According to groundwater sampling in Harvey County, KS, within aquifer 112PLSC, iron was detected in many wells at varying levels without exceeding federal safety thresholds. This record is based on 807 samples from 103 wells collected between 2010 and 2016 and does not describe any individual well’s water quality.
Sources of Constituents in Harvey County Groundwater
Iron Presence Drawn from Natural Aquifer Conditions
Iron occurs naturally in the aquifer material and enters groundwater through rock weathering processes common in Harvey County.
Iron Levels Vary by Well Location and Depth
Sampling showed iron ranging widely, influenced by the geological layers encountered at different well depths.
Iron Is Detected Often but Not Above Federal Limits
Many samples had measurable iron, but none surpassed established federal thresholds, indicating detection alone does not imply a violation.
Water System Changes for Large or Seasonal Residential Properties
Larger Households May Experience More Noticeable Effects from Constituents
Water use volume can influence how constituents affect plumbing and appliances.
Second Homes or Seasonal Properties Might Need Distinct Water Management Approaches
Intermittent use may require specific attention to maintaining water quality when systems are idle.
Equipment Failure Necessitates Prompt Evaluation and Treatment Consideration
When existing equipment fails, timely action helps prevent worsening water quality issues.
Influence of Well Depth and Source Type on Expected Water Quality
Sampled Wells Vary from 27 to 270 Feet Deep
Depth impacts the water chemistry, with deeper wells potentially showing different constituent profiles.
Closer Evaluation Is Needed to Determine Individual Well Conditions
Regional data cannot replace testing of a specific well to understand unique water characteristics.
Water Source Type Affects Treatment Needs and Options
Groundwater from a deep aquifer may require different treatment than shallower sources.
Reliability of Regional Data and Considerations of Sample Size
Over 800 Results from More Than 100 Wells Provide Robust Regional Insight
The large data set supports understanding typical water quality trends in Harvey County aquifer 112PLSC.
Smaller Sample Sets Limit Confidence in Regional Representativeness
Less data would mean greater uncertainty about average water conditions.
Comparing Your Well Requires Local Testing Despite Regional Patterns
Individual testing is essential to tailor treatment to your household’s water.
Key Information to Gather Before Planning Water Treatment
Obtain Recent Water Test Results for Your Specific Well
This is critical to identify constituent levels and treatment requirements.
Document Well Depth and Construction Details
These can influence water quality and appropriate system selection.
Note Any Changes in Water Quality or Equipment Performance Over Time
Tracking symptoms helps pinpoint issues and evaluate treatment effectiveness.
In summary, the regional data for Harvey County aquifer 112PLSC indicates iron is commonly detected in groundwater but without exceeding safety limits. Residents with large households or seasonal properties facing equipment failure should test their own water and consider a water treatment system such as the Autotrol Total Well Chlorination System, which ships ready to configure and offers a capacity of 32,000 grains, to manage water quality effectively.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2016-10-18. 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 (Harvey County): 807 results from 103 wells, median 1590.0 ug/L, range 0.1-34900.0 ug/L; none above any federal threshold
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