Water Words Glossary |
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Please Note: For a more extensive list of abbreviations and definitions, we refer you to an online Water Words Dictionary published by the State of Nevada, Department of Conservation & Natural Resources, Division of Water Resources. [The following glossary was compiled by Sonya Jenssen, in her Comox Valley Drinking Water Reference Guide. The guide may be downloaded from our web site.} Acid RainRainfall containing dissolved toxic industrial gases, maily sulphur and nitrogen oxides. With a pH balance of 5 or less, acid rain becomes damaging for aquatic ecosystems (Pielou, 1998) AcidicA pH below 7; soil normally has a pH of about 6.5 (Rubin, 1989). AirshedGeographical areas in which air quality is a function of the same sources, weather and geography (Ministry of Environment). AlkalineA pH about 7 (Rubin, 1989) Alluvial DepositsAny sediment, including clay, silt, sand, gravel or similar unconsolidated material deposited in a sorted or semi-sorted condition by a watercourse (Humphrey 2000). Ambient Groundwater FlowThe rate of flow and direction of flow of groundwater under unpumped, natural conditions. Alluvial FansA fan shaped accumulation of alluvium deposited at the mouth of a ravine or at juncture of a tributary stream with the main stream (Humphrey 2000). AquiferA body of rock or sediment that holds enough water to serve as a natural underground reservoir. Aquifers vay in size and capacity and may be confined by an almost impereable layer or unconfined so that water rises to the level of the water table (Pielou, 1998). Aquifer Classification SystemClassifies aquifers on the basis of their level of development and vulnerability to contamination. It is map-based and provides a ranking value for aquifers using hydrogeology and water use criteria (Humphrey, 2000). Aquifer ConductivityThe rate of groundwater flow in an aquifer. Rapid groundwater flow in an qaquiferallows for the rapid spread of a contaminant (Piscopo, 2001). Aquifer MediaThe character of the groundwater flow system. The path length and travel time of groundwater within an aquifer will determine how quickly a contaminant will spread through an aquifer (Piscopo, 2001). Aquifer Vulnerability IndexA methodology that can be applied to determine the vulnerability of an aquifer. It is quantitative and based on the thickness of differing overburden types. A numerical index score is generated that can be used to compare groundwater formations (Humphrey, 2000). Aquifer Vulnerability MappingTo map the vulnerability of an aquifer to contamination from sources. Bulnerability mapping does not consider the type of land use abouve an aquifer, only the intrinsic vulnerability of the aquifer, typically based on the type, thickness, and extent of geologic materials overlying an aquifer, depth to water, and type of aquifer materials (Humphrey, 2000). ArtesianAn aquifer and the water in it. It can refer to the release of water to the surface from an aquifer without the aid of a pump (Pielou, 1998). Bed RockRock underlying soil and other consolidated material. Best Management PracticesNow referred to as guidelines (Ministry of Environment, 2006). BiodiversityThe diversity of plants, animals, and other living organisms in all their forms and levels of organization, including genes, species, ecosystems, and the evluntionary and functional processes that link them (BC Watersheds, 2007). BuffersA zone or strip of forest land that separates two areas, usually to protect a sensitive area from the impacts of the adjacent development activities (BE Watersheds, 2007). Catchment AreaAlso referred to as drainage basin. A drainage basin is a region of land where water from rain or snow melt drains downhill into a body of water, such as a river, lake, dam, estuary, wetland, sea or ocean. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels. The drainage basin acts like a funnel - collecting all the water within the area covered by the basin and channeling it into a waterway. Each drainage basin is separated topographically from adjacent basins by a ridge, hill or mountain, which is known as a water divide or a watershed. Especially in North American usage however, watershed refers to the drainage basin itself. Other terms that can be used to describe the same concept are catchment, catchment area, catchment basin, drainage area, river basin and water basin (Wikipedia, 2007). CisternCisterns are commonly used in areas where water is scarce, either because it is rare or because it has been depleted due to heavy use. Early on the water was used for many purposes, including cooking, irrigation, and washing. Present day cisterns are often only used for irrigation, due to concerns over water quality. Cisterns today can also be outfitted with filters or other water purification methods when the water is meant for consumption. Some leave their cisterns open to catch rain or have more elaborate rain-catching systems. It is recommended in these cases to have a system that does not leave the water open to mosquitoes or algae, which are attracted to the water and then carry desease to nearby humans. Some cisterns sit on the top of houses or on