The U.S. Geological Survey sampled groundwater from five wells in Pecos County's aquifer 231DCKM during August 2010 and recorded specific conductance values ranging from 719 to 3400 microsiemens per centimeter, with a median of 1560 uS/cm. All results were below federal safety thresholds. These findings represent area-wide measurements from wells between 342 and 654 feet deep and do not specify your private well's water quality.
Distinguishing Well Pump Sediment from Commonly Confused Water Issues
Well pump sediment specifically refers to solid particles—like sand or silt—that originate from the aquifer and enter the water system through the well pump. This is different from turbidity, which is a measure of water cloudiness caused by suspended particles, and hardness, which relates to dissolved minerals like calcium and magnesium. While turbidity and hardness affect water appearance and scaling, sediment primarily causes physical abrasion and clogging in pipes and appliances.
Understanding 'Detected', 'Median', and 'Range' in the Sampling Record
The term detected means the measurement instrument identified specific conductance values in all samples; it does not indicate a violation or danger. The median is the middle value among samples, representing a typical condition in the area. The range shows the lowest and highest recorded values, illustrating variability across wells. These terms help describe the groundwater's electrical conductivity, which reflects dissolved mineral concentrations but is not a direct measure of sediment presence.
Testing Sequence to Identify Sediment and Related Water Quality Factors
- Begin with visual inspection of tap water for visible particles or cloudiness.
- Check household filters and screens for accumulated sediment or grit.
- Evaluate plumbing components for physical wear or blockage indicative of sediment.
- If uncertainties remain, pursue laboratory particle analysis or well water testing specific to your source.
These steps progress from low-cost observations to more precise assessments, helping homeowners clarify the presence and extent of sediment.
Sampling Depth, Number of Wells, and Interpretative Limitations
The data comes from 10 samples across five wells, each between 342 and 654 feet deep, providing a limited but useful snapshot of Pecos County's aquifer 231DCKM at that time. A small sample size means local variations can exist, and your well's water quality might differ. These measurements do not detect sediment directly but provide context on dissolved minerals influencing water conductivity and potential sediment transport behavior.
How the C-Series Sediment From the Well Pump Filter Addresses Sediment
The C-Series System is designed to capture and remove sediment particles as water enters your household plumbing from the well pump. It functions as a physical barrier, preventing abrasive solids from circulating through your water lines and appliances. By reducing sediment load, this filter helps maintain water clarity and protect plumbing longevity. The system ships ready to configure with your setup and requires no special preparation beyond standard connections.
In summary, the U.S. Geological Survey's record covers groundwater sampling of aquifer 231DCKM in Pecos County between five wells at substantial depths and shows specific conductance values indicative of dissolved minerals but not sediment content itself. For detailed water quality at your home, individual testing is necessary. The government source for this data is available at https://waterdata.usgs.gov/monitoring-location/305112102265901/.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2010-08-31. 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 231DCKM aquifer (Pecos County): 10 results from 5 wells, median 1560.0 uS/cm, range 719.0-3400.0 uS/cm; none above any federal threshold