Recognizing Symptoms Related to Water Quality in Facilities
Dry skin can be a concern in commercial operations where water use is frequent and extensive. While dry skin may arise from many environmental or personal factors, certain water characteristics may contribute to this condition. It is important to distinguish symptoms related to water composition from other causes. Facility-wide dryness affecting employees or production processes could indicate water-related factors at play.
What Navajo County Water Sampling Reveals and What It Does Not
Groundwater samples taken from Navajo County’s aquifer 220NAVJ between 2010 and 2019 show calcium and magnesium hardness ranging from 1.23 to 163.0 mg/L with a median of 2.935 mg/L. These values were detected in 40 samples from 14 wells, between 554 and 3,737 feet deep. Significantly, none of these measurements exceed federal thresholds for water quality. However, these results reflect regional conditions and do not specify the water quality of any single commercial site’s supply.
Fixtures and Processes Most Sensitive to Hardness Variations
Hardness in water, caused primarily by calcium and magnesium, can influence how water interacts with skin and equipment. In facilities, showers, handwashing stations, and any process involving direct water contact are most likely to reveal effects related to water hardness. Dry skin symptoms may appear more pronounced in these locations. Additionally, water hardness can impact cleaning processes and product formulations, though these effects vary depending on hardness levels and usage patterns.
Long-Term Impacts of Untreated Hardness Issues
If hardness-related water characteristics are not addressed over many years, commercial operators might observe progressively drier skin among users of the water. Prolonged exposure may also affect equipment relying on water, causing scaling that reduces efficiency. These effects occur gradually and depend on ongoing water quality and usage intensity rather than an immediate health risk.
Sources of Hardness in Navajo County Groundwater
The calcium and magnesium hardness detected in Navajo County’s aquifer 220NAVJ groundwater originates from natural mineral dissolution in sediment layers accessed by deep wells. This mineral content is typical in many aquifers and varies naturally based on geology and depth. Understanding these sources helps contextualize water quality and guides operators in anticipating water characteristics at their sites.
Conclusions: What Regional Data Does Not Determine
While regional groundwater data provides valuable insight into the general range of water hardness present, it does not establish the exact water quality at any commercial facility. Operators should conduct specific water testing at their location to determine actual hardness and other parameters relevant to dry skin concerns. Based on precise site data, commercial system skids such as the 24 Steel Tanks - Triplex Unit Skid may offer targeted management of water hardness to support facility comfort and operational needs.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2019-08-23. 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 220NAVJ aquifer (Navajo County): 40 results from 14 wells, median 2.935 mg/L, range 1.23-163.0 mg/L; none above any federal threshold
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