the ground highter than the house, and supply the running water needs for the house. They are often supplied not by rainwater harvesting, but by wells with electric pumps, or are filled by manual labor or by truck delivery (Wikipedia, 2007). Climate ChangeDue to an increase in global temperature, evapotranspiration, changes in snowfall and rainfall patterns, and changes in intensity, severity, and timing of storms will occur, which will result in alternations in soil moisture, water runoff, and regional hydrological cycles. The supply of water and the subsequent demand will change, along with water quality. Climate change will have an impact on water resources, hydroelectric generation, human health, navigation and shipping, agriculture, and water quality (Boberg, 2005). Clear CutA silviculture system that removes the entire stand of trees in a single harvesting operation from an area that is one hectare or greater and at least two tree heights in width. A clear-cut is designed to be managed as a even-aged stand where only one ageclass is present (BC Watersheds, 2007). Coal Bed Methane GasA natural gas found in underground coal deposits contained within the coal seam where it is absorbed or attached to coal particles. During extraction, water is pumped out of the coal seams, which lowers the pressure enough to release the gas for collection and sale (Ministry of Environment, 1999). Coli Form BacteriaA large group of bacteria, commonly found in topsoil, bodies of water and animal (fecal) matter (Provincial Health Officer, 2006).
Community WatershedThe drainage area above the downstream point of diversion on a stream for water use that is for human consumption and that is licensed under the Water Act for waterworks purpose or a domestic purpose if the licence is held by or is subject to the control of a water user' community incorporated under the Water Act (Ministry of Forestry, 1996).Confined AquiferAn aquifer bound both below and above by beds of considerably lower permeability than that existing in the aquifer itself. The groundwater in a confined aquifer is under pressure that is significantly greater than that existing in the atmosphere (Humphrey, 2000). ContaminantSolute which through human action intrudes into the hydrologic cycle (Humphrey, 2000) ContaminationImpairment of natural water quality by chemical or bacterial pollution as a result of human activities. The degree of contamination allowed before an actual hazard to public health is created will depend upon the intended end use, or uses of the water (Humphrey, 2000).CryptosporidiumProtozoan that is resistant to chlorine disinfection (Hrudey et. al, 2002). It is a parasite approximately 4-6 micrometers in diameter, most commonly found in mammals. The illness, cryptosporidiosis, consists of watery diarrhea and vomiting. No treatment is available (Provincial Health Officer, 2006). Demand ManagementWater management that is based on short-term cost-benefits to reduce water needs by conserving the resource, saving money and reducing the environmental impact. Demand management looks at how to use less water in the supply system and functions in opposition to supply management. Focuses on strategies to limit water use in cost-effective measures; common demand management strategies include: low-flow toilets, drip irrigation, water recycling (Brandes and Brooks, 2005).Depth To Water TableThis represents the thickness of the geological material above the water table. Ground water is more vulnerable to contamination where the water table is near to the surface. When the barrier zone of soil or rock above the water table is thin, there is little capacity for natural filtration of contaminants before reaching the water table (Piscopo, 2001).DesalinationBased on the concept of vaporizing salt water, leaving the salts behind as concentrated brine, and condensing the produced water vapour for subsequent use. There are three basic methods of desalinisation: distillation, membrane, and reverse osmosis. Water is classified according to its salt content as brackish, dissolved salts of 1,000-3,000 mg/litre, saline with dissolved salts of 3,000-30,000 mg/litre, or seawater with dissolved salts of 3,500 mg/litre (Spulber and Sabbaghi, 1988).Discharge AreaAn area where groundwater and water in the unsaturated zone is released to the ground surface, to surface water or to the atmosphere (Humphrey, 2000).Disinfection By-productsSecondary chemicals produced when a disinfectant reacts with organic matter in water. For example, chlorine reacts to form trihalomethanes. If water is treated to remove organic matter prior to disinfection a lesser amount of by-products will be formed (Provincial Health Officer, 2006).Drainage BasinSee catchment area.Drilled WellA well that is constructed with a drilling rig, such as an air rotary or cable tool drilling rig (Humphrey, 2000).Dug WellA well that is dug by hand or excavated by backhoe. Dug wells are usually shallow (Humphrey, 2000).EcosystemA complete system of living organisms interacting with thesoil, land, water, and nutrients that makes up their environment. An ecosystem is the home of all living things, including humans. An ecosystem can be any size, a