Autotrol Complete Well System

Autotrol Complete Well System

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If Plumbing Materials or Age May Affect Your Water Quality

Before assessing the source water, consider that household plumbing materials and their age can influence water quality characteristics. Metals from older pipes, fittings, or fixtures may contribute to discoloration or deposits that mimic raw water issues. These factors operate independently of what is found naturally in the aquifer. If you observe staining or color changes only intermittently or after water sits in pipes, plumbing components could be the cause rather than groundwater constituents.

If You Want to Understand How Technology Handles Groundwater Constituents

Government monitoring in Pueblo County's aquifer 111ALVM reports iron was detected in most samples, with a median concentration of 15.7 micrograms per liter and a range up to 93.3 micrograms per liter. No federal health thresholds were exceeded. Removal of iron from well water typically involves oxidation and filtration processes that convert dissolved forms into particles that can be trapped.

The Autotrol Complete Well System, featuring a grain capacity of 32,000, uses ion exchange and filtration components to reduce iron concentrations effectively. It processes water to remove oxidized iron solids and neutralize related effects that can impact water clarity and aesthetics. This system ships ready to configure for household use.

If You Want to Know How Iron Gets into Groundwater in Pueblo County

Iron commonly occurs naturally in groundwater due to the dissolution of minerals in soil and rock formations. In Pueblo County’s aquifer 111ALVM, the detected iron concentrations vary by location and well depth (10 to 51 feet). Natural geochemical conditions promote iron’s presence without indicating contamination. Seasonal or hydrological changes can also influence levels temporarily.

If You Are Considering Maintenance Needs for Your Treatment System

The Autotrol Complete Well System requires periodic attention to maintain optimal performance. Routine maintenance includes regenerating the media that captures oxidized iron and checking system settings for flow and hardness. The maintenance frequency depends on water usage and iron load but generally follows a predictable schedule. This regimen helps ensure consistent treated water quality.

If You Want to Understand How Treated Water Quality Changes at the Tap

Once treated by the Autotrol System, water typically appears clearer and free of iron-related staining or cloudiness. The system reduces particles and oxidized iron solids that can discolor water or leave deposits on fixtures and laundry. This results in improved aesthetic qualities without altering naturally occurring mineral balances fundamental to water taste.

If You Are Weighing Public-System Data Against Private Well Testing

The U.S. Geological Survey’s data reflects multiple wells sampled throughout Pueblo County aquifer 111ALVM, providing insights into regional groundwater trends but not specific household well conditions. Private well owners need individual water testing to determine their exact water composition. Area data cannot replace direct testing because concentrations vary significantly even within small distances and at different depths.

Therefore, while regional data suggest typical iron levels and the general absence of health-based violations, only testing of your private well water can confirm your unique water profile and treatment needs.

Do not conclude from area data alone that your own well water matches these results exactly or requires identical treatment. Consider testing your well water to tailor decisions precisely.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2018-02-26. 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 Iron in the 111ALVM aquifer (Pueblo County): 70 results from 15 wells, median 15.7 ug/L, range 4.1-93.3 ug/L; none above any federal threshold

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