Seasonal and Multi-Year Variation in Water Quality Data for Apache County
Water quality samples from Apache County’s aquifer 220NAVJ, collected between June 2010 and August 2013, reveal variation in calcium and magnesium levels. Among eight samples from two wells, concentrations ranged from 6.35 to 26.4 mg/L, with a median of 6.7 mg/L. These readings indicate fluctuations over multiple years and seasons, demonstrating that water characteristics can change but generally remain within measured parameters during this period.
Pathways for Calcium and Magnesium Entering Apache County Groundwater
The calcium and magnesium detected in groundwater here originate naturally from mineral deposits that dissolve as water permeates underground rock formations. The geological context of aquifer 220NAVJ includes minerals that release these elements, which contribute to water hardness. This natural mineral presence can influence water quality by impacting how water interacts with fabrics during laundry.
Sample Size and Well Depth: Understanding the Confidence in Area Data
The data for Apache County’s aquifer 220NAVJ is based on eight samples drawn from two wells ranging in depth from 675 to 1,425 feet. Although this sample size is limited, it provides an indication of regional conditions rather than a complete characterization. Residents should understand that their individual water may differ significantly from these findings and that a personal well test would be necessary for precise details.
Fixtures and Processes Most Affected by Minerals Causing Faded Laundry
Laundry appliances and the washing process show early signs of mineral impacts, with fabrics often experiencing fading and stiffness. Hard minerals such as calcium and magnesium can leave residues on fabrics that dull colors and reduce softness. These effects tend to become noticeable before issues arise in other household systems, making laundry a good initial indicator of mineral presence in water.
Influence of Well Depth and Source Type on Water Characteristics
Wells of different depths can access distinct water layers, which may vary in mineral content. Deeper wells in the 675 to 1,425 feet range, as sampled in this area, might draw water with differing calcium and magnesium levels compared to shallower sources. Homeowners should consider that the depth and type of water source will affect their water’s interaction with fabrics and should guide decisions on suitable treatment approaches.
What Area Data Should Not Imply About Your Water
The Apache County groundwater data reflects regional mineral presence but cannot specify any individual household’s water quality or mineral concentration. Detection of calcium and magnesium in area samples is not a violation or indication of unsafe water. Homeowners should not assume their own water matches these figures without testing. Addressing faded laundry effectively involves knowing your actual water profile and considering the C-Series Faded, Stiff Laundry System, which ships ready to configure and targets mineral-related fabric issues documented in similar regional waters.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2013-08-07. 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 220NAVJ aquifer (Apache County): 8 results from 2 wells, median 6.7 mg/L, range 6.35-26.4 mg/L; none above any federal threshold