Understanding Water from Aquifer 112OTSH in Cumberland County
The water supply from aquifer 112OTSH in Cumberland County originates from shallow wells generally between 22 and 38 feet deep. Water drawn from this source travels through the underground aquifer before reaching household taps. This aquifer's characteristics influence the water's interaction with household plumbing and appliances, particularly concerning corrosivity, which may affect pipe longevity and water quality.
Changes at the Tap When Using the C-Series Corrosive Water Damaging Pipes Filter
When water from aquifer 112OTSH passes through the C-Series Corrosive Water Damaging Pipes Filter, the treated water exhibits reduced corrosivity. This system helps neutralize factors contributing to pipe degradation, resulting in water that is less likely to accelerate wear on plumbing materials. The improvement is noticeable in diminished staining and reduced metallic taste, reflecting a balance that protects pipes and fixtures.
Impact of Well and Sample Depth on Expected Water Quality
The two wells sampled within this aquifer ranged from 22 to 38 feet deep. Well depth can influence water chemistry; shallower wells may be more susceptible to surface contaminants or changes in groundwater composition. The depth range of sampled wells suggests some variation in water quality parameters, but both wells provided comparable chloride levels within the documented results, which informs expectations of corrosivity levels in the region.
Sample Size and What It Means for Understanding Water Quality in This Area
The water quality data from Cumberland County's aquifer 112OTSH is based on 14 samples taken from two wells over seven years. While this sample size is modest, it offers a consistent picture of chloride presence in the aquifer. Chloride was detected in all samples, with no measurements falling below detection limits. The data does not identify any federal water quality standard violations, which means these chloride levels, while present, are within the range considered typical and manageable for water from this source.
Household Fixtures and Appliances Most Vulnerable to Corrosive Water
Corrosive water first affects household components that use metal extensively and are in frequent contact with water, such as faucets, water heaters, and pipe joints. Over time, exposure to corrosive water can cause surface pitting, leaks, or mineral staining, especially in older plumbing systems or fittings made from sensitive metals. Appliance efficiency may decline if corrosion leads to scaling or material degradation inside water heaters or dishwashers.
Long-Term Consequences of Leaving Corrosive Water Untreated
If corrosive water conditions persist without management, gradual deterioration of plumbing components is likely. This includes increased maintenance needs and the potential for leaks or pipe failure. Corrosion can also influence water clarity and taste, possibly leading to a metallic flavor or slight discoloration. Treating the water reduces these risks by maintaining a protective balance in water chemistry that limits pipe damage over time.
How Plumbing Materials and Age Contribute to Corrosion Concerns
The type and age of plumbing materials play a significant role in susceptibility to corrosive water effects. Older pipes made from iron, steel, or copper can react differently to water chemistry than newer plastic piping. Metal pipes may show faster corrosion if water is acidic or contains dissolved minerals that encourage metal leaching. Knowing the materials present and their condition can help homeowners understand the interaction with source water corrosivity and prioritize appropriate water treatment.
Summary of the Water Record and Further Information
In summary, groundwater from Cumberland County's aquifer 112OTSH has consistent chloride detections across 14 samples from two wells, with no federal standard exceedances. This indicates a stable level of water quality influencing corrosivity, though individual tests remain important for specific conditions. For more detailed data, the U.S. Geological Survey provides extensive records on groundwater sampling in this area.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2017-10-05. 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 Chloride in the 112OTSH aquifer (Cumberland County): 14 results from 2 wells, median 60.95 mg/L, range 21.4-91.8 mg/L; none above any federal threshold