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HomeWaterWater treatment
 
 
 
Water treatment Company Bangalore India

Water treatment

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A safe water supply is an essential part of camp hygiene.Water intake for adults in temperate conditions is around 3 litres per day, but this can rise to as much as 10 litres per day in hot climates because of loss due to sweating. In addition, around 4 litres of water per person per day will be needed for cooking and washing up. Therefore considerable supplies may be required both at base camp and by field parties. In many cases, water obtained from rivers, lakes and ponds, as well as from taps and wells, carries a considerable risk of contamination. Spring water collected away from human habitation may be safer but it would be wise to treat even this water source.

Before treating the water to kill any organisms, organic matter and silt need to be removed. This can pose considerable problems if you are trying to obtain supplies for a large expedition, where sedimentation tanks and large ceramic filters would need to be employed. Various methods for water purification will be described in this chapter. Some are more suitable for the base camp and others for field workers. Before deciding on the system to use it is also important to consider the likely infective organisms and the risk posed by them to the expedition.

The continuous water cycle
Nature intended us to have high-quality water. This is why we have the continuous water cycle, whereby water from our oceans, rivers, lakes and streams fall to the ground as rain or snow and becomes filtered as it seeps through the earth’s surface. As the water works its way through the ground it picks up minerals by dissolving limestone, causing water hardness. Water may also come into contact with Iron, Manganese, Arsenic and other contaminants, which cause additional water treatment problems. The chart below lists typical whole house water quality problems and indicates which equipment effectively corrects any problems you may have in your home.

 

Explanation of Water Quality Testing Terminology

 

pH
TDS
Conductivity
Hardness
Turbidity
Manganese
Iron
Nitrate
The letters pH stands for ‘p’ potenz or power, and ‘H’ the symbol for hydrogen. So the pH of a solution describes its hydrogen-ion activity. The pH scale ranges between 0 and 14. Water with a pH of 7 is neutral; less than 7 is acidic, and greater than 7 is alkaline. Dissolved gases such as carbon dioxide, hydrogen sulphide and ammonia strongly influence the pH of a solution. The pH of drinking water, in itself, seems to have no effect on health. On the other hand, corrosion is associated with pH levels less than 6.5. Corrosion releases metals such as lead, zinc, copper and cadmium from pipes and fittings, and these substances can be toxic. If the water has a pH of less than 4, the water may have a sour taste. If greater than 8.5, an unpleasant taste may be present as well as scale which forms on pipes and equipment, and the germicidal qualities of chlorine will be reduced. pH is usually measured with a meter that has a probe which is placed in the solution. Allow some minutes for an accurate reading to be given.
TDS is short for Total Dissolved Solids (or Salts). This term denotes the concentration of mineral constituents dissolved in water. It does not include gases, colloids or sediment but consists chiefly of carbonates, bicarbonates, chlorides, sulphates, phosphates and nitrates of calcium, magnesium, sodium and potassium with traces of iron, manganese and a few others. Many Australian waters have characteristically high levels of dissolved solids, the most common of which are sodium bicarbonate and chloride, and calcium and magnesium bicarbonates and sulphates. Taste thresholds vary depending on the particular dissolved solid present. Supplies of water above a TDS of 1500 mg/litre are generally considered unacceptable for consumption without treatment. Sea water has a TDS of around 34,000.
Conductivity is related to TDS in that conductivity is the ability of a substance (a dissolved solid) to conduct an electric current. It is reported in units of Siemens (S), but since natural waters have conductivity values of far less than 1 siemen (S), the data is generally reported in microsiemens or millionths of a siemen (uS/cm). As a general rule, the conductivity is multiplied by 0.7 in order to estimate the dissolved solids. A TDS and/or conductivity meter with a probe is generally used. Reverse osmosis or distillation is the generally accepted method to lower TDS.
Hard water and soft water are terms that have no exact meaning because water considered hard in one area might be considered soft in another. Hardness is usually associated with what happens when soap is used. Soap does not clean as efficiently in hard water. It leaves insoluble residues in bathtubs, sinks, and clothing. In addition, hard water causes scale to build up in water heaters, boilers and pipes thereby reducing their capacity and heat transfer properties. Hardness is commonly reported in milligrams per litre (mg/l) although other terms can be used. For the most part, hardness depends on the concentration of calcium and magnesium.
A general scale of hardness is shown right:
0 – 9 mg/l Very Soft
10 – 30 mg/l Soft 31 – 60 mg/l Slightly Hard
61 – 120 mg/l Moderately Hard
121 – 185 mg/l Hard
Over 184 mg/l Very Hard
Turbidity in liquids is caused by the presence of un-dissolved but finely dispersed matter such as clay, silt, plankton, algae and other microscopic organisms. It can be said to be a lack of brilliance in water and should not be confused with colour which can result from tannins, lignins, humus and peat materials leached from the soil. Clarity of water is important for human consumption and most manufacturing uses. Small handheld turbidity meters are available that pass light, whether visible or infrared, through a sample of water to test for clarity.
Manganese bearing minerals are common in rocks and soils. Manganese may exist in large concentrations in organic material, since it is a plant nutrient. It does not appear to have toxicological significance in drinking water, at least in concentrations typical of natural waters. The recommended limit for manganese in drinking water, 0.1 mg/l, is based largely on aesthetic and taste considerations. Upon oxidation (mixing with oxygen), manganese in excess of 0.2 mg/l tends to precipitate and form noxious deposits on foods during cooking, and black stains on plumbing fixtures and laundry. Concentrations greater than 0.5 mg/l may impart a metallic taste to both foods and water. Treatment generally recommended is either a water softener or a manganese greensand or DMI-65 filter. The generally used method of testing for manganese is either a meter using the photometric method, or a reagent kit which requires the mixing of various chemicals to provide a reading.
Iron is one of the most common elements in the soil and waters of the world. In ground water, iron usually occurs in the ferrous state, but it may quickly and easily oxidise to the ferric state. Ferrous iron even in large quantities in water will be colourless, but when exposed to the atmosphere will become ferric and will be visible as a reddish brown colour. Iron is always measured in milligrams per litre (mg/l). As little as 0.1 mg/l is sufficient to cause disagreeable staining in laundry, plumbing fixtures, etc. Treatment generally recommended is either a birm filter, manganese greensand filter or DMI-65 filter. Iron can be tested with a meter, reagent kit or snap-off ampoules that suck up sample water through a vacuum process and mix the water with chemicals to give a colour reading.

