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THIS WEB PAGE IS INTENDED TO PROVIDE INFORMATION TO PRIVATE WELL USERS who use shallow aquifers as their drinking water supply. There MAY BE WATER QUALITY PROBLEMS IN SOME IN SHALLOW AQUIFERS in iOWA, especially the SHALLOW BEDROCK Aquifers IN THE KARST REGIONS OF NORTHEAST IOWA.
Good quality drinking water is one of the building blocks for good health. Understanding your drinking water quality can help protect the health of you and your family. You should read this web page if you consume water from a private water well that is finished in any shallow aquifer. Shallow aquifers are more susceptible to contamination due to their close proximity to the ground surface and the influences caused by local land use activities.
Even though your water may look clear and taste good, you will not know if it's safe to consume unless you take the necessary steps to confirm it's safe.
For those connected to a public water supply, the water supply operator performs routine testing and informs the water users if the water is not safe to consume. For private wells, the responsibility of water testing falls solely onto the well owner and anyone else who uses the well water. This means you - as a well user - need to take the steps to ensure that your water supply is tested for the contaminants that may be present in your local area and inform yourself by understanding the analytical results provided by the testing laboratory.
Anyone who consumes unsafe water may experience health issues. Your risks increase if your water is over the EPA maximum contaminant level (MCL) for any contaminant and when you consume contaminated water for longer periods of time.
Modern water wells are designed and constructed by certified well contractors. This helps ensure the safety of your drinking water and the aquifers.
Some wells finished in shallow aquifers can contain high levels of bacteria, nitrates, pesticides and other chemicals and organisms. Any of these contaminants can adversely impact health if consumed.
Even older wells finished in currently safe aquifers can be affected when steel well casing used in the well's construction corrodes and the casing develops small leaks that allows poor quality shallow groundwater to enter the well.
Many farms and homes in Iowa obtain their water from bedrock wells. Deep bedrock wells are generally safe water supplies because they tap deeper aquifers that have natural geologic barriers in place that helps keep contaminants from entering the aquifer. But in some areas of our state, shallow bedrock aquifers exist. Some of this bedrock is defined as "Karst".
Karst bedrock is characterized as bedrock that is close to the land's surface and contains a vast network of underground drainage systems that have direct connections to the land's surface.
In areas of Karst, much of the rainfall that would normally flow to rivers and streams, directly or indirectly flows into the shallow bedrock and becomes part of the groundwater some water wells may utilize. Some of the water that originates at the surface - possibly near sources of contamination - flows undetected into the ground.
This water can contain contaminants that are found on the land's surface and those not bound or utilized by the areas soils and land cover. Once in the ground, this water that was once on the surface becomes part of the groundwater supply.
A well that obtains part or all of its water from a shallow aquifer can have higher levels of contaminants when compared to deeper wells in the same area.
Anytime you consume water that contains unsafe levels of any contaminant, you increase your risk for negative health effects.
This map shows the areas of northeast Iowa where Karst bedrock is likely to occur.
Shallow wells located in areas of Karst bedrock can have poor water quality.
The darker shaded areas are those where sinkholes and bedrock exposures are most likely and water quality concerns are the greatest in shallow bedrock aquifers.
Click on the map to view a larger image.
Shallow aquifers are less protected than deeper aquifers. Karst bedrock aquifers are some of the most susceptible to contamination. Although Karst features can be found in a number of locations across Iowa, they are most abundant in the NE corner our state.
Whether or not your well may be affected will depend on a number variables, like:
In general, if you use a shallow aquifer for your water supply, you may be affected. If your well is located in one of the shaded areas of the NE Iowa Karst Map on this page and obtains any of its water from the shallow aquifer, your well has the potential to be influenced by Karst groundwater. Regardless of location, shallow well users should test their well water to make sure it's safe to consume.
This aerial image is of a Karst landscape in Clayton County. The small depressions or dimples you see are
This type of feature can allow surface water rapid access to shallow groundwater where it affects groundwater quality.
Image courtesy of the Iowa Geological Survey.
Because of the potential surface water influences and the types of land use activities in Karst regions, localized shallow groundwater may have increased levels of nitrates, bacteria, pesticides, and potentially other contaminants.
In addition, the groundwater flow path through Karst bedrock can be unpredictable. This means that some shallow wells in Karst areas may be unaffected by contaminants while other wells show signs of contamination.
Those who use shallow bedrock wells located in the darker shaded areas of the NE Iowa Karst Map on this web page should note that this is where Karst activities are most likely to occur. There is a significant increase in the number of sinkholes and other Karst features in these areas.
Constructing and maintaining a well in Karst areas requires greater care to ensure your drinking water comes from a deep, safe aquifer using construction standards that help protect your drinking water quality and the aquifer.
Normally, rain events create surface water that runs-off into rivers and streams and is absorbed by soils and till. But in areas of Karst, the run-off can rapidly flow into the bedrock - either directly through shallow openings and surface sinkholes, as well as vertical and horizontal fractures or solution channels that are exposed near or at the ground's surface, or indirectly through the pore openings and areas of thin soil overlying the limestone bedrock.
In most areas, we depend on the soils to act as a filter in which biological and chemical interactions take place that help improve the water's quality.
But in areas of Karst, there is little or no soil for the water to flow through before reaching the shallow aquifer. This means there is little or no filtering or treatment that takes place before the water mixes with the shallow groundwater.
