Monday, August 22, 2016

WATER PROBLEMS INVOLVING UNUSUAL COLORS, SMELLS AND TASTES - Since taste and odor work together it is often difficult to distinguish the two. Clean water should be clear with no noticeable color deposits.



Noticeable Water Problems

Colors and Smells
Noticeable water problems tend to involve unusual colors, smells, and tastes. 
Once identified, these aesthetically displeasing elements can be eliminated using a variety of different methods. 

Taste and Odor

Since taste and odor work together it is often difficult to distinguish the two.
Common complaints include:
1.  Strong Chlorine taste or smell - Generally this occurs when the water is treated at the water treatment plant to disinfect it. The addition of chlorine is used to kill off bacteria and other harmful microorganisms.
2.  Metallic taste - Some water systems have a high mineral concentration giving the consumer a salty or soda taste. In the case of Iron and Manganese, a strong metallic taste is readily detected.
3.  Rotten egg odor - This is usually a result of decaying organic deposits underground.
As water flows through these areas, hydrogen sulfide gas is picked up, and when this water reaches the surface or comes out of the faucet, the gas is released into the air.
Hydrogen sulfide gas produces the rotten egg odor, can be corrosive to plumbing at high concentrations, and can tarnish silver rapidly.
In large enough quantities, it is toxic to aquarium fish. As little as 0.5 PPM (parts per million) can be tasted in drinking water.
4.  Musty or unnatural smells - These smells are normally a result of organic matter or even some pesticides in the water supply. Even very low amounts can introduce unpleasant odors into the water.
5.  Turpentine taste or odor - This smell can be a result of MTBE contamination in your water. The odor threshold of MTBE is fairly low, so even though you can smell it, the MTBE is more than likely not at a level to cause harmful effects.
MTBE (methyl tertiary-butyl ether) is a flammable, colorless liquid that dissolves easily in
water. It is part of a group of chemicals known as fuel oxygenates. Oxygenates do not occur naturally in gasoline; they are added to increase gasoline’s oxygen content. MTBE and other oxygenates make gasoline burn better, which lowers harmful carbon monoxide and other emissions from vehicles, reducing air pollution. Evidence supports the conclusion that MTBE is a potential human carcinogen at high doses. cancer.org
  

Color

"Clean" water should be clear with no noticeable color deposits. Common colors include:
1.  Red or Brown Color - A red, brown or rusty color is generally indicative of iron or manganese in your water. Disadvantages to iron in your water include stains in sinks, or discolored laundry.
2.  Yellow Color - This coloration occurs in regions where the water has passed through marshlands and then moved through peat soils. It is more commonly found in surface water supplies and shallow wells.
Although the yellow color may be displeasing, it presents no health hazard, as it is only small particles suspended in the water.
3.  Blue or Green Color - A green or blue color is generally a result
of copper in your water supply, or copper pipes and corrosive water.
The copper can cause staining of your fixtures and your laundry.
Copper is regulated in drinking water by the EPA at 1.3 PPM. This is at a low enough concentration that the copper cannot be tasted (the taste threshold is around 5 PPM).
Copper can become a problem if it is higher than 30 PPM in your water.
Effects at this dose are vomiting, diarrhea, and general gastrointestinal distress. If you are using well water as your primary source of water and copper is a concern in your area, it would be to your advantage to have your water tested for copper.
4.  Cloudy White or Foamy - Cloudy water is usually due to turbidity. Turbidity is caused by finely divided particles in the water.
When light hits the water, it is scattered, giving a cloudy look to the water. The particles may be of either organic or inorganic nature. Neither one causes any harmful effects to the body, although they can cause abrasions to pipes, or possible staining of sinks.
    Before any treatment is done on your water, it is best to arm yourself with some information as to what options are available to you.
    Obviously the best choice to improve water quality  is to remove the source of contamination. In some cases this may be possible, i.e. removal of a leaking underground fuel tank and contaminated soil.
However, source removal is impractical in most cases. It is here that treatment options come into play.
When choosing a water treatment plan it is important to keep in mind operating and maintenance costs. Also, remember what needs to be removed from the water. Some chemicals may be easily removed using a filter, while others may need a chemical pump. In either case, the best choice is to contact a professional.
Typical water problems and some common treatments are listed below. 
Common Water Problems
Treatment
Fuel Products
Oxidizing filter, followed by a carbon filter, or chlorination followed by a sediment filter
Water softener or iron filter
Metals
pH
Sediment