Nitrate in water supplies owes its origin to several possible sources, including the atmosphere, legume plants, plant debris, animal excrement and sewage, as well as nitrogenous fertilisers and some industrial wastes. Nitrate concentrations in water are reported as either nitrate (NO3) or nitrate-nitrogen (as N). Most analysis will use the latter. Nitrate (as N) in concentrations greater than 10 mg/l has been known to cause infant methemoglobinemia, a condition characterised by cyanosis, a bluish colouration of the skin. A similar problem will be seen in livestock with abnormally high mortality rates in baby pigs and calves, and abortion in brood animals. Taste & Odour

Disagreeable odours are caused by a variety of materials, particularly living micro-organisms, decaying organic matter, sewage, and some industrial wastes. Probably the most common odours are the rotten-egg gas smell of hydrogen sulphide, the gasoline smell in supplies polluted by certain hydrocarbons, and the pungent smell of chlorine. A bitter taste may be due to the presence of iron, manganese, large amounts of sulphate, or excess lime. Waters containing a large amount of sodium bicarbonate are often described as faintly inky or sometimes soapy. Water containing an unusual quantity of salt will have a brackish taste. An activated carbon filter is the most practical remedy for removal of most taste and odour problems. However on non-chlorinated supplies, a carbon filter will be biologically fouled by bacteria and will have a limited life span. A combination of disinfection (chlorine, UV, or ozone) and carbon would be recommended.

 

Health Hazards Pollutants
Non Health Hazards Pollutants
Contaminant or Problem Symptoms Possible Cause of Problem Solutions
The following pollutants are health hazards and must be treated for the safety of your family. If you cannot successfully remove these pollutants, you should find an alternative source of water.
Arsenic   Naturally occurring in water in some areas Reverse osmosis; ion exchange
Bacteria   Well not sealed; sewage, manure or surface runoff Remove source of bacteria; chlorination;  ozonation; UV disinfection
Lead   Corrosive water, lead pipes or lead solder Replace plumbing; reverse osmosis; distillation
Nitrate   Well not sealed; faulty septic system; animal waste; fertilizers Remove source of nitrate; distillation; reverse osmosis; anion exchange (water softener)
Pesticides & Organic chemicals   Pesticides & Organic chemicals Use of pesticides, chemicals near water source Activated carbon filter; reverseosmosis; distillation
The contaminants below are not health hazards, but you may choose to treat because of aesthetic reasons.

The following pollutants are health hazards and must be treated for the safety of your family. If you cannot successfully remove these pollutants, you should find an alternative source of water.