log, pond, field, forest, but it always functions as a whole unit (Ministry of Environment, 2006). In other words, the relationship between climate/atmosphere, biodiversity, and the soil/water is dynamic (Meppem et. at, 2005).ErosionThe unnatural accelerated rate of movement of soils and material leading to band failure, mass movements, and scouring of stream banks. Erosion does occur at a slower rate due as a natural process resulting from water currents, rainfall runoff, or wind. Particular forms of erosion include landslides, debris flows and slumps. Single particles dislodged by erosion form sediment that can clog fish gills and bury fish-spawning gravels. Fine silt particles suspended in water are very difficult to remove (Ministry of Environment, 2006).EvaporationWater evaporation from the surface of waters, the land, moist soil, and living vegetation into the air as water vapour (Pielou, 1998).EvapotranspirationThe combination of evaporation from soil and transpiration from plants. A one-hectare stand of Douglas firs evapotranspire about 235 bathtubs full of water vapour (Pielou, 1998).FiltrationA water treatment process that uses a filter medium such as anthracite coal or sand, membranes, activated carbon, etc.) to remove micro-organisms, organic matter, and silts and clays. Filtration reduces turbidity to less than 0.3 NTU at source, removes 99.9 percent of Giardia and Cryptosporidium micro-organisms, reduce chlorine demand and will help to remove unwanted tastes, colour, and odours from the water. The Greater Vancouver Regional district will begin delivering filtered water in 2008 (GVRD, 2008).Finished WaterWater that is delivered to consumers after receiving treament (Davies and Mazumder, 2003).FloodplainA level, low-lying area adjacent to streams that is periodically flooded by stream water. It includes lands at the same elevation as areas with evidence of movin water, such as active or inactive flood channels, recent fluvial soils, and sediment on the ground surface or in tree bark, rafted debris, and tree scarring (BC Watersheds, 2007).Fractured MediaThe characteristics of complex fractured bedrock aquifers that influence the rate and character of groundwater flow and the movility of contaminants (Piscopo, 2001).Fresh WaterFresh water accounts for 2.% of the world's total of water; only 30% of fresh water is in circulation. The fresh water not in circulation is immobilized in polar ice sheets or fossil and/or juvenile groundewater (Pielou, 1998).GiardiaProtozoan parasite present in fresh water, most commonly referred to as beaver fever (Emery, 1994). Giardia can cause diarrhea, abdominal cramps, nausea or vomiting, weight loss and fatigue lasting weeks. Giardia can be carried by humans as well as certain domestic and wild animals (Provincial Health Officer, 2006). Greenhouse GasesGases that play a part in the greenhouse effect include carbon dioxide (CO2 is the most significant greenhouse gas), methane, nitrous oxide, ozone, water vapour, CFCs and other trace gases (Ministry of Environment). Grey WaterWaste water that is recycled for re-use (Emery, 1994). GroundwaterWater that saturates the ground filling all available spaces also known as the saturation zone. There are three types of groundwater: 1. meteoric water that circulates as part of the water cycle; 2. fossil water that is trapped in ancient sediments; and 3. juvenile water that is given off by magna rock. Fossil and juvenile water are not a part of the water cycle but will at some point become released and join the water cycle (Pielou, 1998). Groundwater TableIt is the surface of a body of unconfined grundwater at which the pressure is atmospheric and where rock, gravel, and sand are saturated (Humphrey, 2000). Groundwater VulnerabilityBenerated by concerns about groundwater contamination, the vulnerability of groundwater is relative and not directly measurable. It can be assessed through a measure known as DRASTIC:
Hard WaterWater containing dissolved minerals (Emery, 1994). As water moves through soil and rock, it dissolves very small amounts of minerals. Calcium and magnesium are the two most common minerals that produce hard water; hard water is regarded as healthier to drink than soft water but causes mineral build-up on fixtures and dissolves laundry detergents poorly (Stauffer, 2004, www.hardwater.org). HumidityThe amount of water vapour present in the air. Absolute humidity is measured in grams of water per cubic meter of air (Pielou, 1998). Hydraulic GradientThe slope of the groundwater level or water table (Humphrey, 2000). Hydraulic HeadThe level to which water rises in a well with reference to a datum such as sea level (Humphrey, 2000). Hydro-fracturingHydro-fracturing originated in the oil drilling business with its popularity in the water well drilling industry having grown over the past few years. When a drilled well is hydro-fractured high pressure water is injected through a pipe to expand, clear, or fracture the fissures with the expectation that well production will increase. Hydro-fracturing is not legislated. There are no requirements for the distances from the ocean or neighbouring wells if one wants to hydro-fracture a well to increase groundwater