Typical Treatment Systems
1.  Carbon Filters: These filters can remove most organic compounds that cause aesthetic problems (odor and taste). The longer the water is in contact with the filter, the more effective it is in removing the foreign matter. However, the filter may actually serve as a place for bacteria to live and grow.
Typical carbon filters include faucet mounted, in line, line bypass, point of entry, pour through, and specialty filters. 
Faucet mounted filters are attached to the faucet directly. 
In line filters are located under the sink on the cold water supply line; this means that hot water is not filtered. 
Line bypass models use a separate faucet at the sink which supplies only filtered water.
Water from existing fixtures will remain untreated. 
Point of entry (POE) systems feature a filter that treats all water entering the home.
These systems will also remove volatile organic compounds that would otherwise disperse into the air. However, these are also the most expensive. 
Pour through filters are the most common. These filters are not attached to a water line in your house, but instead you pour the water through the filtering system. These systems are the least expensive, but they do not filter large quantities of water, and may not be the most effective type of carbon filter.
The final type of filter is the specialty filter which can attach to water supply lines on refrigerators and ice makers. With all of these, it is important to realize that the filter must be replaced should the odor or taste problem reappear. These filters do not regenerate themselves.
2.  Fiber Filters: Fiber filters remove suspended material in the water. They may not be as effective at removing taste and odor problems as the carbon filter, so in some instances, it may be better to use both a fiber and carbon filter to remove these problems.
These filters are made of fibrous material such as cellulose or rayon. They can be bought in a variety of weaves, but those with the smallest weaves may need frequent replacement, since more particles are trapped.
These filters need to be changed when problems reoccur, just like the carbon filters. The price varies greatly, so it is best to know what type of contaminant you are dealing with to choose the most effective filter.
3.  Reverse Osmosis Units: These units are similar to an all-in-one unit in that they have different types of filters, membranes,
Reverse Osmosis with Steel Tank
storage tanks, and drainage tanks. They remove inorganic chemicals like nitrates.
They include a filter to remove sediment, a carbon filter to remove odors and tastes, a membrane that water is forced through under pressure, a tank to hold water, and a drain to remove all the compounds that were captured.
These units tend to be the most expensive. Additionally, there are maintenance costs to be considered. It may be best to compare the total price of the unit versus less expensive alternatives.
4.  Distillers: A distiller is one of the most effective ways to clean your water. Tap water is boiled and when steam is produced, it condenses at the top of the distiller and is moved to condensing coils where it cools down and is deposited into a separate container. The contaminants are left behind.
These units can be expensive depending on their capacity, maintenance, etc. They do require electricity to run.
Again, a cost benefit analysis may be necessary to determine if this is the best alternative for you.
5.  Neutralizing Filters and Chemical Feed
Tachmina Solenoid-Driven
Chemical Feed Pump
Pumps
: Both of these units work similarly in that they both adjust the pH of the water. They both add neutralizing solutions to the water so that it is not corrosive.
6.  The disadvantage of these is that they tend to make the water harder due to the injection of the neutralizing agents.
Ultra-Violet Bactericidal System
with Pre-Filters
7.  Disinfection: Disinfection is used to kill bacteria and microorganisms.  Chlorination is the usual method; other methods use ultraviolet light or ozone.
With chlorination, a residual chlorine taste may be present, which can be removed with a carbon filter.
There are professional services that will disinfect your system, but often the best way to treat a well is with shock chlorination.
8.  Water Softeners: Water softeners are used to
         Multi-Media Filter, Highly-Activated Carbon Filter,
Zeolite-Process Water-Softener with Brine Tank,
(Fully Automatic Backwash & Regeneration)  
 
treat 
hard water, and involve a system that exchanges sodium ions with the calcium or magnesium present in your water. The sodium is bound to a resin that is either regenerated at the home or by the softener supplier.


http://extoxnet.orst.edu/faqs/safedrink/colors.htm
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Saturday, August 20, 2016

GROUNDWATER, AQUIFERS AND WATER MOVEMENT - Groundwater occurs in the saturated soil and rock below the water table. If the aquifer is shallow enough and permeable enough to allow water to move through it at a rapid-enough rate, then people can drill wells into it and withdraw water.