Contaminant or Problem Symptoms Possible Cause of Problem Solutions
Bad odor, color, taste, chlorine Chlorine taste; foul odors; damage to hair; itchy skin. Variety of sources Ion exchange; activated carbonfilter; chlorination
Turbidity Cloudy or dirty water Cloudy water; sediment, sand, silt and rust particles. Fine sand, clay, or other particles Mechanical filter
Hardness   Mineral deposits on dishes and glassware; stiff, dingy laundry; high soap usage and need for fabric  softeners; dry, itchy skin and scalp; unmanageable hair; extra work to remove soap curd on bathtubs and shower stalls; high energy costs due to scale build-up in pipes and on appliances Naturally occurring minerals in water Ion exchange (water softener)
Rotten egg odor Hydrogen sulfide gas Chlorination and activated carbon filter
Staining of sink and/or laundry, from iron or manganese Unpleasant metallic tastes; rust particles; staining on plumbing Fixtures; red water; odors. Naturally occurring in water, especiallydeep wells Ion exchange or green sand filter(0-10 ppm); chlorination and filtration (if over 10 ppm)
Acidic water(low pH)  Green stains on bathroom sinks and other porcelain (surfaces; blue green water. (Acidic water mayCause corrosion of pipes & plumbing fixtures.) Acid neutralizer usingCalcite Acid Neutralizing Systems
All of the above All of the above Reverse Osmosis Systems
Scale Built-up   Internal scale formation on plumbing surfaces, appliances and plumbingFixtures One Flow® One Flow Systems
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FAQ's

 

What is the World Water Crisis ?

Rapid population growth, combined with industrialisation, urbanisation, and agricultural intensification and water intensive lifestyles is resulting in a global water crisis. In 2000, at least 1.1 billion of the world’s people – about one in five – did not have access to safe water. Asia contains 65 per cent of the population without safe water and Africa 28 per cent. During the 1990s, there were some positive developments: about 438 million people in developing countries gained access to safe water but due to rapid population growth, the number of urban dwellers lacking access to safe water increased by nearly 62 million.

Falling water tables are widespread and cause serious problems, both because they lead to water shortages and, in coastal areas, to salt intrusion. Both contamination of drinking water and nitrate and heavy metal pollution of rivers, lakes and reservoirs are common problems throughout the world. The world supply of freshwater cannot be increased. More and more people are becoming dependent on limited supplies of freshwater that are becoming more polluted. Water security, like food security, is becoming a major national and regional priority in many areas of the world.

How is fresh water distributed on earth ?

Water is our most vital natural resource, supporting life and life support processes. While there is as much as 1,400 million km3 of water on earth, only one-hundredth of 1% of this amount is easily available for human use. The amount of water available for each person will continue to decrease as the world’s population expands. Unfortunately our present and future water supplies in many parts of the world are being degraded by pollution from domestic wastewater, solid waste, industrial effluent and agricultural drainage to name a few. As our natural waters become more polluted, less water is available for our needs and the needs of the natural environment. Every year, approximately 25 million people die, by either drinking polluted water or because they do not have enough water to meet their daily needs.

A single person needs at least half a liter (0.11 gallons) per day to meet basic survival needs and two liters (0.44 gallons) per day to avoid thirst. Some 27 to 200 liters (6 to 44 gallons) are needed per person per day for drinking, sanitation, bathing and cooking. Household water needs vary depending on the type of dwelling, number of residents and type of plumbing fixtures. (1 gallon=3.785ltrs) More important is for each one of us to learn as how to save even a drop of water.

Is there a Need of Rain water harvesting system ?

For all the above problems, one of the best remedy & simple, cost effective solution is Rain water harvesting system, today, scarcity of good quality water has become a major cause of concern. However Rain water which is pure and of good quality is lost as runoff.

What is the Concept and Technology of Rainwater Harvesting?

Rainwater is a free source of nearly pure water and rainwater harvesting refers to collection and storage of rainwater and other activities aimed at harvesting surface and groundwater. It also includes prevention of losses through evaporation and seepage and all other hydrological and engineering interventions, aimed at conservation and efficient utilisation of the limited water endowment of physiographic unit such as a watershed. In general, water harvesting is the activity of direct collection of rainwater. The rainwater collected can be stored for direct use or can be recharged into the ground water. Rain is the first form of water that we know in the hydrological cycle, hence is a primary source of water for us.

Where does all our water come from?

Rivers, lakes and groundwater are all secondary sources of water. In present times, we depend entirely on such Secondary sources of water. In the process, generally, it is forgotten that rain is the ultimate source that feeds all these secondary sources. Water harvesting means making optimum use of rainwater at the place where it falls so as to attain self-sufficiency in water supply, without being dependent on remote water sources.

Cities get lot of rain, yet cities have water shortage. Why? Because people living there have not reflected enough on the value of the raindrop. The annual rainfall over India is computed to be 1,170 mm (46 inches). This is higher compared to the global average of 800 mm (32 inches). However, this rainfall occurs during short spells of high intensity. Because of such intensities and short duration of heavy rain, most of the rain falling on the surface tends to flow away rapidly, leaving very little for the recharge of groundwater. This makes most parts of India experience lack of water even for domestic uses. Ironically,

Even Cherrapunji, India, which receives about 11,000 mm of rainfall annually, suffers from acute shortage of drinking water. This is because the rainwater is not conserved and is allowed to drain away. Thus it does not matter as to how much rain falls at a place, if it is not captured or harvested there for use. This highlights the need to implement measures to ensure that the rain falling over a region is tapped as fully as possible through water harvesting, either by recharging it into the groundwater aquifers or storing it for direct use.

