What 'Detected,' 'Median,' and 'Range' Mean in the Sampling Record for Stark County Aquifer Water
The U.S. Geological Survey sampled groundwater from three wells in the Stark County aquifer in June 2016, measuring calcium and magnesium which contribute to water hardness. "Detected" means the constituent was measured in all three samples. The "median" value, 111.0 mg/L, represents the middle result of the range, which spans from 14.8 to 156.0 mg/L. These figures describe regional water conditions but do not specify the hardness in any individual well or tap.
How Seasonal or Multi-Year Variation Shows in the Record Dates and Ranges
The sampling took place over a brief period of four days in mid-June 2016, so seasonal or year-to-year changes are not represented in this dataset. While calcium and magnesium levels can vary with time, the limited sample dates mean operators should consider additional testing if they require data reflecting other seasons or years for their specific water source.
How Sample Depth, Well Depth, or Source Type Changes What a Reader Should Expect
The three sampled wells ranged in depth from 235 to 301 feet. Deeper wells like these often draw from more stable aquifers, potentially leading to more consistent water quality. However, shallower wells or other water sources in Stark County might have different mineral concentrations, so these results serve as a regional guide rather than a precise forecast of an individual facility’s water hardness.
How Public-System Records Differ from Private-Well Testing in What They Establish
The data cited comes from public groundwater sampling focused on a regional aquifer. Unlike individual private well testing, which measures conditions specific to one site, this sampling provides an overview of the area’s water qualities. Public records show no violations above federal health thresholds for hardness-related minerals, indicating the levels found are typical and not classified as unsafe per federal standards.
The Facility Symptoms That Do and Do Not Point to Soap Lather Issues
Common signs that water hardness affects soap performance include weak or no lather and soap scum buildup on equipment or surfaces. These symptoms suggest calcium and magnesium interfere with soap effectiveness. However, poor soap lathering alone does not prove water hardness is the cause; other factors like soap formulation or water temperature also matter.
Symptoms unrelated to soap lather issues include foul odors, discoloration, or taste problems, which typically come from different water quality concerns not linked to hardness minerals.
Recommended Test to Settle the Soap Lather Question
To determine if your commercial facility’s water is causing soap lather difficulties, order a water hardness test focused on calcium and magnesium levels specific to your source. This test will confirm whether the mineral content aligns with the regional values reported by the USGS or deviates enough to require intervention.
If hardness is confirmed at levels impairing soap effectiveness, the 42 Steel Tanks - Twin Unit Skid, a commercial system skid, ships ready to configure and can address these conditions reliably, restoring proper soap lather and improving cleaning results.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2016-06-16. 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 aquifer (Stark County): 3 results from 3 wells, median 111.0 mg/L, range 14.8-156.0 mg/L; none above any federal threshold
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