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