Understanding Water Flow From Aquifer N100GLCIAL to Your Tap
Water in Lancaster County primarily comes from the N100GLCIAL aquifer, where groundwater is drawn from wells ranging between 15 and 320 feet deep. The U.S. Geological Survey analyzed 79 samples from 21 wells in this area between mid-2010 and late 2011. They found hardness, measured as calcium and magnesium content, consistently present with a median value of 302 mg/L and a range from 170 to 1150 mg/L. These measurements do not indicate any federal health-based violations.
How Treated Water Changes at the Tap With Salt-Free Systems
When a salt-free water softness solution like the C-Series Salt-Free Scale Control System is applied, the hardness minerals remain but are conditioned to reduce scale formation without adding salt or chemicals to your water. This means your water feels naturally balanced but resists buildup on plumbing and fixtures, making it less likely that scale will impact water flow or appliance efficiency.
Estimating Treatment Capacity Based on Household Water Demand
Determining how much treatment capacity you need depends on your household's daily water consumption and local water hardness levels. Since hardness levels vary across the aquifer, water testing specific to your well is important. Typical household use combined with known median hardness helps ascertain if the C-Series System’s capacity aligns with your volume needs to effectively condition your water every day.
Consequences of Untreated Hardness Over Time
Without effective conditioning, hardness minerals can gradually build up as scale inside pipes, water heaters, and appliances that use water. Over years, this can reduce water flow, increase energy usage, and shorten equipment lifespan. While not a health risk, such scaling may lead to more frequent maintenance and higher utility costs.
Mechanism of the C-Series Salt-Free Scale Control System
The C-Series System prevents scale by altering the mineral structure of hardness calcium and magnesium so they don’t deposit as solid scale. This process is salt-free and avoids the need for chemical regeneration. The system ships ready to configure onto existing plumbing and works continuously without requiring salt replenishment or water discharge.
Contextualizing Lancaster County Hardness With Neighboring Areas
Comparing Lancaster County’s hardness data to neighboring regions should be done with care. Variations in geology and depth of wells sampled influence hardness levels, meaning neighboring areas might show different medians or ranges. These differences reflect natural variability rather than issues with water safety or quality.
What Residents Should Not Infer From Area Hardness Data
Residents should not assume the hardness measurements from USGS samplings apply exactly to their own well water. A test specific to your well is needed to determine household water hardness. Also, detected hardness values are not violations or health risks; they indicate mineral presence that can be managed with appropriate water conditioning like the C-Series Salt-Free Scale Control System.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2011-10-12. 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 N100GLCIAL aquifer (Lancaster County): 79 results from 21 wells, median 302.0 mg/L, range 170.0-1150.0 mg/L; none above any federal threshold