Groundwater, Aquifers and Water 
Movement
.
Aquifers and Groundwater
hole at the beach
I hope you appreciate my spending an hour in the blazing sun to dig this hole at the beach.
It is a great way to illustrate the concept of how, below a certain depth, the ground, if it is permeable enough to hold water, is saturated with water.
The upper surface of this zone of saturation is called the water table. The saturated zone beneath the water table is called an aquifer, and aquifers are huge storehouses of water.
What you are looking at in this picture is a "well" that exposes the water table, with an aquifer beneath it.
Of course, I am cheating here, as at the beach, the level of the water table is always at the same level as the ocean, which is just below the surface of the beach.
Groundwater is one of our most valuable resource - even though you probably never see it or even realize it is there.
As you may have read, most of the void spaces in the rocks below the water table are filled with water.
But rocks have different porosity and permeability characteristics, which means that water does not move around the same way in all rocks below ground.
When a water-bearing rock readily transmits water to wells and springs, it is called an aquifer. 
Wells can be drilled into the aquifers and water can be pumped out. Precipitation eventually adds water (recharge) into the porous rock of the aquifer.
The rate of recharge is not the same for all aquifers, though, and that must be considered when pumping water from a well.
Pumping too much water too fast draws down the water in the aquifer and eventually causes a well to yield less and less water and even run dry.
In fact, pumping your well too much can even cause your neighbor's well to run dry if you both are pumping from the same aquifer.
In the diagram below, you can see how the ground below the water table (the blue area) is saturated with water.
The "unsaturated zone" above the water table (the greenish area) still contains water (after all, plants' roots live in this area), but it is not totally saturated with water.
You can see this in the two drawings at the bottom of the diagram, which show a close-up of how water is stored in between underground rock particles.
Sometimes the porous rock layers become tilted in the earth. There might be a confining layer of less porous rock both above and below the porous layer.
This is an example of a confined aquifer. In this case, the rocks surrounding the aquifer confines the pressure in the porous rock and its water.
If a well is drilled into this "pressurized" aquifer, the internal pressure might (depending on the ability of the rock to transport water) be enough to push the water up the well and up to the surface without the aid of a pump, sometimes completely out of the well.
This type of well is called artesian. The pressure of water from an artesian well can be quite dramatic.
A relationship does not necessarily exist between the water-bearing capacity of rocks and the depth at which they are found. A very dense granite that will yield little or no water to a well may be exposed at the land surface.
Conversely, a porous sandstone, such as the Dakota Sandstone mentioned previously, may lie hundreds or thousands of feet below the land surface and may yield hundreds of gallons per minute of water.
Rocks that yield freshwater have been found at depths of more than 6,000 feet, and salty water has come from oil wells at depths of more than 30,000 feet.
On the average, however, the porosity and permeability of rocks decrease as their depth below land surface increases; the pores and cracks in rocks at great depths are closed or greatly reduced in size because of the weight of overlying rocks.

Pumping can affect the level of the water table

Groundwater occurs in the saturated soil and rock below the water table.
If the aquifer is shallow enough and permeable enough to allow water to move through it at a rapid-enough rate, then people can drill wells into it and withdraw water.
The level of the water table can naturally change over time due to changes in weather cycles and precipitation patterns, streamflow and geologic changes, and even human-induced changes, such as the increase in impervious surfaces on the landscape.
The pumping of wells can have a great deal of influence on water levels below ground, especially in the vicinity of the well, as this diagram shows.
If water is withdrawn from the ground at a faster rate that it is replenished, either by infiltration from the surface or from streams, then the water table can become lower, resulting in a "cone ofdepression" around the well.
Depending on geologic and hydrologic conditions of the aquifer, the impact on the level of the water table can be short-lived or last for decades, and it can fall a small amount or many hundreds of feet.
Excessive pumping can lower the water table so much that the wells no longer supply water—they can "go dry."

Water movement in aquifers

Water movement in aquifers is highly dependent of the permeability of the aquifer material.
Permeable material contains interconnected cracks or spaces that are both numerous enough and large enough to allow water to move freely.
In some permeable materials groundwater may move several meters in a day; in other places, it moves only a few centimeters in a century. Groundwater moves very slowly through relatively impermeable materials such as clay and shale. 
After entering an aquifer, water moves slowly toward lower lying places and eventually is discharged from the aquifer from springs, seeps into streams, or is withdrawn from the ground by wells.
Groundwater in aquifers between layers of poorly permeable rock, such as clay or shale, may be confined under pressure.
If such a confined aquifer is tapped by a well, water will rise above the top of the aquifer and may even flow from the well onto the land surface.
Water confined in this way is said to be under artesian pressure, and the aquifer is called an artesian aquifer.
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What is water dowsing?
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Groundwater 
is the name used to describe water which is stored underground in permeable rocks
CLICK HERE . . .
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water.usgs.gov