access. This practice can redirect or increase flows, which may affect neighbouring wells via reduced production or a higher salinity count (Mayne Island Integrated Water Systems Society). HydrogeologyStudy of groundwater in its geological context (Humprhey, 2000). Hydrologic CycleAlso known as the water cycle, water is constantly circulating. Fresh water falls as rain or snow on land and sea flowing seaward on the land surface or below it. Water vapours rise into the air from land and sea condensing into clouds and repeating the first step again by falling as rain or snow. HydrologistPractitioners who studies the movement, distribution, and quality of water throughout the Earth, and thus addresses both the hydrologic cycle and wter resources (Wikipedia, 2007). HydrologyThe science of water, its properties and movement over and under land surfaces (BC Watersheds, 2007). ImpermeableImpervious to flow of fluids (Humphrey, 2000). Infiltration GalleryA technique that draws water from an adjacent surface water source and filters it. Pipes are placed parallel to the surface water below the water table in a sub-surface collection system that collects the water through perforated pipes into a chamber where water is then pumped to the distribution system (IDRC, 2007).IrrigationWater that is directed in order to supply water for vegetation (Emery, 1994).. LimnologistPractitioners who study inland, fresh waters (Wikipedia, 2007). LimnologyThe study of inland waters (fresh), including their biological, physical, chemical, geological and hydrological aspects. This includes the study of (natural and man-made) lakes and ponds, rivers and streams, wetlands and groundwater (Wikipedia, 2007). LithologyAll the physical properties, the visible characterristics of mineral composition, structure, grain size, etc. that give individuality to a rock (Humphrey, 2000). Membrane FiltrationA technique that permits removal of particles from a drinking water source on the basisof their molecular size and shape with the use of pressure and specially designed semi-permeable membranes (Provincial Health Officer, 2006). Multi-barrier ApproachAn integrated system of procedures, processes and tools that collectively prevent or reduce the contamination of drinking water from source to tap (Provincial Health Officer, 2006). NitrateAn essential plant nutrient found in fertilizers produced during the breakdown of organic waste. Excessive fertilizer application, improper agricultural waste management or underground septic tanks may increase nitrate levels in groundwater. Nitrates reduce the ability of blood to carry oxygen. Infants under six months are particularly at risk from drinking well-water containing excessive nitrates (Ministry of Environment). Non-point Source PollutionWater pollution caused by one or more activities taking place over a broad area. Agriculture, forestry and urban development are examples of activities that contribute to NPS pollution. Non-point source pollution in aquatic ecosystems can be grouped into five main categories (Ministry of Environment, 1999): 1. Pathogens 2. Oxygen Depleting Substances 3. Nutrients 4. Sediments 5. Toxins Observation WellA well constructed for the objective of undertaking observatioins such as water levels, pressure readings and groundwater quality (Humphrey, 2000). Perched Water TableA separate continuous body of groundwater lying (perched) above the main water table. Clay beds located within a sedimentary sequence, if of limited aerial extent, may have a shallow perched groundwater body overlying them (Humphrey, 2000). PermeabilityThe property of a porous rock, sediment or soil for transmitting a fluid, it is a test of relative ease of fluid floe in a porous medium (Humphrey, 2000). Precautionary PrincipleWhere there is the possibility that a practice may cause serious or irreversible damage to the environment that practice should be modified or curtailed (Ministry of Environment, 1999). This principle recognized the dynamic nature of ecosystems and humanity's current limited understanding abou the interrelationships between parts of the system and how they function (BC Watersheds, 2007). Point Source PollutionWater pollution caused from a single, identifiable source, such as a pipe through which an industrial or municipal treatment plant releases wastewater and pollutants into a water body. Point sources are often controlled through effluent standards, water quality guidelines, permitting programs and liquid waste management plans (Ministry of Environment, 1999). Potable WaterWater provided by a domestic water system that meets the standards prescribed by regulation and is safe to drink and fit for domestic purposes without further treatment (Ministry of Health, 2001). Prescribed Water Supply SystemA water supply system that is of a class prescribed by regulation or is prescribed by regulation (Ministry of Health, 2001). Primary TreatmentTo physically remove settled solids and most discrete suspended and floating solids from the wastewater stream by neutralization, filtration, and sedimentation. This wastewater influent is divided into three output pathways: primary effluent, primary sludge, and aerosols (Spulber and