Background of Utah County's Aquifer 100VLFL Water Supply
Residents relying on water from Utah County's aquifer 100VLFL receive groundwater drawn from wells ranging between 90 and 700 feet deep. This aquifer’s water quality has been sampled across 28 separate wells between July 2010 and June 2021. These samples provide a broad view of the mineral content affecting household water but do not specify the quality of any individual well or tap.
Evaluating Treatment Capacity Relative to Household Laundry Demand
Consider Daily Water Use Volume vs. Equipment Capacity
Effective laundering depends on water treatment equipment matching the household’s daily water consumption. If the current system cannot keep pace, visible laundry effects like fading may occur despite equipment operation.
Monitor for Signs of Mineral Overload
When treatment capacity falls short, calcium and magnesium minerals present in the water may not be adequately managed, contributing to fabric dullness or stiffness.
Long-Term Effects of Untreated Mineral Content
Gradual Fabric Color Loss Over Time
Consistent exposure to calcium and magnesium minerals can leave deposits on textiles, causing colors to appear faded or less vibrant after repeated washes.
Potential Increase in Fabric Wear
Mineral residues may also contribute to fabric roughness, which can accelerate wear and reduce garment lifespan if left unaddressed.
Interpreting Utah County Mineral Range in Relation to Federal Standards
Mineral Concentrations Found in Area-Aquifer Samples
The U.S. Geological Survey recorded calcium and magnesium concentrations ranging from 138.0 to 621.0 mg/L, with a median of 284.0 mg/L in Utah County's aquifer 100VLFL. These levels are common for the area and none exceeded federal safety thresholds.
Detection Is Not an Indicator of Safety Exceedance
All samples detected mineral presence, but detection does not imply violation of health or safety standards.
Seasonal and Multi-Year Variation in Mineral Content
Sampling Date Range Reflects Variation
The 67 samples from 2010 through 2021 show variability in mineral concentrations over time, reflecting natural changes rather than equipment or local condition failures.
Expect Fluctuations Within Documented Range
Variations are typical and should be anticipated when evaluating water quality and treatment system performance.
Source of Calcium and Magnesium in Groundwater
Natural Dissolution from Aquifer Minerals
Calcium and magnesium enter the groundwater as a result of natural rock and soil mineral dissolution within the aquifer system, influenced by geological formations beneath Utah County.
Deep Well Extraction Brings Mineral-Rich Water
Water drawn from depths of 90 to 700 feet commonly carries these dissolved minerals into household plumbing.
In summary, Utah County's aquifer 100VLFL water naturally contains measurable levels of calcium and magnesium that can impact laundry appearance over time. Evaluating household water use against treatment system capacity and confirming actual water hardness through individual testing are important steps. For homes experiencing faded laundry despite functioning equipment, the Fleck Faded, Stiff Laundry System, which ships ready to configure, represents a documented option to address mineral-related fabric effects.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2021-06-16. 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 100VLFL aquifer (Utah County): 67 results from 28 wells, median 284.0 mg/L, range 138.0-621.0 mg/L; none above any federal threshold
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