Understanding Water from the 112PLSC Aquifer Serving Sedgwick County Residences
Water drawn from wells tapping the 112PLSC aquifer across Sedgwick County reaches homes after underground movement through varying depths between 25 and 248 feet. This aquifer is the source for many domestic wells, contributing to household water systems across the county.
Considering Household Size and Use Patterns
Larger households or seasonal homes in Sedgwick County may observe variation in water characteristics, such as iron bacteria presence, influenced by water usage rates and storage times. Lower usage in second homes could encourage conditions that allow iron bacteria to develop more noticeably, while consistent use in full-time residences may distribute effects differently.
Contextualizing Sedgwick County Iron Data Compared to Nearby Regions
The U.S. Geological Survey sampled 27 wells within Sedgwick County's 112PLSC aquifer from 2010 to 2016, recording 275 iron measurements. Iron was detected in 31 results, with a median concentration of 320 micrograms per liter and a range from 0.6 to 970 micrograms per liter. These findings provide an area-wide overview but do not indicate individual well conditions. Comparing these numbers to neighboring counties requires attention to differences in aquifer geology and sampling methods, avoiding direct conclusions about local well quality without specific testing.
Early Signs of Iron Bacteria Effects on Household Fixtures and Appliances
Fixtures such as faucets, toilets, and water-using appliances may display slime buildup or staining linked to iron bacteria activity. These effects tend to appear first in places with slower water flow or standing water. Understanding these initial impacts helps prioritize testing and treatment but does not alone quantify iron levels in the water.
Differentiating Iron Bacteria from Other Water Issues
Iron bacteria can be mistaken for other water concerns like general iron staining or microbial contamination. Unlike isolated iron presence, iron bacteria produce slime and biofilm that can clog pipes and affect taste or appearance. Recognizing the difference guides appropriate response without assuming a violation of safety standards.
Pathways of Iron Entry into Sedgwick County Groundwater
Iron naturally occurs in the geological formations of the 112PLSC aquifer. It dissolves from minerals into groundwater as it moves, influenced by soil composition, oxygen levels, and water chemistry. This natural origin explains the detected iron in sampled wells but does not indicate man-made contamination or exceedance of regulatory health limits.
Interpreting Terms in the Government Sampling Record
The term 'detected' signifies that instruments measured iron presence above a minimal threshold but does not equate to a safety violation or problem by itself. The 'median' value represents the middle concentration of all samples, offering a typical measure for the area, while the 'range' shows the lowest and highest detected concentrations, illustrating variability. No measurements in this dataset exceeded federal safety or secondary thresholds.
Summary of Sedgwick County Iron Sampling and Treatment Approach
This record from 27 wells sampled between 2010 and 2016 reflects the occurrence of iron in the 112PLSC aquifer serving Sedgwick County. It helps identify the possibility of iron bacteria-related issues in household water but does not replace testing of individual wells for precise conditions. For targeted iron bacteria management, the Autotrol Iron Bacteria & Slime Filter system is available, shipping ready to configure for residential water use and designed specifically to address slime and iron bacteria by reducing their impact on plumbing and appliances.
Source: U.S. Geological Survey groundwater data for Sedgwick County, aquifer 112PLSC (https://waterdata.usgs.gov/monitoring-location/375115097294601/).
Where this information comes from
Source: USGS groundwater sampling. Sampled 2016-09-15. 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 112PLSC aquifer (Sedgwick County): 275 results from 27 wells, median 320.0 ug/L, range 0.6-970.0 ug/L; none above any federal threshold
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