In addition, when water flows directly into the bedrock via sinkholes, losing streams and a system of voids or fractures that reach deep into the ground, there is no filtering that takes place before the water mixes with the shallow groundwater.
Once in the ground, the water rapidly flows through the large openings in shallow bedrock which further reduces any opportunity for the water to undergo natural water treatment.
When surface water moves into a shallow aquifer, the potential for poor well water quality in the aquifer increases.
This diagram provided by Iowa Geological Survey shows a cross section of a Karst bedrock setting. You can click on the diagram to view a larger image.
The dark blue areas indicate groundwater stored in openings of the bedrock. This groundwater is part of the shallow aquifer and available to the well visible in the diagram.
You can see the open spaces in the bedrock blocks that allows for storage and transport of the groundwater. You can also view how the land surface and stream visible in the diagram can directly interact with the water stored within the bedrock.
In Karst systems, soil infiltration, surface water run-off and streams can drain directly into the shallow bedrock and become part of the shallow groundwater and aquifer.
This means that the contaminants found on the land surface and in surface water, may also be present in wells that tap the shallow aquifer.
The only way to determine if your well water is safe to consume is to take a sample of the water and send it to a drinking water laboratory.
Your local county environmental health office can help you arrange for testing or you can obtain a water sample test kit, sample the water yourself and send it to a certified drinking water laboratory for analysis.
The primary indicator tests normally performed include coliform
bacteria, nitrate, and nitrite. Testing for these contaminants is easy, inexpensive and can be used to provide basic information on drinking water safety.
There are also other water tests you should consider. Contaminants like arsenic, fluoride, radium, and lead are naturally occurring in some aquifers and may require specialized water treatment to reduce or eliminate the exposure risk.
You should also consider testing shallow wells periodically for pesticides.
Private wells do not fall under mandated state or national water quality standards. Because of this, you should use the Environmental Protection Agency (EPA) contaminant standards for public water supplies as the recommended standards for your private water supply.
The presence of any contaminant above the EPA's maximum contaminant level (MCL) means that you should not consume the water without proper treatment, water system repairs that eliminates the source of contamination, or replacing the well with one constructed to provide safe water.
For more information on specific water testing you may want to consider, please contact the
State Hygienic Laboratory at the University of Iowa, 800-421-4692, or any other Iowa certified drinking water laboratory, your local Iowa DNR Certified Well Contractor or the Iowa DNR.
This image from the State Hygienic Laboratory shows a lab technician performing water analysis.
Laboratory analysis of drinking water requires controlled conditions, expensive technical equipment and highly trained professional staff.
This photo shows what's included in a water sample test kit when obtained from the State Hygienic Laboratory. It consists of sampling bottle(s), a request form and mailing materials.
All drinking water samples must be analyzed by a State Certified Drinking Water Laboratory.
There are currently over 40 certified labs who can provide water analysis for private well owners.
There is a statewide grant program called the Grants to Counties Water Well Program that can provide you with basic water testing for free. For more information, please contact your local county
environmental health specialist.
You increase your risk for illness and disease if you drink contaminated water. Each type of contaminant has its own health impacts depending on the level of contamination, how much of the contaminated water you consume and your individual sensitivity to the contaminant(s).
Here is some basic information on the most commonly detected contaminants.
For additional information on water borne diseases please see the
Centers for Disease Control, Iowa Department of Public Health or your local county environmental health office.
Water-related diseases and Contaminants that may be found in unsafe drinking water.
Source - The Centers for Disease Control and Prevention
Knowledge of your water quality will empower you and help you make informed decisions about your consumable water and long term health.
First and foremost, ensure that all the water you consume is safe. Laboratory analysis of your well water is the only way to determine this. Your local county environmental health specialist or certified drinking water laboratory can help you decide which tests make sense for your well depth and location.
How often you test your supply should be based on several things. They include what your previous water testing found, who is using the water, changes in the water quality you can see, taste or smell, and the type of potential contaminants applied to land near your well.
At a minimum, all private well users should test their water supply at least once each year for a minimum of coliform bacteria and nitrates, and have at least one arsenic test performed on the well water.
You should test your well more often if:
If your water analysis finds the water is unsafe for any contaminant, do not drink the water. You should obtain all of your drinking and consumable water from a known safe water source, like a well recently proven safe by water testing and analysis, a water treatment device connected to your water supply that is designed to remove the contaminant(s) found, a public water supply, or buy bottled water. This reduces or eliminates your immediate risk and allows time for you to investigate the long term options for managing your water system.
Water Treatment Options
This informational booklet by the State Hygienic Laboratory at the University of Iowa provides a guide to well water contaminants and effective water treatment devices.
Well Consumer Information Booklet
This booklet is designed to help private well owners understand private well construction and ownership.
The term "consumable water" includes:
Your lab report
Iowa's Groundwater Basics published by the Iowa Geological Survey is a geological guide to the occurrence, use and vulnerability of Iowa's Groundwater. The publication is full of good information, interesting diagrams and wonderful pictures.
- For more information contact -
Russell Tell, Environmental Specialist Senior
Wallace State Office Building
502 E. 9th Street
Des Moines, IA 50319-0034
(515) 725-0462 or by Fax: (515) 725-8202