Understanding How Treated Water Differs at the Tap
Water Source Characteristics in Somerset County
The groundwater supplying commercial properties in Somerset County originates from bedrock aquifers. Water travels through deep wells, ranging between 100 and 555 feet in depth, before reaching taps. This source water contains dissolved minerals including calcium and magnesium, measured in government sampling with a median concentration of 164.85 mg/L and a range from 59.2 to 266.0 mg/L.
Effect of Treatment on Mineral Content
When a Commercial System Skid such as the 48 Steel Tanks - Twin Unit Skid is applied, it modifies the mineral content in water, reducing components associated with hardness. This adjustment can help alleviate dry skin conditions influenced by water mineral levels, by providing a more manageable water quality for commercial facility use.
Why Aesthetic Secondary Standards Differ from Health-Based Limits
Distinction Between Measurement and Safety
Calcium and magnesium measurements in Somerset County wells do not exceed federal health-based limits. These mineral levels are not violations nor indicate unsafe water. Instead, they relate to aesthetic factors such as water feel and appearance, which may influence skin comfort.
Role of Secondary Standards
Secondary standards address concerns like taste, staining, and feel of water rather than health. The detected mineral content is typical for bedrock aquifer sources and does not imply health risks, but it may contribute to sensations such as dryness on contact.
Changes for Different Property Types and Use Patterns
Large Commercial Facilities
Water use and flow rates in larger commercial properties increase demand on treatment systems. This requires equipment capable of maintaining consistent conditioning without interruption, which the 48 Steel Tanks - Twin Unit Skid system is designed for.
Seasonal or Secondary Properties
Properties with intermittent use may experience variations in water quality feel on re-entry after idle periods. The treatment system must accommodate such fluctuations to maintain water quality that minimizes skin dryness.
Symptoms That Indicate and Do Not Indicate Water-Related Dry Skin
Symptoms Possibly Linked to Water Quality
Dryness, tightness, or mild irritation of the skin after water contact may relate to mineral content and water hardness. This can be notable in commercial settings with frequent water use, such as hospitality or healthcare.
Symptoms Not Directly Related to Water
Skin conditions caused by allergies, environmental factors, or personal care products require separate consideration. Water quality adjustment alone will not resolve these issues.
Checklist: Order of Ruling Out Causes of Dry Skin
Initial Low-Cost Checks
- Review usage of soaps and detergents that affect skin moisture.
- Assess humidity and heating conditions in the facility environment.
Water Testing Steps
- Obtain laboratory analysis of actual water to confirm mineral concentrations and other constituents in your specific supply.
- Verify if water conditioning equipment currently affects the hardness or mineral balance.
Affected Fixtures, Appliances, and Processes in Commercial Settings
Water-Contact Surfaces
Fixtures such as sinks, showers, and wash stations are most affected by mineral content influencing water feel and skin contact effects.
Equipment Handling High Water Volume
Boilers, heat exchangers, and washing machines experience mineral scaling and may benefit from consistent water quality management to optimize operation and minimize residue affecting skin comfort.
Choosing the right treatment system for your commercial operation starts with assessing your water demand and quality. The 48 Steel Tanks - Twin Unit Skid ships ready to configure to adjust water mineral content in Somerset County’s bedrock aquifer context, helping address dry skin concerns while supporting facility water needs effectively.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2011-09-27. 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 BEDROCK aquifer (Somerset County): 4 results from 4 wells, median 164.85 mg/L, range 59.2-266.0 mg/L; none above any federal threshold