Sabbaghi, 1998). Raw WaterWater that is untreated or unfiltered (Davies and Mazumder, 2003). Recharge AreaThis reflectes the amount of water that percolates from the surface to the water table. The greater the flow of water the more likely that contaminants will pollute the groundwater below the water table from the water flow (Piscope, 2001). Recycled WaterSee grey water. RegulationA law which is passed by the provincial or federal Cabinet, the executive branch of government. Cabinet may only pass regulations where the legislature or parliament has delegated the power to do so through an enactment (BC Watersheds, 2007). ReservoirsA human produced surface body of water created when a dam in constructed. The creation of a reservoir entails the flooding of land and the submergence of vegetation, which increases the introduction of mercury into the food chain, and carbon dioxide, and methane in the atmosphere (Pielou, 1998). RiparianArea adjacent to a stream that may be subject to temporary, frequent, or seasonal inundation and supports plant species that are typical of an area inundated or saturated soil conditions that are distinct from plant species on freely drained adjacent upland sites due to the presence of water (Ministry of Environment, 1999). RunoffThe amount of water that leaves a watershed. The formula used to measure this is [Runnoff = (Precipitation - Evapotranspiration)] (Pielou, 1998). Salt Water IntrusionMovement of salty or brackish groundwater into wells and into aquifers previously occupied by fresh or less mineralized groundwater either through upcoming or sea water encroachment (Humphrey, 2000). SandstoneA sedimentary rock composed of mostly sand-sized particles (Humphrey, 2000). Saturated ZoneThe subsurface zone in which all voids are ideally filled with water under pressure greater than atmospheric (Humphrey, 2000). Sea Water EncroachmentThe lateral landwater movement of sea water into wells and freshwater aquifers (Humphrey, 2000). Secondary TreatmentTo remove biodegradable organic materials by the precipitation of metal hydroxides and the absorpiton of elemental contaminants (Spulber and Sabbaghi, 1998). SedimentationThe process of subsidence and deposition by gravity of suspended matter carried in water; usually the result of the reduction of water velocity below the point at which it can transport the material in suspended form (BC Watersheds, 2007). Sensitive EcosystemParticular to the east coast of Vancouver Island and the Gult Islands, the Ministry of Environment and Environment Canada have mapped out sensitive ecosystems to include: wetlands, reparian, older forest, woodland, coastal bluff, terrestrial herbaceous, sparsely vegated. Human activity has modified 80% of this area (MOE, 2006). SewerAn artificial conduct or system of conduits used to remove human sewage and to provide drainage. Sewers are generally gravity powered (Wikipedia, 2007). ShaleA fine-grained sedimentary rock formed by the consolidation of clay, silt, or mud characterized by finely laminating structure and is sufficiently hardened so that it will not fall part on wetting (Humphrey, 2000). Soft PathA planning approach for fresh water that views water as a means t accomplish certain tasks rather than viewing water as the end product. 'Why use water in this application at all' is the driving philosophy. The soft path works within ecological limits and promotes public participation. It is called the soft path partly because it requires less steel and concrete, ie., less infrastructure, better on the environment, and also because it relies on solving society's water problems by working with nature rather than trying to overcome it (Brandes and Brooks, 2005). Soil ErosionThe wearing away of the earth's surface by water, gravity, wind, and ice (BC Watersheds, 2007). Soil MediaThe effectiveness of the sol to act as a barrier to surface contaminants depends on its physical properties. For example, thin, permeable soils are ineffective barriers (Piscopo, 2001). Solar AquaticsSun-based method of purifying waste without hazardous chemicals; this water treatment process mimics the natural cycle at an increased rate (Todd, 1990). Source to TapA way of looking at the entire water supply system, from the source water in a watershed through to the treatment and distribution systems to where water reaches the consumer (Provincial Health Officer, 2006). Source WaterThe body of water from which a drinking water supply originates. Source water can be surface water or goundwater (Provincial Health Officer, 2006). Specific CapacityThe rate of discharge from a well per unit drawn (Humphrey, 2000). Specific Conductance (groundwater)The ability of a water sample to conduct an electric current related to the concentration of dissolved solids in a water sample (Humphrey, 2000). SpringNatural appearance of groundwater that comes to the surface (Emery, 1994). Static Water LevelThe level of water in a well that is not being influenced by groundwater withdrawals. The distance to water in a well is measured with respect to some datum, usually the top of the well casing or ground level (Humphrey, 2000). StewardshipStewardship refers to the concept of responsibly managing