Adjusting Sediment Solutions for Household Size and Property Use
When considering sediment management for a residential well in El Paso County, the size and usage patterns of your household can influence your choice of equipment. Larger households or homes used seasonally may face different sediment loads or flow demands than smaller, full-time residences. These factors affect how often sediment filters need attention and what flow rates are necessary to sustain household water needs without compromising system performance.
Key Information to Gather Before Choosing Treatment
Before selecting sediment control equipment, note your well’s depth, water usage rates, and if you have any existing water treatment components. Testing your own well water for sediment load and particle size distribution is essential, as regional data cannot specify your well's conditions. Understanding the specific conductance of your well water can provide insight into total dissolved solids but does not directly measure sediment.
Influence of Sample and Well Depths on Sediment Expectations
The U.S. Geological Survey sampled wells ranging from 390 to 1155 feet deep in El Paso County’s aquifer 112HCBL. Deeper wells may show different sediment characteristics than shallower wells due to geological formations encountered. Your own well’s depth will help predict the sediment nature you might experience, as some layers produce more particulate matter. This variability means treatment must be adaptable to these differing sediment profiles.
Origin of Sediment and Specific Conductance in Local Groundwater
Specific conductance, a measure of water’s ability to conduct electricity, reflects dissolved solids in groundwater but is not a direct measure of suspended sediment. In El Paso County, all 52 sampled wells detected specific conductance, with median levels around 1160 microsiemens per centimeter, well within federal thresholds. Sediment in the well pump system could result from natural rock and mineral particles in the aquifer or from wear in the pump and piping system rather than dissolved constituents measured by conductance.
Differences Between Public Water Records and Private Well Testing
Public water system records report quality metrics based on treated water and regulatory compliance, which may not reflect private well conditions. The data from the aquifer 112HCBL provides a regional snapshot but does not substitute for individual well analysis. Private well owners must conduct their own sediment testing and water analysis to accurately characterize their water and inform treatment selection.
How the Pentair Sediment From the Well Pump Filter Addresses Sediment
The Pentair System designed for well pump sediment control ships ready to configure with your existing well setup. It mechanically removes suspended particles that enter the water stream at the pump, protecting plumbing and appliances. By filtering sediment at the source, it helps maintain clear water and extends the life of downstream equipment without altering water chemistry tied to specific conductance or dissolved solids.
In summary, choosing the right sediment management equipment for your El Paso County home requires understanding your household’s water demand, your well’s attributes, and testing your own water for sediment. While regional aquifer 112HCBL data offers useful context, personal water analysis is key to informed decisions. The Pentair Sediment From the Well Pump Filter provides a practical technology for reducing particulate matter entering your household water system.
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
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