example roads and landings. Leaf litter also shelters the soil from the impact of falling raindrops, which is a significant agent of erosion. Heavy grazing can reduce vegetation enough to increase erosion. EROSION (cont.) The factor that is most subject to change is the amount and type of ground cover. In an undisturbed forest, the mineral soil is protected by a litter layer and an organic layer. These two layers protect the soil by absorbing the impact of rain drops. These layers and the underlaying soil in a forest is porous and highly permeable to rainfall. Typically only the most severe rainfall and large hailstorm events will lead to overland flow in a forest. If the trees are removed by fire or logging, infiltration rates remain high and erosion low to the degree the forest floor remains intact. Severe fires can lead to significantly increased erosion if followed by heavy rainfall. In the case of construction or road building when the litter layer is removed or compacted the susceptibility of the soil to erosion is greatly increased. Alluvial fan http://www.uoregon.edu/~millerm/fan.html http://geology.about.com/library/bl/images/blalluvfan.htm Roads are especially likely to cause increased rates of erosion because, in addition to removing ground cover, they can significantly change drainage patterns . When large numbers of hikers use trails or extensive off road vehicle use occurs, erosive effects often follow, arising from vegetation removal and furrowing of foot traffic and off road vehicle tires. Mass Movement is the down-slope movement of rock and sediments, mainly due to the force of gravity. Mass Movement is an important part of the erosional process, as it moves material from higher elevations to lower elevations. What’s the difference between weathering and erosion? Weathering involves two processes that often work in concert to decompose rocks. Both processes occur in place. No movement is involved in weathering. Chemical weathering involves a chemical change in at least some of the minerals within a rock. Mechanical weathering involves physically breaking rocks into fragments without changing the chemical make-up of the minerals within it. It’s important to keep in mind that weathering is a surface or near-surface process. As you know, metamorphism also produces chemical changes in rocks, but metamorphic chemical changes occur at depth where either the temperature and/or pressure are significantly higher than conditions found on the Earth’s surface. As soon as a rock particle (loosened by one of the two weathering processes) moves, we call it erosion or mass wasting. Mass wasting is simply movement down slope due to gravity. Rock falls, slumps, and debris flows are all examples of mass wasting. We call it erosion if the rock particle is moved by some flowing agent such as air, water or ice. So, here it is: if a particle is loosened, chemically or mechanically, but stays put, call it weathering. Once the particle starts moving, call it erosion. CONSERVATION All living organisms are dependent upon the availability of clean water and air and a healthy environment. While the supply of water seems limitless, water is not an infinite resource. Usable fresh water is actually quite limited and is scarce in some places. Local, state, and federal governments have significant roles in managing and protecting air, water, plant, and wildlife resources. Regulations, incentives, and voluntary efforts help conserve resources and protect environmental quality. Conservation of resources and environmental protection begin with the individual. Understanding the watershed is the first step in protecting water and other natural resources. What goes on upstream can make water downstream unfit to use, forcing downstream users to clean up the water before it can be used again. Use of renewable and nonrenewable resources must be considered in terms of their cost/benefit tradeoffs. Preventive measures, such as pollution prevention or thoughtfully planned and enforced landuse restrictions, can reduce the impact of problems in the future. Pollution prevention and waste management are usually less costly than cleanup. Renewable resources should be managed so that they produce continuously. Sustainable development makes decisions about long-term use of land and natural resources with concern for maximum community benefit for the longest time and with the least environmental damage. The availability of fresh water may not be a problem in the United States today, but it is a problem in other parts of the world, such as the Middle East and northern Africa. The greatest influence on water availability is the number of people competing for it. As population grows, fresh water becomes increasingly less available. China and Canada receive about the same amount of water due to precipitation. However, China’s population is over 40 times that of Canada. It is projected that by the year 2025, one-fourth of the world’s population will be in need of more water. Besides higher populations, higher standards of living increase the demand for water. In the United States, for example, each individual uses approximately 250 liters of water each day, whereas in African nations, the average person uses only slightly more than 29 liters. WATERSHED VOCABULARY 1. abiotic factors - Physical environmental factors (i.e. water, temperature, soil, light) that influence the composition and growth of an ecosystem. 