natural resources for the benefit of present and future generations and encouraging the active participation of persons or groups, including citizens, communities, government and industry (Ministry of Environment, 1999). StormwaterWater that originates during pecipitation events. It may also be used to apply to water that originates with snowmelt or runoff water from over-watering that enters the stormwater system. Stormwater that does not soak into the ground becomes surface runoff, which either flows into surface waterways or is channeled into storm sewers. Stormwater is of concern for two main issues - one related to the volume and timing of runoff water (flood control and water supplies ) and the other ralted to potential contaminants that the water is carrying (water pollution). Because impervious surfaces (parking lots, roads, buildings) do not allow rain to infiltrate into the ground, more runoff is generated than in the undeveloped condition. This additional runoff can erode watercourses (streams and rivers) as well as cause flooding when the water is flushed out of the watershed during the storm event, little infiltrates the soil, replenishes groundwater, or supplies stream base flow in dry weather (Wikipedia, 2007). Effects of Urbanization on Stormwater (Ministry of Environment, 2006)
Storm SewersLarge pipes that transport storm water runoff from streets to natural bodies of bodies to avoid street flooding (Widipedia, 2007). StatigraphyThe study of rock strata, especially the distribution, deposition and age of sedimentary rocks (Humphrey, 2000). Supply ManagementA water management philosophy that strives to meet the water demands of the consumers in contrast to demand management. Policies are based on the presumed need for new infrastructure and how to best meet projected water needs given current trends in water use and population growth (Brandes and Brooks, 2005). Sustainable DevelopmentDevelopment that meets the needs of the present without compromising the ability of future generations to meet their own needs is the most widely used definition from the Brundtland commission. this is a compelx term that could refer to the goal of establishing a balance between environmental, social, and economic interactions. The concept of sustainable water development is now widely considered essential in most countries in the world albeit sustainable water management is inherenlty impossible to achieve (Tortajada, 2005). Sustained YieldRate at which groundwater can be withdrawn from an aquifer without long-term depletion of the supply (Humphrey, 2000). SwaleA low tract of land that is moist or marshy. The term can refer to a natural landscape feature or a human-created one. When created by humans, this open drain sstem is designed to manage water runoff (Wikipedia, 2007). Tertiary TreamtnetThis type of treatment is divided into three processes: sludge treatment, nitrification, and de-nitrification; single or mulit-media filtration; and granular carbon absorption and ion exchange (Spulber and Sabbaghi, 1998). Topography SlopeThe slope of the land and changes in the slope can influence the proportion of rainfall that stays on the surface as runoff versus how much infiltrates into the soil. Flatter ground at the base of steeper slopes can be important areas of water infiltration (Piscopo, 2001). TranspirationWhen plants absorb water from the ground and exhale it into the air as water vapour (Pielou, 1998). TransmissivityGroundwater flow (Piscopo, 2001). Values expressed in square metres per day (m2/day) or as square meters per second (m2/s). TurbidityIs commonly known as cloudy water and is a measure of the interference of the passage of light through water. Turbidity in the water can interfere with: disinfection by creating a potential shield for disease-causing organisms; maintenance of an effective chloring residual; and bacterial testing of water (Spulber and Sabbaghi, 1998). Turbidity is measured in units called nephelometric turbidity units (NTUs); the Greater Vancouver Regional Districk measures turbidity levels daily (GVRD, 2007). Ultraviolet (UV) disinfectionA physical process rather than a chemical one that decreases the use of chemicals in water treatment. A superior way to protect against pathogens such as giardia and cryptosporidium (GVRD, 2007). Unconfined AquiferAn aquifer in which the water table is free to fluctuate under atmospheric pressure (Humphrey, 2000) Vadose ZoneThe texture of the partly-saturated soil and rock above the water table. It determines how quickly water and also contaminants can infiltrate to the water table (Piscopo, 2001). Wastewater Collection SystemThe portion of a wastewater system including pumping stations in which wastewater is conveyed from the property line in the instance of a residential or commercial connection or the perimeter of a unit process in the case of an industrial connection to the wastewater treatment plant or the receiving water (EOCP, 2006). Wastewater Treatment PlantThe portion of a wastewater system that improves or alters the physical, chemical, microbiological quality of the wastewater other than through the process of screening and/or disinfection prior to discharge to the