How Water from Aquifer 112DFSF Reaches Your Home
In FIPS 180, Connecticut, household water commonly comes from wells drawing from aquifer 112DFSF. This groundwater source circulates through varied soil and rock layers before entering wells that range between 10 and 80 feet in depth. Water travels up from the aquifer, passes through your well casing, and into your home plumbing, supplying your fixtures and appliances.
First Affected Fixtures, Appliances, and Processes
Water quality factors associated with this aquifer often impact appliances like water heaters, dishwashers, and faucets gradually. Fixtures with aerators or internal screens might show early signs of particulate effects, and laundry or dishwashing processes can reflect water changes before noticeable household-wide impacts emerge.
Distinguishing This from Other Common Water Treatment Issues
This water condition should not be confused with hardness or microbial contamination, which involve very different treatment approaches. Unlike those, the primary issue recorded in the area relates to measured trace metals in groundwater, which necessitates specific treatment considerations tailored to dissolved substances rather than scaling or sanitizing processes.
Interpreting Certified Laboratory Reports for Your Well Water
A certified laboratory report measuring constituents from your well water will report concentrations in micrograms per liter (ug/L). For the field component identified in this aquifer, median results from 19 wells showed 19.5 ug/L, with results ranging from 0.04 to 700.0 ug/L. However, 49 results were below detection levels. Your laboratory report will indicate whether concentrations are detected or below a reporting limit, but detection alone does not indicate a safety or compliance issue.
Comparing This Aquifer’s Data With Neighboring Counties Without Overreading
When comparing the groundwater data for FIPS 180 with adjacent counties, it is important not to infer exact conditions in wells outside the sampled region. Regional data shows variability in concentration but does not predict your well’s specific condition. Use these records to understand general trends while recognizing your own testing reveals your actual water quality.
How Well and Sample Depth Affect Water Expectations
Samples for this aquifer were taken from wells between 10 and 80 feet deep. Depth can influence constituent levels due to varying geology and water movement. Deeper or shallower wells may demonstrate different profiles, so sample depth should be considered when reviewing test results and selecting treatment.
Closing Summary and Sources
This summary reflects groundwater sampling data from 70 results across 19 wells in aquifer 112DFSF, FIPS 180, CT, collected between 2015 and 2025. None exceeded federal safety thresholds. For a precise understanding of your well water, laboratory testing is necessary. The U.S. Geological Survey site documents these findings and offers access to detailed data.
Regarding treatment, systems like the Fleck Complete Well System, with a grain capacity of 32,000, ship ready to configure for addressing well water concerns sourced from this area.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2025-11-21. 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 Iron in the 112DFSF aquifer (FIPS 180): 70 results from 19 wells, median 19.5 ug/L, range 0.04-700.0 ug/L; none above any federal threshold
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