Many urban centers in Asia and other regions are facing an ironical situation today. On the one hand there is an acute water scarcity and on the other, streets are generally flooded during rains. This has led to serious problems with quality and quantity of groundwater. One of the solutions to the urban water crisis is rainwater harvesting – Capturing the runoff. The advantage of Rainwater Harvesting is more where surface water is inadequate to meet our demand and exploitation of groundwater resource has resulted in decline in water levels in most part of the Country.

What is the potential of Water availability through Rooftop Water Harvesting in Bangalore city?

Bangalore (South India) Bangalore receives 970 mm rainfall annually and the number of rainy days is 60.highest amount of rainfall is received during April to November, while the rest of the months receive scanty rainfall. Peak runoff is 50 millimeters per hour. Due to the availability of rainwater throughout the year, water is basically stored in the rainwater harvesting systems and used for non-potable purposes. Water from the rooftops is led into storage structures. Providing an extra length of pipe to collect the polluted 2.5 mm of rainfall normally does the first flushing. Filters are made of sponge and a mixture of sand, gravel and charcoal. After first flushing and filtration water is led into underground sumps (which are very common in Bangalore) or to a new storage tank. The overflow from this tank is taken to an open well to recharge the aquifer.

The geological formations are predominantly granite and granitic gneiss, with joints and fractures in abundance due to intense chemical weathering of rocks. The depth of weathering varies from 0.2 m to 20 m. This geological set-up offers an immense scope for recharging of ground aquifers. The undulating terrain with gentle slopes draining into lakes offers an ideal situation for water harvesting. In the urban area of Bangalore water bodies cover about 5 per cent of land.

A study made by the Centre for Ecological Studies and Indian Institute of Sciences revealed that out of 262 lakes in 1960 only 82 exist now, of which less than 10 have water. Forty per cent of the city population is dependent on groundwater. The demand supply gap is met by groundwater exploitation. Even the surface water is pumped from Cauvery River flowing at a distance of 95 kilometers and about 500 meters below the city necessitating huge pumping costs and energy usage.

What is the water scenario in Kolkata and Bangalore?

In Kolkata, India, about half the population that lives in the slum or squatter settlements collect water from stand posts. The rest of the slum population do not have access to the municipal water supply and have to make their own arrangements – for instance relying on hand pumps/drawing from tube wells. In Bangalore, India a city of some 6 million inhabitants, it is estimated that more than half depends on public fountains. Almost a third of the population has partial or no access to piped water.

To further illustrate, India’s population as per 2001 census is 1027.02 million. Over 60 per cent of households in India meet their drinking water requirements from underground water sources such as hand pumps, tube wells and wells. In urban areas while 68.7 per cent households use tap water, 29 per cent of the households directly use those underground water resources. Intense use of underground water has resulted in depletion of subterrene water resources in many parts of India.

How is Global Demographic trends in regards to Water ?

The World population has more than doubled since 1950 and reached 6.15 billion in 2001. The most recent population forecasts from the United Nations indicate that, under a medium-fertility scenario, global population is likely to peak at about 8.9 billion in 2050.

In parallel with these demographic changes, there have been profound demographic shifts as people continue to migrate from rural to urban areas in search of work and new opportunities. The number of people living in urban areas has jumped from 750 million in 1950 to nearly 2.93 billion in 2001. Currently, some 61 million people are added to cities each year through rural to urban migration, natural increase within cities, and the transformation of villages into urban areas. By 2025, the total urban population is projected to increase to more than five billion, and 90 per cent of this increase is expected to occur in developing countries. Sixty per cent of the global population is living in Asia. Urban population growth in Asia at 2.7 per cent per annum is 27 per cent higher than the global average. Asia’s population living in urban areas is projected at 43.0 per cent for 2010 and will represent 50.8 per cent of world’s total urban population. Asia is expected to double its urban population by the year 2020. By 2025, the majority of this region’s population will live in cities. By 2015, there will be 153 cities of one million inhabitants, 22 cities with 8 or more million people and 15 with 10 to 20 million people.

Types of Rainwater Harvesting Systems

Typically, a rainwater harvesting system consists of three basic elements: the collection system, the conveyance system, and the storage system.Collection systems can vary from simple types within a household to bigger systems where a large catchment area contributes to an impounding reservoir from which water is either gravitated or pumped to water treatment plants. The categorization of rainwater harvesting systems depends on factors like the size and nature of the catchment areas and whether the systems are in urban or rural settings. Some of the systems are described below.

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