receiving environment (EOCP, 2006). Water BalanceA record of the outflow from, inflow to, and storage in a hydrologic unit like an aquifer or drainage basin (Humphrey, 2000). Water Distribution SystemThe portion of a potable and/or process water system in which water is conveyed from the water treatment plant or point of supply to the point of consumption (EOCP, 2006). Water ManagementWater supply, water treatment, water distribution, wastewater collection and processing, flood control, navigation, hydropower production, and aquatic recreation, all of which interact with one another and through government policies (Spulber and Sabbaghi, 1998). Water QualityComprised of selected physical, chemical, biological, and microbiological indicators that classify water according to their quality (Spulber and Sabbaghi, 1998). Water RightsRights to a claim on water that include formal rights embodied in permits and legislation, less formal rights based on customary patterns, and rights that are implicit in social norms and local practices. For example, it is our customary pattern to receive water twenty-four hours a day whereas this is not uniform practice globally. In Canada, the right to access water is based on riparian law and prior allocation. There are federal, provincial, and regional laws regulating one's right to water making water allocation not a singular legal process but a negotiated process that involves many stakeholders, laws, history, and practices (Meinzen-Dick and Bruns, 2000). Water ScarcityWhen the demand for water exceeds the available supply. Demographic variables stronly influence demand for water, thus, water-scarcity is also economically and socially driven. Scacity can be classified into three different causes: absolute scarcity is limited by technology and is a function of the hydrological climate; economic scarcity is limited by economic choices and while there may be plenty of water in an area it is located far from where it is needed; and induced scarcity is from the political choices that cause to procure scarcity acerbated by human behaviour (Boberg, 2005). Water SupplierA person who is the owner of a water supply system (Ministry of Health, 2001). Water Supply SystemTwo plus hook-ups are considered a water system; a water operator is someone certified to maintain this system, and a water purveyor is a combination of the engineering, technical, and staff that provide water to people connected on the water system (Ministry of Health, 2001). Water TableAlso known as water-table aquifer, a water table is the upper surface of groundwater. Below the water table is an unsaturated zone where pores and cracks are only partially filed with water containing air as well. Only swamps and marshes do not have an unsaturated zone (Pielou, 1998). Water Treatment PlantThe portion of the water system, exclusive of the act of disinfection or fluoridation, which improves or alters the physical, chemical, or microbiological quality of the water being treated (EOCP, 2006). Water UsersClassified by the type of water one needs and the economic capabilities linked to those decisions. Different water users include: households, industry, public utilities, agriculture, and tourism (Spulber and Sabbaghi, 19998). Regions vary in their water demands and vary dependent on the geography, the amount of time, quantity used relative to which economic sector exists in the region, seasonal fluctuations, population size, migration, urbanization, but generally on a global scale agriculture uses 70%, industry uses 20%, and domestic uses 10% (Boberg, 2000). Water VapourAn invisible gas that is evaporated water from its liquid state. Water molecules that are a part of water vapour in the atmosphere tend to return quite quickly as they are in constant motion (Pielou, 1998). WatershedA drainage basin containing the land that drains into the entire watershed where streams and tributaries contribute to a larger network of the river's watershed. Each watershed in a region is biologically isolated from the others, and the plants and animals have mutually adapted to living in a self-contained community (Pielou, 1998). Water systems in a watershed include: interception (forest canopy), surface run-off (top soil), interflow (soil), and groundwater (aquifer) (Marsh, 2006). WellsA hole dug in the ground to access groundwater (Emery, 1994). Well InterferenceWhen an area of influence, or the cone of depression around water well comes into contact with or overlaps that of a neighbouring well pumping from the same aquifer and thereby causing additional drawdown or drawdown interference in the wells (Humphrey, 2000). Well Recharge ZoneThe area of land from which water percolates into an aquifer and is transmitted into one or more wells that are used or are intended to be used to provide drinking water (Ministry of Health, 2001). WetlandLand that is inundated or saturated by surface or groundwater at a frequency and duration sufficient to support, and under normal conditions does support, vegetation typically adapted for life in saturated soil conditions including swamps, marshes, bogs, and estuaries (Fish Protection Act).
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