environmental engg -i

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    The main sources of water

    Rain

    Surface source :

    Oceans,

    Rivers and streams ,

    ponds & lakes, Storage reservoirs

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    Subsurface sources

    Springs

    Infiltration galleries

    Infiltration wells

    Wells and tube wells

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    Rain water is the purest water in nature.

    Physically, it is clear, bright and sparkling.

    Chemically, it is very soft water containingonly traces of dissolved solids (0.0005percent).

    Being soft, it has a corrosive action on leadpipes.

    Bacteriologically, rain water from cleandistricts is free from pathogenic agents.

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    Rain water tends to become impure as itpasses through the atmosphere.

    It picks up suspended impurities from theatmosphere such as

    Dust

    Soot and microorganisms

    Gases such as carbon dioxide, nitrogen,

    oxygen and ammonia.

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    Gaseous sulphur and nitrogen oxidesthat use fossil fuels.

    React with atmospheric water, formingdilute solution of sulphuric and nitricacid.

    Precipitation of these acids (acid rain)

    has serious impacts on surface waterquality.

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    picks up the characteristics of the surfaceover which it passes.

    If water flows across a parking lot, gasoline,oil, and other contaminants may be carriedby or dissolved into the water.

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    Dependable supply of water.

    Grossly polluted

    River water is turbid during rainy season

    Clarity of water is no guarantee that the riverwater is safe for drinking

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    Water may pick up

    fertilizers,

    road salts,

    radioactivity, andbiological contaminant from farms, as well as

    countless other biological, physical, and chemical

    pollutants

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    Contains dissolved and suspended impurities The bacterial count, including the human

    intestinal organisms may be very high.

    The impurities of river water are derived fromSurface washings,

    Sewage and sullage water,

    Industrial and trade wastes, and

    Drainage from agricultural areas.

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    Natural forces of purification such as

    Dilution

    Sedimentation

    Aeration Oxidation

    Sunlight, plant and animal life

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    Adequate to supply the water demand of thetown

    Reasonably surplus

    Compensate losses

    Evaluated for drought

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    Basin constructed across a river or valley tostore water during excess river flow

    Created either across the river or off the

    riverWater stored can be used for other purposes

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    Quantity of water available

    Quality of water

    Possibility of constructing a water tightreservoir

    Distance of the source from the city

    Elevation of the site with reference to theelevation of the city

    Source of contamination

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    Topography of the valley to decide theheight of dam

    Length of dam

    Value of the land

    Need for displacement of people, wildlife etc

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    Geology of the catchment area, dam site,reservoir area

    Study the nature of the catchment area,

    reservoir area and dam site Presence of permeable strata may account

    for high percolation losses

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    Based on flow expected once in 3 years

    Determined from the contour map of thearea

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    Evaporation losses

    Absorption loss

    Percolation loss

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    Natural depression

    Contribution by small natural streams andG.W springs

    Quantity depends by

    Size

    Catchment area

    Annual rainfall

    Geological formation

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    Ground water is the cheapest and mostpractical means of providing water to smallcommunities.

    Ground water is superior to surface water,because the ground itself provides aneffective filtering medium.

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    It is likely to be free from pathogenic agents;

    It usually requires no treatment

    The supply is likely to be certain evenduring dry season

    It is less subject to contamination thansurface water.

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    It is high in mineral content, e.g., salts ofcalcium and magnesium which increase thewater hard

    It requires pumping or some arrangementto lift the water.

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    When ground water comes to the surfaceand flows freely under natural pressure, it iscalled a "spring".

    Springs may be of two typesShallow springs - Dry up quickly during

    summer months

    Deep springs - Do not show seasonalfluctuations in the flowof water

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    In some geographic areas, springs constitutean important source of water.

    Springs are simpler to exploit, as no

    pumping is needed to bring the water to thesurface.

    Springs are exposed to contamination.

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    Quantity of water

    Quality Of water

    Location of source

    Cost of water supply project