The Role of Plumbing Materials and Age vs. Source Water Sediment in El Paso County
Water in El Paso County primarily comes from the 112HCBL aquifer, with groundwater drawn from wells ranging between 390 and 1155 feet deep. Government sampling by the U.S. Geological Survey shows that specific conductance—a measure influenced by the total dissolved solids and mineral content—varies from 514 to 3700 microSiemens per centimeter. This variation can affect sediment levels but does not indicate contamination or unsafe water. However, the presence and condition of plumbing materials inside a home have a separate effect on sediment. Older pipes or materials prone to corrosion or mineral buildup can add particulate matter independently of the source water quality.
Which Fixtures, Appliances, and Processes Are Affected First by Sediment?
Parts of the home that draw water frequently and involve fine mechanisms tend to show sediment effects first. Faucets with aerators, showerheads, and water-using appliances such as dishwashers and washing machines may experience clogging or visible sediment deposits earlier. Sediment can also cause wear on water heaters and reduce efficiency. These impacts typically arise because sediments suspended in water settle or accumulate at points of lower flow or where screens and seals narrow the passage.
How Sediment and Specific Conductance Enter Groundwater and Distribution in El Paso County
In this region, sediment in groundwater primarily originates from natural mineral dissolution and surface material infiltration into the deep 112HCBL aquifer. Specific conductance readings reflect the concentration of dissolved ions that can contribute to sediment and scaling potential; however, federal monitoring found no measurements surpassing health-based limits. Sediment particles may also enter the distribution system through well pump operation, where mechanical action agitates deposits around the well screen or inside the pump housing.
What a Certified Laboratory Test Reports for Sediment and Conductance and How to Interpret It
Laboratories testing well water for sediment typically report turbidity or particulate levels, along with specific conductance. The U.S. Geological Survey’s data reflects only the latter as a proxy related to dissolved solids rather than sediment concentration. A certified lab report for your well water should specify sediment presence separately from dissolved ion content. Understanding these distinctions helps determine whether sediment is principally from source water or plumbing infrastructure. Testing sediment levels regularly guides the choice of an appropriate filtration threshold.
How Household Size, Seasonal Use, or a Second Home Alters Sediment Treatment Needs
Larger households or those with increased water demand often experience sediment accumulation impacting appliances faster due to volume and frequency of water use. Seasonal homes or properties with intermittent water flow can face sediment settling during inactivity, causing sudden release upon reactivation. These variations in use cycle influence the selection of sediment filtration options, tailoring capacity and maintenance requirements to the household’s specific patterns.
Meeting these sediment challenges is addressed by the C-Series Sediment From the Well Pump Filter, which ships ready to configure. By matching its performance specifications to the sediment levels and demand of your household, it provides targeted filtration to protect plumbing and appliances from sediment-related issues.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2016-09-23. 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 112HCBL aquifer (El Paso County): 52 results from 25 wells, median 1160.0 uS/cm, range 514.0-3700.0 uS/cm; none above any federal threshold