Well Pump Sediment in Fayette County: Understanding Area Data on Specific Conductance
Area water quality data can help recognize potential issues with well pump sediment but cannot specify the degree or presence in any individual household. Fayette County's aquifer 327KNWH has documented measurements for specific conductance from government sampling. These figures provide context but do not define your well's condition.
Household Symptoms Related to Well Pump Sediment
Cloudy or turbid water at faucets
May suggest suspended particles but not confirm sediment levels.
Frequent clogging of faucet aerators or filters
Points to physical particles but not their chemical nature.
Unexpected sediment deposits in plumbing fixtures
Indicates solids presence but requires testing to identify composition.
Water discoloration or visible particles
Can appear due to sediment but might also come from other sources.
Understanding Laboratory Reports on Specific Conductance
Definition of specific conductance
Measures water's ability to conduct electricity, related to dissolved ions but not a direct sediment measure.
How test results are reported
Reported in microsiemens per centimeter (uS/cm); a numeric range rather than a sediment concentration.
Relation to sediment
High specific conductance can correlate with dissolved solids but does not specify suspended sediment.
Influence of Sampling Depth and Well Characteristics
Sample depths ranged from 55 to 289 feet
Indicates data reflect various well depths but individual well profiles may differ.
Sampled wells represent the area aquifer 327KNWH
Generalizes regional groundwater quality but not all individual wells.
Water source type affects sediment presence
Deeper wells often have different sediment profiles than shallow wells.
Interpreting 'Detected,' 'Median,' and 'Range' in the Sampling Record
"Detected" means the instrument measured specific conductance in all samples
This does not indicate a violation or unsafe condition.
Median value of 90.5 uS/cm
Represents the middle value of the area samples, not a household-specific reading.
Range from 74.0 to 290.0 uS/cm
Shows variability among sampled wells but not necessarily in your own water.
Meaning of the Measured Range Relative to Federal Standards
No federal threshold was exceeded in any sample
This means the area’s specific conductance levels are within acceptable limits.
Specific conductance itself is an aesthetic secondary standard
It relates to taste or staining potential rather than safety.
Elevated specific conductance does not confirm sediment problems
Other tests must identify actual sediment particles.
Sample Size and Its Implications
Six samples from three wells provide limited but useful area context
Small sample size means wider uncertainty for individual well conditions.
Sampling dates from August 2016
Reflect historic groundwater quality but may not represent current conditions exactly.
More extensive testing recommended for household-specific assessment
Professional laboratory analysis will define actual sediment and conductance values for your water.
This government record summarizes specific conductance in Fayette County's aquifer 327KNWH based on samples from a few wells. These regional figures offer insight but do not replace a certified water test for any household well. For managing well pump sediment, consider direct testing and using the Autotrol Sediment From the Well Pump Filter, a system designed to address sediment from the well pump and improve water clarity. The product ships ready to configure, suitable for residential use.
Source: U.S. Geological Survey groundwater sampling data (https://waterdata.usgs.gov/monitoring-location/380657080570601/)
Where this information comes from
Source: USGS groundwater sampling. Sampled 2016-08-23. 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 327KNWH aquifer (Fayette County): 6 results from 3 wells, median 90.5 uS/cm, range 74.0-290.0 uS/cm; none above any federal threshold