2. aerobic - Any process that requires oxygen. 3. algal bloom - An explosive population increase in algae that occurs when large amounts of phosphates and/or nitrates enter a body of water in the presence of warm temperatures. 4. anaerobic - Lacking or not needing oxygen. 5. aquatic - Living or growing in or on the water. 6. bank erosion - The process in which individual soil particles of a .a* stream bank are carried away as the stream channel moves. The amount of erosion is affected by vegetation, soil composition of the bank, flow of water in the stream, and runoff from the land. 7. bank vegetation - Trees, shrubs, grasses, and other vegetation growing on the stream bank. 8. bay - A body of water partly enclosed by land, but having a wide outlet to the sea. 9. clarity - Clearness. 10. compost - A mixture of decaying organic matter, such as leaves and manure, that can be used as a plant fertilizer. 11. dissolved oxygen (DO) - The amount of oxygen dissolved in water; varies with water temperature and pressure. 12. drainage basin - A watershed; the land area where precipitation runs into streams, rivers, lakes, and reservoirs. It can be identified by tracing a line along the highest elevations, often a ridge, between two areas on a map 13. eradicate - To remove all traces of; to erase. 14. erosion - Process by which earth material is transported from one area to another by an agent such as water or wind. 15. estuary - A place where fresh and salt water mix (i.e. a bay, salt marsh); where a river enters an ocean. 16. ground water - Water that flows or seeps downward and saturates soil or rock, supplying springs and wells; also water stored underground in rock crevices and in the pores of geologic materials that make up the Earth's crust. 17. herbicide - A toxic substance used to destroy plants. 18. inorganic - Compounds which come from non-living things that do not contain carbon. 19. invasive species - Organisms that spread and take over the habitat of native species. (Snakehead fish!) 20. landfill - A huge pit in the ground that is lined with clay or plastic and filled with garbage. Layers of garbage are spread out and alternated with layers of dirt or plastic. 21. non-point source pollution - Pollution discharged over a wide land area, not from one specific location; Diffuse water pollution caused by sediment, nutrients, and organic or inorganic toxic substances carried to lakes and streams by surface runoff. 22. permeability - The ability of a material to allow a liquid to pass through it. Permeable materials, such as gravel and sand, allow water to move quickly through them. 23. phosphate - A form of phosphorous; an essential nutrient for plants and animals; usually present in natural waters as phosphate. Phosphate is an ion composed of one phosphorus atom and four oxygen atoms. 24. pollution - Contamination of air, water, or soil by toxic organic or inorganic substances (e.g., industrial or agricultural waste byproducts, engine exhausts, factory emissions, or human waste). Pollution can come from a single source (point-source) or be discharged over a wide area from many sources (non-point source). 25. respiration - The process that involves the transfer of oxygen to cells and the breakdown of food to release energy. In complex animals, respiration involves the intake of oxygen and the discharge of carbon dioxide. 26. riffle - A rapid, turbulent flow of water over a shallow area in a stream. Riffles add oxygen to the water as water is churned, and provide habitat for many invertebrates. 27. riparian area - The land adjacent to streams, rivers, or other bodies of water that directly affects, or is affected by, the water. A unique habitat that exists in mutual balance with the river channel. 29. runoff - That part of the precipitation, snow melt, or irrigation water that appears in uncontrolled surface streams, rivers, drains, or sewers. 30. sediment - Loose materials such as rock fragments and mineral grains that have been transported by wind, water, or glaciers. 31. stream - A body of water flowing in a natural channel and containing water at least part of the year. 32. tributary - A smaller river or stream that flows into a larger river or stream. Usually, a number of smaller tributaries merge to form a river. 33. turbidity - The amount of solid particles suspended in water that cause light rays shining through the water to scatter. 34. velocity of a stream - The speed and direction of the water flowing in a stream, an important factor in determining what organisms can live in the stream. Measured in units such as feet/sec or meters/sec. 35. wetland - A lowland habitat, such as a marsh, swamp, or bog that has periodically waterlogged soils or is covered with a shallow layer of water resulting in reduced soil conditions yet it still permits standing vegetation.