Government Sampling in Leflore County Shows Widespread Hardness
The U.S. Geological Survey sampled groundwater from multiple wells across Leflore County’s aquifer 112MRVA between 2016 and 2020. Hardness, measured as the combined concentrations of calcium and magnesium, was detected in every sample, with a median level of 230.0 mg/L and a range from 41.6 to 464.0 mg/L. These results come from wells between 28 and 220 feet deep and represent an area-wide profile rather than any individual household’s water.
Adjustments for Large Households, Seasonal, or Second Properties
Households with more residents or additional properties using the same water source may experience higher total daily water demand, affecting treatment capacity needs. Seasonal homes might require adjustments to accommodate periods of non-use and later higher flow rates when reoccupied. It is important to consider these variations when planning water treatment to ensure consistent effectiveness, especially when addressing both acid and hardness factors.
Information to Collect Before Seeking Water Treatment Advice
Before evaluating treatment options, write down the specific results of a recent water test from your own well or water source. Note the concentrations of hardness components – calcium and magnesium – along with any pH measurements that indicate acidity levels. Also, record your household’s daily water usage. This information is essential because government data provides area-level context but cannot substitute for an individual water test.
Implications of Untreated Acid and Hardness Over Time
Without treatment, persistent hardness and acidity can cause mineral scale buildup inside plumbing and appliances, reducing efficiency and lifespan. Acidic water may contribute to corrosion risks, potentially releasing metals from pipes. These effects generally develop gradually over years and can result in higher maintenance needs, increased energy use, and aesthetic issues such as staining.
Difference Between Public System Records and Private Well Testing
Public water system records, including federal sampling data, summarize quality conditions across broad areas or distribution networks. These records indicate typical or median conditions but do not provide specifics for any one household’s supply. Private well testing is the only way to determine your own water’s exact hardness and acidity levels. Consulting these records alongside personal testing can guide appropriate treatment choices.
Understanding Hardness Levels Compared to Federal Secondary Standards
The federal secondary standard for total dissolved solids, which influences taste and scaling, helps contextualize hardness values. Leflore County’s sampled median hardness of 230.0 mg/L falls within common ranges and did not exceed any regulatory thresholds during the sampling period. However, presence of hardness at these levels can still affect household water quality, independent of regulatory status. It is also important to note that detection alone does not imply a violation or unsafe condition.
Addressing acid and hardness effectively depends on knowing your household’s demand and water specifics. The Fleck Acidic Water + Hard Water (Well) System, with a capacity of 32,000 grains, ships ready to configure and can be sized to match measured demand. This documented treatment technology can reduce hardness and mitigate acidic conditions, improving water quality based on your own testing and usage data.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2020-07-23. 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 Hardness, Ca, Mg in the 112MRVA aquifer (Leflore County): 21 results from 12 wells, median 230.0 mg/L, range 41.6-464.0 mg/L; none above any federal threshold