C-Series Sensitive Skin & Eczema System

C-Series Sensitive Skin & Eczema System

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How do calcium and magnesium naturally enter the bedrock aquifer groundwater in Rockingham County?

Calcium and magnesium become part of groundwater through a natural process called mineral dissolution. As water moves through the bedrock — composed of various minerals — it gradually dissolves calcium and magnesium compounds present in the rocks. This process results in measurable levels of these minerals in the groundwater. In Rockingham County, the bedrock aquifer's geological composition contributes to consistent detection of these minerals in water sampled from various wells.

What does the median and range of calcium and magnesium levels mean for a homeowner considering sensitive skin?

The U.S. Geological Survey sampled six separate wells from 2011 to 2019, finding calcium and magnesium levels ranging from 71.0 to 237.0 milligrams per liter, with a median of 144.0 milligrams per liter. While these figures reflect the range of mineral presence in the area’s groundwater, they do not indicate the specific concentration in any individual well or household. Understanding this range helps homeowners realize that water mineral content can vary widely and that their own water’s effect on sensitive skin will depend on their well's specific mineral makeup.

What is the maintenance rhythm for the C-Series Sensitive Skin & Eczema System, and how does it help?

The C-Series System is designed to address water factors that may influence sensitive skin by managing calcium and magnesium levels. It ships ready to configure and operates on a grain capacity of 32,000 grains. Typically, maintenance involves monitoring system prompts to know when to regenerate or refresh media, which helps ensure effective treatment consistent with the household's water hardness levels. Regular attention to the system's indicators supports sustained performance tailored to sensitive skin needs.

How do the measured mineral ranges compare to federal water quality standards, and what should they not be taken to mean?

None of the 96 groundwater samples from Rockingham County’s bedrock aquifer exceeded federal thresholds. It is important to note that detection of calcium and magnesium at these levels is not a safety concern and does not represent a water quality violation. Instead, these minerals primarily affect water’s aesthetic qualities such as taste or potential for scaling. For sensitive skin considerations, their presence alone does not indicate unsafe water; rather, they inform decisions about treatment options that might alleviate skin sensitivity triggered by mineral content.

How does public water system data differ from private well testing when assessing sensitive skin causes?

Public system records provide area-wide data based on samples from multiple wells, giving insight into typical water quality in the Rockingham County bedrock aquifer. However, these records cannot indicate the unique mineral content of an individual private well. To accurately understand if water mineral content is contributing to sensitive skin symptoms in your household, a private well water test is essential. This test will identify the actual calcium and magnesium levels affecting your water and guide treatment decisions accordingly.

To settle whether local water quality is influencing your sensitive skin, order a private water test focusing on calcium and magnesium concentrations. Knowing your own water’s mineral profile is the key step before considering the C-Series Sensitive Skin & Eczema System or any other treatment approach.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2019-08-21. 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 (Rockingham County): 96 results from 6 wells, median 144.0 mg/L, range 71.0-237.0 mg/L; none above any federal threshold

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