Fleck Complete Well System

Buy Now

View full details

Step 1: How the Documented Treatment Technology Removes or Neutralizes the Constituent

Water drawn from wells in Richland County sources from the aquifer 211MDDF, where calcium and magnesium contribute to water hardness. While hardness is not a safety concern, it affects household water usability by causing scale buildup and reducing soap effectiveness. The Fleck Complete Well System uses ion exchange technology to target and reduce hardness components, particularly calcium and magnesium ions. This process replaces hardness ions with sodium or potassium ions, making water more compatible with home plumbing and appliances and improving cleaning results.

Step 2: What You Should Write Down Before Asking Anyone for Treatment Advice

Before considering treatment options, gather key information to provide a complete picture to any water professional or for self-assessment. Record your well’s depth, estimated daily water use, and any previous water analysis reports you have. Since hardness levels can vary significantly within the same aquifer, testing your own water through a certified laboratory is essential to know exact concentrations of calcium and magnesium. Also, note any aesthetic issues such as scaling on fixtures or reduced soap lather, as these observations relate to water hardness severity but do not confirm exact values.

Step 3: A Worked Example: Reading the Record's Median and Range as a Homeowner Would

According to U.S. Geological Survey groundwater samples from 26 wells in Richland County’s aquifer 211MDDF collected between 2011 and 2016, calcium plus magnesium hardness values ranged from 1.73 to 19.1 mg/L with a median of 7.485 mg/L. These values are all below any federal threshold for water quality. As a homeowner, this range suggests typical regional variability in hardness. You might expect your own well water hardness to lie somewhere within this range, but only direct testing can determine your specific level. Understanding the median helps set expectations for average conditions, while the full range shows the maximum observed values sampled in this aquifer.

Step 4: How Many Samples and Wells Stand Behind the Figures, and What a Small Sample Means

The data comes from 30 sample results from 26 distinct wells, each between 9 and 140 feet deep, collected over five years. This relatively broad set of samples provides a reliable overview of hardness characteristics within aquifer 211MDDF in Richland County but is limited to this specific region and timeframe. A small number of wells does not cover every variation in water quality, particularly for deeper or less common wells. For any individual household, a direct water test remains necessary to confirm local conditions and determine the appropriate treatment capacity.

Step 5: How to Compare This Area's Record with a Neighboring County's Without Overreading It

When looking beyond Richland County, note that groundwater hardness can differ because of geologic formations and water pathways unique to each aquifer. Comparing the U.S. Geological Survey data from Richland County’s 211MDDF aquifer to neighboring county aquifers should be done cautiously. Differences in sampling periods, well depths, and geological contexts mean that no direct assumptions about your water's quality can be made from adjacent areas. Use neighboring data as a general guide rather than a precise predictor of your well water's hardness.

For households needing complete well water treatment addressing hardness in Richland County, the Fleck Complete Well System offers a documented solution with a 32,000-grain capacity. This system ships ready to configure and can meet the demand measured from your personal water analysis, providing reliable removal of calcium and magnesium hardness to improve your home's water quality and usability.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2016-09-01. 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 Hardness, Ca, Mg in the 211MDDF aquifer (Richland County): 30 results from 26 wells, median 7.485 mg/L, range 1.73-19.1 mg/L; none above any federal threshold