What the Median and Range of Specific Conductance Mean for a Well Owner
In aquifer 110AVTN, part of Connecticut's area coded FIPS 180, government sampling shows specific conductance values from eight results at one well ranging from 460 to 1150 microsiemens per centimeter, with a median of 1020 µS/cm. Specific conductance, a measure of water’s ability to conduct electricity, relates to dissolved solids in the water which can contribute to sediment buildup near your well pump. While these values do not directly equate to sediment concentration or quality in your household water, they indicate mineral and dissolved solids levels typical for the area’s shallow groundwater.
Why Comparing Nearby Counties’ Records Needs Care
Adjacent regions may have different aquifer characteristics and sampling results. For example, other counties might report higher or lower specific conductance ranges due to geology or land use. However, these figures are local area medians and ranges, not precise readings from your own well. Comparing them should highlight relative groundwater mineralization, not predict exactly what sediment your system handles or the pump's sediment load.
What Happens at the Tap After Filtering Sediment
Once a sediment filtration system designed for well pumps is placed before your household plumbing, noticeable changes can include reduced gritty particles in water, less wear on appliances using water, and potentially clearer water appearance. The documented Fleck Sediment From the Well Pump Filter system ships ready to configure and is engineered to handle sediment while maintaining flow rates that meet typical household demand. It does not itself alter the chemical content of water such as minerals measured by specific conductance but removes physical particles.
Public-System Records Are Not a Substitute for Private Well Testing
Government groundwater sampling, like the USGS data available for aquifer 110AVTN, provides useful regional context but cannot measure water quality in an individual well. Testing your own well water is the only way to confirm sediment levels and other characteristics affecting your household system’s performance. Public data does not identify unique well conditions, so relying on these statistics alone to diagnose sediment challenges is incomplete.
Well Pump Sediment Is Different from Other Water Quality Issues
The sediment you see or experience is a physical matter issue, distinct from dissolved minerals or chemical constituents. Specific conductance helps gauge dissolved solids but does not measure sediment particles directly. Other common confusions include mistaking mineral content for sediment load or conflating sediment with corrosion products. Proper sediment filtration targets physical particles suspended in water, not dissolved substances indicated by specific conductance.
Assessing Treatment Capacity Relative to Household Demand
To determine if a sediment filtration system meets your household’s needs, measure your daily water use and flow rates from the well pump. The documented Fleck Sediment From the Well Pump Filter system is built to handle typical residential flow and sediment loads found in areas like aquifer 110AVTN. Ensuring the filter capacity aligns with your water consumption helps prevent clogging and maintains pump efficiency, addressing the issue where existing equipment cannot keep up.
Conclusion
For households in Connecticut’s FIPS 180 area drawing from aquifer 110AVTN, government water quality records show typical dissolved solids levels but do not reveal exact sediment conditions in your well. To address well pump sediment that existing equipment struggles with, test your own water and measure daily usage. Then, the Fleck Sediment From the Well Pump Filter system, designed and ready to configure, offers a documented method to handle physical sediment reliably at flow rates matching household demand.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2011-02-20. 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 Specific conductance in the 110AVTN aquifer (FIPS 180): 8 results from 1 wells, median 1020.0 uS/cm, range 460.0-1150.0 uS/cm; none above any federal threshold
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