How Sample Depth, Well Depth, or Source Type Changes What to Expect
Sampling Depth Reflects Typical Household Well Conditions
Groundwater data for aquifer 112DFSF in CT come from wells 10 to 80 feet deep. This range aligns with many residential wells, so water quality findings are relevant for typical household water usage.
Variability Across Wells Indicates Local Differences
Wells sampled vary in location and depth, which causes changes in water constituents like iron. Expect some difference between your well's water and area samples since each well's conditions are unique.
Source Type Influences Water Constituents
The data represent groundwater from a regional aquifer, excluding surface water sources. If your household well taps different strata or sources, water quality may differ, requiring customized consideration.
What Additional Questions Commercial or Industrial Operators Face
Higher Volume Demands Affect Equipment Choice
Commercial or industrial uses require treatment systems sized for larger water volumes, influencing capacity and regeneration frequency, unlike typical household needs.
Regulatory Compliance for Commercial Users
Businesses must often meet stricter monitoring and reporting standards, adding complexity beyond residential concerns where personal testing guides treatment.
Operational Downtime Considerations
Industries may require continuous water availability, emphasizing equipment redundancy or backup systems less common in home applications.
How Seasonal or Multi-Year Variation Appears in the Record
Data Span Over a Decade
The USGS sampling from 2015 through late 2025 captures changes over about ten years, allowing observation of trends rather than a snapshot.
Iron Levels Range Widely
Median iron in sampled area wells is 19.5 micrograms per liter, ranging from 0.04 to 700. This variability reflects natural fluctuations and localized influences on groundwater quality over time.
Most Samples Below Detection Limits
In 70 results, 49 were below reporting limits, showing many wells have very low or undetectable iron, highlighting the importance of individual testing for accurate assessment.
How the Documented Treatment Technology Removes or Neutralizes the Constituent
Oxidation and Filtration Address Well Water Concerns
The Fleck Total Well Chlorination System oxidizes constituents like iron, converting dissolved forms to particulate matter that can be filtered out, improving water clarity and reducing staining.
Capacity Supports Household Volume Needs
With a grain capacity of 32,000, the system is sized to handle typical residential daily water usage, ensuring effective treatment without overcapacity or frequent maintenance.
Ships Ready to Configure for User Setup
This system arrives prepared for customer setup without requiring professional services, allowing homeowners to tailor its configuration to their specific water treatment needs.
How Public-System Records Differ from Private-Well Testing in What They Establish
Area Data Suggest Regional Trends, Not Individual Water Quality
The USGS findings represent regional aquifer conditions, serving as a guide rather than a definitive report of your water’s exact composition.
Testing Your Well Water Is Essential
To know your household water quality, obtain a current test of your own well water since local geology and well construction affect constituent levels.
Public Records Provide Context for Treatment Decisions
Government sampling helps anticipate likely water constituents and informs the choice and sizing of treatment equipment, complementing but not replacing personal water analysis.
Summary
The groundwater sampling for aquifer 112DFSF in CT, covering about ten years and multiple wells from 10 to 80 feet deep, shows a range of iron detections with none exceeding federal thresholds. This regional record offers useful context for residential water treatment choices. For full details, consult the USGS groundwater monitoring data at https://waterdata.usgs.gov/monitoring-location/413644072080501/. The Fleck Total Well Chlorination System provides a documented solution sized and designed to address such well water conditions, shipping ready to configure for household use.
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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