Fleck Well Rust + Hardness System

Buy Now

View full details

How should Licking County's iron data be compared with neighboring counties without reading too much into it?

The U.S. Geological Survey has sampled groundwater from nine wells in Licking County's aquifer between late 2012 and early 2013. These samples measured iron concentrations ranging from 12.1 to 2450.0 micrograms per liter with a median value of 1280.0 micrograms per liter. Seventeen of the nineteen results detected iron at or above the reporting limit.

When comparing these figures to neighboring counties, keep in mind that variations in geology, aquifer depth, and well construction influence measurements. Differences in sampling methods and timing also affect values. Therefore, while neighboring counties may show higher or lower median iron levels, these differences reflect broad regional trends rather than specific well conditions for individual households.

For homeowners, regional data provides context but cannot substitute for testing your home's water. Iron presence in Licking County's aquifer is common, but its exact concentration in your well water remains unknown without direct analysis.

How can a homeowner interpret the record's median and range when considering their own water?

The median iron concentration of 1280 micrograms per liter represents the middle value among the sampled wells, indicating that half of the measurements were above and half below this point. The range—from as low as 12.1 to as high as 2450.0 micrograms per liter—shows variability across locations and wells.

This range indicates that some wells in Licking County have very low iron levels while others have higher amounts. Because these are separate wells sampled during a defined period, this data cannot pinpoint conditions at a single property. Instead, it provides a reasonable estimate of what iron concentrations might be encountered in the area.

What does the measured iron range mean in relation to federal standards, and what does it not mean?

Iron levels found in the Licking County aquifer samples were never above any federal threshold. This means the water quality record shows no health-based violation for iron in this sampling set. However, detection and concentration do not imply health risk, as iron is a naturally occurring element commonly found in groundwater.

Federal secondary standards or recommendations exist for iron primarily to address aesthetic concerns such as staining, taste, and color. Exceeding these does not indicate unsafe water but signals conditions that can affect household plumbing and water appearance.

What is the recommended order to rule out causes of rust and hardness, starting from the simplest checks to laboratory tests?

Since household equipment has failed, start with straightforward assessments:

• Check visible signs of rust stains on fixtures, appliances, and laundry to confirm iron presence.
• Evaluate water hardness using readily available test strips or kits.
• Inspect water clarity and taste for possible iron influence.
• If results confirm issues, collect a water sample following proper protocols for professional laboratory analysis. This step provides precise iron concentration and hardness levels specific to your water supply.

Collecting your own water test results is essential as regional data alone cannot diagnose household water quality.

How should treatment capacity be judged relative to a household’s daily water use?

The Fleck Well Rust + Hardness System provides a grain capacity of 32,000 grains. Grain capacity refers to the total amount of hardness the system can treat before regeneration or recharge is needed.

Match this capacity with your household’s typical daily water consumption and hardness level to determine how often the system will need to cycle. For example, a household using more water or experiencing higher hardness might require more frequent regeneration. Proper sizing ensures effective rust and hardness control while optimizing system performance.

Why do aesthetic secondary standards for iron differ from health-based limits?

Iron's presence in water is generally not a health concern at levels found in Licking County’s aquifer. Secondary standards for iron focus on aesthetics and usability—such as preventing rust-colored staining, metallic taste, and discoloration in water.

These standards help guide treatment decisions that improve water appearance and extend the lifespan of plumbing and appliances but do not indicate health risks. When iron is detected, proper treatment addresses these practical considerations rather than safety issues.

What should homeowners NOT conclude from Licking County area iron data?

Area-wide iron measurements do not establish the exact iron concentration in any individual well. Detection does not equal a violation or unsafe water. The presence of iron in regional aquifer samples confirms iron can be expected but does not guarantee its levels or impact at your home.

Testing your specific water supply is essential to make informed decisions about rust and hardness treatment. The Fleck Well Rust + Hardness System ships ready to configure, providing a documented solution designed to handle iron and hardness challenges based on your household’s needs and water characteristics.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2013-04-23. These figures describe groundwater sampled in this area. They are not a test of any individual private well - only a test of that well can establish its own water.

On record: U.S. Geological Survey sampling of Iron in the aquifer (Licking County): 19 results from 9 wells, median 1280.0 ug/L, range 12.1-2450.0 ug/L; none above any federal threshold